The nature of the tectonic shortening in Central Andes : = Die Beschaffenheit der tektonischen Verkürzung in den Zentralanden

The Andean Cordillera is a mountain range located at the western South American margin and is part of the Eastern- Circum-Pacific orogenic Belt. The ~7000 km long mountain range is one of the longest on Earth and hosts the second largest orogenic plateau in the world, the Altiplano-Puna plateau. The...
Ausführliche Beschreibung

Gespeichert in:

Autor*in:	Pons, Michaël [verfasserIn] Sobolev, Stephan [akademischer betreuerIn] Krüger, Frank [akademischer betreuerIn] Čížková, Hanna [akademischer betreuerIn] Le Breton, Eline [akademischer betreuerIn]
Körperschaften:	Universität Potsdam [Grad-verleihende Institution]
Hochschulschrift:	Dissertation ; Universität Potsdam ; 2023

Format:	E-Book
Sprache:	Englisch

Erschienen:	Potsdam: 2023?

Formangabe:	Hochschulschrift

Anmerkung:	Volltext: PDF kumulative Dissertation Literaturverzeichnis: Seite 139-160 Ort und Tag der Disputation: Potsdam, 17.03.2023
Umfang:	1 Online-Ressource (xvi Seiten, Seite 17-160, 41699 KB) ; Illustrationen, Diagramme, Karten

Weitere Ausgabe:	Erscheint auch als Druck-Ausgabe Pons, Michaël: The nature of the tectonic shortening in Central Andes - Potsdam, 2023

Links:	Link aufrufen Link aufrufen Link aufrufen Link aufrufen Link aufrufen

DOI / URN:	urn:nbn:de:kobv:517-opus4-600892 10.25932/publishup-60089

Katalog-ID:	185898985X

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topic_title	551.8 DE-101 550 DE-101 2027 01 DE-105 00 s ebook The nature of the tectonic shortening in Central Andes = Die Beschaffenheit der tektonischen Verkürzung in den Zentralanden Michaël Pons ; Gutachter*in(nen): Stephan Sobolev, Hanna Čížková, Eline le Breton ; Betreuer: Stephan Sobolev, Frank Krüger
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title_full	The nature of the tectonic shortening in Central Andes = Die Beschaffenheit der tektonischen Verkürzung in den Zentralanden Michaël Pons ; Gutachter*in(nen): Stephan Sobolev, Hanna Čížková, Eline le Breton ; Betreuer: Stephan Sobolev, Frank Krüger
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title_sub	= Die Beschaffenheit der tektonischen Verkürzung in den Zentralanden
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title_sort	nature of the tectonic shortening in central andes = die beschaffenheit der tektonischen verkürzung in den zentralanden
title_auth	The nature of the tectonic shortening in Central Andes = Die Beschaffenheit der tektonischen Verkürzung in den Zentralanden
abstract	The Andean Cordillera is a mountain range located at the western South American margin and is part of the Eastern- Circum-Pacific orogenic Belt. The ~7000 km long mountain range is one of the longest on Earth and hosts the second largest orogenic plateau in the world, the Altiplano-Puna plateau. The Andes are known as a non-collisional subduction-type orogen which developed as a result of the interaction between the subducted oceanic Nazca plate and the South American continental plate. The different Andean segments exhibit along-strike variations of morphotectonic provinces characterized by different elevations, volcanic activity, deformation styles, crustal thickness, shortening magnitude and oceanic plate geometry. Most of the present-day elevation can be explained by crustal shortening in the last ~50 Ma, with the shortening magnitude decreasing from ~300 km in the central (15°S-30°S) segment to less than half that in the southern part (30°S-40°S). Several factors were proposed that might control the magnitude and acceleration of ... Volltext: PDF kumulative Dissertation Literaturverzeichnis: Seite 139-160 Ort und Tag der Disputation: Potsdam, 17.03.2023
