The Manihiki Plateau : Magmatic and tectonic evolution of a Large Igneous Province through time
Large Igneous Province, Manihiki Plateau, seismic reflection data, Pacific Plate.
Autor*in: |
Pietsch, Ricarda [verfasserIn] |
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Körperschaften: |
Universität Bremen [Grad-verleihende Institution] |
Hochschulschrift: |
Dissertation ; Universität Bremen ; 2016 |
Format: |
E-Book |
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Sprache: |
Englisch |
Erschienen: |
Bremen: 2015 |
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Formangabe: |
Hochschulschrift |
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Umfang: |
1 Online-Ressource (xi, 125 Seiten) ; Illustrationen |
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Weitere Ausgabe: |
Erscheint auch als Druck-Ausgabe Pietsch, Ricarda: The Manihiki Plateau - Bremen, 2015 |
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Links: |
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DOI / URN: |
urn:nbn:de:gbv:46-00105277-18 |
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Katalog-ID: |
862891833 |
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520 | |a The Pacific Plate is highly engraved by volcanism that has formed oceanic plateaus and hotspot chains. The Manihiki Plateau (MP) is a large igneous province (LIP) located in the central Pacific that has an areal extent of 600000 km2. In 2006, Taylor proposed a joint emplacement of the MP with the Ontong Java Plateau, the Hikurangi Plateau and two missing fragments during the Cretaceous in a "Super-LIP" called Ontong Java Nui (OJN). The emplacement of OJN with an aerial extent of 1.1% of the earth's surface would have had major impacts on Earth's climate. An investigation of the initital volcanic emplacement history of the Manihiki Plateau and its break-up processes can contribute to a better understanding of LIP-impact on the paleo-climate. Analysis and interpretation of a new, high-resolution multi-channel seismic reflection dataset has provided a detailed and improved volcanic history of the Manihiki Plateau. The new model consists of three volcanic phases instead of the previously assumed two volcanic phases. It includes the initial formation phase (>125 Ma) that formed a spatially localized nucleus, which was extended to the East. The expansion phase (125-116 Ma) erupted massive tholeiitic basalts and break-up processes into the other LIP-fragments occurred. The third phase is a phase of secondary volcanism that leveled out the overall topography and was intense at the tectonically altered margins. Since the late Cretaceous/early Cenozoic, the morphology of the Manihiki Plateau was engraved by tectonic and volcanic features that were strongly related to the kinematics of the Pacific Plate. During the Pleistocene, a major Pacific plate-reorganization occurred that caused changes of inner-lithospheric stress fields. In this study, the origin of the Suvarov Trough has been investigated. Age and spatial extension point towards a cause that is in a good correlation to this major Pleistocene event. Strain within a LIP crust due to applied stress field changes appears to be similar to continental crust and different to the surrounding oceanic crust. During the Cenozoic, the seafloor morphology in the central Pacific is dominated by the formation of age-progressive hotspot seamount chains. Neogene igneous diapirs in the southwestern MP have been investigated within this study. Age and location characteristics support a hotspot origin, which might be related to the Society Islands Hotspot. The characteristic appearance of the diapirs is different to hotspot volcanism within oceanic lithosphere, which can probably be related to the anomalous thick crust of the Manihiki Plateau. The magmatic and tectonic history of the Manihiki Plateau reveals that this LIP acts similar to continental crust on applied external forces, although its chemical composition resembles thick oceanic crust. | ||
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In 2006, Taylor proposed a joint emplacement of the MP with the Ontong Java Plateau, the Hikurangi Plateau and two missing fragments during the Cretaceous in a "Super-LIP" called Ontong Java Nui (OJN). The emplacement of OJN with an aerial extent of 1.1% of the earth's surface would have had major impacts on Earth's climate. An investigation of the initital volcanic emplacement history of the Manihiki Plateau and its break-up processes can contribute to a better understanding of LIP-impact on the paleo-climate. Analysis and interpretation of a new, high-resolution multi-channel seismic reflection dataset has provided a detailed and improved volcanic history of the Manihiki Plateau. The new model consists of three volcanic phases instead of the previously assumed two volcanic phases. It includes the initial formation phase (>125 Ma) that formed a spatially localized nucleus, which was extended to the East. The expansion phase (125-116 Ma) erupted massive tholeiitic basalts and break-up processes into the other LIP-fragments occurred. The third phase is a phase of secondary volcanism that leveled out the overall topography and was intense at the tectonically altered margins. Since the late Cretaceous/early Cenozoic, the morphology of the Manihiki Plateau was engraved by tectonic and volcanic features that were strongly related to the kinematics of the Pacific Plate. During the Pleistocene, a major Pacific plate-reorganization occurred that caused changes of inner-lithospheric stress fields. In