Accretionary Prisms and Convergent Margin Tectonics in the Northwest Pacific Basin
Accretionary prisms in convergent margins are natural laboratories for exploring initial orogenic processes and mountain building episodes. They are also an important component of continental growth both vertically and laterally. Accretionary prisms are seismically highly active and their internal...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Ogawa, Yujiro [verfasserIn] |
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| Format: |
E-Book |
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| Sprache: |
Englisch |
| Erschienen: |
Dordrecht: Springer Science+Business Media B.V ; 2011 |
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| Schlagwörter: |
Japan / Meeresboden / Meeresgeologie / Ozeanische Erdkruste / Gesteinskunde Pazifischer Ozean / Akkretionskeil / Akkretion, Geologie / Rifting / Subduktion / Geologie |
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| Schlagwörter: | |
| Formangabe: |
Aufsatzsammlung |
| Systematik: |
|
|---|
| Anmerkung: |
Includes bibliographical references and index |
|---|---|
| Umfang: |
Online-Ressource (XX, 277p. 123 illus., 69 illus. in color, digital) |
| Weitere Ausgabe: |
Buchausg. u.d.T.: Accretionary prisms and convergent margin tectonics in the Northwest Pacific basin - Dordrecht : Springer, 2011 |
|---|
| Reihe: |
Modern Approaches in Solid Earth Sciences ; 8 SpringerLink ; Bücher |
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| Links: |
Link aufrufen |
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| ISBN: |
978-90-481-8885-7 |
| DOI / URN: |
10.1007/978-90-481-8885-7 |
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| Katalog-ID: |
1650945701 |
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| 245 | 1 | 0 | |a Accretionary Prisms and Convergent Margin Tectonics in the Northwest Pacific Basin |c edited by Yujiro Ogawa, Ryo Anma, Yildirim Dilek |
| 264 | 1 | |a Dordrecht |b Springer Science+Business Media B.V |c 2011 | |
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| 505 | 8 | 0 | |a Accretionary Prisms and Convergent Margin Tectonics in the Northwest Pacific Basin; Preface; Acknowledgements; Contents; Contributors; Bending-Related Topographic Structures of the Subducting Plate in the Northwestern Pacific Ocean; 1 Introduction; 2 Data and Methods; 2.1 Bathymetric Data; 2.2 Geomagnetic Data; 3 Results; 3.1 Overview of the Bathymetric Features; 3.2 Topographic Expression of the Trenches; 3.3 Bending-Related Structures of the Oceanward Trench Slopes; 3.3.1 Kuril Trench; 3.3.2 Japan Trench; 3.3.3 Izu-Ogasawara Trench; 3.4 Magnetic Anomalies; 4 Discussion |
| 505 | 8 | 0 | |a 4.1 Strike of Bending-Related Topographic Structures4.2 Topographic Expression of Bending-Related Structures; 5 Conclusions; References; Erosional Subduction Zonein the Northern Japan Trench: Review of Submersible Dive Reports; 1 Introduction; 2 Oceanward Slope Topography and Geology off Miyako; 3 Landward Slope Topography and Geology off Miyako; 4 Lineaments of the Oceanward and Landward Slopes off Miyako; 5 Conclusions; References; Boso TTT-Type Triple Junction: Formation of Miocene to Quaternary Accretionary Prisms and Present-Day Gravitational Collapse; 1 Introduction |
| 505 | 8 | 0 | |a 2 Review of Sedimentation, Topography, and Plate Configuration2.1 Sedimentation; 2.2 Topographic Development of the Area from the Eastern Margin of the Sagami Trough to the Boso Triple Junction; 2.3 Katsuura Basin and Mogi Submarine Fan in the Bando Deepsea Basin; 2.4 Review of 3D Structure Based on Multichannel Seismic Profiles and Multibeam Echosounder Data; 2.5 Relationship Between the Tectonic and Age Data; 3 Diatom Analysis; 3.1 Materials, Method, and Results; 3.2 Diatom Biostratigraphy; 3.2.1 Pleistocene to Holocene Samples; 3.2.2 Middle Miocene Sample; 3.3 Summary of Age of Samples |
| 505 | 8 | 0 | |a 3.4 Correlation to the Marine Rocks of the Izu Forearc4 Tectonic Synthesis: Summary and Conclusion; References; Rifting Structure of Central Izu-Ogasawara (Bonin) Arc Crust: Results of Seismic Crustal Imaging; 1 Introduction; 2 Data Acquisition; 3 Data and Modeling Procedure; 4 Description of Velocity Images; 4.1 Line IBr9; 4.2 Line IBr10; 5 Discussion; 5.1 Structural Commonalities and Differences; 5.2 Origin of the Arc Crust; 5.3 History of the Rifted Crust; 5.4 Reason for the Thin Crust in the Central Izu-Ogasawara Arc; 6 Conclusion; References |
| 505 | 8 | 0 | |a Seafloor Geology of the Basement Serpentinite Body in the Ohmachi Seamount (Izu-Bonin Arc) as Exhumed Parts of a Subduction Zone Within the Philippine Sea1 Introduction; 2 Geologic Setting and Bathymetry; 3 Lithology; 3.1 Serpentinites; 3.1.1 Massive Serpentinite; 3.1.2 Schistose Serpentinite; 3.2 Amphibole Schist; 3.3 Paleogene Volcanic Rocks; 3.4 Miocene Turbidite; 3.5 Soft Mud Beds; 4 Dive and Dredge Results; 4.1 Dive 6K#341; 4.2 Dive 6K#570; 4.3 Dive 6K#571; 4.4 Dive 6K#575; 4.5 Dive 6K#608; 4.6 Dive 6K#609; 4.7 Dive 6K#610; 4.8 Dive 6K#1064; 4.9 Dive 6K#1065; 4.10 Dive 6K#1066 |
| 505 | 8 | 0 | |a 4.11 Dive 6K#1067 |
| 520 | |a Accretionary prisms in convergent margins are natural laboratories for exploring initial orogenic processes and mountain building episodes. They are also an important component of continental growth both vertically and laterally. Accretionary prisms are seismically highly active and their internal deformation via megathrusting and out-of-sequence faulting are a big concern for earthquake and tsunami damage in many coastal cities around the Pacific Rim. The geometries and structures of modern accretionary prisms have been well imaged seismically and through deep drilling projects of the Ocean Drilling Program (and recently IODP) during the last 15 years. Better understanding of the spatial distribution and temporal progression of accretionary prism deformation, structural and hydrologic evolution of the décollement zone (tectonic interface between the subducting slab and the upper plate), chemical gradients and fluid flow paths within accretionary prisms, contrasting stratigraphic and deformational framework along-strike in accretionary prisms, and the distribution and ecosystems of biological communities in accretionary prism settings is most important in interpreting the evolution of ancient complex sedimentary terrains and orogenic belts in terms of subduction-related processes. This book is a collection of interdisciplinary papers documenting the geological, geophysical, geochemical, and paleontological features of modern accretionay prisms and trenches in the northwestern Pacific Ocean, based on many submersible dive cruises, ODP drilling projects, and geophysical surveys during the last 10 years. It also includes several papers presenting the results of systematic integrated studies of recent to ancient on-land accretionary prisms in comparison to modern analogues. The individual chapters are data and image rich, providing a major resource of information and knowledge from these critical components of convergent margins for researchers, faculty members, and graduate and undergraduate students. As such, the book will be a major and unique contribution in the broad fields of global tectonics, geodynamics, marine geology and geophysics, and structural geology and sedimentology. | ||
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Accretionary Prisms and Convergent Margin Tectonics in the Northwest Pacific Basin; Preface; Acknowledgements; Contents; Contributors; Bending-Related Topographic Structures of the Subducting Plate in the Northwestern Pacific Ocean; 1 Introduction; 2 Data and Methods; 2.1 Bathymetric Data; 2.2 Geomagnetic Data; 3 Results; 3.1 Overview of the Bathymetric Features; 3.2 Topographic Expression of the Trenches; 3.3 Bending-Related Structures of the Oceanward Trench Slopes; 3.3.1 Kuril Trench; 3.3.2 Japan Trench; 3.3.3 Izu-Ogasawara Trench; 3.4 Magnetic Anomalies; 4 Discussion 4.1 Strike of Bending-Related Topographic Structures4.2 Topographic Expression of Bending-Related Structures; 5 Conclusions; References; Erosional Subduction Zonein the Northern Japan Trench: Review of Submersible Dive Reports; 1 Introduction; 2 Oceanward Slope Topography and Geology off Miyako; 3 Landward Slope Topography and Geology off Miyako; 4 Lineaments of the Oceanward and Landward Slopes off Miyako; 5 Conclusions; References; Boso TTT-Type Triple Junction: Formation of Miocene to Quaternary Accretionary Prisms and Present-Day Gravitational Collapse; 1 Introduction 2 Review of Sedimentation, Topography, and Plate Configuration2.1 Sedimentation; 2.2 Topographic Development of the Area from the Eastern Margin of the Sagami Trough to the Boso Triple Junction; 2.3 Katsuura Basin and Mogi Submarine Fan in the Bando Deepsea Basin; 2.4 Review of 3D Structure Based on Multichannel Seismic Profiles and Multibeam Echosounder Data; 2.5 Relationship Between the Tectonic and Age Data; 3 Diatom Analysis; 3.1 Materials, Method, and Results; 3.2 Diatom Biostratigraphy; 3.2.1 Pleistocene to Holocene Samples; 3.2.2 Middle Miocene Sample; 3.3 Summary of Age of Samples 3.4 Correlation to the Marine Rocks of the Izu Forearc4 Tectonic Synthesis: Summary and Conclusion; References; Rifting Structure of Central Izu-Ogasawara (Bonin) Arc Crust: Results of Seismic Crustal Imaging; 1 Introduction; 2 Data Acquisition; 3 Data and Modeling Procedure; 4 Description of Velocity Images; 4.1 Line IBr9; 4.2 Line IBr10; 5 Discussion; 5.1 Structural Commonalities and Differences; 5.2 Origin of the Arc Crust; 5.3 History of the Rifted Crust; 5.4 Reason for the Thin Crust in the Central Izu-Ogasawara Arc; 6 Conclusion; References Seafloor Geology of the Basement Serpentinite Body in the Ohmachi Seamount (Izu-Bonin Arc) as Exhumed Parts of a Subduction Zone Within the Philippine Sea1 Introduction; 2 Geologic Setting and Bathymetry; 3 Lithology; 3.1 Serpentinites; 3.1.1 Massive Serpentinite; 3.1.2 Schistose Serpentinite; 3.2 Amphibole Schist; 3.3 Paleogene Volcanic Rocks; 3.4 Miocene Turbidite; 3.5 Soft Mud Beds; 4 Dive and Dredge Results; 4.1 Dive 6K#341; 4.2 Dive 6K#570; 4.3 Dive 6K#571; 4.4 Dive 6K#575; 4.5 Dive 6K#608; 4.6 Dive 6K#609; 4.7 Dive 6K#610; 4.8 Dive 6K#1064; 4.9 Dive 6K#1065; 4.10 Dive 6K#1066 4.11 Dive 6K#1067 |
