Structural and strain analysis in the Late Paleozoic coastal accretionary wedge of central Chile

Abstract: In this study structural and finite strain data are used to explore the tectonic evolution and the exhumation history of the Chilean accretionary wedge. The Chilean accretionary wedge is part of a Late Paleozoic subduction complex that developed during subduction of the Pacific plate under...
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Gespeichert in:

Autor*in:	Richter, Peter Paul Erich - 1976-
Hochschulschrift:	Mainz, Univ., Diss, 2007

Format:	E-Book
Sprache:	Englisch

Erschienen:	2007

Formangabe:	Hochschulschrift

Umfang:	Online-Ressource (96 S.)

Links:	Link aufrufen Volltext Volltext Volltext Volltext

DOI / URN:	urn:nbn:de:hebis:77-14450

Katalog-ID:	565554433

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Indexfelder

matchkey_str	richterpeterpaulerich:2007----:tutrlnsriaayiiteaeaezicatlcrto
oclc_num	227344583
hierarchy_sort_str	2007
bklnumber	38.36
publishDate	2007
allfields	08,H05,1439 dnb 98648394X DE-101 urn:nbn:de:hebis:77-14450 urn (DE-627)565554433 (DE-599)DNB98648394X (OCoLC)227344583 DE-627 ger DE-627 rakwb eng XA-DE 550 16,13 ssgn 38.36 bkl Structural and strain analysis in the Late Paleozoic coastal accretionary wedge of central Chile Peter Paul Erich Richter 2007 Online-Ressource (96 S.) Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Mainz, Univ., Diss, 2007 Abstract: In this study structural and finite strain data are used to explore the tectonic evolution and the exhumation history of the Chilean accretionary wedge. The Chilean accretionary wedge is part of a Late Paleozoic subduction complex that developed during subduction of the Pacific plate underneath South America. The wedge is commonly subdivided into a structurally lower Western Series and an upper Eastern Series. This study shows the progressive development of structures and finite strain from the least deformed rocks in the eastern part of the Eastern Series of the accretionary wedge to higher grade schist of the Western Series at the Pacific coast. Furthermore, this study reports finite-strain data to quantify the contribution of vertical ductile shortening to exhumation. Vertical ductile shortening is, together with erosion and normal faulting, a process that can aid the exhumation of high-pressure rocks. In the east, structures are characterized by upright chevron folds of sedimentary layering which are associated with a penetrative axial-plane foliation, S1. As the F1 folds became slightly overturned to the west, S1 was folded about recumbent open F2 folds and an S2 axial-plane foliation developed. Near the contact between the Western and Eastern Series S2 represents a prominent subhorizontal transposition foliation. Towards the structural deepest units in the west the transposition foliation became progressively flat lying. Finite-strain data as obtained by Rf/Phi and PDS analysis in metagreywacke and X-ray texture goniometry in phyllosilicate-rich rocks show a smooth and gradual increase in strain magnitude from east to west... Hochschulschrift (DE-588)4113937-9 (DE-627)105825778 (DE-576)209480580 gnd-content Richter, Peter Paul Erich 1976- (DE-588)133643573 (DE-627)550290079 (DE-576)299992799 oth Mainz uvp http://ubm.opus.hbz-nrw.de/volltexte/2007/1445/pdf/diss.pdf Verlag Volltext http://ubm.opus.hbz-nrw.de/volltexte/2007/1445/index.html Verlag Volltext http://d-nb.info/98648394X/34 Verlag Volltext Volltext http://nbn-resolving.de/urn:nbn:de:hebis:77-14450 Resolving-System Volltext GBV_ILN_20 ISIL_DE-84 SYSFLAG_1 GBV_KXP SSG-OPC-GGO SSG-OPC-GEO 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_110 ISIL_DE-Luen4 GBV_ILN_370 