abstractGer	The Andean Cordillera is a mountain range located at the western South American margin and is part of the Eastern- Circum-Pacific orogenic Belt. The ~7000 km long mountain range is one of the longest on Earth and hosts the second largest orogenic plateau in the world, the Altiplano-Puna plateau. The Andes are known as a non-collisional subduction-type orogen which developed as a result of the interaction between the subducted oceanic Nazca plate and the South American continental plate. The different Andean segments exhibit along-strike variations of morphotectonic provinces characterized by different elevations, volcanic activity, deformation styles, crustal thickness, shortening magnitude and oceanic plate geometry. Most of the present-day elevation can be explained by crustal shortening in the last ~50 Ma, with the shortening magnitude decreasing from ~300 km in the central (15°S-30°S) segment to less than half that in the southern part (30°S-40°S). Several factors were proposed that might control the magnitude and acceleration of ... Volltext: PDF kumulative Dissertation Literaturverzeichnis: Seite 139-160 Ort und Tag der Disputation: Potsdam, 17.03.2023
abstract_unstemmed	The Andean Cordillera is a mountain range located at the western South American margin and is part of the Eastern- Circum-Pacific orogenic Belt. The ~7000 km long mountain range is one of the longest on Earth and hosts the second largest orogenic plateau in the world, the Altiplano-Puna plateau. The Andes are known as a non-collisional subduction-type orogen which developed as a result of the interaction between the subducted oceanic Nazca plate and the South American continental plate. The different Andean segments exhibit along-strike variations of morphotectonic provinces characterized by different elevations, volcanic activity, deformation styles, crustal thickness, shortening magnitude and oceanic plate geometry. Most of the present-day elevation can be explained by crustal shortening in the last ~50 Ma, with the shortening magnitude decreasing from ~300 km in the central (15°S-30°S) segment to less than half that in the southern part (30°S-40°S). Several factors were proposed that might control the magnitude and acceleration of ... Volltext: PDF kumulative Dissertation Literaturverzeichnis: Seite 139-160 Ort und Tag der Disputation: Potsdam, 17.03.2023
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author2	Sobolev, Stephan Krüger, Frank Čížková, Hanna Le Breton, Eline Universität Potsdam
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allfields	23,O09 dnb 1300440473 DE-101 urn:nbn:de:kobv:517-opus4-600892 urn 10.25932/publishup-60089 doi (DE-627)185898985X (DE-599)DNB1300440473 DE-627 ger DE-627 rda eng XA-DE-BB 551.8 DE-101 550 DE-101 Pons, Michaël verfasserin (DE-588)1302565532 (DE-627)185957095X aut The nature of the tectonic shortening in Central Andes = Die Beschaffenheit der tektonischen Verkürzung in den Zentralanden Michaël Pons ; Gutachter*in(nen): Stephan Sobolev, Hanna Čížková, Eline le Breton ; Betreuer: Stephan Sobolev, Frank Krüger Übersetzung des Haupttitels Die Beschaffenheit der tektonischen Verkürzung in den Zentralanden Die Beschaffenheit der tektonischen Verkürzung in den Zentralanden Potsdam [2023?] 