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Accretionary Prisms and Convergent Margin Tectonics in the Northwest Pacific Basin; Preface; Acknowledgements; Contents; Contributors; Bending-Related Topographic Structures of the Subducting Plate in the Northwestern Pacific Ocean; 1 Introduction; 2 Data and Methods; 2.1 Bathymetric Data; 2.2 Geomagnetic Data; 3 Results; 3.1 Overview of the Bathymetric Features; 3.2 Topographic Expression of the Trenches; 3.3 Bending-Related Structures of the Oceanward Trench Slopes; 3.3.1 Kuril Trench; 3.3.2 Japan Trench; 3.3.3 Izu-Ogasawara Trench; 3.4 Magnetic Anomalies; 4 Discussion 4.1 Strike of Bending-Related Topographic Structures4.2 Topographic Expression of Bending-Related Structures; 5 Conclusions; References; Erosional Subduction Zonein the Northern Japan Trench: Review of Submersible Dive Reports; 1 Introduction; 2 Oceanward Slope Topography and Geology off Miyako; 3 Landward Slope Topography and Geology off Miyako; 4 Lineaments of the Oceanward and Landward Slopes off Miyako; 5 Conclusions; References; Boso TTT-Type Triple Junction: Formation of Miocene to Quaternary Accretionary Prisms and Present-Day Gravitational Collapse; 1 Introduction 2 Review of Sedimentation, Topography, and Plate Configuration2.1 Sedimentation; 2.2 Topographic Development of the Area from the Eastern Margin of the Sagami Trough to the Boso Triple Junction; 2.3 Katsuura Basin and Mogi Submarine Fan in the Bando Deepsea Basin; 2.4 Review of 3D Structure Based on Multichannel Seismic Profiles and Multibeam Echosounder Data; 2.5 Relationship Between the Tectonic and Age Data; 3 Diatom Analysis; 3.1 Materials, Method, and Results; 3.2 Diatom Biostratigraphy; 3.2.1 Pleistocene to Holocene Samples; 3.2.2 Middle Miocene Sample; 3.3 Summary of Age of Samples 3.4 Correlation to the Marine Rocks of the Izu Forearc4 Tectonic Synthesis: Summary and Conclusion; References; Rifting Structure of Central Izu-Ogasawara (Bonin) Arc Crust: Results of Seismic Crustal Imaging; 1 Introduction; 2 Data Acquisition; 3 Data and Modeling Procedure; 4 Description of Velocity Images; 4.1 Line IBr9; 4.2 Line IBr10; 5 Discussion; 5.1 Structural Commonalities and Differences; 5.2 Origin of the Arc Crust; 5.3 History of the Rifted Crust; 5.4 Reason for the Thin Crust in the Central Izu-Ogasawara Arc; 6 Conclusion; References Seafloor Geology of the Basement Serpentinite Body in the Ohmachi Seamount (Izu-Bonin Arc) as Exhumed Parts of a Subduction Zone Within the Philippine Sea1 Introduction; 2 Geologic Setting and Bathymetry; 3 Lithology; 3.1 Serpentinites; 3.1.1 Massive Serpentinite; 3.1.2 Schistose Serpentinite; 3.2 Amphibole Schist; 3.3 Paleogene Volcanic Rocks; 3.4 Miocene Turbidite; 3.5 Soft Mud Beds; 4 Dive and Dredge Results; 4.1 Dive 6K#341; 4.2 Dive 6K#570; 4.3 Dive 6K#571; 4.4 Dive 6K#575; 4.5 Dive 6K#608; 4.6 Dive 6K#609; 4.7 Dive 6K#610; 4.8 Dive 6K#1064; 4.9 Dive 6K#1065; 4.10 Dive 6K#1066 4.11 Dive 6K#1067 Ogawa, Yujiro misc QE1-996.5 misc QE79 rvk TP 6920 misc Geography misc Geology misc Geology, Structural misc Physical geography misc Oceanography misc Sedimentology misc Earth Sciences gnd Japan gnd Meeresboden gnd Meeresgeologie gnd Ozeanische Erdkruste gnd Gesteinskunde gnd Pazifischer Ozean gnd Akkretionskeil gnd Akkretion gnd Rifting gnd Subduktion gnd Geologie 2027 ebook Accretionary Prisms and Convergent Margin Tectonics in the Northwest Pacific Basin |
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Accretionary Prisms and Convergent Margin Tectonics in the Northwest Pacific Basin |
| abstract |
Accretionary prisms in convergent margins are natural laboratories for exploring initial orogenic processes and mountain building episodes. They are also an important component of continental growth both vertically and laterally. Accretionary prisms are seismically highly active and their internal deformation via megathrusting and out-of-sequence faulting are a big concern for earthquake and tsunami damage in many coastal cities around the Pacific Rim. The geometries and structures of modern accretionary prisms have been well imaged seismically and through deep drilling projects of the Ocean Drilling Program (and recently IODP) during the last 15 years. Better understanding of the spatial distribution and temporal progression of accretionary prism deformation, structural and hydrologic evolution of the décollement zone (tectonic interface between the subducting slab and the upper plate), chemical gradients and fluid flow paths within accretionary prisms, contrasting stratigraphic and deformational framework along-strike in accretionary prisms, and the distribution and ecosystems of biological communities in accretionary prism settings is most important in interpreting the evolution of ancient complex sedimentary terrains and orogenic belts in terms of subduction-related processes. This book is a collection of interdisciplinary papers documenting the geological, geophysical, geochemical, and paleontological features of modern accretionay prisms and trenches in the northwestern Pacific Ocean, based on many submersible dive cruises, ODP drilling projects, and geophysical surveys during the last 10 years. It also includes several papers presenting the results of systematic integrated studies of recent to ancient on-land accretionary prisms in comparison to modern analogues. The individual chapters are data and image rich, providing a major resource of information and knowledge from these critical components of convergent margins for researchers, faculty members, and graduate and undergraduate students. As such, the book will be a major and unique contribution in the broad fields of global tectonics, geodynamics, marine geology and geophysics, and structural geology and sedimentology. Includes bibliographical references and index |
| abstractGer |
Accretionary prisms in convergent margins are natural laboratories for exploring initial orogenic processes and mountain building episodes. They are also an important component of continental growth both vertically and laterally. Accretionary prisms are seismically highly active and their internal deformation via megathrusting and out-of-sequence faulting are a big concern for earthquake and tsunami damage in many coastal cities around the Pacific Rim. The geometries and structures of modern accretionary prisms have been well imaged seismically and through deep drilling projects of the Ocean Drilling Program (and recently IODP) during the last 15 years. Better understanding of the spatial distribution and temporal progression of accretionary prism deformation, structural and hydrologic evolution of the décollement zone (tectonic interface between the subducting slab and the upper plate), chemical gradients and fluid flow paths within accretionary prisms, contrasting stratigraphic and deformational framework along-strike in accretionary prisms, and the distribution and ecosystems of biological communities in accretionary prism settings is most important in interpreting the evolution of ancient complex sedimentary terrains and orogenic belts in terms of subduction-related processes. This book is a collection of interdisciplinary papers documenting the geological, geophysical, geochemical, and paleontological features of modern accretionay prisms and trenches in the northwestern Pacific Ocean, based on many submersible dive cruises, ODP drilling projects, and geophysical surveys during the last 10 years. It also includes several papers presenting the results of systematic integrated studies of recent to ancient on-land accretionary prisms in comparison to modern analogues. The individual chapters are data and image rich, providing a major resource of information and knowledge from these critical components of convergent margins for researchers, faculty members, and graduate and undergraduate students. As such, the book will be a major and unique contribution in the broad fields of global tectonics, geodynamics, marine geology and geophysics, and structural geology and sedimentology. Includes bibliographical references and index |
| abstract_unstemmed |
Accretionary prisms in convergent margins are natural laboratories for exploring initial orogenic processes and mountain building episodes. They are also an important component of continental growth both vertically and laterally. Accretionary prisms are seismically highly active and their internal deformation via megathrusting and out-of-sequence faulting are a big concern for earthquake and tsunami damage in many coastal cities around the Pacific Rim. The geometries and structures of modern accretionary prisms have been well imaged seismically and through deep drilling projects of the Ocean Drilling Program (and recently IODP) during the last 15 years. Better understanding of the spatial distribution and temporal progression of accretionary prism deformation, structural and hydrologic evolution of the décollement zone (tectonic interface between the subducting slab and the upper plate), chemical gradients and fluid flow paths within accretionary prisms, contrasting stratigraphic and deformational framework along-strike in accretionary prisms, and the distribution and ecosystems of biological communities in accretionary prism settings is most important in interpreting the evolution of ancient complex sedimentary terrains and orogenic belts in terms of subduction-related processes. This book is a collection of interdisciplinary papers documenting the geological, geophysical, geochemical, and paleontological features of modern accretionay prisms and trenches in the northwestern Pacific Ocean, based on many submersible dive cruises, ODP drilling projects, and geophysical surveys during the last 10 years. It also includes several papers presenting the results of systematic integrated studies of recent to ancient on-land accretionary prisms in comparison to modern analogues. The individual chapters are data and image rich, providing a major resource of information and knowledge from these critical components of convergent margins for researchers, faculty members, and graduate and undergraduate students. As such, the book will be a major and unique contribution in the broad fields of global tectonics, geodynamics, marine geology and geophysics, and structural geology and sedimentology. Includes bibliographical references and index |