this study, the origin of the Suvarov Trough has been investigated. Age and spatial extension point towards a cause that is in a good correlation to this major Pleistocene event. Strain within a LIP crust due to applied stress field changes appears to be similar to continental crust and different to the surrounding oceanic crust. During the Cenozoic, the seafloor morphology in the central Pacific is dominated by the formation of age-progressive hotspot seamount chains. Neogene igneous diapirs in the southwestern MP have been investigated within this study. Age and location characteristics support a hotspot origin, which might be related to the Society Islands Hotspot. The characteristic appearance of the diapirs is different to hotspot volcanism within oceanic lithosphere, which can probably be related to the anomalous thick crust of the Manihiki Plateau. The magmatic and tectonic history of the Manihiki Plateau reveals that this LIP acts similar to continental crust on applied external forces, although its chemical composition resembles thick oceanic crust. 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16,O08 dnb 1106374568 DE-101 urn:nbn:de:gbv:46-00105277-18 urn (DE-627)862891833 (DE-576)9862891831 (DE-599)GBV862891833 (OCoLC)953396126 DE-627 ger DE-627 rda eng XA-DE 550 DE-101 Pietsch, Ricarda verfasserin aut The Manihiki Plateau Magmatic and tectonic evolution of a Large Igneous Province through time vorgelegt von Ricarda Pietsch Bremen 2015 1 Online-Ressource (xi, 125 Seiten) Illustrationen Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Dissertation Universität Bremen 2016 Large Igneous Province, Manihiki Plateau, seismic reflection data, Pacific Plate. The Pacific Plate is highly engraved by volcanism that has formed oceanic plateaus and hotspot chains. The Manihiki Plateau (MP) is a large igneous province (LIP) located in the central Pacific that has an areal extent of 600000 km2. In 2006, Taylor proposed a joint emplacement of the MP with the Ontong Java Plateau, the Hikurangi Plateau and two missing fragments during the Cretaceous in a "Super-LIP" called Ontong Java Nui (OJN). The emplacement of OJN with an aerial extent of 1.1% of the earth's surface would have had major impacts on Earth's climate. An investigation of the initital volcanic emplacement history of the Manihiki Plateau and its break-up processes can contribute to a better understanding of LIP-impact on the paleo-climate. Analysis and interpretation of a new, high-resolution multi-channel seismic reflection dataset has provided a detailed and improved volcanic history of the Manihiki Plateau. The new model consists of three volcanic phases instead of the previously assumed two volcanic phases. It includes the initial formation phase (>125 Ma) that formed a spatially localized nucleus, which was extended to the East. The expansion phase (125-116 Ma) erupted massive tholeiitic basalts and break-up processes into the other LIP-fragments occurred. The third phase is a phase of secondary volcanism that leveled out the overall topography and was intense at the tectonically altered margins. Since the late Cretaceous/early Cenozoic, the morphology of the Manihiki Plateau was engraved by tectonic and volcanic features that were strongly related to the kinematics of the Pacific Plate. During the Pleistocene, a major Pacific plate-reorganization occurred that caused changes of inner-lithospheric stress fields. In this study, the origin of the Suvarov Trough has been investigated. Age and spatial extension point towards a cause that is in a good correlation to this major Pleistocene event. Strain within a LIP crust due to applied stress field changes appears to be similar to continental crust and different to the surrounding oceanic crust. During the Cenozoic, the seafloor morphology in the central Pacific is dominated by the formation of age-progressive hotspot seamount chains. Neogene igneous diapirs in the southwestern MP have been investigated within this study. Age and location characteristics support a hotspot origin, which might be related to the Society Islands Hotspot. The characteristic appearance of the diapirs is different to hotspot volcanism within oceanic lithosphere, which can probably be related to the anomalous thick crust of the Manihiki Plateau. The magmatic and tectonic history of the Manihiki Plateau reveals that this LIP acts similar to continental crust on applied external forces, although its chemical composition resembles thick oceanic crust. Langzeitarchivierung gewährleistet pdager Hochschulschrift (DE-588)4113937-9 (DE-627)105825778 (DE-576)209480580 gnd-content Universität Bremen Grad-verleihende Institution (DE-588)2001386-3 (DE-627)101380429 (DE-576)191575038 dgg Bremen (DE-588)4008135-7 (DE-627)106369636 (DE-576)208874569 uvp Erscheint auch als Druck-Ausgabe Pietsch, Ricarda The Manihiki Plateau Bremen, 2015 xi, 125 Seiten (DE-627)862891736 http://nbn-resolving.de/urn:nbn:de:gbv:46-00105277-18 Resolving-System kostenfrei Volltext http://nbn-resolving.de/urn:nbn:de:gbv:46-00105277-18 2016-08-03 Resolving-System Volltext http://d-nb.info/1106374568/34 2016-08-03 Langzeitarchivierung Nationalbibliothek Volltext http://elib.suub.uni-bremen.de/edocs/00105277-1.pdf 2016-08-03 Verlag kostenfrei Volltext GBV-ODiss GBV_ILN_20 ISIL_DE-84 SYSFLAG_1 GBV_KXP SSG-OPC-GGO GBV_ILN_21 ISIL_DE-46 GBV_ILN_22 ISIL_DE-18 GBV_ILN_23 ISIL_DE-830 GBV_ILN_30 ISIL_DE-104 GBV_ILN_40 ISIL_DE-7 GBV_ILN_60 ISIL_DE-705 GBV_ILN_63 ISIL_DE-Wim2 GBV_ILN_65 ISIL_DE-3 GBV_ILN_70 ISIL_DE-89 GBV_ILN_105 ISIL_DE-841 GBV_ILN_110 