1 Online-Ressource (xvi Seiten, Seite 17-160, 41699 KB) Illustrationen, Diagramme, Karten Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Volltext: PDF kumulative Dissertation Literaturverzeichnis: Seite 139-160 Ort und Tag der Disputation: Potsdam, 17.03.2023 Dissertation Universität Potsdam 2023 kumulative Dissertation The Andean Cordillera is a mountain range located at the western South American margin and is part of the Eastern- Circum-Pacific orogenic Belt. The ~7000 km long mountain range is one of the longest on Earth and hosts the second largest orogenic plateau in the world, the Altiplano-Puna plateau. The Andes are known as a non-collisional subduction-type orogen which developed as a result of the interaction between the subducted oceanic Nazca plate and the South American continental plate. The different Andean segments exhibit along-strike variations of morphotectonic provinces characterized by different elevations, volcanic activity, deformation styles, crustal thickness, shortening magnitude and oceanic plate geometry. Most of the present-day elevation can be explained by crustal shortening in the last ~50 Ma, with the shortening magnitude decreasing from ~300 km in the central (15°S-30°S) segment to less than half that in the southern part (30°S-40°S). Several factors were proposed that might control the magnitude and acceleration of ... Archivierung/Langzeitarchivierung gewährleistet pdager DE-101 Hochschulschrift (DE-588)4113937-9 (DE-627)105825778 (DE-576)209480580 gnd-content Sobolev, Stephan akademischer betreuerin (DE-588)116719490X (DE-627)1030884366 (DE-576)511032412 dgs Krüger, Frank akademischer betreuerin dgs Čížková, Hanna akademischer betreuerin dgs Le Breton, Eline akademischer betreuerin dgs Universität Potsdam Grad-verleihende Institution (DE-588)2120681-8 (DE-627)101653735 (DE-576)193975041 dgg Potsdam (DE-588)4046948-7 (DE-627)106196332 (DE-576)209071575 uvp Erscheint auch als Druck-Ausgabe Pons, Michaël The nature of the tectonic shortening in Central Andes Potsdam, 2023 xvi Seiten, Seite 17-160 (DE-627)1859837158 https://doi.org/10.25932/publishup-60089 Resolving-System kostenfrei https://nbn-resolving.org/urn:nbn:de:kobv:517-opus4-600892 Resolving-System kostenfrei https://d-nb.info/1300440473/34 Langzeitarchivierung Nationalbibliothek kostenfrei https://publishup.uni-potsdam.de/frontdoor/index/index/docId/60089 application/pdf Verlag kostenfrei GBV-ODiss GBV_ILN_20 ISIL_DE-84 SYSFLAG_1 GBV_KXP 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_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_285 ISIL_DE-517 GBV_ILN_293 ISIL_DE-960-3 GBV_ILN_370 ISIL_DE-1373 GBV_ILN_2027 ISIL_DE-105 GBV_ILN_2403 ISIL_DE-LFER BO 20 01 0084 4376357804 x 15-09-23 21 01 0046 4376410934 z 15-09-23 22 01 0018 4376466352 SUBolrd xu 15-09-23 23 01 0830 4376488046 olr-d x 15-09-23 30 01 0104 4376505293 z 15-09-23 40 01 0007 4376524816 xsn 15-09-23 60 01 0705 4376545864 OLRD z 15-09-23 63 01 3401 4376557064 ORD x 15-09-23 70 01 0089 4376571075 zdo 15-09-23 105 01 0841 4376701645 z 15-09-23 110 01 3110 4376588342 x 15-09-23 132 01 0959 4376620998 OLR-DISS x 15-09-23 151 01 0546 4376630322 OLR-ODISS z 15-09-23 161 01 0960 4376642320 ORD z 15-09-23 285 01 0517 437628162X 00 9300 --%%-- s --%%-- ACQ Das E-Book steht unter einer CC-Lizenz. Weitere Informationen finden Sie unter: https://creativecommons.org/licenses/ z 15-09-23 293 01 3293 4376681563 ORD z 15-09-23 370 01 4370 4376684171 x 15-09-23 2027 01 DE-105 4389778552 00 --%%-- Dn --%%-- --%%-- l01 16-10-23 2403 01 DE-LFER 4378016346 00 --%%-- --%%-- n --%%-- l01 20-09-23 20 01 0084 https://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-600892 21 01 0046 https://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-600892 22 01 0018 https://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-600892 23 01 0830 https://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-600892 30 01 0104 https://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-600892 40 01 0007 https://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-600892 60 01 0705 