ISIL_DE-1373 38.36 Tektonik (DE-627)106407147 BO 20 01 0084 873668014 z 13-05-08 21 01 0046 200194585 z 19-12-08 22 01 0018 200278878 SUBolrd xu 19-12-08 23 01 0830 200361546 olr-d x 19-12-08 30 01 0104 200406108 z 19-12-08 40 01 0007 880720980 ksn 04-07-08 60 01 0705 200452673 z 19-12-08 110 01 3110 200536966 x 19-12-08 370 01 4370 200619403 x 19-12-08 21 01 0046 http://d-nb.info/98648394X/34 22 01 0018 http://d-nb.info/98648394X/34 23 01 0830 http://d-nb.info/98648394X/34 30 01 0104 http://d-nb.info/98648394X/34 40 01 0007 http://ubm.opus.hbz-nrw.de/volltexte/2007/1445/pdf/diss.pdf 60 01 0705 http://d-nb.info/98648394X/34 110 01 3110 http://d-nb.info/98648394X/34 370 01 4370 http://d-nb.info/98648394X/34 40 00 DE-7 00 (DE-627)623606976 TSX 500 Chile {Geophysik} 40 00 DE-7 01 (DE-627)625046234 VAE 812 Variszisch-herzynische Orogene {Tektonik} 60 01 0705 10 ho 21 01 0046 OLRD 30 01 0104 OLRD 60 01 0705 OLRD 110 01 3110 OLRD 370 01 4370 OLRD 22 01 0018 SUBolrd 23 01 0830 olr-d 23 01 0830 2008-12-19:09:09:46 40 01 0007 2008-07 9
spelling	08,H05,1439 dnb 98648394X DE-101 urn:nbn:de:hebis:77-14450 urn (DE-627)565554433 (DE-599)DNB98648394X (OCoLC)227344583 DE-627 ger DE-627 rakwb eng XA-DE 550 16,13 ssgn 38.36 bkl Structural and strain analysis in the Late Paleozoic coastal accretionary wedge of central Chile Peter Paul Erich Richter 2007 Online-Ressource (96 S.) Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Mainz, Univ., Diss, 2007 Abstract: In this study structural and finite strain data are used to explore the tectonic evolution and the exhumation history of the Chilean accretionary wedge. The Chilean accretionary wedge is part of a Late Paleozoic subduction complex that developed during subduction of the Pacific plate underneath South America. The wedge is commonly subdivided into a structurally lower Western Series and an upper Eastern Series. This study shows the progressive development of structures and finite strain from the least deformed rocks in the eastern part of the Eastern Series of the accretionary wedge to higher grade schist of the Western Series at the Pacific coast. Furthermore, this study reports finite-strain data to quantify the contribution of vertical ductile shortening to exhumation. Vertical ductile shortening is, together with erosion and normal faulting, a process that can aid the exhumation of high-pressure rocks. In the east, structures are characterized by upright chevron folds of sedimentary layering which are associated with a penetrative axial-plane foliation, S1. As the F1 folds became slightly overturned to the west, S1 was folded about recumbent open F2 folds and an S2 axial-plane foliation developed. Near the contact between the Western and Eastern Series S2 represents a prominent subhorizontal transposition foliation. Towards the structural deepest units in the west the transposition foliation became progressively flat lying. Finite-strain data as obtained by Rf/Phi and PDS analysis in metagreywacke and X-ray texture goniometry in phyllosilicate-rich rocks show a smooth and gradual increase in strain magnitude from east to west... Hochschulschrift (DE-588)4113937-9 (DE-627)105825778 (DE-576)209480580 gnd-content Richter, Peter Paul Erich 1976- (DE-588)133643573 (DE-627)550290079 (DE-576)299992799 oth Mainz uvp http://ubm.opus.hbz-nrw.de/volltexte/2007/1445/pdf/diss.pdf Verlag Volltext http://ubm.opus.hbz-nrw.de/volltexte/2007/1445/index.html Verlag Volltext http://d-nb.info/98648394X/34 Verlag Volltext Volltext http://nbn-resolving.de/urn:nbn:de:hebis:77-14450 Resolving-System Volltext GBV_ILN_20 ISIL_DE-84 SYSFLAG_1 GBV_KXP SSG-OPC-GGO SSG-OPC-GEO 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_110 