ISIL_DE-Luen4 GBV_ILN_132 ISIL_DE-959 GBV_ILN_151 ISIL_DE-546 GBV_ILN_161 ISIL_DE-960 GBV_ILN_293 ISIL_DE-960-3 GBV_ILN_370 ISIL_DE-1373 GBV_ILN_381 ISIL_DE-Ki130 GBV_ILN_2403 ISIL_DE-LFER BO 20 01 0084 1645563472 x 11-11-16 21 01 0046 1624969992 ebook_2016_dissbremen Kostenloser Zugriff zza 11-07-16 22 01 0018 1648893147 SUBolrd xu 02-12-16 23 01 0830 1645707814 olr-d x 11-11-16 30 01 0104 1645757730 z 11-11-16 40 01 0007 1645811883 xsn 11-11-16 60 01 0705 164588709X OLRD z 11-11-16 63 01 3401 1645951871 ORD x 11-11-16 65 01 0003 4167729075 GBV-ODiss Open Access z 16-07-22 70 01 0089 1645993124 zdo 11-11-16 105 01 0841 1646380037 z 11-11-16 110 01 3110 1646043073 x 11-11-16 132 01 0959 1646102150 OLR-DISS x 11-11-16 151 01 0546 3583606698 OLR-ODISS z 31-01-20 161 01 0960 1646170539 ORD x 11-11-16 293 01 3293 1646316967 ORD xf 11-11-16 370 01 4370 1646356403 x 11-11-16 381 01 4381 1676004130 00 --%%-- --%%-- --%%-- --%%-- z 07-04-17 2403 01 DE-LFER 3475566001 00 --%%-- --%%-- n --%%-- l01 13-05-19 20 01 0084 http://nbn-resolving.de/urn:nbn:de:gbv:46-00105277-18 21 01 0046 http://nbn-resolving.de/urn:nbn:de:gbv:46-00105277-18 LF 22 01 0018 http://nbn-resolving.de/urn:nbn:de:gbv:46-00105277-18 23 01 0830 http://nbn-resolving.de/urn:nbn:de:gbv:46-00105277-18 30 01 0104 http://nbn-resolving.de/urn:nbn:de:gbv:46-00105277-18 40 01 0007 http://nbn-resolving.de/urn:nbn:de:gbv:46-00105277-18 60 01 0705 http://nbn-resolving.de/urn:nbn:de:gbv:46-00105277-18 63 01 3401 E-Book http://nbn-resolving.de/urn:nbn:de:gbv:46-00105277-18 LF 65 01 0003 http://nbn-resolving.de/urn:nbn:de:gbv:46-00105277-18 70 01 0089 http://nbn-resolving.de/urn:nbn:de:gbv:46-00105277-18 105 01 0841 http://nbn-resolving.de/urn:nbn:de:gbv:46-00105277-18 110 01 3110 http://nbn-resolving.de/urn:nbn:de:gbv:46-00105277-18 132 01 0959 http://nbn-resolving.de/urn:nbn:de:gbv:46-00105277-18 151 01 0546 Volltext http://nbn-resolving.de/urn:nbn:de:gbv:46-00105277-18 161 01 0960 http://nbn-resolving.de/urn:nbn:de:gbv:46-00105277-18 293 01 3293 http://nbn-resolving.de/urn:nbn:de:gbv:46-00105277-18 370 01 4370 http://nbn-resolving.de/urn:nbn:de:gbv:46-00105277-18 381 01 4381 http://elib.suub.uni-bremen.de/edocs/00105277-1.pdf 34 2403 01 DE-LFER http://nbn-resolving.de/urn:nbn:de:gbv:46-00105277-18 21 00 DE-46 00 Universität Bremen 21 00 DE-46 00 Fachbereich 05: Geowissenschaften (FB 05) 381 00 DE-Ki130 00 Annette-Barthelt-Preis 21 00 DE-46 99 07 60 01 0705 10 ho 20 01 0084 OLRD 110 01 3110 OLRD 370 01 4370 OLRD 21 01 0046 ebook_2016_dissbremen 22 01 0018 SUBolrd 23 01 0830 olr-d 60 01 0705 OLRD 63 01 3401 ORD 65 01 0003 GBV-ODiss 132 01 0959 OLR-DISS 151 01 0546 OLR-ODISS 161 01 0960 ORD 293 01 3293 ORD 23 01 0830 2016-11-11:17:52:41 |
allfields_unstemmed |
16,O08 dnb 1106374568 DE-101 urn:nbn:de:gbv:46-00105277-18 urn (DE-627)862891833 (DE-576)9862891831 (DE-599)GBV862891833 (OCoLC)953396126 DE-627 ger DE-627 rda eng XA-DE 550 DE-101 Pietsch, Ricarda verfasserin aut The Manihiki Plateau Magmatic and tectonic evolution of a Large Igneous Province through time vorgelegt von Ricarda Pietsch Bremen 2015 1 Online-Ressource (xi, 125 Seiten) Illustrationen Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Dissertation Universität Bremen 2016 Large Igneous Province, Manihiki Plateau, seismic reflection data, Pacific Plate. The Pacific Plate is highly engraved by volcanism that has formed oceanic plateaus and hotspot chains. The Manihiki Plateau (MP) is a large igneous province (LIP) located in the central Pacific that has an areal extent of 600000 km2. In 2006, Taylor proposed a joint emplacement of the MP with the Ontong Java Plateau, the Hikurangi Plateau and two missing fragments during the Cretaceous in a "Super-LIP" called Ontong Java Nui (OJN). The emplacement of OJN with an aerial extent of 1.1% of the earth's surface would have had major impacts on Earth's climate. An investigation of the initital volcanic emplacement history of the Manihiki Plateau and its break-up processes can contribute to a better understanding of LIP-impact on the paleo-climate. Analysis and interpretation of a new, high-resolution multi-channel seismic reflection dataset has provided a detailed and improved volcanic history of the Manihiki Plateau. The new model consists of three volcanic phases instead of the previously assumed two volcanic phases. It includes the initial formation phase (>125 Ma) that formed a spatially localized nucleus, which was extended to the East. The expansion phase (125-116 Ma) erupted massive tholeiitic basalts and break-up processes into the other LIP-fragments occurred. The third phase is a phase of secondary volcanism that leveled out the overall topography and was intense at the tectonically altered margins. Since the late Cretaceous/early Cenozoic, the morphology of the Manihiki Plateau was engraved by tectonic and volcanic features that were strongly related to the kinematics of the Pacific Plate. During the Pleistocene, a major Pacific plate-reorganization occurred that caused changes of inner-lithospheric stress fields. In this study, the origin of the Suvarov Trough has been investigated. Age and spatial extension point towards a cause that is in a good correlation to this major Pleistocene event. Strain within a LIP crust due to applied stress field changes appears to be similar to continental crust and different to the surrounding oceanic crust. During the Cenozoic, the seafloor morphology in the central Pacific is dominated by the formation of age-progressive hotspot seamount chains. Neogene igneous diapirs in the southwestern MP