https://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-600892 63 01 3401 E-Book https://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-600892 LF 70 01 0089 https://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-600892 105 01 0841 https://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-600892 110 01 3110 https://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-600892 132 01 0959 https://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-600892 151 01 0546 Volltext https://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-600892 161 01 0960 https://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-600892 285 01 0517 https://doi.org/10.25932/publishup-60089 LF 293 01 3293 https://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-600892 370 01 4370 https://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-600892 2403 01 DE-LFER https://doi.org/10.25932/publishup-60089 2403 01 DE-LFER https://nbn-resolving.org/urn:nbn:de:kobv:517-opus4-600892 2027 01 DE-105 00 s ebook 60 01 0705 10 ho 285 00 DE-517 00 UT 2250 285 00 DE-517 00 TG 4150 285 00 DE-517 00 TP 8925 20 01 0084 OLRD 110 01 3110 OLRD 370 01 4370 OLRD 22 01 0018 SUBolrd 23 01 0830 olr-d 60 01 0705 OLRD 63 01 3401 ORD 132 01 0959 OLR-DISS 151 01 0546 OLR-ODISS 161 01 0960 ORD 285 01 0517 ACQ 293 01 3293 ORD 23 01 0830 2023-09-15:10:10:26
spelling	23,O09 dnb 1300440473 DE-101 urn:nbn:de:kobv:517-opus4-600892 urn 10.25932/publishup-60089 doi (DE-627)185898985X (DE-599)DNB1300440473 DE-627 ger DE-627 rda eng XA-DE-BB 551.8 DE-101 550 DE-101 Pons, Michaël verfasserin (DE-588)1302565532 (DE-627)185957095X aut The nature of the tectonic shortening in Central Andes = Die Beschaffenheit der tektonischen Verkürzung in den Zentralanden Michaël Pons ; Gutachter*in(nen): Stephan Sobolev, Hanna Čížková, Eline le Breton ; Betreuer: Stephan Sobolev, Frank Krüger Übersetzung des Haupttitels Die Beschaffenheit der tektonischen Verkürzung in den Zentralanden Die Beschaffenheit der tektonischen Verkürzung in den Zentralanden Potsdam [2023?] 1 Online-Ressource (xvi Seiten, Seite 17-160, 41699 KB) Illustrationen, Diagramme, Karten Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Volltext: PDF kumulative Dissertation Literaturverzeichnis: Seite 139-160 Ort und Tag der Disputation: Potsdam, 17.03.2023 Dissertation Universität Potsdam 2023 kumulative Dissertation The Andean Cordillera is a mountain range located at the western South American margin and is part of the Eastern- Circum-Pacific orogenic Belt. The ~7000 km long mountain range is one of the longest on Earth and hosts the second largest orogenic plateau in the world, the Altiplano-Puna plateau. The Andes are known as a non-collisional subduction-type orogen which developed as a result of the interaction between the subducted oceanic Nazca plate and the South American continental plate. The different Andean segments exhibit along-strike variations of morphotectonic provinces characterized by different elevations, volcanic activity, deformation styles, crustal thickness, shortening magnitude and oceanic plate geometry. Most of the present-day elevation can be explained by crustal shortening in the last ~50 Ma, with the shortening magnitude decreasing from ~300 km in the central (15°S-30°S) segment to less than half that in the southern part (30°S-40°S). Several factors were proposed that might control the magnitude and acceleration of ... Archivierung/Langzeitarchivierung gewährleistet pdager DE-101 Hochschulschrift (DE-588)4113937-9 (DE-627)105825778 (DE-576)209480580 gnd-content Sobolev, Stephan akademischer betreuerin (DE-588)116719490X (DE-627)1030884366 (DE-576)511032412 dgs Krüger, Frank akademischer betreuerin dgs