ISIL_DE-Luen4 GBV_ILN_370 ISIL_DE-1373 38.36 Tektonik (DE-627)106407147 BO 20 01 0084 873668014 z 13-05-08 21 01 0046 200194585 z 19-12-08 22 01 0018 200278878 SUBolrd xu 19-12-08 23 01 0830 200361546 olr-d x 19-12-08 30 01 0104 200406108 z 19-12-08 40 01 0007 880720980 ksn 04-07-08 60 01 0705 200452673 z 19-12-08 110 01 3110 200536966 x 19-12-08 370 01 4370 200619403 x 19-12-08 21 01 0046 http://d-nb.info/98648394X/34 22 01 0018 http://d-nb.info/98648394X/34 23 01 0830 http://d-nb.info/98648394X/34 30 01 0104 http://d-nb.info/98648394X/34 40 01 0007 http://ubm.opus.hbz-nrw.de/volltexte/2007/1445/pdf/diss.pdf 60 01 0705 http://d-nb.info/98648394X/34 110 01 3110 http://d-nb.info/98648394X/34 370 01 4370 http://d-nb.info/98648394X/34 40 00 DE-7 00 (DE-627)623606976 TSX 500 Chile {Geophysik} 40 00 DE-7 01 (DE-627)625046234 VAE 812 Variszisch-herzynische Orogene {Tektonik} 60 01 0705 10 ho 21 01 0046 OLRD 30 01 0104 OLRD 60 01 0705 OLRD 110 01 3110 OLRD 370 01 4370 OLRD 22 01 0018 SUBolrd 23 01 0830 olr-d 23 01 0830 2008-12-19:09:09:46 40 01 0007 2008-07 9
allfields_unstemmed	08,H05,1439 dnb 98648394X DE-101 urn:nbn:de:hebis:77-14450 urn (DE-627)565554433 (DE-599)DNB98648394X (OCoLC)227344583 DE-627 ger DE-627 rakwb eng XA-DE 550 16,13 ssgn 38.36 bkl Structural and strain analysis in the Late Paleozoic coastal accretionary wedge of central Chile Peter Paul Erich Richter 2007 Online-Ressource (96 S.) Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Mainz, Univ., Diss, 2007 Abstract: In this study structural and finite strain data are used to explore the tectonic evolution and the exhumation history of the Chilean accretionary wedge. The Chilean accretionary wedge is part of a Late Paleozoic subduction complex that developed during subduction of the Pacific plate underneath South America. The wedge is commonly subdivided into a structurally lower Western Series and an upper Eastern Series. This study shows the progressive development of structures and finite strain from the least deformed rocks in the eastern part of the Eastern Series of the accretionary wedge to higher grade schist of the Western Series at the Pacific coast. Furthermore, this study reports finite-strain data to quantify the contribution of vertical ductile shortening to exhumation. Vertical ductile shortening is, together with erosion and normal faulting, a process that can aid the exhumation of high-pressure rocks. In the east, structures are characterized by upright chevron folds of sedimentary layering which are associated with a penetrative axial-plane foliation, S1. As the F1 folds became slightly overturned to the west, S1 was folded about recumbent open F2 folds and an S2 axial-plane foliation developed. Near the contact between the Western and Eastern Series S2 represents a prominent subhorizontal transposition foliation. Towards the structural deepest units in the west the transposition foliation became progressively flat lying. Finite-strain data as obtained by Rf/Phi and PDS analysis in metagreywacke and X-ray texture goniometry in phyllosilicate-rich rocks show a smooth and gradual increase in strain magnitude from east to west... Hochschulschrift (DE-588)4113937-9 (DE-627)105825778 (DE-576)209480580 gnd-content Richter, Peter Paul Erich 1976- (DE-588)133643573 (DE-627)550290079 (DE-576)299992799 oth Mainz uvp http://ubm.opus.hbz-nrw.de/volltexte/2007/1445/pdf/diss.pdf Verlag Volltext http://ubm.opus.hbz-nrw.de/volltexte/2007/1445/index.html Verlag Volltext http://d-nb.info/98648394X/34 Verlag Volltext Volltext http://nbn-resolving.de/urn:nbn:de:hebis:77-14450 Resolving-System Volltext GBV_ILN_20 ISIL_DE-84 SYSFLAG_1 GBV_KXP SSG-OPC-GGO SSG-OPC-GEO 