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9789048188857 978-90-481-8885-7 10.1007/978-90-481-8885-7 doi (DE-627)1650945701 (DE-576)345803701 (DE-599)BSZ345803701 (OCoLC)740949297 (OCoLC)740949297 (DE-He213)978-90-481-8885-7 DE-627 ger DE-627 rakwb eng XA-NL QE1-996.5 QE79 RBG bicssc SCI031000 bisacsh TP 6920 SEPA rvk (DE-625)rvk/144668: Ogawa, Yujiro verfasserin aut Accretionary Prisms and Convergent Margin Tectonics in the Northwest Pacific Basin edited by Yujiro Ogawa, Ryo Anma, Yildirim Dilek Dordrecht Springer Science+Business Media B.V 2011 Online-Ressource (XX, 277p. 123 illus., 69 illus. in color, digital) Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Modern Approaches in Solid Earth Sciences 8 SpringerLink Bücher Includes bibliographical references and index Accretionary Prisms and Convergent Margin Tectonics in the Northwest Pacific Basin; Preface; Acknowledgements; Contents; Contributors; Bending-Related Topographic Structures of the Subducting Plate in the Northwestern Pacific Ocean; 1 Introduction; 2 Data and Methods; 2.1 Bathymetric Data; 2.2 Geomagnetic Data; 3 Results; 3.1 Overview of the Bathymetric Features; 3.2 Topographic Expression of the Trenches; 3.3 Bending-Related Structures of the Oceanward Trench Slopes; 3.3.1 Kuril Trench; 3.3.2 Japan Trench; 3.3.3 Izu-Ogasawara Trench; 3.4 Magnetic Anomalies; 4 Discussion 4.1 Strike of Bending-Related Topographic Structures4.2 Topographic Expression of Bending-Related Structures; 5 Conclusions; References; Erosional Subduction Zonein the Northern Japan Trench: Review of Submersible Dive Reports; 1 Introduction; 2 Oceanward Slope Topography and Geology off Miyako; 3 Landward Slope Topography and Geology off Miyako; 4 Lineaments of the Oceanward and Landward Slopes off Miyako; 5 Conclusions; References; Boso TTT-Type Triple Junction: Formation of Miocene to Quaternary Accretionary Prisms and Present-Day Gravitational Collapse; 1 Introduction 2 Review of Sedimentation, Topography, and Plate Configuration2.1 Sedimentation; 2.2 Topographic Development of the Area from the Eastern Margin of the Sagami Trough to the Boso Triple Junction; 2.3 Katsuura Basin and Mogi Submarine Fan in the Bando Deepsea Basin; 2.4 Review of 3D Structure Based on Multichannel Seismic Profiles and Multibeam Echosounder Data; 2.5 Relationship Between the Tectonic and Age Data; 3 Diatom Analysis; 3.1 Materials, Method, and Results; 3.2 Diatom Biostratigraphy; 3.2.1 Pleistocene to Holocene Samples; 3.2.2 Middle Miocene Sample; 3.3 Summary of Age of Samples 3.4 Correlation to the Marine Rocks of the Izu Forearc4 Tectonic Synthesis: Summary and Conclusion; References; Rifting Structure of Central Izu-Ogasawara (Bonin) Arc Crust: Results of Seismic Crustal Imaging; 1 Introduction; 2 Data Acquisition; 3 Data and Modeling Procedure; 4 Description of Velocity Images; 4.1 Line IBr9; 4.2 Line IBr10; 5 Discussion; 5.1 Structural Commonalities and Differences; 5.2 Origin of the Arc Crust; 5.3 History of the Rifted Crust; 5.4 Reason for the Thin Crust in the Central Izu-Ogasawara Arc; 6 Conclusion; References Seafloor Geology of the Basement Serpentinite Body in the Ohmachi Seamount (Izu-Bonin Arc) as Exhumed Parts of a Subduction Zone Within the Philippine Sea1 Introduction; 2 Geologic Setting and Bathymetry; 3 Lithology; 3.1 Serpentinites; 3.1.1 Massive Serpentinite; 3.1.2 Schistose Serpentinite; 3.2 Amphibole Schist; 3.3 Paleogene Volcanic Rocks; 3.4 Miocene Turbidite; 3.5 Soft Mud Beds; 4 Dive and Dredge Results; 4.1 Dive 6K#341; 4.2 Dive 6K#570; 4.3 Dive 6K#571; 4.4 Dive 6K#575; 4.5 Dive 6K#608; 4.6 Dive 6K#609; 4.7 Dive 6K#610; 4.8 Dive 6K#1064; 4.9 Dive 6K#1065; 4.10 Dive 6K#1066 4.11 Dive 6K#1067 Accretionary prisms in convergent margins are natural laboratories for exploring initial orogenic processes and mountain building episodes. They are also an important component of continental growth both vertically and laterally. Accretionary prisms are seismically highly active and their internal deformation via megathrusting and out-of-sequence faulting are a big concern for earthquake and tsunami damage in many coastal cities around the Pacific Rim. The geometries and structures of modern accretionary prisms have been well imaged seismically and through deep drilling projects of the Ocean Drilling Program (and recently IODP) during the last 15 years. Better understanding of the spatial distribution and temporal progression of accretionary prism deformation, structural and hydrologic evolution of the décollement zone (tectonic interface between the subducting slab and the upper plate), chemical gradients and fluid flow paths within accretionary prisms, contrasting stratigraphic and deformational framework along-strike in accretionary prisms, and the distribution and ecosystems of biological communities in accretionary prism settings is most important in interpreting the evolution of ancient complex sedimentary terrains and orogenic belts in terms of subduction-related processes. This book is a collection of interdisciplinary papers documenting the geological, geophysical, geochemical, and paleontological features of modern accretionay prisms and trenches in the northwestern Pacific Ocean, based on many submersible dive cruises, ODP drilling projects, and geophysical surveys during the last 10 years. It also includes several papers presenting the results of systematic integrated studies of recent to ancient on-land accretionary prisms in comparison to modern analogues. The individual chapters are data and image rich, providing a major resource of information and knowledge from these critical components of convergent margins for researchers, faculty members, and graduate and undergraduate students. As such, the book will be a major and unique contribution in the broad fields of global tectonics, geodynamics, marine geology and geophysics, and structural geology and sedimentology. Geography Geology Geology, Structural Physical geography Oceanography Sedimentology Earth Sciences Geography Geology Geology, Structural Physical geography Oceanography Sedimentology Aufsatzsammlung (DE-588)4143413-4 (DE-627)105605727 (DE-576)209726091 gnd-content g (DE-588)4028495-5 (DE-627)104585102 (DE-576)208977503 Japan gnd s (DE-588)4129066-5 (DE-627)105712590 (DE-576)209607432 Meeresboden gnd s (DE-588)4038316-7 (DE-627)106232916 (DE-576)209029463 Meeresgeologie gnd s (DE-588)4401814-9 (DE-627)19331813X (DE-576)21206777X Ozeanische Erdkruste gnd s (DE-588)4020740-7 (DE-627)106316915 (DE-576)208934626 Gesteinskunde gnd (DE-627) g (DE-588)4255480-9 (DE-627)104706228 (DE-576)210547766 Pazifischer Ozean Nordwest gnd s (DE-588)4418304-5 (DE-627)213357410 (DE-576)212237373 Akkretionskeil gnd s (DE-588)4507349-1 (DE-627)246123729 (DE-576)213144794 Akkretion Geologie gnd s (DE-588)4619283-9 (DE-627)326427570 (DE-576)214330656 Rifting gnd s (DE-588)4183899-3 (DE-627)105299286 (DE-576)210021926 Subduktion gnd s (DE-588)4020227-6 (DE-627)106318810 (DE-576)20893247X Geologie gnd (DE-627) Anma, Ryo oth Dilek, Yildirim oth 9789048188840 Buchausg. u.d.T. Accretionary prisms and convergent margin tectonics in the Northwest Pacific basin 1. ed. Dordrecht : Springer, 2011 XX, 277 S. (DE-627)619693886 (DE-576)320687104 9048188849 9789048188840 https://doi.org/10.1007/978-90-481-8885-7 Verlag Volltext http://dx.doi.org/10.1007/978-90-481-8885-7 Resolving-System lizenzpflichtig Volltext https://swbplus.bsz-bw.de/bsz345803701cov.jpg V:DE-576 X:springer image/jpeg 20150507143318 Cover https://swbplus.bsz-bw.de/bsz320687104inh.htm V:DE-576;B:DE-105 application/pdf 20110728124932 Inhaltsverzeichnis http://www.gbv.de/dms/bowker/toc/9789048188840.pdf V:DE-601 X:Bowker pdf/application 2011-12-20 Verlag Inhaltsverzeichnis Inhaltsverzeichnis (DE-627)664555047 ZDB-2-EES 2011 GBV_ILN_22 ISIL_DE-18 SYSFLAG_1 GBV_KXP GBV_ILN_22_i05715 GBV_ILN_60 ISIL_DE-705 GBV_ILN_62 ISIL_DE-28 GBV_ILN_65 ISIL_DE-3 GBV_ILN_69 ISIL_DE-9 GBV_ILN_110 ISIL_DE-Luen4 GBV_ILN_120 ISIL_DE-715 GBV_ILN_285 ISIL_DE-517 GBV_ILN_370 ISIL_DE-1373 GBV_ILN_2027 ISIL_DE-105 GBV_ILN_2050 ISIL_DE-Zi4 GBV_ILN_2061 ISIL_DE-520 GBV_ILN_2148 ISIL_DE-950 GBV ExPruef TP 6920 Japan Geowissenschaften Regionale Geologie Asien (ohne GUS) Ostasien Japan (DE-627)1271946629 (DE-625)rvk/144668: (DE-576)201946629 BO 045F 551 045F 551.1 22 01 0018 1266756787 00 --%%-- --%%-- s --%%-- h57-ees Vervielfältigungen (z.B. 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9789048188857 978-90-481-8885-7 10.1007/978-90-481-8885-7 doi (DE-627)1650945701 (DE-576)345803701 (DE-599)BSZ345803701 (OCoLC)740949297 (OCoLC)740949297 (DE-He213)978-90-481-8885-7 DE-627 ger DE-627 rakwb eng XA-NL QE1-996.5 QE79 RBG bicssc SCI031000 bisacsh TP 6920 SEPA rvk (DE-625)rvk/144668: Ogawa, Yujiro verfasserin aut Accretionary Prisms and Convergent Margin Tectonics in the Northwest Pacific Basin edited by Yujiro Ogawa, Ryo Anma, Yildirim Dilek Dordrecht Springer Science+Business Media B.V 2011 Online-Ressource (XX, 277p. 123 illus., 69 illus. in color, digital) Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Modern Approaches in Solid Earth Sciences 8 SpringerLink Bücher Includes bibliographical references and index Accretionary Prisms and Convergent Margin Tectonics in the Northwest Pacific Basin; Preface; Acknowledgements; Contents; Contributors; Bending-Related Topographic Structures of the Subducting Plate in the Northwestern Pacific Ocean; 1 Introduction; 2 Data and Methods; 2.1 Bathymetric Data; 2.2 Geomagnetic Data; 3 Results; 3.1 Overview of the Bathymetric Features; 3.2 Topographic Expression of the Trenches; 3.3 Bending-Related Structures of the Oceanward Trench Slopes; 3.3.1 Kuril Trench; 3.3.2 Japan Trench; 3.3.3 Izu-Ogasawara Trench; 3.4 Magnetic Anomalies; 4 Discussion 4.1 Strike of Bending-Related Topographic Structures4.2 Topographic Expression of Bending-Related Structures; 5 Conclusions; References; Erosional Subduction Zonein the Northern Japan Trench: Review of Submersible Dive Reports; 1 Introduction; 2 Oceanward Slope Topography and Geology off Miyako; 3 Landward Slope Topography and Geology off Miyako; 4 Lineaments of the Oceanward and Landward Slopes off Miyako; 5 Conclusions; References; Boso TTT-Type Triple Junction: Formation of Miocene to Quaternary Accretionary Prisms and Present-Day Gravitational Collapse; 1 Introduction 2 Review of Sedimentation, Topography, and Plate Configuration2.1 Sedimentation; 2.2 Topographic Development of the Area from the Eastern Margin of the Sagami Trough to the Boso Triple Junction; 2.3 Katsuura Basin and Mogi Submarine Fan in the Bando Deepsea Basin; 2.4 Review of 3D Structure Based on Multichannel Seismic Profiles and Multibeam Echosounder Data; 2.5 Relationship Between the Tectonic and Age Data; 3 Diatom Analysis; 3.1 Materials, Method, and Results; 3.2 Diatom Biostratigraphy; 3.2.1 Pleistocene to Holocene Samples; 3.2.2 Middle Miocene Sample; 3.3 Summary of Age of Samples 3.4 Correlation to the Marine Rocks of the Izu Forearc4 Tectonic Synthesis: Summary and Conclusion; References; Rifting Structure of Central Izu-Ogasawara (Bonin) Arc Crust: Results of Seismic Crustal Imaging; 1 Introduction; 2 Data Acquisition; 3 Data and Modeling Procedure; 4 Description of Velocity Images; 4.1 Line IBr9; 4.2 Line IBr10; 5 Discussion; 5.1 Structural Commonalities and Differences; 5.2 Origin of the Arc Crust; 5.3 History of the Rifted Crust; 5.4 Reason for the Thin Crust in the Central Izu-Ogasawara Arc; 6 Conclusion; References Seafloor Geology of the Basement Serpentinite Body in the Ohmachi Seamount (Izu-Bonin Arc) as Exhumed Parts of a Subduction Zone Within the Philippine Sea1 Introduction; 2 Geologic Setting and Bathymetry; 3 Lithology; 3.1 Serpentinites; 3.1.1 Massive Serpentinite; 3.1.2 Schistose Serpentinite; 3.2 Amphibole Schist; 3.3 Paleogene Volcanic Rocks; 3.4 Miocene Turbidite; 3.5 Soft Mud Beds; 4 Dive and Dredge Results; 4.1 Dive 6K#341; 4.2 Dive 6K#570; 4.3 Dive 6K#571; 4.4 Dive 6K#575; 4.5 Dive 6K#608; 4.6 Dive 6K#609; 4.7 Dive 6K#610; 4.8 Dive 6K#1064; 4.9 Dive 6K#1065; 4.10 Dive 6K#1066 4.11 Dive 6K#1067 Accretionary prisms in convergent margins are natural laboratories for exploring initial orogenic processes and mountain building episodes. They are also an important component of continental growth both vertically and laterally. Accretionary prisms are seismically highly active and their internal deformation via megathrusting and out-of-sequence faulting are a big concern