Čížková, Hanna akademischer betreuerin dgs Le Breton, Eline akademischer betreuerin dgs Universität Potsdam Grad-verleihende Institution (DE-588)2120681-8 (DE-627)101653735 (DE-576)193975041 dgg Potsdam (DE-588)4046948-7 (DE-627)106196332 (DE-576)209071575 uvp Erscheint auch als Druck-Ausgabe Pons, Michaël The nature of the tectonic shortening in Central Andes Potsdam, 2023 xvi Seiten, Seite 17-160 (DE-627)1859837158 https://doi.org/10.25932/publishup-60089 Resolving-System kostenfrei https://nbn-resolving.org/urn:nbn:de:kobv:517-opus4-600892 Resolving-System kostenfrei https://d-nb.info/1300440473/34 Langzeitarchivierung Nationalbibliothek kostenfrei https://publishup.uni-potsdam.de/frontdoor/index/index/docId/60089 application/pdf Verlag kostenfrei GBV-ODiss GBV_ILN_20 ISIL_DE-84 SYSFLAG_1 GBV_KXP 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_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_285 ISIL_DE-517 GBV_ILN_293 ISIL_DE-960-3 GBV_ILN_370 ISIL_DE-1373 GBV_ILN_2027 ISIL_DE-105 GBV_ILN_2403 ISIL_DE-LFER BO 20 01 0084 4376357804 x 15-09-23 21 01 0046 4376410934 z 15-09-23 22 01 0018 4376466352 SUBolrd xu 15-09-23 23 01 0830 4376488046 olr-d x 15-09-23 30 01 0104 4376505293 z 15-09-23 40 01 0007 4376524816 xsn 15-09-23 60 01 0705 4376545864 OLRD z 15-09-23 63 01 3401 4376557064 ORD x 15-09-23 70 01 0089 4376571075 zdo 15-09-23 105 01 0841 4376701645 z 15-09-23 110 01 3110 4376588342 x 15-09-23 132 01 0959 4376620998 OLR-DISS x 15-09-23 151 01 0546 4376630322 OLR-ODISS z 15-09-23 161 01 0960 4376642320 ORD z 15-09-23 285 01 0517 437628162X 00 9300 --%%-- s --%%-- ACQ Das E-Book steht unter einer CC-Lizenz. Weitere Informationen finden Sie unter: https://creativecommons.org/licenses/ z 15-09-23 293 01 3293 4376681563 ORD z 15-09-23 370 01 4370 4376684171 x 15-09-23 2027 01 DE-105 4389778552 00 --%%-- Dn --%%-- --%%-- l01 16-10-23 2403 01 DE-LFER 4378016346 00 --%%-- --%%-- n --%%-- l01 20-09-23 20 01 0084 https://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-600892 21 01 0046 https://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-600892 22 01 0018 https://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-600892 23 01 0830 https://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-600892 30 01 0104 https://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-600892 40 01 0007 https://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-600892 60 01 0705 https://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-600892 63 01 3401 E-Book https://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-600892 LF 70 01 0089 https://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-600892 105 01 0841 https://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-600892 110 01 3110 https://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-600892 132 01 0959 https://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-600892 151 01 0546 Volltext https://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-600892 161 01 0960 https://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-600892 285 01 0517 https://doi.org/10.25932/publishup-60089 LF 293 01 3293 https://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-600892 370 01 4370 https://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-600892 2403 01 DE-LFER https://doi.org/10.25932/publishup-60089 2403 01 DE-LFER https://nbn-resolving.org/urn:nbn:de:kobv:517-opus4-600892 2027 01 DE-105 00 s ebook 60 01 0705 10 ho 285 00 DE-517 00 UT 2250 285 00 DE-517 00 TG 4150 285 00 DE-517 00 TP 8925 20 01 0084 OLRD 110 01 3110 OLRD 370 01 4370 OLRD 22 01 0018 SUBolrd 23 01 0830 olr-d 60 01 0705 OLRD 63 01 3401 ORD 132 01 0959 OLR-DISS 151 01 0546 OLR-ODISS 161 01 0960 ORD 285 01 0517 ACQ 293 01 3293 ORD 23 01 0830 2023-09-15:10:10:26