have been investigated within this study. Age and location characteristics support a hotspot origin, which might be related to the Society Islands Hotspot. The characteristic appearance of the diapirs is different to hotspot volcanism within oceanic lithosphere, which can probably be related to the anomalous thick crust of the Manihiki Plateau. The magmatic and tectonic history of the Manihiki Plateau reveals that this LIP acts similar to continental crust on applied external forces, although its chemical composition resembles thick oceanic crust. Langzeitarchivierung gewährleistet pdager Hochschulschrift (DE-588)4113937-9 (DE-627)105825778 (DE-576)209480580 gnd-content Universität Bremen Grad-verleihende Institution (DE-588)2001386-3 (DE-627)101380429 (DE-576)191575038 dgg Bremen (DE-588)4008135-7 (DE-627)106369636 (DE-576)208874569 uvp Erscheint auch als Druck-Ausgabe Pietsch, Ricarda The Manihiki Plateau Bremen, 2015 xi, 125 Seiten (DE-627)862891736 http://nbn-resolving.de/urn:nbn:de:gbv:46-00105277-18 Resolving-System kostenfrei Volltext http://nbn-resolving.de/urn:nbn:de:gbv:46-00105277-18 2016-08-03 Resolving-System Volltext http://d-nb.info/1106374568/34 2016-08-03 Langzeitarchivierung Nationalbibliothek Volltext http://elib.suub.uni-bremen.de/edocs/00105277-1.pdf 2016-08-03 Verlag kostenfrei Volltext GBV-ODiss GBV_ILN_20 ISIL_DE-84 SYSFLAG_1 GBV_KXP SSG-OPC-GGO GBV_ILN_21 ISIL_DE-46 GBV_ILN_22 ISIL_DE-18 GBV_ILN_23 ISIL_DE-830 GBV_ILN_30 ISIL_DE-104 GBV_ILN_40 ISIL_DE-7 GBV_ILN_60 ISIL_DE-705 GBV_ILN_63 ISIL_DE-Wim2 GBV_ILN_65 ISIL_DE-3 GBV_ILN_70 ISIL_DE-89 GBV_ILN_105 ISIL_DE-841 GBV_ILN_110 ISIL_DE-Luen4 GBV_ILN_132 ISIL_DE-959 GBV_ILN_151 ISIL_DE-546 GBV_ILN_161 ISIL_DE-960 GBV_ILN_293 ISIL_DE-960-3 GBV_ILN_370 ISIL_DE-1373 GBV_ILN_381 ISIL_DE-Ki130 GBV_ILN_2403 ISIL_DE-LFER BO 20 01 0084 1645563472 x 11-11-16 21 01 0046 1624969992 ebook_2016_dissbremen Kostenloser Zugriff zza 11-07-16 22 01 0018 1648893147 SUBolrd xu 02-12-16 23 01 0830 1645707814 olr-d x 11-11-16 30 01 0104 1645757730 z 11-11-16 40 01 0007 1645811883 xsn 11-11-16 60 01 0705 164588709X OLRD z 11-11-16 63 01 3401 1645951871 ORD x 11-11-16 65 01 0003 4167729075 GBV-ODiss Open Access z 16-07-22 70 01 0089 1645993124 zdo 11-11-16 105 01 0841 1646380037 z 11-11-16 110 01 3110 1646043073 x 11-11-16 132 01 0959 1646102150 OLR-DISS x 11-11-16 151 01 0546 3583606698 OLR-ODISS z 31-01-20 161 01 0960 1646170539 ORD x 11-11-16 293 01 3293 1646316967 ORD xf 11-11-16 370 01 4370 1646356403 x 11-11-16 381 01 4381 1676004130 00 --%%-- --%%-- --%%-- --%%-- z 07-04-17 2403 01 DE-LFER 3475566001 00 --%%-- --%%-- n --%%-- l01 13-05-19 20 01 0084 http://nbn-resolving.de/urn:nbn:de:gbv:46-00105277-18 21 01 0046 http://nbn-resolving.de/urn:nbn:de:gbv:46-00105277-18 LF 22 01 0018 http://nbn-resolving.de/urn:nbn:de:gbv:46-00105277-18 23 01 0830 http://nbn-resolving.de/urn:nbn:de:gbv:46-00105277-18 30 01 0104 http://nbn-resolving.de/urn:nbn:de:gbv:46-00105277-18 40 01 0007 http://nbn-resolving.de/urn:nbn:de:gbv:46-00105277-18 60 01 0705 http://nbn-resolving.de/urn:nbn:de:gbv:46-00105277-18 63 01 3401 E-Book http://nbn-resolving.de/urn:nbn:de:gbv:46-00105277-18 LF 65 01 0003 http://nbn-resolving.de/urn:nbn:de:gbv:46-00105277-18 70 01 0089 http://nbn-resolving.de/urn:nbn:de:gbv:46-00105277-18 105 01 0841 http://nbn-resolving.de/urn:nbn:de:gbv:46-00105277-18 110 01 3110 http://nbn-resolving.de/urn:nbn:de:gbv:46-00105277-18 132 01 0959 http://nbn-resolving.de/urn:nbn:de:gbv:46-00105277-18 151 01 0546 Volltext http://nbn-resolving.de/urn:nbn:de:gbv:46-00105277-18 161 01 0960 http://nbn-resolving.de/urn:nbn:de:gbv:46-00105277-18 293 01 3293 http://nbn-resolving.de/urn:nbn:de:gbv:46-00105277-18 370 01 4370 http://nbn-resolving.de/urn:nbn:de:gbv:46-00105277-18 381 01 4381 http://elib.suub.uni-bremen.de/edocs/00105277-1.pdf 34 2403 01 DE-LFER http://nbn-resolving.de/urn:nbn:de:gbv:46-00105277-18 21 00 DE-46 00 Universität Bremen 21 00 DE-46 00 Fachbereich 05: Geowissenschaften (FB 05) 381 00 DE-Ki130 00 Annette-Barthelt-Preis 21 00 DE-46 99 07 60 01 0705 10 ho 20 01 0084 OLRD 110 01 3110 OLRD 370 01 4370 OLRD 21 01 0046 ebook_2016_dissbremen 22 01 0018 SUBolrd 23 01 0830 olr-d 60 01 0705 OLRD 63 01 3401 ORD 65 01 0003 GBV-ODiss 132 01 0959 OLR-DISS 151 01 0546 OLR-ODISS 161 01 0960 ORD 293 01 3293 ORD 23 01 0830 2016-11-11:17:52:41 |
allfieldsGer |
16,O08 dnb 1106374568 DE-101 urn:nbn:de:gbv:46-00105277-18 urn (DE-627)862891833 (DE-576)9862891831 (DE-599)GBV862891833 (OCoLC)953396126 DE-627 ger DE-627 rda eng XA-DE 550 DE-101 Pietsch, Ricarda verfasserin aut The Manihiki Plateau Magmatic and tectonic evolution of a Large Igneous Province through time vorgelegt von Ricarda Pietsch Bremen 2015 1 Online-Ressource (xi, 125 Seiten) Illustrationen Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Dissertation Universität Bremen 2016 Large Igneous Province, Manihiki Plateau, seismic reflection data, Pacific Plate. The Pacific Plate is highly engraved by volcanism that has formed oceanic plateaus and hotspot chains. The Manihiki Plateau (MP) is a large igneous province (LIP) located in the central Pacific that has an areal extent of 600000 km2. In 2006, Taylor proposed a joint emplacement of the MP with the Ontong Java Plateau, the Hikurangi Plateau and two missing fragments during the Cretaceous in a "Super-LIP" called Ontong Java Nui (OJN). The emplacement of OJN with an aerial extent of 1.1% of the earth's surface would have had major impacts on Earth's climate. An investigation of the initital volcanic emplacement history of the Manihiki Plateau and