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_110 ISIL_DE-Luen4 GBV_ILN_370 ISIL_DE-1373 38.36 Tektonik (DE-627)106407147 BO 20 01 0084 873668014 z 13-05-08 21 01 0046 200194585 z 19-12-08 22 01 0018 200278878 SUBolrd xu 19-12-08 23 01 0830 200361546 olr-d x 19-12-08 30 01 0104 200406108 z 19-12-08 40 01 0007 880720980 ksn 04-07-08 60 01 0705 200452673 z 19-12-08 110 01 3110 200536966 x 19-12-08 370 01 4370 200619403 x 19-12-08 21 01 0046 http://d-nb.info/98648394X/34 22 01 0018 http://d-nb.info/98648394X/34 23 01 0830 http://d-nb.info/98648394X/34 30 01 0104 http://d-nb.info/98648394X/34 40 01 0007 http://ubm.opus.hbz-nrw.de/volltexte/2007/1445/pdf/diss.pdf 60 01 0705 http://d-nb.info/98648394X/34 110 01 3110 http://d-nb.info/98648394X/34 370 01 4370 http://d-nb.info/98648394X/34 40 00 DE-7 00 (DE-627)623606976 TSX 500 Chile {Geophysik} 40 00 DE-7 01 (DE-627)625046234 VAE 812 Variszisch-herzynische Orogene {Tektonik} 60 01 0705 10 ho 21 01 0046 OLRD 30 01 0104 OLRD 60 01 0705 OLRD 110 01 3110 OLRD 370 01 4370 OLRD 22 01 0018 SUBolrd 23 01 0830 olr-d 23 01 0830 2008-12-19:09:09:46 40 01 0007 2008-07 9
allfieldsGer	08,H05,1439 dnb 98648394X DE-101 urn:nbn:de:hebis:77-14450 urn (DE-627)565554433 (DE-599)DNB98648394X (OCoLC)227344583 DE-627 ger DE-627 rakwb eng XA-DE 550 16,13 ssgn 38.36 bkl Structural and strain analysis in the Late Paleozoic coastal accretionary wedge of central Chile Peter Paul Erich Richter 2007 Online-Ressource (96 S.) Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Mainz, Univ., Diss, 2007 Abstract: In this study structural and finite strain data are used to explore the tectonic evolution and the exhumation history of the Chilean accretionary wedge. The Chilean accretionary wedge is part of a Late Paleozoic subduction complex that developed during subduction of the Pacific plate underneath South America. The wedge is commonly subdivided into a structurally lower Western Series and an upper Eastern Series. This study shows the progressive development of structures and finite strain from the least deformed rocks in the eastern part of the Eastern Series of the accretionary wedge to higher grade schist of the Western Series at the Pacific coast. Furthermore, this study reports finite-strain data to quantify the contribution of vertical ductile shortening to exhumation. Vertical ductile shortening is, together with erosion and normal faulting, a process that can aid the exhumation of high-pressure rocks. In the east, structures are characterized by upright chevron folds of sedimentary layering which are associated with a penetrative axial-plane foliation, S1. As the F1 folds became slightly overturned to the west, S1 was folded about recumbent open F2 folds and an S2 axial-plane foliation developed. Near the contact between the Western and Eastern Series S2 represents a prominent subhorizontal transposition foliation. Towards the structural deepest units in the west the transposition foliation became progressively flat lying. Finite-strain data as obtained by Rf/Phi and PDS analysis in metagreywacke and X-ray texture goniometry in phyllosilicate-rich rocks show a smooth and gradual increase in strain magnitude from east to west... Hochschulschrift (DE-588)4113937-9 (DE-627)105825778 (DE-576)209480580 gnd-content Richter, Peter Paul Erich 1976- (DE-588)133643573 (DE-627)550290079 (DE-576)299992799 oth Mainz uvp http://ubm.opus.hbz-nrw.de/volltexte/2007/1445/pdf/diss.pdf Verlag Volltext http://ubm.opus.hbz-nrw.de/volltexte/2007/1445/index.html Verlag Volltext http://d-nb.info/98648394X/34 Verlag Volltext Volltext http://nbn-resolving.de/urn:nbn:de:hebis:77-14450 Resolving-System Volltext GBV_ILN_20 ISIL_DE-84 