allfields_unstemmed	23,O09 dnb 1300440473 DE-101 urn:nbn:de:kobv:517-opus4-600892 urn 10.25932/publishup-60089 doi (DE-627)185898985X (DE-599)DNB1300440473 DE-627 ger DE-627 rda eng XA-DE-BB 551.8 DE-101 550 DE-101 Pons, Michaël verfasserin (DE-588)1302565532 (DE-627)185957095X aut The nature of the tectonic shortening in Central Andes = Die Beschaffenheit der tektonischen Verkürzung in den Zentralanden Michaël Pons ; Gutachter*in(nen): Stephan Sobolev, Hanna Čížková, Eline le Breton ; Betreuer: Stephan Sobolev, Frank Krüger Übersetzung des Haupttitels Die Beschaffenheit der tektonischen Verkürzung in den Zentralanden Die Beschaffenheit der tektonischen Verkürzung in den Zentralanden Potsdam [2023?] 1 Online-Ressource (xvi Seiten, Seite 17-160, 41699 KB) Illustrationen, Diagramme, Karten Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Volltext: PDF kumulative Dissertation Literaturverzeichnis: Seite 139-160 Ort und Tag der Disputation: Potsdam, 17.03.2023 Dissertation Universität Potsdam 2023 kumulative Dissertation The Andean Cordillera is a mountain range located at the western South American margin and is part of the Eastern- Circum-Pacific orogenic Belt. The ~7000 km long mountain range is one of the longest on Earth and hosts the second largest orogenic plateau in the world, the Altiplano-Puna plateau. The Andes are known as a non-collisional subduction-type orogen which developed as a result of the interaction between the subducted oceanic Nazca plate and the South American continental plate. The different Andean segments exhibit along-strike variations of morphotectonic provinces characterized by different elevations, volcanic activity, deformation styles, crustal thickness, shortening magnitude and oceanic plate geometry. Most of the present-day elevation can be explained by crustal shortening in the last ~50 Ma, with the shortening magnitude decreasing from ~300 km in the central (15°S-30°S) segment to less than half that in the southern part (30°S-40°S). Several factors were proposed that might control the magnitude and acceleration of ... Archivierung/Langzeitarchivierung gewährleistet pdager DE-101 Hochschulschrift (DE-588)4113937-9 (DE-627)105825778 (DE-576)209480580 gnd-content Sobolev, Stephan akademischer betreuerin (DE-588)116719490X (DE-627)1030884366 (DE-576)511032412 dgs Krüger, Frank akademischer betreuerin dgs Čížková, Hanna akademischer betreuerin dgs Le Breton, Eline akademischer betreuerin dgs Universität Potsdam Grad-verleihende Institution (DE-588)2120681-8 (DE-627)101653735 (DE-576)193975041 dgg Potsdam (DE-588)4046948-7 (DE-627)106196332 (DE-576)209071575 uvp Erscheint auch als Druck-Ausgabe Pons, Michaël The nature of the tectonic shortening in Central Andes Potsdam, 2023 xvi Seiten, Seite 17-160 (DE-627)1859837158 https://doi.org/10.25932/publishup-60089 Resolving-System kostenfrei https://nbn-resolving.org/urn:nbn:de:kobv:517-opus4-600892 Resolving-System kostenfrei https://d-nb.info/1300440473/34 Langzeitarchivierung Nationalbibliothek kostenfrei https://publishup.uni-potsdam.de/frontdoor/index/index/docId/60089 application/pdf Verlag kostenfrei GBV-ODiss GBV_ILN_20 ISIL_DE-84 SYSFLAG_1 GBV_KXP 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_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_285 ISIL_DE-517 GBV_ILN_293 ISIL_DE-960-3 GBV_ILN_370 ISIL_DE-1373 GBV_ILN_2027 ISIL_DE-105 GBV_ILN_2403 ISIL_DE-LFER BO 20 01 0084 4376357804 x 15-09-23 21 01 0046 4376410934 z 15-09-23 22 01 0018 4376466352 SUBolrd xu 15-09-23 23 01 0830 4376488046 olr-d x 15-09-23 30 01 0104 4376505293 z 15-09-23 40 01 0007 4376524816 xsn 15-09-23 60 01 0705 