for earthquake and tsunami damage in many coastal cities around the Pacific Rim. The geometries and structures of modern accretionary prisms have been well imaged seismically and through deep drilling projects of the Ocean Drilling Program (and recently IODP) during the last 15 years. Better understanding of the spatial distribution and temporal progression of accretionary prism deformation, structural and hydrologic evolution of the décollement zone (tectonic interface between the subducting slab and the upper plate), chemical gradients and fluid flow paths within accretionary prisms, contrasting stratigraphic and deformational framework along-strike in accretionary prisms, and the distribution and ecosystems of biological communities in accretionary prism settings is most important in interpreting the evolution of ancient complex sedimentary terrains and orogenic belts in terms of subduction-related processes. This book is a collection of interdisciplinary papers documenting the geological, geophysical, geochemical, and paleontological features of modern accretionay prisms and trenches in the northwestern Pacific Ocean, based on many submersible dive cruises, ODP drilling projects, and geophysical surveys during the last 10 years. It also includes several papers presenting the results of systematic integrated studies of recent to ancient on-land accretionary prisms in comparison to modern analogues. The individual chapters are data and image rich, providing a major resource of information and knowledge from these critical components of convergent margins for researchers, faculty members, and graduate and undergraduate students. As such, the book will be a major and unique contribution in the broad fields of global tectonics, geodynamics, marine geology and geophysics, and structural geology and sedimentology. Geography Geology Geology, Structural Physical geography Oceanography Sedimentology Earth Sciences Geography Geology Geology, Structural Physical geography Oceanography Sedimentology Aufsatzsammlung (DE-588)4143413-4 (DE-627)105605727 (DE-576)209726091 gnd-content g (DE-588)4028495-5 (DE-627)104585102 (DE-576)208977503 Japan gnd s (DE-588)4129066-5 (DE-627)105712590 (DE-576)209607432 Meeresboden gnd s (DE-588)4038316-7 (DE-627)106232916 (DE-576)209029463 Meeresgeologie gnd s (DE-588)4401814-9 (DE-627)19331813X (DE-576)21206777X Ozeanische Erdkruste gnd s (DE-588)4020740-7 (DE-627)106316915 (DE-576)208934626 Gesteinskunde gnd (DE-627) g (DE-588)4255480-9 (DE-627)104706228 (DE-576)210547766 Pazifischer Ozean Nordwest gnd s (DE-588)4418304-5 (DE-627)213357410 (DE-576)212237373 Akkretionskeil gnd s (DE-588)4507349-1 (DE-627)246123729 (DE-576)213144794 Akkretion Geologie gnd s (DE-588)4619283-9 (DE-627)326427570 (DE-576)214330656 Rifting gnd s (DE-588)4183899-3 (DE-627)105299286 (DE-576)210021926 Subduktion gnd s (DE-588)4020227-6 (DE-627)106318810 (DE-576)20893247X Geologie gnd (DE-627) Anma, Ryo oth Dilek, Yildirim oth 9789048188840 Buchausg. u.d.T. Accretionary prisms and convergent margin tectonics in the Northwest Pacific basin 1. ed. Dordrecht : Springer, 2011 XX, 277 S. (DE-627)619693886 (DE-576)320687104 9048188849 9789048188840 https://doi.org/10.1007/978-90-481-8885-7 Verlag Volltext http://dx.doi.org/10.1007/978-90-481-8885-7 Resolving-System lizenzpflichtig Volltext https://swbplus.bsz-bw.de/bsz345803701cov.jpg V:DE-576 X:springer image/jpeg 20150507143318 Cover https://swbplus.bsz-bw.de/bsz320687104inh.htm V:DE-576;B:DE-105 application/pdf 20110728124932 Inhaltsverzeichnis http://www.gbv.de/dms/bowker/toc/9789048188840.pdf V:DE-601 X:Bowker pdf/application 2011-12-20 Verlag Inhaltsverzeichnis Inhaltsverzeichnis (DE-627)664555047 ZDB-2-EES 2011 GBV_ILN_22 ISIL_DE-18 SYSFLAG_1 GBV_KXP GBV_ILN_22_i05715 GBV_ILN_60 ISIL_DE-705 GBV_ILN_62 ISIL_DE-28 GBV_ILN_65 ISIL_DE-3 GBV_ILN_69 ISIL_DE-9 GBV_ILN_110 ISIL_DE-Luen4 GBV_ILN_120 ISIL_DE-715 GBV_ILN_285 ISIL_DE-517 GBV_ILN_370 ISIL_DE-1373 GBV_ILN_2027 ISIL_DE-105 GBV_ILN_2050 ISIL_DE-Zi4 GBV_ILN_2061 ISIL_DE-520 GBV_ILN_2148 ISIL_DE-950 GBV ExPruef TP 6920 Japan Geowissenschaften Regionale Geologie Asien (ohne GUS) Ostasien Japan (DE-627)1271946629 (DE-625)rvk/144668: (DE-576)201946629 BO 045F 551 045F 551.1 22 01 0018 1266756787 00 --%%-- --%%-- s --%%-- h57-ees Vervielfältigungen (z.B. 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Kopien, Downloads) sind nur von einzelnen Kapiteln oder Seiten und nur zum eigenen wissenschaftlichen Gebrauch erlaubt. Die Weitergabe an Dritte sowie systematisches Downloaden sind untersagt. k3o 02-01-17 69 01 0009 1257218883 OLR-SEB-ZDB-2-EES Vervielfältigungen (z.B. Kopien, Downloads) sind nur von einzelnen Kapiteln oder Seiten und nur zum eigenen wissenschaftlichen Gebrauch erlaubt. Keine Weitergabe an Dritte. Kein systematisches Downloaden durch Robots. z 26-07-11 110 01 3110 430502604X 00 --%%-- --%%-- s --%%-- OLR-SEB Vervielfältigungen (z.B. Kopien, Downloads) sind nur von einzelnen Kapiteln oder Seiten und nur zum eigenen wissenschaftlichen Gebrauch erlaubt. Keine Weitergabe an Dritte. Kein systematisches Downloaden durch Robots. z 07-04-23 120 01 0715 1840114584 OLR-ESP Campusweiter Zugriff (Universität Oldenburg). - Vervielfältigungen (z.B. Kopien, Downloads) sind nur von einzelnen Kapiteln oder Seiten und nur zum eigenen wissenschaftlichen Gebrauch erlaubt. 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Kein systematisches Downloaden durch Robots. i z 26-07-11 2027 01 DE-105 3340379459 00 --%%-- --%%-- n --%%-- Campuslizenz l01 17-05-11 2050 01 DE-Zi4 3340379467 00 --%%-- --%%-- n --%%-- Elektronischer Volltext - Campuslizenz l01 17-05-11 2061 01 DE-520 3340379475 00 --%%-- --%%-- n --%%-- eBook, Link nur im Campusbereich nutzbar l01 17-05-11 2148 01 DE-950 3340379491 00 --%%-- eBook Springer --%%-- n Elektronischer Volltext - Campuslizenz l01 10-06-11 22 01 0018 Volltextzugang Campus https://doi.org/10.1007/978-90-481-8885-7 22 01 0018 Nur für Angehörige der Universität Hamburg: Volltextzugang von außerhalb des Campus http://emedien.sub.uni-hamburg.de/han/SpringerEbooks/doi.org/10.1007/978-90-481-8885-7 60 01 0705 Volltextzugang Campus https://doi.org/10.1007/978-90-481-8885-7 62 01 0028 https://doi.org/10.1007/978-90-481-8885-7 65 01 0003 Volltextzugang Campus https://doi.org/10.1007/978-90-481-8885-7 69 01 0009 https://doi.org/10.1007/978-90-481-8885-7 110 01 3110 https://doi.org/10.1007/978-90-481-8885-7 120 01 0715 http://dx.doi.org/10.1007/978-90-481-8885-7 120 02 0715 http://49gbv-uob-primo.hosted.exlibrisgroup.com/openurl/49GBV_UOB/UOB_services_page?u.ignore_date_coverage=true&rft.mms_id=991016137662403501 285 01 0517 E-books (Springer) https://doi.org/10.1007/978-90-481-8885-7 370 01 4370 E-Book: Zugriff im HCU-Netz. Zugriff von außerhalb nur für HCU-Angehörige möglich https://doi.org/10.1007/978-90-481-8885-7 2050 01 DE-Zi4 http://dx.doi.org/10.1007/978-90-481-8885-7 2061 01 DE-520 http://dx.doi.org/10.1007/978-90-481-8885-7 2148 01 DE-950 http://dx.doi.org/10.1007/978-90-481-8885-7 2027 01 DE-105 00 s ebook 120 00 DE-715 99 ww 120 01 0715 YH 2020 22 01 0018 h57-ees 60 01 0705 SpringerLink 62 01 0028 OLR-SEB 62 01 0028 OLR-EES 65 01 0003 OLR-SEB-ZDB-2-EES 69 01 0009 OLR-SEB-ZDB-2-EES 110 01 3110 OLR-SEB 120 01 0715 OLR-ESP 120 02 0715 alma 285 01 0517 OLR-ESP-EES 370 01 4370 olr-springer |
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9789048188857 978-90-481-8885-7 10.1007/978-90-481-8885-7 doi (DE-627)1650945701 (DE-576)345803701 (DE-599)BSZ345803701 (OCoLC)740949297 (OCoLC)740949297 (DE-He213)978-90-481-8885-7 DE-627 ger DE-627 rakwb eng XA-NL QE1-996.5 QE79 RBG bicssc SCI031000 bisacsh TP 6920 SEPA rvk (DE-625)rvk/144668: Ogawa, Yujiro verfasserin aut Accretionary Prisms and Convergent Margin Tectonics in the Northwest Pacific Basin edited by Yujiro Ogawa, Ryo Anma, Yildirim Dilek Dordrecht Springer Science+Business Media B.V 2011 Online-Ressource (XX, 277p. 123 illus., 69 illus. in color, digital) Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Modern Approaches in Solid Earth Sciences 8 SpringerLink Bücher Includes bibliographical references and index Accretionary Prisms and Convergent Margin Tectonics in the Northwest Pacific Basin; Preface; Acknowledgements; Contents; Contributors; Bending-Related Topographic Structures of the Subducting Plate in the Northwestern Pacific Ocean; 1 Introduction; 2 Data and Methods; 2.1 Bathymetric Data; 2.2 Geomagnetic Data; 3 Results; 3.1 Overview of the Bathymetric Features; 3.2 Topographic Expression of the Trenches; 3.3 Bending-Related Structures of the Oceanward Trench Slopes; 3.3.1 Kuril Trench; 3.3.2 Japan Trench; 3.3.3 Izu-Ogasawara Trench; 3.4 Magnetic Anomalies; 4 Discussion 4.1 Strike of Bending-Related Topographic Structures4.2 Topographic Expression of Bending-Related Structures; 5 Conclusions; References; Erosional Subduction Zonein the Northern Japan Trench: Review of Submersible Dive Reports; 1 Introduction; 2 Oceanward Slope Topography and Geology off Miyako; 3 Landward Slope Topography and Geology off Miyako; 4 Lineaments of the Oceanward and Landward Slopes off Miyako; 5 Conclusions; References; Boso TTT-Type Triple Junction: Formation of Miocene to Quaternary Accretionary Prisms and Present-Day Gravitational Collapse; 1 Introduction 2 Review of Sedimentation, Topography, and Plate Configuration2.1 Sedimentation; 2.2 Topographic Development of the Area from the Eastern Margin of the Sagami Trough to the Boso Triple Junction; 2.3 Katsuura Basin and Mogi Submarine Fan in the Bando Deepsea Basin; 2.4 Review of 3D Structure Based on Multichannel Seismic Profiles and Multibeam Echosounder Data; 2.5 Relationship Between the Tectonic and Age Data; 3 Diatom Analysis; 3.1 Materials, Method, and Results; 3.2 Diatom Biostratigraphy; 3.2.1 Pleistocene to Holocene Samples; 3.2.2 Middle Miocene Sample; 3.3 Summary of Age of Samples 3.4 Correlation to the Marine Rocks of the Izu Forearc4 Tectonic Synthesis: Summary and Conclusion; References; Rifting Structure of Central Izu-Ogasawara (Bonin) Arc Crust: Results of Seismic Crustal Imaging; 1 Introduction; 2 Data Acquisition; 3 Data and Modeling Procedure; 4 Description of Velocity Images; 4.1 Line IBr9; 4.2 Line IBr10; 5 Discussion; 5.1 Structural Commonalities and Differences; 5.2 Origin of the Arc Crust; 5.3 History of the Rifted Crust; 5.4 Reason for the Thin Crust in the Central Izu-Ogasawara Arc; 6 Conclusion; References Seafloor Geology of the Basement Serpentinite Body in the Ohmachi Seamount (Izu-Bonin Arc) as Exhumed Parts of a Subduction Zone Within the Philippine Sea1 Introduction; 2 Geologic Setting and Bathymetry; 3 Lithology; 3.1 Serpentinites; 3.1.1 Massive Serpentinite; 3.1.2 Schistose Serpentinite; 3.2 Amphibole Schist; 3.3 Paleogene Volcanic Rocks; 3.4 Miocene Turbidite; 3.5 Soft Mud Beds; 4 Dive and Dredge Results; 4.1 Dive 6K#341; 4.2 Dive 6K#570; 4.3 Dive 6K#571; 4.4 Dive 6K#575; 4.5 Dive 6K#608; 4.6 Dive 6K#609; 4.7 Dive 6K#610; 4.8 Dive 6K#1064; 4.9 Dive 6K#1065; 4.10 Dive 6K#1066 4.11 Dive 6K#1067 Accretionary prisms