SYSFLAG_1 GBV_KXP SSG-OPC-GGO SSG-OPC-GEO 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_110 ISIL_DE-Luen4 GBV_ILN_370 ISIL_DE-1373 38.36 Tektonik (DE-627)106407147 BO 20 01 0084 873668014 z 13-05-08 21 01 0046 200194585 z 19-12-08 22 01 0018 200278878 SUBolrd xu 19-12-08 23 01 0830 200361546 olr-d x 19-12-08 30 01 0104 200406108 z 19-12-08 40 01 0007 880720980 ksn 04-07-08 60 01 0705 200452673 z 19-12-08 110 01 3110 200536966 x 19-12-08 370 01 4370 200619403 x 19-12-08 21 01 0046 http://d-nb.info/98648394X/34 22 01 0018 http://d-nb.info/98648394X/34 23 01 0830 http://d-nb.info/98648394X/34 30 01 0104 http://d-nb.info/98648394X/34 40 01 0007 http://ubm.opus.hbz-nrw.de/volltexte/2007/1445/pdf/diss.pdf 60 01 0705 http://d-nb.info/98648394X/34 110 01 3110 http://d-nb.info/98648394X/34 370 01 4370 http://d-nb.info/98648394X/34 40 00 DE-7 00 (DE-627)623606976 TSX 500 Chile {Geophysik} 40 00 DE-7 01 (DE-627)625046234 VAE 812 Variszisch-herzynische Orogene {Tektonik} 60 01 0705 10 ho 21 01 0046 OLRD 30 01 0104 OLRD 60 01 0705 OLRD 110 01 3110 OLRD 370 01 4370 OLRD 22 01 0018 SUBolrd 23 01 0830 olr-d 23 01 0830 2008-12-19:09:09:46 40 01 0007 2008-07 9
allfieldsSound	08,H05,1439 dnb 98648394X DE-101 urn:nbn:de:hebis:77-14450 urn (DE-627)565554433 (DE-599)DNB98648394X (OCoLC)227344583 DE-627 ger DE-627 rakwb eng XA-DE 550 16,13 ssgn 38.36 bkl Structural and strain analysis in the Late Paleozoic coastal accretionary wedge of central Chile Peter Paul Erich Richter 2007 Online-Ressource (96 S.) Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Mainz, Univ., Diss, 2007 Abstract: In this study structural and finite strain data are used to explore the tectonic evolution and the exhumation history of the Chilean accretionary wedge. The Chilean accretionary wedge is part of a Late Paleozoic subduction complex that developed during subduction of the Pacific plate underneath South America. The wedge is commonly subdivided into a structurally lower Western Series and an upper Eastern Series. This study shows the progressive development of structures and finite strain from the least deformed rocks in the eastern part of the Eastern Series of the accretionary wedge to higher grade schist of the Western Series at the Pacific coast. Furthermore, this study reports finite-strain data to quantify the contribution of vertical ductile shortening to exhumation. Vertical ductile shortening is, together with erosion and normal faulting, a process that can aid the exhumation of high-pressure rocks. In the east, structures are characterized by upright chevron folds of sedimentary layering which are associated with a penetrative axial-plane foliation, S1. As the F1 folds became slightly overturned to the west, S1 was folded about recumbent open F2 folds and an S2 axial-plane foliation developed. Near the contact between the Western and Eastern Series S2 represents a prominent subhorizontal transposition foliation. Towards the structural deepest units in the west the transposition foliation became progressively flat lying. Finite-strain data as obtained by Rf/Phi and PDS analysis in metagreywacke and X-ray texture goniometry in phyllosilicate-rich rocks show a smooth and gradual increase in strain magnitude from east to west... Hochschulschrift (DE-588)4113937-9 (DE-627)105825778 (DE-576)209480580 gnd-content Richter, Peter Paul Erich 1976- (DE-588)133643573 (DE-627)550290079 (DE-576)299992799 oth Mainz uvp http://ubm.opus.hbz-nrw.de/volltexte/2007/1445/pdf/diss.pdf Verlag Volltext http://ubm.opus.hbz-nrw.de/volltexte/2007/1445/index.html Verlag Volltext http://d-nb.info/98648394X/34 Verlag Volltext Volltext http://nbn-resolving.de/urn:nbn:de:hebis:77-14450 Resolving-System