its break-up processes can contribute to a better understanding of LIP-impact on the paleo-climate. Analysis and interpretation of a new, high-resolution multi-channel seismic reflection dataset has provided a detailed and improved volcanic history of the Manihiki Plateau. The new model consists of three volcanic phases instead of the previously assumed two volcanic phases. It includes the initial formation phase (>125 Ma) that formed a spatially localized nucleus, which was extended to the East. The expansion phase (125-116 Ma) erupted massive tholeiitic basalts and break-up processes into the other LIP-fragments occurred. The third phase is a phase of secondary volcanism that leveled out the overall topography and was intense at the tectonically altered margins. Since the late Cretaceous/early Cenozoic, the morphology of the Manihiki Plateau was engraved by tectonic and volcanic features that were strongly related to the kinematics of the Pacific Plate. During the Pleistocene, a major Pacific plate-reorganization occurred that caused changes of inner-lithospheric stress fields. In this study, the origin of the Suvarov Trough has been investigated. Age and spatial extension point towards a cause that is in a good correlation to this major Pleistocene event. Strain within a LIP crust due to applied stress field changes appears to be similar to continental crust and different to the surrounding oceanic crust. During the Cenozoic, the seafloor morphology in the central Pacific is dominated by the formation of age-progressive hotspot seamount chains. Neogene igneous diapirs in the southwestern MP have been investigated within this study. Age and location characteristics support a hotspot origin, which might be related to the Society Islands Hotspot. The characteristic appearance of the diapirs is different to hotspot volcanism within oceanic lithosphere, which can probably be related to the anomalous thick crust of the Manihiki Plateau. The magmatic and tectonic history of the Manihiki Plateau reveals that this LIP acts similar to continental crust on applied external forces, although its chemical composition resembles thick oceanic crust. Langzeitarchivierung gewährleistet pdager Hochschulschrift (DE-588)4113937-9 (DE-627)105825778 (DE-576)209480580 gnd-content Universität Bremen Grad-verleihende Institution (DE-588)2001386-3 (DE-627)101380429 (DE-576)191575038 dgg Bremen (DE-588)4008135-7 (DE-627)106369636 (DE-576)208874569 uvp Erscheint auch als Druck-Ausgabe Pietsch, Ricarda The Manihiki Plateau Bremen, 2015 xi, 125 Seiten (DE-627)862891736 http://nbn-resolving.de/urn:nbn:de:gbv:46-00105277-18 Resolving-System kostenfrei Volltext http://nbn-resolving.de/urn:nbn:de:gbv:46-00105277-18 2016-08-03 Resolving-System Volltext http://d-nb.info/1106374568/34 2016-08-03 Langzeitarchivierung Nationalbibliothek Volltext http://elib.suub.uni-bremen.de/edocs/00105277-1.pdf 2016-08-03 Verlag kostenfrei Volltext GBV-ODiss GBV_ILN_20 ISIL_DE-84 SYSFLAG_1 GBV_KXP SSG-OPC-GGO GBV_ILN_21 ISIL_DE-46 GBV_ILN_22 ISIL_DE-18 GBV_ILN_23 ISIL_DE-830 GBV_ILN_30 ISIL_DE-104 GBV_ILN_40 ISIL_DE-7 GBV_ILN_60 ISIL_DE-705 GBV_ILN_63 ISIL_DE-Wim2 GBV_ILN_65 ISIL_DE-3 GBV_ILN_70 ISIL_DE-89 GBV_ILN_105 ISIL_DE-841 GBV_ILN_110 ISIL_DE-Luen4 GBV_ILN_132 ISIL_DE-959 GBV_ILN_151 ISIL_DE-546 GBV_ILN_161 ISIL_DE-960 GBV_ILN_293 ISIL_DE-960-3 GBV_ILN_370 ISIL_DE-1373 GBV_ILN_381 ISIL_DE-Ki130 GBV_ILN_2403 ISIL_DE-LFER BO 20 01 0084 1645563472 x 11-11-16 21 01 0046 1624969992 ebook_2016_dissbremen Kostenloser Zugriff zza 11-07-16 22 01 0018 1648893147 SUBolrd xu 02-12-16 23 01 0830 1645707814 olr-d x 11-11-16 30 01 0104 1645757730 z 11-11-16 40 01 0007 1645811883 xsn 11-11-16 60 01 0705 164588709X OLRD z 11-11-16 63 01 3401 1645951871 ORD x 11-11-16 65 01 0003 4167729075 GBV-ODiss Open Access z 16-07-22 70 01 0089 1645993124 zdo 11-11-16 105 01 0841 1646380037 z 11-11-16 110 01 3110 1646043073 x 11-11-16 132 01 0959 1646102150 OLR-DISS x 11-11-16 151 01 0546 3583606698 OLR-ODISS z 31-01-20 161 01 0960 1646170539 ORD x 11-11-16 293 01 3293 1646316967 ORD xf 11-11-16 370 01 4370 1646356403 x 11-11-16 381 01 4381 1676004130 00 --%%-- --%%-- --%%-- --%%-- z 07-04-17 2403 01 DE-LFER 3475566001 00 --%%-- --%%-- n --%%-- l01 13-05-19 20 01 0084 http://nbn-resolving.de/urn:nbn:de:gbv:46-00105277-18 21 01 0046 http://nbn-resolving.de/urn:nbn:de:gbv:46-00105277-18 LF 22 01 0018 http://nbn-resolving.de/urn:nbn:de:gbv:46-00105277-18 23 01 0830 http://nbn-resolving.de/urn:nbn:de:gbv:46-00105277-18 30 01 0104 http://nbn-resolving.de/urn:nbn:de:gbv:46-00105277-18 40 01 0007 http://nbn-resolving.de/urn:nbn:de:gbv:46-00105277-18 60 01 0705 http://nbn-resolving.de/urn:nbn:de:gbv:46-00105277-18 63 01 3401 E-Book http://nbn-resolving.de/urn:nbn:de:gbv:46-00105277-18 LF 65 01 0003 http://nbn-resolving.de/urn:nbn:de:gbv:46-00105277-18 70 01 0089 http://nbn-resolving.de/urn:nbn:de:gbv:46-00105277-18 105 01 0841 http://nbn-resolving.de/urn:nbn:de:gbv:46-00105277-18 110 01 3110 http://nbn-resolving.de/urn:nbn:de:gbv:46-00105277-18 132 01 0959 http://nbn-resolving.de/urn:nbn:de:gbv:46-00105277-18 151 01 0546 Volltext http://nbn-resolving.de/urn:nbn:de:gbv:46-00105277-18 161 01 0960 http://nbn-resolving.de/urn:nbn:de:gbv:46-00105277-18 293 01 3293 http://nbn-resolving.de/urn:nbn:de:gbv:46-00105277-18 370 01 4370 http://nbn-resolving.de/urn:nbn:de:gbv:46-00105277-18 381 01 4381 http://elib.suub.uni-bremen.de/edocs/00105277-1.pdf 34 2403 01 DE-LFER http://nbn-resolving.de/urn:nbn:de:gbv:46-00105277-18 21 00 DE-46 00 Universität Bremen 21 00 DE-46 00 Fachbereich 05: Geowissenschaften (FB 05) 381 00 DE-Ki130 00 Annette-Barthelt-Preis 21 00 DE-46 99 07 60 01 0705 10 ho 20 01 0084 OLRD 110 01 3110 OLRD 370 01 4370 OLRD 21 01 0046 ebook_2016_dissbremen 22 01 0018 SUBolrd 23 01 0830 olr-d 60 01 0705 OLRD 63 01 3401 ORD 65 01 0003 GBV-ODiss 132 01 0959 OLR-DISS 151 01 0546 OLR-ODISS 161 01 0960 ORD 293 01 3293 ORD 23 01 0830 2016-11-11:17:52:41 |