in convergent margins are natural laboratories for exploring initial orogenic processes and mountain building episodes. They are also an important component of continental growth both vertically and laterally. Accretionary prisms are seismically highly active and their internal deformation via megathrusting and out-of-sequence faulting are a big concern for earthquake and tsunami damage in many coastal cities around the Pacific Rim. The geometries and structures of modern accretionary prisms have been well imaged seismically and through deep drilling projects of the Ocean Drilling Program (and recently IODP) during the last 15 years. Better understanding of the spatial distribution and temporal progression of accretionary prism deformation, structural and hydrologic evolution of the décollement zone (tectonic interface between the subducting slab and the upper plate), chemical gradients and fluid flow paths within accretionary prisms, contrasting stratigraphic and deformational framework along-strike in accretionary prisms, and the distribution and ecosystems of biological communities in accretionary prism settings is most important in interpreting the evolution of ancient complex sedimentary terrains and orogenic belts in terms of subduction-related processes. This book is a collection of interdisciplinary papers documenting the geological, geophysical, geochemical, and paleontological features of modern accretionay prisms and trenches in the northwestern Pacific Ocean, based on many submersible dive cruises, ODP drilling projects, and geophysical surveys during the last 10 years. It also includes several papers presenting the results of systematic integrated studies of recent to ancient on-land accretionary prisms in comparison to modern analogues. The individual chapters are data and image rich, providing a major resource of information and knowledge from these critical components of convergent margins for researchers, faculty members, and graduate and undergraduate students. As such, the book will be a major and unique contribution in the broad fields of global tectonics, geodynamics, marine geology and geophysics, and structural geology and sedimentology. Geography Geology Geology, Structural Physical geography Oceanography Sedimentology Earth Sciences Geography Geology Geology, Structural Physical geography Oceanography Sedimentology Aufsatzsammlung (DE-588)4143413-4 (DE-627)105605727 (DE-576)209726091 gnd-content g (DE-588)4028495-5 (DE-627)104585102 (DE-576)208977503 Japan gnd s (DE-588)4129066-5 (DE-627)105712590 (DE-576)209607432 Meeresboden gnd s (DE-588)4038316-7 (DE-627)106232916 (DE-576)209029463 Meeresgeologie gnd s (DE-588)4401814-9 (DE-627)19331813X (DE-576)21206777X Ozeanische Erdkruste gnd s (DE-588)4020740-7 (DE-627)106316915 (DE-576)208934626 Gesteinskunde gnd (DE-627) g (DE-588)4255480-9 (DE-627)104706228 (DE-576)210547766 Pazifischer Ozean Nordwest gnd s (DE-588)4418304-5 (DE-627)213357410 (DE-576)212237373 Akkretionskeil gnd s (DE-588)4507349-1 (DE-627)246123729 (DE-576)213144794 Akkretion Geologie gnd s (DE-588)4619283-9 (DE-627)326427570 (DE-576)214330656 Rifting gnd s (DE-588)4183899-3 (DE-627)105299286 (DE-576)210021926 Subduktion gnd s (DE-588)4020227-6 (DE-627)106318810 (DE-576)20893247X Geologie gnd (DE-627) Anma, Ryo oth Dilek, Yildirim oth 9789048188840 Buchausg. u.d.T. Accretionary prisms and convergent margin tectonics in the Northwest Pacific basin 1. ed. Dordrecht : Springer, 2011 XX, 277 S. (DE-627)619693886 (DE-576)320687104 9048188849 9789048188840 https://doi.org/10.1007/978-90-481-8885-7 Verlag Volltext http://dx.doi.org/10.1007/978-90-481-8885-7 Resolving-System lizenzpflichtig Volltext https://swbplus.bsz-bw.de/bsz345803701cov.jpg V:DE-576 X:springer image/jpeg 20150507143318 Cover https://swbplus.bsz-bw.de/bsz320687104inh.htm V:DE-576;B:DE-105 application/pdf 20110728124932 Inhaltsverzeichnis http://www.gbv.de/dms/bowker/toc/9789048188840.pdf V:DE-601 X:Bowker pdf/application 2011-12-20 Verlag Inhaltsverzeichnis Inhaltsverzeichnis (DE-627)664555047 ZDB-2-EES 2011 GBV_ILN_22 ISIL_DE-18 SYSFLAG_1 GBV_KXP GBV_ILN_22_i05715 GBV_ILN_60 ISIL_DE-705 GBV_ILN_62 ISIL_DE-28 GBV_ILN_65 ISIL_DE-3 GBV_ILN_69 ISIL_DE-9 GBV_ILN_110 ISIL_DE-Luen4 GBV_ILN_120 ISIL_DE-715 GBV_ILN_285 ISIL_DE-517 GBV_ILN_370 ISIL_DE-1373 GBV_ILN_2027 ISIL_DE-105 GBV_ILN_2050 ISIL_DE-Zi4 GBV_ILN_2061 ISIL_DE-520 GBV_ILN_2148 ISIL_DE-950 GBV ExPruef TP 6920 Japan Geowissenschaften Regionale Geologie Asien (ohne GUS) Ostasien Japan (DE-627)1271946629 (DE-625)rvk/144668: (DE-576)201946629 BO 045F 551 045F 551.1 22 01 0018 1266756787 00 --%%-- --%%-- s --%%-- h57-ees Vervielfältigungen (z.B. Kopien, Downloads) sind nur von einzelnen Kapiteln oder Seiten und nur zum eigenen wissenschaftlichen Gebrauch erlaubt. Keine Weitergabe an Dritte. Kein systematisches Downloaden durch Robots. zi05715 26-08-11 60 01 0705 4304954830 SpringerLink Vervielfältigungen (z.B. Kopien, Downloads) sind nur von einzelnen Kapiteln oder Seiten und nur zum eigenen wissenschaftlichen Gebrauch erlaubt. Keine Weitergabe an Dritte. Kein systematisches Downloaden durch Robots. Nur für Angehörige der HSU: Volltextzugang von außerhalb des Campus mit Anmeldung über Shibboleth mit Ihrer Bibliothekskennung z 07-04-23 62 01 0028 1257290495 OLR-SEB Vervielfältigungen (z.B. Kopien, Downloads) sind nur von einzelnen Kapiteln oder Seiten und nur zum eigenen wissenschaftlichen Gebrauch erlaubt. Die Weitergabe an Dritte sowie systematisches Downloaden sind untersagt. z 26-07-11 65 01 0003 1655665189 03 --%%-- ebook --%%-- --%%-- OLR-SEB-ZDB-2-EES Vervielfältigungen (z.B. Kopien, Downloads) sind nur von einzelnen Kapiteln oder Seiten und nur zum eigenen wissenschaftlichen Gebrauch erlaubt. Die Weitergabe an Dritte sowie systematisches Downloaden sind untersagt. k3o 02-01-17 69 01 0009 1257218883 OLR-SEB-ZDB-2-EES Vervielfältigungen (z.B. Kopien, Downloads) sind nur von einzelnen Kapiteln oder Seiten und nur zum eigenen wissenschaftlichen Gebrauch erlaubt. Keine Weitergabe an Dritte. Kein systematisches Downloaden durch Robots. z 26-07-11 110 01 3110 430502604X 00 --%%-- --%%-- s --%%-- OLR-SEB Vervielfältigungen (z.B. Kopien, Downloads) sind nur von einzelnen Kapiteln oder Seiten und nur zum eigenen wissenschaftlichen Gebrauch erlaubt. Keine Weitergabe an Dritte. Kein systematisches Downloaden durch Robots. z 07-04-23 120 01 0715 1840114584 OLR-ESP Campusweiter Zugriff (Universität Oldenburg). - Vervielfältigungen (z.B. Kopien, Downloads) sind nur von einzelnen Kapiteln oder Seiten und nur zum eigenen wissenschaftlichen Gebrauch erlaubt. Keine Weitergabe an Dritte. Kein systematisches Downloaden. z 13-01-19 120 02 0715 3577164786 00 --%%-- --%%-- g --%%-- alma z 20-01-20 285 01 0517 1257282514 00 --%%-- --%%-- s --%%-- OLR-ESP-EES Vervielfältigungen (z.B. Kopien, Downloads) sind nur von einzelnen Kapiteln oder Seiten und nur zum eigenen wissenschaftlichen Gebrauch erlaubt. Keine Weitergabe an Dritte. Kein systematisches Downloaden durch Robots. z 26-07-11 370 01 4370 1257150286 olr-springer Vervielfältigungen (z.B. Kopien, Downloads) sind nur von einzelnen Kapiteln oder Seiten und nur zum eigenen wissenschaftlichen Gebrauch erlaubt. Keine Weitergabe an Dritte. Kein systematisches Downloaden durch Robots. i z 26-07-11 2027 01 DE-105 3340379459 00 --%%-- --%%-- n --%%-- Campuslizenz l01 17-05-11 2050 01 DE-Zi4 3340379467 00 --%%-- --%%-- n --%%-- Elektronischer Volltext - Campuslizenz l01 17-05-11 2061 01 DE-520 3340379475 00 --%%-- --%%-- n --%%-- eBook, Link nur im Campusbereich nutzbar l01 17-05-11 2148 01 DE-950 3340379491 00 --%%-- eBook Springer --%%-- n Elektronischer Volltext - Campuslizenz l01 10-06-11 22 01 0018 Volltextzugang Campus https://doi.org/10.1007/978-90-481-8885-7 22 01 0018 Nur für Angehörige der Universität Hamburg: Volltextzugang von außerhalb des Campus http://emedien.sub.uni-hamburg.de/han/SpringerEbooks/doi.org/10.1007/978-90-481-8885-7 60 01 0705 Volltextzugang Campus https://doi.org/10.1007/978-90-481-8885-7 62 01 0028 https://doi.org/10.1007/978-90-481-8885-7 65 01 0003 Volltextzugang Campus https://doi.org/10.1007/978-90-481-8885-7 69 01 0009 https://doi.org/10.1007/978-90-481-8885-7 110 01 3110 https://doi.org/10.1007/978-90-481-8885-7 120 01 0715 http://dx.doi.org/10.1007/978-90-481-8885-7 120 02 0715 http://49gbv-uob-primo.hosted.exlibrisgroup.com/openurl/49GBV_UOB/UOB_services_page?u.ignore_date_coverage=true&rft.mms_id=991016137662403501 285 01 0517 E-books (Springer) https://doi.org/10.1007/978-90-481-8885-7 370 01 4370 E-Book: Zugriff im HCU-Netz. Zugriff von außerhalb nur für HCU-Angehörige möglich https://doi.org/10.1007/978-90-481-8885-7 2050 01 DE-Zi4 http://dx.doi.org/10.1007/978-90-481-8885-7 2061 01 DE-520 http://dx.doi.org/10.1007/978-90-481-8885-7 2148 01 DE-950 http://dx.doi.org/10.1007/978-90-481-8885-7 2027 01 DE-105 00 s ebook 120 00 DE-715 99 ww 120 01 0715 YH 2020 22 01 0018 h57-ees 60 01 0705 SpringerLink 62 01 0028 OLR-SEB 62 01 0028 OLR-EES 65 01 0003 OLR-SEB-ZDB-2-EES 69 01 0009 OLR-SEB-ZDB-2-EES 110 01 3110 OLR-SEB 120 01 0715 OLR-ESP 120 02 0715 alma 285 01 0517 OLR-ESP-EES 370 01 4370 olr-springer |
| allfieldsGer |
9789048188857 978-90-481-8885-7 10.1007/978-90-481-8885-7 doi (DE-627)1650945701 (DE-576)345803701 (DE-599)BSZ345803701 (OCoLC)740949297 (OCoLC)740949297 (DE-He213)978-90-481-8885-7 DE-627 ger DE-627 rakwb eng XA-NL QE1-996.5 QE79 RBG bicssc SCI031000 bisacsh TP 6920 SEPA rvk (DE-625)rvk/144668: Ogawa, Yujiro verfasserin aut Accretionary Prisms and Convergent Margin Tectonics in the Northwest Pacific Basin edited by Yujiro Ogawa, Ryo Anma, Yildirim Dilek Dordrecht Springer Science+Business Media B.V 2011 Online-Ressource (XX, 277p. 123 illus., 69 illus. in color, digital) Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Modern Approaches in Solid Earth Sciences 8 SpringerLink Bücher Includes bibliographical references and index Accretionary Prisms and Convergent Margin Tectonics in the Northwest Pacific Basin; Preface; Acknowledgements; Contents; Contributors; Bending-Related Topographic Structures of the Subducting Plate in the Northwestern Pacific Ocean; 1 Introduction; 2 Data and Methods; 2.1 Bathymetric Data; 2.2 Geomagnetic Data; 3 Results; 3.1 Overview of the Bathymetric Features; 3.2 Topographic Expression of the Trenches; 3.3 Bending-Related Structures of the Oceanward Trench Slopes; 3.3.1 Kuril Trench; 3.3.2 Japan Trench; 3.3.3 Izu-Ogasawara Trench; 3.4 Magnetic Anomalies; 4 Discussion 4.1 Strike of Bending-Related Topographic Structures4.2 Topographic Expression of Bending-Related Structures; 5 Conclusions; References; Erosional Subduction Zonein the Northern Japan Trench: Review of Submersible Dive Reports; 1 Introduction; 2 Oceanward Slope Topography and Geology off Miyako; 3 Landward Slope Topography and Geology off Miyako; 4 Lineaments of the Oceanward and Landward Slopes off Miyako; 5 Conclusions; References; Boso TTT-Type Triple Junction: Formation of Miocene to Quaternary Accretionary Prisms and Present-Day Gravitational