Volltext GBV_ILN_20 ISIL_DE-84 SYSFLAG_1 GBV_KXP SSG-OPC-GGO SSG-OPC-GEO 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_110 ISIL_DE-Luen4 GBV_ILN_370 ISIL_DE-1373 38.36 Tektonik (DE-627)106407147 BO 20 01 0084 873668014 z 13-05-08 21 01 0046 200194585 z 19-12-08 22 01 0018 200278878 SUBolrd xu 19-12-08 23 01 0830 200361546 olr-d x 19-12-08 30 01 0104 200406108 z 19-12-08 40 01 0007 880720980 ksn 04-07-08 60 01 0705 200452673 z 19-12-08 110 01 3110 200536966 x 19-12-08 370 01 4370 200619403 x 19-12-08 21 01 0046 http://d-nb.info/98648394X/34 22 01 0018 http://d-nb.info/98648394X/34 23 01 0830 http://d-nb.info/98648394X/34 30 01 0104 http://d-nb.info/98648394X/34 40 01 0007 http://ubm.opus.hbz-nrw.de/volltexte/2007/1445/pdf/diss.pdf 60 01 0705 http://d-nb.info/98648394X/34 110 01 3110 http://d-nb.info/98648394X/34 370 01 4370 http://d-nb.info/98648394X/34 40 00 DE-7 00 (DE-627)623606976 TSX 500 Chile {Geophysik} 40 00 DE-7 01 (DE-627)625046234 VAE 812 Variszisch-herzynische Orogene {Tektonik} 60 01 0705 10 ho 21 01 0046 OLRD 30 01 0104 OLRD 60 01 0705 OLRD 110 01 3110 OLRD 370 01 4370 OLRD 22 01 0018 SUBolrd 23 01 0830 olr-d 23 01 0830 2008-12-19:09:09:46 40 01 0007 2008-07 9
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topic_title	550 16,13 ssgn 38.36 bkl Structural and strain analysis in the Late Paleozoic coastal accretionary wedge of central Chile Peter Paul Erich Richter
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title	Structural and strain analysis in the Late Paleozoic coastal accretionary wedge of central Chile
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title_full	Structural and strain analysis in the Late Paleozoic coastal accretionary wedge of central Chile Peter Paul Erich Richter
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title_sort	structural and strain analysis in the late paleozoic coastal accretionary wedge of central chile
title_auth	Structural and strain analysis in the Late Paleozoic coastal accretionary wedge of central Chile
abstract	Abstract: In this study structural and finite strain data are used to explore the tectonic evolution and the exhumation history of the Chilean accretionary wedge. The Chilean accretionary wedge is part of a Late Paleozoic subduction complex that developed during subduction of the Pacific plate underneath South America. The wedge is commonly subdivided into a structurally lower Western Series and an upper Eastern Series. This study shows the progressive development of structures and finite strain from the least deformed rocks in the eastern part of the Eastern Series of the accretionary wedge to higher grade schist of the Western Series at the Pacific coast. Furthermore, this study reports finite-strain data to quantify the contribution of vertical ductile shortening to exhumation. Vertical ductile shortening is, together with erosion and normal faulting, a process that can aid the exhumation of high-pressure rocks. In the east, structures are characterized by upright chevron folds of sedimentary layering which are associated with a penetrative axial-plane foliation, S1. As the F1 folds became slightly overturned to the west, S1 was folded about recumbent open F2 folds and an S2 axial-plane foliation developed. Near the contact between the Western and Eastern Series S2 represents a prominent subhorizontal transposition foliation. Towards the structural deepest units in the west the transposition foliation became progressively flat lying. Finite-strain data as obtained by Rf/Phi and PDS analysis in metagreywacke and X-ray texture goniometry in phyllosilicate-rich rocks show a smooth and gradual increase in strain magnitude from east to west...