allfieldsSound |
16,O08 dnb 1106374568 DE-101 urn:nbn:de:gbv:46-00105277-18 urn (DE-627)862891833 (DE-576)9862891831 (DE-599)GBV862891833 (OCoLC)953396126 DE-627 ger DE-627 rda eng XA-DE 550 DE-101 Pietsch, Ricarda verfasserin aut The Manihiki Plateau Magmatic and tectonic evolution of a Large Igneous Province through time vorgelegt von Ricarda Pietsch Bremen 2015 1 Online-Ressource (xi, 125 Seiten) Illustrationen Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Dissertation Universität Bremen 2016 Large Igneous Province, Manihiki Plateau, seismic reflection data, Pacific Plate. The Pacific Plate is highly engraved by volcanism that has formed oceanic plateaus and hotspot chains. The Manihiki Plateau (MP) is a large igneous province (LIP) located in the central Pacific that has an areal extent of 600000 km2. In 2006, Taylor proposed a joint emplacement of the MP with the Ontong Java Plateau, the Hikurangi Plateau and two missing fragments during the Cretaceous in a "Super-LIP" called Ontong Java Nui (OJN). The emplacement of OJN with an aerial extent of 1.1% of the earth's surface would have had major impacts on Earth's climate. An investigation of the initital volcanic emplacement history of the Manihiki Plateau and its break-up processes can contribute to a better understanding of LIP-impact on the paleo-climate. Analysis and interpretation of a new, high-resolution multi-channel seismic reflection dataset has provided a detailed and improved volcanic history of the Manihiki Plateau. The new model consists of three volcanic phases instead of the previously assumed two volcanic phases. It includes the initial formation phase (>125 Ma) that formed a spatially localized nucleus, which was extended to the East. The expansion phase (125-116 Ma) erupted massive tholeiitic basalts and break-up processes into the other LIP-fragments occurred. The third phase is a phase of secondary volcanism that leveled out the overall topography and was intense at the tectonically altered margins. Since the late Cretaceous/early Cenozoic, the morphology of the Manihiki Plateau was engraved by tectonic and volcanic features that were strongly related to the kinematics of the Pacific Plate. During the Pleistocene, a major Pacific plate-reorganization occurred that caused changes of inner-lithospheric stress fields. In this study, the origin of the Suvarov Trough has been investigated. Age and spatial extension point towards a cause that is in a good correlation to this major Pleistocene event. Strain within a LIP crust due to applied stress field changes appears to be similar to continental crust and different to the surrounding oceanic crust. During the Cenozoic, the seafloor morphology in the central Pacific is dominated by the formation of age-progressive hotspot seamount chains. Neogene igneous diapirs in the southwestern MP have been investigated within this study. Age and location characteristics support a hotspot origin, which might be related to the Society Islands Hotspot. The characteristic appearance of the diapirs is different to hotspot volcanism within oceanic lithosphere, which can probably be related to the anomalous thick crust of the Manihiki Plateau. The magmatic and tectonic history of the Manihiki Plateau reveals that this LIP acts similar to continental crust on applied external forces, although its chemical composition resembles thick oceanic crust. 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The Manihiki Plateau (MP) is a large igneous province (LIP) located in the central Pacific that has an areal extent of 600000 km2. In 2006, Taylor proposed a joint emplacement of the MP with the Ontong Java Plateau, the Hikurangi Plateau and two missing fragments during the Cretaceous in a "Super-LIP" called Ontong Java Nui (OJN). The emplacement of OJN with an aerial extent of 1.1% of the earth's surface would have had major impacts on Earth's climate. An investigation of the initital volcanic emplacement history of the Manihiki Plateau and its break-up processes can contribute to a better understanding of LIP-impact on the paleo-climate. Analysis and interpretation of a new, high-resolution multi-channel seismic reflection dataset has provided a detailed and improved volcanic history of the Manihiki Plateau. The new model consists of three volcanic phases instead of the previously assumed two volcanic phases. It includes the initial formation phase (>125 Ma) that formed a spatially localized nucleus, which was extended to the East. The expansion phase (125-116 Ma) erupted massive tholeiitic basalts and break-up processes into the other LIP-fragments occurred. The third phase is a phase of secondary volcanism that leveled out the overall topography and was intense at the tectonically altered margins. Since the late Cretaceous/early Cenozoic, the morphology of the Manihiki Plateau was engraved by tectonic and volcanic features that were strongly related to the kinematics of the Pacific Plate. During the Pleistocene, a major Pacific plate-reorganization occurred that caused changes of inner-lithospheric stress fields. In this study, the origin of the Suvarov Trough has been investigated. Age and spatial extension point towards a cause that is in a good correlation to this major Pleistocene event. 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The Manihiki Plateau Magmatic and tectonic evolution of a Large Igneous Province through time |