Collapse; 1 Introduction 2 Review of Sedimentation, Topography, and Plate Configuration2.1 Sedimentation; 2.2 Topographic Development of the Area from the Eastern Margin of the Sagami Trough to the Boso Triple Junction; 2.3 Katsuura Basin and Mogi Submarine Fan in the Bando Deepsea Basin; 2.4 Review of 3D Structure Based on Multichannel Seismic Profiles and Multibeam Echosounder Data; 2.5 Relationship Between the Tectonic and Age Data; 3 Diatom Analysis; 3.1 Materials, Method, and Results; 3.2 Diatom Biostratigraphy; 3.2.1 Pleistocene to Holocene Samples; 3.2.2 Middle Miocene Sample; 3.3 Summary of Age of Samples 3.4 Correlation to the Marine Rocks of the Izu Forearc4 Tectonic Synthesis: Summary and Conclusion; References; Rifting Structure of Central Izu-Ogasawara (Bonin) Arc Crust: Results of Seismic Crustal Imaging; 1 Introduction; 2 Data Acquisition; 3 Data and Modeling Procedure; 4 Description of Velocity Images; 4.1 Line IBr9; 4.2 Line IBr10; 5 Discussion; 5.1 Structural Commonalities and Differences; 5.2 Origin of the Arc Crust; 5.3 History of the Rifted Crust; 5.4 Reason for the Thin Crust in the Central Izu-Ogasawara Arc; 6 Conclusion; References Seafloor Geology of the Basement Serpentinite Body in the Ohmachi Seamount (Izu-Bonin Arc) as Exhumed Parts of a Subduction Zone Within the Philippine Sea1 Introduction; 2 Geologic Setting and Bathymetry; 3 Lithology; 3.1 Serpentinites; 3.1.1 Massive Serpentinite; 3.1.2 Schistose Serpentinite; 3.2 Amphibole Schist; 3.3 Paleogene Volcanic Rocks; 3.4 Miocene Turbidite; 3.5 Soft Mud Beds; 4 Dive and Dredge Results; 4.1 Dive 6K#341; 4.2 Dive 6K#570; 4.3 Dive 6K#571; 4.4 Dive 6K#575; 4.5 Dive 6K#608; 4.6 Dive 6K#609; 4.7 Dive 6K#610; 4.8 Dive 6K#1064; 4.9 Dive 6K#1065; 4.10 Dive 6K#1066 4.11 Dive 6K#1067 Accretionary prisms in convergent margins are natural laboratories for exploring initial orogenic processes and mountain building episodes. They are also an important component of continental growth both vertically and laterally. Accretionary prisms are seismically highly active and their internal deformation via megathrusting and out-of-sequence faulting are a big concern for earthquake and tsunami damage in many coastal cities around the Pacific Rim. The geometries and structures of modern accretionary prisms have been well imaged seismically and through deep drilling projects of the Ocean Drilling Program (and recently IODP) during the last 15 years. Better understanding of the spatial distribution and temporal progression of accretionary prism deformation, structural and hydrologic evolution of the décollement zone (tectonic interface between the subducting slab and the upper plate), chemical gradients and fluid flow paths within accretionary prisms, contrasting stratigraphic and deformational framework along-strike in accretionary prisms, and the distribution and ecosystems of biological communities in accretionary prism settings is most important in interpreting the evolution of ancient complex sedimentary terrains and orogenic belts in terms of subduction-related processes. This book is a collection of interdisciplinary papers documenting the geological, geophysical, geochemical, and paleontological features of modern accretionay prisms and trenches in the northwestern Pacific Ocean, based on many submersible dive cruises, ODP drilling projects, and geophysical surveys during the last 10 years. It also includes several papers presenting the results of systematic integrated studies of recent to ancient on-land accretionary prisms in comparison to modern analogues. The individual chapters are data and image rich, providing a major resource of information and knowledge from these critical components of convergent margins for researchers, faculty members, and graduate and undergraduate students. As such, the book will be a major and unique contribution in the broad fields of global tectonics, geodynamics, marine geology and geophysics, and structural geology and sedimentology. Geography Geology Geology, Structural Physical geography Oceanography Sedimentology Earth Sciences Geography Geology Geology, Structural Physical geography Oceanography Sedimentology Aufsatzsammlung (DE-588)4143413-4 (DE-627)105605727 (DE-576)209726091 gnd-content g (DE-588)4028495-5 (DE-627)104585102 (DE-576)208977503 Japan gnd s (DE-588)4129066-5 (DE-627)105712590 (DE-576)209607432 Meeresboden gnd s (DE-588)4038316-7 (DE-627)106232916 (DE-576)209029463 Meeresgeologie gnd s (DE-588)4401814-9 (DE-627)19331813X (DE-576)21206777X Ozeanische Erdkruste gnd s (DE-588)4020740-7 (DE-627)106316915 (DE-576)208934626 Gesteinskunde gnd (DE-627) g (DE-588)4255480-9 (DE-627)104706228 (DE-576)210547766 Pazifischer Ozean Nordwest gnd s (DE-588)4418304-5 (DE-627)213357410 (DE-576)212237373 Akkretionskeil gnd s (DE-588)4507349-1 (DE-627)246123729 (DE-576)213144794 Akkretion Geologie gnd s (DE-588)4619283-9 (DE-627)326427570 (DE-576)214330656 Rifting gnd s (DE-588)4183899-3 (DE-627)105299286 (DE-576)210021926 Subduktion gnd s (DE-588)4020227-6 (DE-627)106318810 (DE-576)20893247X Geologie gnd (DE-627) Anma, Ryo oth Dilek, Yildirim oth 9789048188840 Buchausg. u.d.T. Accretionary prisms and convergent margin tectonics in the Northwest Pacific basin 1. ed. Dordrecht : Springer, 2011 XX, 277 S. (DE-627)619693886 (DE-576)320687104 9048188849 9789048188840 https://doi.org/10.1007/978-90-481-8885-7 Verlag Volltext http://dx.doi.org/10.1007/978-90-481-8885-7 Resolving-System lizenzpflichtig Volltext https://swbplus.bsz-bw.de/bsz345803701cov.jpg V:DE-576 X:springer image/jpeg 20150507143318 Cover https://swbplus.bsz-bw.de/bsz320687104inh.htm V:DE-576;B:DE-105 application/pdf 20110728124932 Inhaltsverzeichnis http://www.gbv.de/dms/bowker/toc/9789048188840.pdf V:DE-601 X:Bowker pdf/application 2011-12-20 Verlag Inhaltsverzeichnis Inhaltsverzeichnis (DE-627)664555047 ZDB-2-EES 2011 GBV_ILN_22 ISIL_DE-18 SYSFLAG_1 GBV_KXP GBV_ILN_22_i05715 GBV_ILN_60 ISIL_DE-705 GBV_ILN_62 ISIL_DE-28 GBV_ILN_65 ISIL_DE-3 GBV_ILN_69 ISIL_DE-9 GBV_ILN_110 ISIL_DE-Luen4 GBV_ILN_120 ISIL_DE-715 GBV_ILN_285 ISIL_DE-517 GBV_ILN_370 ISIL_DE-1373 GBV_ILN_2027 ISIL_DE-105 GBV_ILN_2050 ISIL_DE-Zi4 GBV_ILN_2061 ISIL_DE-520 GBV_ILN_2148 ISIL_DE-950 GBV ExPruef TP 6920 Japan Geowissenschaften Regionale Geologie Asien (ohne GUS) Ostasien Japan (DE-627)1271946629 (DE-625)rvk/144668: (DE-576)201946629 BO 045F 551 045F 551.1 22 01 0018 1266756787 00 --%%-- --%%-- s --%%-- h57-ees Vervielfältigungen (z.B. Kopien, Downloads) sind nur von einzelnen Kapiteln oder Seiten und nur zum eigenen wissenschaftlichen Gebrauch erlaubt. Keine Weitergabe an Dritte. Kein systematisches Downloaden durch Robots. zi05715 26-08-11 60 01 0705 4304954830 SpringerLink Vervielfältigungen (z.B. Kopien, Downloads) sind nur von einzelnen Kapiteln oder Seiten und nur zum eigenen wissenschaftlichen Gebrauch erlaubt. Keine Weitergabe an Dritte. Kein systematisches Downloaden durch Robots. Nur für Angehörige der HSU: Volltextzugang von außerhalb des Campus mit Anmeldung über Shibboleth mit Ihrer Bibliothekskennung z 07-04-23 62 01 0028 1257290495 OLR-SEB Vervielfältigungen (z.B. Kopien, Downloads) sind nur von einzelnen Kapiteln oder Seiten und nur zum eigenen wissenschaftlichen Gebrauch erlaubt. Die Weitergabe an Dritte sowie systematisches Downloaden sind untersagt. z 26-07-11 65 01 0003 1655665189 03 --%%-- ebook --%%-- --%%-- OLR-SEB-ZDB-2-EES Vervielfältigungen (z.B. Kopien, Downloads) sind nur von einzelnen Kapiteln oder Seiten und nur zum eigenen wissenschaftlichen Gebrauch erlaubt. Die Weitergabe an Dritte sowie systematisches Downloaden sind untersagt. k3o 02-01-17 69 01 0009 1257218883 OLR-SEB-ZDB-2-EES Vervielfältigungen (z.B. Kopien, Downloads) sind nur von einzelnen Kapiteln oder Seiten und nur zum eigenen wissenschaftlichen Gebrauch erlaubt. Keine Weitergabe an Dritte. Kein systematisches Downloaden durch Robots. z 26-07-11 110 01 3110 430502604X 00 --%%-- --%%-- s --%%-- OLR-SEB Vervielfältigungen (z.B. Kopien, Downloads) sind nur von einzelnen Kapiteln oder Seiten und nur zum eigenen wissenschaftlichen Gebrauch erlaubt. Keine Weitergabe an Dritte. Kein systematisches Downloaden durch Robots. z 07-04-23 120 01 0715 1840114584 OLR-ESP Campusweiter Zugriff (Universität Oldenburg). - Vervielfältigungen (z.B. Kopien, Downloads) sind nur von einzelnen Kapiteln oder Seiten und nur zum eigenen wissenschaftlichen Gebrauch erlaubt. Keine Weitergabe an Dritte. Kein systematisches Downloaden. z 13-01-19 120 02 0715 3577164786 00 --%%-- --%%-- g --%%-- alma z 20-01-20 285 01 0517 1257282514 00 --%%-- --%%-- s --%%-- OLR-ESP-EES Vervielfältigungen (z.B. Kopien, Downloads) sind nur von einzelnen Kapiteln oder Seiten und nur zum eigenen wissenschaftlichen Gebrauch erlaubt. Keine Weitergabe an Dritte. Kein systematisches Downloaden durch Robots. z 26-07-11 370 01 4370 1257150286 olr-springer Vervielfältigungen (z.B. Kopien, Downloads) sind nur von einzelnen Kapiteln oder Seiten und nur zum eigenen wissenschaftlichen Gebrauch erlaubt. Keine Weitergabe an Dritte. Kein systematisches Downloaden durch Robots. i z 26-07-11 2027 01 DE-105 3340379459 00 --%%-- --%%-- n --%%-- Campuslizenz l01 17-05-11 2050 01 DE-Zi4 3340379467 00 --%%-- --%%-- n --%%-- Elektronischer Volltext - Campuslizenz l01 17-05-11 2061 01 DE-520 3340379475 00 --%%-- --%%-- n --%%-- eBook, Link nur im Campusbereich nutzbar l01 17-05-11 2148 01 DE-950 3340379491 00 --%%-- eBook Springer --%%-- n Elektronischer Volltext - Campuslizenz l01 10-06-11 22 01 0018 Volltextzugang Campus https://doi.org/10.1007/978-90-481-8885-7 22 01 0018 Nur für Angehörige der Universität Hamburg: Volltextzugang von außerhalb des Campus http://emedien.sub.uni-hamburg.de/han/SpringerEbooks/doi.org/10.1007/978-90-481-8885-7 60 01 0705 Volltextzugang Campus https://doi.org/10.1007/978-90-481-8885-7 62 01 0028 https://doi.org/10.1007/978-90-481-8885-7 65 01 0003 Volltextzugang Campus https://doi.org/10.1007/978-90-481-8885-7 69 01 0009 https://doi.org/10.1007/978-90-481-8885-7 110 01 3110 https://doi.org/10.1007/978-90-481-8885-7 120 01 0715 http://dx.doi.org/10.1007/978-90-481-8885-7 120 02 0715 http://49gbv-uob-primo.hosted.exlibrisgroup.com/openurl/49GBV_UOB/UOB_services_page?u.ignore_date_coverage=true&rft.mms_id=991016137662403501 285 01 0517 E-books (Springer) https://doi.org/10.1007/978-90-481-8885-7 370 01 4370 E-Book: Zugriff im HCU-Netz. 