abstractGer	Abstract: In this study structural and finite strain data are used to explore the tectonic evolution and the exhumation history of the Chilean accretionary wedge. The Chilean accretionary wedge is part of a Late Paleozoic subduction complex that developed during subduction of the Pacific plate underneath South America. The wedge is commonly subdivided into a structurally lower Western Series and an upper Eastern Series. This study shows the progressive development of structures and finite strain from the least deformed rocks in the eastern part of the Eastern Series of the accretionary wedge to higher grade schist of the Western Series at the Pacific coast. Furthermore, this study reports finite-strain data to quantify the contribution of vertical ductile shortening to exhumation. Vertical ductile shortening is, together with erosion and normal faulting, a process that can aid the exhumation of high-pressure rocks. In the east, structures are characterized by upright chevron folds of sedimentary layering which are associated with a penetrative axial-plane foliation, S1. As the F1 folds became slightly overturned to the west, S1 was folded about recumbent open F2 folds and an S2 axial-plane foliation developed. Near the contact between the Western and Eastern Series S2 represents a prominent subhorizontal transposition foliation. Towards the structural deepest units in the west the transposition foliation became progressively flat lying. Finite-strain data as obtained by Rf/Phi and PDS analysis in metagreywacke and X-ray texture goniometry in phyllosilicate-rich rocks show a smooth and gradual increase in strain magnitude from east to west...
abstract_unstemmed	Abstract: In this study structural and finite strain data are used to explore the tectonic evolution and the exhumation history of the Chilean accretionary wedge. The Chilean accretionary wedge is part of a Late Paleozoic subduction complex that developed during subduction of the Pacific plate underneath South America. The wedge is commonly subdivided into a structurally lower Western Series and an upper Eastern Series. This study shows the progressive development of structures and finite strain from the least deformed rocks in the eastern part of the Eastern Series of the accretionary wedge to higher grade schist of the Western Series at the Pacific coast. Furthermore, this study reports finite-strain data to quantify the contribution of vertical ductile shortening to exhumation. Vertical ductile shortening is, together with erosion and normal faulting, a process that can aid the exhumation of high-pressure rocks. In the east, structures are characterized by upright chevron folds of sedimentary layering which are associated with a penetrative axial-plane foliation, S1. As the F1 folds became slightly overturned to the west, S1 was folded about recumbent open F2 folds and an S2 axial-plane foliation developed. Near the contact between the Western and Eastern Series S2 represents a prominent subhorizontal transposition foliation. Towards the structural deepest units in the west the transposition foliation became progressively flat lying. Finite-strain data as obtained by Rf/Phi and PDS analysis in metagreywacke and X-ray texture goniometry in phyllosilicate-rich rocks show a smooth and gradual increase in strain magnitude from east to west...
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title_short	Structural and strain analysis in the Late Paleozoic coastal accretionary wedge of central Chile
url	http://ubm.opus.hbz-nrw.de/volltexte/2007/1445/pdf/diss.pdf http://ubm.opus.hbz-nrw.de/volltexte/2007/1445/index.html http://d-nb.info/98648394X/34 http://nbn-resolving.de/urn:nbn:de:hebis:77-14450
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Structural and strain analysis in the Late Paleozoic coastal accretionary wedge of central Chile

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