abstract |
Large Igneous Province, Manihiki Plateau, seismic reflection data, Pacific Plate. The Pacific Plate is highly engraved by volcanism that has formed oceanic plateaus and hotspot chains. The Manihiki Plateau (MP) is a large igneous province (LIP) located in the central Pacific that has an areal extent of 600000 km2. In 2006, Taylor proposed a joint emplacement of the MP with the Ontong Java Plateau, the Hikurangi Plateau and two missing fragments during the Cretaceous in a "Super-LIP" called Ontong Java Nui (OJN). The emplacement of OJN with an aerial extent of 1.1% of the earth's surface would have had major impacts on Earth's climate. An investigation of the initital volcanic emplacement history of the Manihiki Plateau and its break-up processes can contribute to a better understanding of LIP-impact on the paleo-climate. Analysis and interpretation of a new, high-resolution multi-channel seismic reflection dataset has provided a detailed and improved volcanic history of the Manihiki Plateau. The new model consists of three volcanic phases instead of the previously assumed two volcanic phases. It includes the initial formation phase (>125 Ma) that formed a spatially localized nucleus, which was extended to the East. The expansion phase (125-116 Ma) erupted massive tholeiitic basalts and break-up processes into the other LIP-fragments occurred. The third phase is a phase of secondary volcanism that leveled out the overall topography and was intense at the tectonically altered margins. Since the late Cretaceous/early Cenozoic, the morphology of the Manihiki Plateau was engraved by tectonic and volcanic features that were strongly related to the kinematics of the Pacific Plate. During the Pleistocene, a major Pacific plate-reorganization occurred that caused changes of inner-lithospheric stress fields. In this study, the origin of the Suvarov Trough has been investigated. Age and spatial extension point towards a cause that is in a good correlation to this major Pleistocene event. Strain within a LIP crust due to applied stress field changes appears to be similar to continental crust and different to the surrounding oceanic crust. During the Cenozoic, the seafloor morphology in the central Pacific is dominated by the formation of age-progressive hotspot seamount chains. Neogene igneous diapirs in the southwestern MP have been investigated within this study. Age and location characteristics support a hotspot origin, which might be related to the Society Islands Hotspot. The characteristic appearance of the diapirs is different to hotspot volcanism within oceanic lithosphere, which can probably be related to the anomalous thick crust of the Manihiki Plateau. The magmatic and tectonic history of the Manihiki Plateau reveals that this LIP acts similar to continental crust on applied external forces, although its chemical composition resembles thick oceanic crust. |
abstractGer |
Large Igneous Province, Manihiki Plateau, seismic reflection data, Pacific Plate. The Pacific Plate is highly engraved by volcanism that has formed oceanic plateaus and hotspot chains. The Manihiki Plateau (MP) is a large igneous province (LIP) located in the central Pacific that has an areal extent of 600000 km2. In 2006, Taylor proposed a joint emplacement of the MP with the Ontong Java Plateau, the Hikurangi Plateau and two missing fragments during the Cretaceous in a "Super-LIP" called Ontong Java Nui (OJN). The emplacement of OJN with an aerial extent of 1.1% of the earth's surface would have had major impacts on Earth's climate. An investigation of the initital volcanic emplacement history of the Manihiki Plateau and its break-up processes can contribute to a better understanding of LIP-impact on the paleo-climate. Analysis and interpretation of a new, high-resolution multi-channel seismic reflection dataset has provided a detailed and improved volcanic history of the Manihiki Plateau. The new model consists of three volcanic phases instead of the previously assumed two volcanic phases. It includes the initial formation phase (>125 Ma) that formed a spatially localized nucleus, which was extended to the East. The expansion phase (125-116 Ma) erupted massive tholeiitic basalts and break-up processes into the other LIP-fragments occurred. The third phase is a phase of secondary volcanism that leveled out the overall topography and was intense at the tectonically altered margins. Since the late Cretaceous/early Cenozoic, the morphology of the Manihiki Plateau was engraved by tectonic and volcanic features that were strongly related to the kinematics of the Pacific Plate. During the Pleistocene, a major Pacific plate-reorganization occurred that caused changes of inner-lithospheric stress fields. In this study, the origin of the Suvarov Trough has been investigated. Age and spatial extension point towards a cause that is in a good correlation to this major Pleistocene event. Strain within a LIP crust due to applied stress field changes appears to be similar to continental crust and different to the surrounding oceanic crust. During the Cenozoic, the seafloor morphology in the central Pacific is dominated by the formation of age-progressive hotspot seamount chains. Neogene igneous diapirs in the southwestern MP have been investigated within this study. Age and location characteristics support a hotspot origin, which might be related to the Society Islands Hotspot. The characteristic appearance of the diapirs is different to hotspot volcanism within oceanic lithosphere, which can probably be related to the anomalous thick crust of the Manihiki Plateau. The magmatic and tectonic history of the Manihiki Plateau reveals that this LIP acts similar to continental crust on applied external forces, although its chemical composition resembles thick oceanic crust. |