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9789048188857 978-90-481-8885-7 10.1007/978-90-481-8885-7 doi (DE-627)1650945701 (DE-576)345803701 (DE-599)BSZ345803701 (OCoLC)740949297 (OCoLC)740949297 (DE-He213)978-90-481-8885-7 DE-627 ger DE-627 rakwb eng XA-NL QE1-996.5 QE79 RBG bicssc SCI031000 bisacsh TP 6920 SEPA rvk (DE-625)rvk/144668: Ogawa, Yujiro verfasserin aut Accretionary Prisms and Convergent Margin Tectonics in the Northwest Pacific Basin edited by Yujiro Ogawa, Ryo Anma, Yildirim Dilek Dordrecht Springer Science+Business Media B.V 2011 Online-Ressource (XX, 277p. 123 illus., 69 illus. in color, digital) Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Modern Approaches in Solid Earth Sciences 8 SpringerLink Bücher Includes bibliographical references and index Accretionary Prisms and Convergent Margin Tectonics in the Northwest Pacific Basin; Preface; Acknowledgements; Contents; Contributors; Bending-Related Topographic Structures of the Subducting Plate in the Northwestern Pacific Ocean; 1 Introduction; 2 Data and Methods; 2.1 Bathymetric Data; 2.2 Geomagnetic Data; 3 Results; 3.1 Overview of the Bathymetric Features; 3.2 Topographic Expression of the Trenches; 3.3 Bending-Related Structures of the Oceanward Trench Slopes; 3.3.1 Kuril Trench; 3.3.2 Japan Trench; 3.3.3 Izu-Ogasawara Trench; 3.4 Magnetic Anomalies; 4 Discussion 4.1 Strike of Bending-Related Topographic Structures4.2 Topographic Expression of Bending-Related Structures; 5 Conclusions; References; Erosional Subduction Zonein the Northern Japan Trench: Review of Submersible Dive Reports; 1 Introduction; 2 Oceanward Slope Topography and Geology off Miyako; 3 Landward Slope Topography and Geology off Miyako; 4 Lineaments of the Oceanward and Landward Slopes off Miyako; 5 Conclusions; References; Boso TTT-Type Triple Junction: Formation of Miocene to Quaternary Accretionary Prisms and Present-Day Gravitational Collapse; 1 Introduction 2 Review of Sedimentation, Topography, and Plate Configuration2.1 Sedimentation; 2.2 Topographic Development of the Area from the Eastern Margin of the Sagami Trough to the Boso Triple Junction; 2.3 Katsuura Basin and Mogi Submarine Fan in the Bando Deepsea Basin; 2.4 Review of 3D Structure Based on Multichannel Seismic Profiles and Multibeam Echosounder Data; 2.5 Relationship Between the Tectonic and Age Data; 3 Diatom Analysis; 3.1 Materials, Method, and Results; 3.2 Diatom Biostratigraphy; 3.2.1 Pleistocene to Holocene Samples; 3.2.2 Middle Miocene Sample; 3.3 Summary of Age of Samples 3.4 Correlation to the Marine Rocks of the Izu Forearc4 Tectonic Synthesis: Summary and Conclusion; References; Rifting Structure of Central Izu-Ogasawara (Bonin) Arc Crust: Results of Seismic Crustal Imaging; 1 Introduction; 2 Data Acquisition; 3 Data and Modeling Procedure; 4 Description of Velocity Images; 4.1 Line IBr9; 4.2 Line IBr10; 5 Discussion; 5.1 Structural Commonalities and Differences; 5.2 Origin of the Arc Crust; 5.3 History of the Rifted Crust; 5.4 Reason for the Thin Crust in the Central Izu-Ogasawara Arc; 6 Conclusion; References Seafloor Geology of the Basement Serpentinite Body in the Ohmachi Seamount (Izu-Bonin Arc) as Exhumed Parts of a Subduction Zone Within the Philippine Sea1 Introduction; 2 Geologic Setting and Bathymetry; 3 Lithology; 3.1 Serpentinites; 3.1.1 Massive Serpentinite; 3.1.2 Schistose Serpentinite; 3.2 Amphibole Schist; 3.3 Paleogene Volcanic Rocks; 3.4 Miocene Turbidite; 3.5 Soft Mud Beds; 4 Dive and Dredge Results; 4.1 Dive 6K#341; 4.2 Dive 6K#570; 4.3 Dive 6K#571; 4.4 Dive 6K#575; 4.5 Dive 6K#608; 4.6 Dive 6K#609; 4.7 Dive 6K#610; 4.8 Dive 6K#1064; 4.9 Dive 6K#1065; 4.10 Dive 6K#1066 4.11 Dive 6K#1067 Accretionary prisms in convergent margins are natural laboratories for exploring initial orogenic processes and mountain building episodes. They are also an important component of continental growth both vertically and laterally. Accretionary prisms are seismically highly active and their internal deformation via megathrusting and out-of-sequence faulting are a big concern for earthquake and tsunami damage in many coastal cities around the Pacific Rim. The geometries and structures of modern accretionary prisms have been well imaged seismically and through deep drilling projects of the Ocean Drilling Program (and recently IODP) during the last 15 years. Better understanding of the spatial distribution and temporal progression of accretionary prism deformation, structural and hydrologic evolution of the décollement zone (tectonic interface between the subducting slab and the upper plate), chemical gradients and fluid flow paths within accretionary prisms, contrasting stratigraphic and deformational framework along-strike in accretionary prisms, and the distribution and ecosystems of biological communities in accretionary prism settings is most important in interpreting the evolution of ancient complex sedimentary terrains and orogenic belts in terms of subduction-related processes. This book is a collection of interdisciplinary papers documenting the geological, geophysical, geochemical, and paleontological features of modern accretionay prisms and trenches in the northwestern Pacific Ocean, based on many submersible dive cruises, ODP drilling projects, and geophysical surveys during the last 10 years. It also includes several papers presenting the results of systematic integrated studies of recent to ancient on-land accretionary prisms in comparison to modern analogues. The individual chapters are data and image rich, providing a major resource of information and knowledge from these critical components of convergent margins for researchers, faculty members, and graduate and undergraduate students. As such, the book will be a major and unique contribution in the broad fields of global tectonics, geodynamics, marine geology and geophysics, and structural geology and sedimentology. Geography Geology Geology, Structural Physical geography Oceanography Sedimentology Earth Sciences Geography Geology Geology, Structural Physical geography Oceanography Sedimentology Aufsatzsammlung (DE-588)4143413-4 (DE-627)105605727 (DE-576)209726091 gnd-content g (DE-588)4028495-5 (DE-627)104585102 (DE-576)208977503 Japan gnd s (DE-588)4129066-5 (DE-627)105712590 (DE-576)209607432 Meeresboden gnd s (DE-588)4038316-7 (DE-627)106232916 (DE-576)209029463 Meeresgeologie gnd s (DE-588)4401814-9 (DE-627)19331813X (DE-576)21206777X Ozeanische Erdkruste gnd s (DE-588)4020740-7 (DE-627)106316915 (DE-576)208934626 Gesteinskunde gnd (DE-627) g (DE-588)4255480-9 (DE-627)104706228 (DE-576)210547766 Pazifischer Ozean Nordwest gnd s (DE-588)4418304-5 (DE-627)213357410 (DE-576)212237373 Akkretionskeil gnd s (DE-588)4507349-1 (DE-627)246123729 (DE-576)213144794 Akkretion Geologie gnd s (DE-588)4619283-9 (DE-627)326427570 (DE-576)214330656 Rifting gnd s (DE-588)4183899-3 (DE-627)105299286 (DE-576)210021926 Subduktion gnd s (DE-588)4020227-6 (DE-627)106318810 (DE-576)20893247X Geologie gnd (DE-627) Anma, Ryo oth Dilek, Yildirim oth 9789048188840 Buchausg. u.d.T. Accretionary prisms and convergent margin tectonics in the Northwest Pacific basin 1. ed. Dordrecht : Springer, 2011 XX, 277 S. 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| title_short |
Accretionary Prisms and Convergent Margin Tectonics in the Northwest Pacific Basin |
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Beiträge <Formschlagwort> Einzelbeiträge Sammelwerk <Formschlagwort> Aufsatzsammlung Nippon (Staat) Empire du Japon Japon Nihon Dainippon Japão Nihon (Staat) Nippon Dainihon Zenkoku Nihon-koku Zen-Nihon Yapan Japan Meeresgrund Meeresboden Submarine Geologie Meeresboden / Geologie Meeresgeologie Meer / Erdkruste Ozeanische Kruste Ozeanische Erdkruste Gesteinsbeschreibung Petrografie Petrographie Petrologie Gesteinskunde Nordwestpazifik Pazifischer Ozean (Nordwest) Akkretionskeil Akkretion <Geologie> Grabenbildung Rifting Subduktionszone Subduktion Allgemeine Geologie Dynamische Geologie Geognosie Geologie |
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Beiträge <Formschlagwort> Einzelbeiträge Sammelwerk <Formschlagwort> Aufsatzsammlung Nippon (Staat) Empire du Japon Japon Nihon Dainippon Japão Nihon (Staat) Nippon Dainihon Zenkoku Nihon-koku Zen-Nihon Yapan Japan Meeresgrund Meeresboden Submarine Geologie Meeresboden / Geologie Meeresgeologie Meer / Erdkruste Ozeanische Kruste Ozeanische Erdkruste Gesteinsbeschreibung Petrografie Petrographie Petrologie Gesteinskunde Nordwestpazifik Pazifischer Ozean (Nordwest) Akkretionskeil Akkretion <Geologie> Grabenbildung Rifting Subduktionszone Subduktion Allgemeine Geologie Dynamische Geologie Geognosie Geologie |
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| doi_str |
10.1007/978-90-481-8885-7 |
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QE1-996.5 |
| up_date |
2024-07-15T21:52:58.905Z |
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Preface; Acknowledgements; Contents; Contributors; Bending-Related Topographic Structures of the Subducting Plate in the Northwestern Pacific Ocean; 1 Introduction; 2 Data and Methods; 2.1 Bathymetric Data; 2.2 Geomagnetic Data; 3 Results; 3.1 Overview of the Bathymetric Features; 3.2 Topographic Expression of the Trenches; 3.3 Bending-Related Structures of the Oceanward Trench Slopes; 3.3.1 Kuril Trench; 3.3.2 Japan Trench; 3.3.3 Izu-Ogasawara Trench; 3.4 Magnetic Anomalies; 4 Discussion</subfield></datafield><datafield tag="505" ind1="8" ind2="0"><subfield code="a">4.1 Strike of Bending-Related Topographic Structures4.2 Topographic Expression of Bending-Related Structures; 5 Conclusions; References; Erosional Subduction Zonein the Northern Japan Trench: Review of Submersible Dive Reports; 1 Introduction; 2 Oceanward Slope Topography and Geology off Miyako; 3 Landward Slope Topography and Geology off Miyako; 4 Lineaments of the Oceanward and Landward Slopes off Miyako; 5 Conclusions; 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4.4 Dive 6K#575; 4.5 Dive 6K#608; 4.6 Dive 6K#609; 4.7 Dive 6K#610; 4.8 Dive 6K#1064; 4.9 Dive 6K#1065; 4.10 Dive 6K#1066</subfield></datafield><datafield tag="505" ind1="8" ind2="0"><subfield code="a">4.11 Dive 6K#1067</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Accretionary prisms in convergent margins are natural laboratories for exploring initial orogenic processes and mountain building episodes. They are also an important component of continental growth both vertically and laterally. Accretionary prisms are seismically highly active and their internal deformation via megathrusting and out-of-sequence faulting are a big concern for earthquake and tsunami damage in many coastal cities around the Pacific Rim. The geometries and structures of modern accretionary prisms have been well imaged seismically and through deep drilling projects of the Ocean Drilling Program (and recently IODP) during the last 15 years. Better understanding of the spatial distribution and temporal progression of accretionary prism deformation, structural and hydrologic evolution of the décollement zone (tectonic interface between the subducting slab and the upper plate), chemical gradients and fluid flow paths within accretionary prisms, contrasting stratigraphic and deformational framework along-strike in accretionary prisms, and the distribution and ecosystems of biological communities in accretionary prism settings is most important in interpreting the evolution of ancient complex sedimentary terrains and orogenic belts in terms of subduction-related processes. This book is a collection of interdisciplinary papers documenting the geological, geophysical, geochemical, and paleontological features of modern accretionay prisms and trenches in the northwestern Pacific Ocean, based on many submersible dive cruises, ODP drilling projects, and geophysical surveys during the last 10 years. 