abstract_unstemmed |
Large Igneous Province, Manihiki Plateau, seismic reflection data, Pacific Plate. The Pacific Plate is highly engraved by volcanism that has formed oceanic plateaus and hotspot chains. The Manihiki Plateau (MP) is a large igneous province (LIP) located in the central Pacific that has an areal extent of 600000 km2. In 2006, Taylor proposed a joint emplacement of the MP with the Ontong Java Plateau, the Hikurangi Plateau and two missing fragments during the Cretaceous in a "Super-LIP" called Ontong Java Nui (OJN). The emplacement of OJN with an aerial extent of 1.1% of the earth's surface would have had major impacts on Earth's climate. An investigation of the initital volcanic emplacement history of the Manihiki Plateau and its break-up processes can contribute to a better understanding of LIP-impact on the paleo-climate. Analysis and interpretation of a new, high-resolution multi-channel seismic reflection dataset has provided a detailed and improved volcanic history of the Manihiki Plateau. The new model consists of three volcanic phases instead of the previously assumed two volcanic phases. It includes the initial formation phase (>125 Ma) that formed a spatially localized nucleus, which was extended to the East. The expansion phase (125-116 Ma) erupted massive tholeiitic basalts and break-up processes into the other LIP-fragments occurred. The third phase is a phase of secondary volcanism that leveled out the overall topography and was intense at the tectonically altered margins. Since the late Cretaceous/early Cenozoic, the morphology of the Manihiki Plateau was engraved by tectonic and volcanic features that were strongly related to the kinematics of the Pacific Plate. During the Pleistocene, a major Pacific plate-reorganization occurred that caused changes of inner-lithospheric stress fields. In this study, the origin of the Suvarov Trough has been investigated. Age and spatial extension point towards a cause that is in a good correlation to this major Pleistocene event. Strain within a LIP crust due to applied stress field changes appears to be similar to continental crust and different to the surrounding oceanic crust. During the Cenozoic, the seafloor morphology in the central Pacific is dominated by the formation of age-progressive hotspot seamount chains. Neogene igneous diapirs in the southwestern MP have been investigated within this study. Age and location characteristics support a hotspot origin, which might be related to the Society Islands Hotspot. The characteristic appearance of the diapirs is different to hotspot volcanism within oceanic lithosphere, which can probably be related to the anomalous thick crust of the Manihiki Plateau. The magmatic and tectonic history of the Manihiki Plateau reveals that this LIP acts similar to continental crust on applied external forces, although its chemical composition resembles thick oceanic crust. |
collection_details |
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title_short |
The Manihiki Plateau |
url |
http://nbn-resolving.de/urn:nbn:de:gbv:46-00105277-18 http://d-nb.info/1106374568/34 http://elib.suub.uni-bremen.de/edocs/00105277-1.pdf |
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author2 |
Universität Bremen |
author2Str |
Universität Bremen |
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862891736 |
GND_str_mv |
Hochschulschrift Universidad de Bremen Uniwersytet w Bremie University of Bremen Université de Brême Univ. Bremen Uniwersytet Bremeński Bremenskij Universitet Uni Bremen Universität Bremen Free Hanseatic City of Bremen Bremischer Staat Fabiranum Bremeischer Staat Phabiranum Pregmensis civitas Land Freie Hansestadt Bremen Bremae Stadtgemeinde Bremen Freie und Hansestadt Bremen Premensis civitas Brema Bremia Land und Stadtgemeinde Bremen Land Bremen Bremensis civitas Freie Hansestadt Bremen Hansestadt Bremen Fabirana Saxonum Heberanum Brême Bremen |
GND_txt_mv |
Hochschulschrift Universidad de Bremen Uniwersytet w Bremie University of Bremen Université de Brême Univ. Bremen Uniwersytet Bremeński Bremenskij Universitet Uni Bremen Universität Bremen Free Hanseatic City of Bremen Bremischer Staat Fabiranum Bremeischer Staat Phabiranum Pregmensis civitas Land Freie Hansestadt Bremen Bremae Stadtgemeinde Bremen Freie und Hansestadt Bremen Premensis civitas Brema Bremia Land und Stadtgemeinde Bremen Land Bremen Bremensis civitas Freie Hansestadt Bremen Hansestadt Bremen Fabirana Saxonum Heberanum Brême Bremen |
GND_txtF_mv |
Hochschulschrift Universidad de Bremen Uniwersytet w Bremie University of Bremen Université de Brême Univ. Bremen Uniwersytet Bremeński Bremenskij Universitet Uni Bremen Universität Bremen Free Hanseatic City of Bremen Bremischer Staat Fabiranum Bremeischer Staat Phabiranum Pregmensis civitas Land Freie Hansestadt Bremen Bremae Stadtgemeinde Bremen Freie und Hansestadt Bremen Premensis civitas Brema Bremia Land und Stadtgemeinde Bremen Land Bremen Bremensis civitas Freie Hansestadt Bremen Hansestadt Bremen Fabirana Saxonum Heberanum Brême Bremen |
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