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Die Weitergabe an Dritte sowie systematisches Downloaden sind untersagt.</subfield><subfield code="y">z</subfield><subfield code="z">26-07-11</subfield></datafield><datafield tag="980" ind1=" " ind2=" "><subfield code="2">65</subfield><subfield code="1">01</subfield><subfield code="x">0003</subfield><subfield code="b">1655665189</subfield><subfield code="c">03</subfield><subfield code="f">--%%--</subfield><subfield code="d">ebook</subfield><subfield code="e">--%%--</subfield><subfield code="j">--%%--</subfield><subfield code="h">OLR-SEB-ZDB-2-EES</subfield><subfield code="k">Vervielfältigungen (z.B. Kopien, Downloads) sind nur von einzelnen Kapiteln oder Seiten und nur zum eigenen wissenschaftlichen Gebrauch erlaubt. 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Bending-Related Topographic Structures of the Subducting Plate in the Northwestern Pacific Ocean … Erosional Subduction Zone in the Northern Japan Trench: Review of Submersible Dive Reports … Boso TTT-Type Triple Junction: Formation of Miocene to Quaternary Accretionary Prisms and Present-Day Gravitational Collapse … Rifting Structure of Central Izu-Ogasawara (Bonin) Arc Crust: Results of Seismic Crustal Imaging … Seafloor Geology of the Basement Serpentinite Body in the Ohmachi Seamount (Izu-Boninp. … Arc) as Exhumed Parts of a Subduction Zone Within the Philippine Sea Petrology and Mineralogy of Mantle Peridotites from the Southern Marianas … Tectonics of Unusual Crustal Accretion in the Parece Vela Basin … Structural Profile and Development of the Accretionary Complex in the Nankai Trough, Southwest Japan: Results of Submersible Studies … Submarine Outcrop Evidence for Transpressional Deformation Within the Nankai Accretionary Prism, Tenryu Canyon, Japan … Rapid Exhumation of Subducted Sediments Along an Out-of-Sequence Thrust in the Modern … Eastern Nankai Accretionary Prism Dark Bands in the Submarine Nankai Accretionary Prism - Comparisons with Miocene-Pliocene Onshore Examples from Boso Peninsula … Gas Chemistry of Pore Fluids from Oomine Ridge on the Nankai Accretionary Prism … Long-Term Stability of Acoustic Benchmarks Deployed on Thick Sediment for GPS/Acoustic Seafloor Positioning … Index … Contents Bending-Related Topographic Structures of the Subducting Plate in the Northwestern Pacific Ocean … Masao Nakanishi Erosional Subduction Zone in the Northern Japan Trench: Review of Submersible Dive Reports … Yujiro Ogawa Boso TTT-Type Triple Junction: Formation of Miocene to Quaternary Accretionary Prisms and Present-Day Gravitational Collapse … Yujiro Ogawa and Yukio Yanagisawa Rifting Structure of Central Izu-Ogasawara (Bonin) Arc Crust: Results of Seismic Crustal Imaging … Narumi Takahashi, Mikiya Yamashita, Shuichi Kodaira, Seiichi Miura, Takeshi Sato, Tetsuo No, Kaoru Takizawa, Yoshiyuki Tatsumi, and Yoshiyuki Kaneda Seafloor Geology of the Basement Serpentinite Body in the Ohmachi Seamount (Izu-Bonin Arc) as Exhumed Parts of a Subduction Zone Within the Philippine Sea … Hayato Ueda, Kiyoaki Niida, Tadashi Usuki, Ken-ich Hirauchi, Martin Meschede, Ryo Miura, Yujiro Ogawa, Makoto Yuasa, Izumi Sakamoto, Tae Chiba, Takahiro Izumino, Yoshiyuki Kuramoto, Toyoto Azuma, Toru Takeshita, Takeshi Imayama, Yuki Miyajima, and Takahiro Saito Petrology and Mineralogy of Mantle Peridotites from the Southern Marianas … Hiroshi Sato and Teruaki Ishii XI xii Contents Tectonics of Unusual Crustal Accretion in the Parece Vela Basin … Yasuhiko Ohara, Kyoko Okino, and Jonathan E. Snow Structural Profile and Development of the Accretionary Complex in the Nankai Trough, Southwest Japan: Results of Submersible Studies … Ryo Anma, Yujiro Ogawa, Gregory F. Moore, Kiichiro Kawamura, Tomoyuki Sasaki, Shunsuke Kawakami, Yildirim Dilek, Yoko Michiguchi, Ryota Endo, Shunji Akaiwa, Satoro Hirano Submarine Outcrop Evidence for Transpressional Deformation Within the Nankai Accretionary Prism, Tenryu Canyon, Japan … Nicholas W. Hayman, Kurds C. Burmeister, Kiichiro Kawamura, Ryo Anma, and Yasuhiro Yamada Rapid Exhumation of Subducted Sediments Along an Out-of-Sequence Thrust in the Modern Eastern Nankai Accretionary Prism … Kiichiro Kawamura, Yujiro Ogawa, Hidetoshi Hara, Ryo Anma, Yildirim Dilek, Shunsuke Kawakami, Shun Chiyonobu, Hideki Mukoyoshi, Satoshi Hirano, and Isao Motoyama Dark Bands in the Submarine Nankai Accretionary Prism - Comparisons with Miocene-Pliocene Onshore Examples from Boso Peninsula … Yoko Michiguchi and Yujiro Ogawa Gas Chemistry of Pore Fluids from Oomine Ridge on the Nankai Accretionary Prism … Tomohiro Toki, Kenji Maegawa, Urumu Tsunogai, Shinsuke Kawagucci, Naoto Takahata, Yuji Sano, Juichiro Ashi, Masataka Kinoshita, and Toshitaka Gamo Long-Term Stability of Acoustic Benchmarks Deployed on Thick Sediment for GPS/Acoustic Seafloor Positioning … Hiromi Fujimoto, Motoyuki Kido, Yukihito Osada, Keiichi Tadokoro, Takashi Okuda, Yoshihiro Matsumoto, and Kozue Kurihara Index … |
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4.4 Dive 6K#575; 4.5 Dive 6K#608; 4.6 Dive 6K#609; 4.7 Dive 6K#610; 4.8 Dive 6K#1064; 4.9 Dive 6K#1065; 4.10 Dive 6K#1066</subfield></datafield><datafield tag="505" ind1="8" ind2="0"><subfield code="a">4.11 Dive 6K#1067</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Accretionary prisms in convergent margins are natural laboratories for exploring initial orogenic processes and mountain building episodes. 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Better understanding of the spatial distribution and temporal progression of accretionary prism deformation, structural and hydrologic evolution of the décollement zone (tectonic interface between the subducting slab and the upper plate), chemical gradients and fluid flow paths within accretionary prisms, contrasting stratigraphic and deformational framework along-strike in accretionary prisms, and the distribution and ecosystems of biological communities in accretionary prism settings is most important in interpreting the evolution of ancient complex sedimentary terrains and orogenic belts in terms of subduction-related processes. This book is a collection of interdisciplinary papers documenting the geological, geophysical, geochemical, and paleontological features of modern accretionay prisms and trenches in the northwestern Pacific Ocean, based on many submersible dive cruises, ODP drilling projects, and geophysical surveys during the last 10 years. 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GUS)</subfield><subfield code="k">Ostasien</subfield><subfield code="k">Japan</subfield><subfield code="0">(DE-627)1271946629</subfield><subfield code="0">(DE-625)rvk/144668:</subfield><subfield code="0">(DE-576)201946629</subfield></datafield><datafield tag="951" ind1=" " ind2=" "><subfield code="a">BO</subfield></datafield><datafield tag="953" ind1=" " ind2=" "><subfield code="2">045F</subfield><subfield code="a">551</subfield></datafield><datafield tag="953" ind1=" " ind2=" "><subfield code="2">045F</subfield><subfield code="a">551.1</subfield></datafield><datafield tag="980" ind1=" " ind2=" "><subfield code="2">22</subfield><subfield code="1">01</subfield><subfield code="x">0018</subfield><subfield code="b">1266756787</subfield><subfield code="c">00</subfield><subfield code="f">--%%--</subfield><subfield code="d">--%%--</subfield><subfield code="e">s</subfield><subfield code="j">--%%--</subfield><subfield code="h">h57-ees</subfield><subfield code="k">Vervielfältigungen (z.B. 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Kein systematisches Downloaden durch Robots.</subfield><subfield code="k">Nur für Angehörige der HSU: Volltextzugang von außerhalb des Campus mit Anmeldung über Shibboleth mit Ihrer Bibliothekskennung</subfield><subfield code="y">z</subfield><subfield code="z">07-04-23</subfield></datafield><datafield tag="980" ind1=" " ind2=" "><subfield code="2">62</subfield><subfield code="1">01</subfield><subfield code="x">0028</subfield><subfield code="b">1257290495</subfield><subfield code="h">OLR-SEB</subfield><subfield code="k">Vervielfältigungen (z.B. Kopien, Downloads) sind nur von einzelnen Kapiteln oder Seiten und nur zum eigenen wissenschaftlichen Gebrauch erlaubt. Die Weitergabe an Dritte sowie systematisches Downloaden sind untersagt.</subfield><subfield code="y">z</subfield><subfield code="z">26-07-11</subfield></datafield><datafield tag="980" ind1=" " ind2=" "><subfield code="2">65</subfield><subfield code="1">01</subfield><subfield code="x">0003</subfield><subfield code="b">1655665189</subfield><subfield code="c">03</subfield><subfield code="f">--%%--</subfield><subfield code="d">ebook</subfield><subfield code="e">--%%--</subfield><subfield code="j">--%%--</subfield><subfield code="h">OLR-SEB-ZDB-2-EES</subfield><subfield code="k">Vervielfältigungen (z.B. Kopien, Downloads) sind nur von einzelnen Kapiteln oder Seiten und nur zum eigenen wissenschaftlichen Gebrauch erlaubt. Die Weitergabe an Dritte sowie systematisches Downloaden sind untersagt.</subfield><subfield code="y">k3o</subfield><subfield code="z">02-01-17</subfield></datafield><datafield tag="980" ind1=" " ind2=" "><subfield code="2">69</subfield><subfield code="1">01</subfield><subfield code="x">0009</subfield><subfield code="b">1257218883</subfield><subfield code="h">OLR-SEB-ZDB-2-EES</subfield><subfield code="k">Vervielfältigungen (z.B. Kopien, Downloads) sind nur von einzelnen Kapiteln oder Seiten und nur zum eigenen wissenschaftlichen Gebrauch erlaubt. Keine Weitergabe an Dritte. Kein systematisches Downloaden durch Robots.</subfield><subfield code="y">z</subfield><subfield code="z">26-07-11</subfield></datafield><datafield tag="980" ind1=" " ind2=" "><subfield code="2">110</subfield><subfield code="1">01</subfield><subfield code="x">3110</subfield><subfield code="b">430502604X</subfield><subfield code="c">00</subfield><subfield code="f">--%%--</subfield><subfield code="d">--%%--</subfield><subfield code="e">s</subfield><subfield code="j">--%%--</subfield><subfield code="h">OLR-SEB</subfield><subfield code="k">Vervielfältigungen (z.B. Kopien, Downloads) sind nur von einzelnen Kapiteln oder Seiten und nur zum eigenen wissenschaftlichen Gebrauch erlaubt. Keine Weitergabe an Dritte. Kein systematisches Downloaden durch Robots.</subfield><subfield code="y">z</subfield><subfield code="z">07-04-23</subfield></datafield><datafield tag="980" ind1=" " ind2=" "><subfield code="2">120</subfield><subfield code="1">01</subfield><subfield code="x">0715</subfield><subfield code="b">1840114584</subfield><subfield code="h">OLR-ESP</subfield><subfield code="k">Campusweiter Zugriff (Universität Oldenburg). - Vervielfältigungen (z.B. Kopien, Downloads) sind nur von einzelnen Kapiteln oder Seiten und nur zum eigenen wissenschaftlichen Gebrauch erlaubt. Keine Weitergabe an Dritte. 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