4376545864 OLRD z 15-09-23 63 01 3401 4376557064 ORD x 15-09-23 70 01 0089 4376571075 zdo 15-09-23 105 01 0841 4376701645 z 15-09-23 110 01 3110 4376588342 x 15-09-23 132 01 0959 4376620998 OLR-DISS x 15-09-23 151 01 0546 4376630322 OLR-ODISS z 15-09-23 161 01 0960 4376642320 ORD z 15-09-23 285 01 0517 437628162X 00 9300 --%%-- s --%%-- ACQ Das E-Book steht unter einer CC-Lizenz. Weitere Informationen finden Sie unter: https://creativecommons.org/licenses/ z 15-09-23 293 01 3293 4376681563 ORD z 15-09-23 370 01 4370 4376684171 x 15-09-23 2027 01 DE-105 4389778552 00 --%%-- Dn --%%-- --%%-- l01 16-10-23 2403 01 DE-LFER 4378016346 00 --%%-- --%%-- n --%%-- l01 20-09-23 20 01 0084 https://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-600892 21 01 0046 https://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-600892 22 01 0018 https://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-600892 23 01 0830 https://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-600892 30 01 0104 https://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-600892 40 01 0007 https://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-600892 60 01 0705 https://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-600892 63 01 3401 E-Book https://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-600892 LF 70 01 0089 https://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-600892 105 01 0841 https://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-600892 110 01 3110 https://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-600892 132 01 0959 https://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-600892 151 01 0546 Volltext https://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-600892 161 01 0960 https://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-600892 285 01 0517 https://doi.org/10.25932/publishup-60089 LF 293 01 3293 https://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-600892 370 01 4370 https://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-600892 2403 01 DE-LFER https://doi.org/10.25932/publishup-60089 2403 01 DE-LFER https://nbn-resolving.org/urn:nbn:de:kobv:517-opus4-600892 2027 01 DE-105 00 s ebook 60 01 0705 10 ho 285 00 DE-517 00 UT 2250 285 00 DE-517 00 TG 4150 285 00 DE-517 00 TP 8925 20 01 0084 OLRD 110 01 3110 OLRD 370 01 4370 OLRD 22 01 0018 SUBolrd 23 01 0830 olr-d 60 01 0705 OLRD 63 01 3401 ORD 132 01 0959 OLR-DISS 151 01 0546 OLR-ODISS 161 01 0960 ORD 285 01 0517 ACQ 293 01 3293 ORD 23 01 0830 2023-09-15:10:10:26
allfieldsGer	23,O09 dnb 1300440473 DE-101 urn:nbn:de:kobv:517-opus4-600892 urn 10.25932/publishup-60089 doi (DE-627)185898985X (DE-599)DNB1300440473 DE-627 ger DE-627 rda eng XA-DE-BB 551.8 DE-101 550 DE-101 Pons, Michaël verfasserin (DE-588)1302565532 (DE-627)185957095X aut The nature of the tectonic shortening in Central Andes = Die Beschaffenheit der tektonischen Verkürzung in den Zentralanden Michaël Pons ; Gutachter*in(nen): Stephan Sobolev, Hanna Čížková, Eline le Breton ; Betreuer: Stephan Sobolev, Frank Krüger Übersetzung des Haupttitels Die Beschaffenheit der tektonischen Verkürzung in den Zentralanden Die Beschaffenheit der tektonischen Verkürzung in den Zentralanden Potsdam [2023?] 1 Online-Ressource (xvi Seiten, Seite 17-160, 41699 KB) Illustrationen, Diagramme, Karten Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Volltext: PDF kumulative Dissertation Literaturverzeichnis: Seite 139-160 Ort und Tag der Disputation: Potsdam, 17.03.2023 Dissertation Universität Potsdam 2023 kumulative Dissertation The Andean Cordillera is a mountain range located at the western South American margin and is part of the Eastern- Circum-Pacific orogenic Belt. The ~7000 km long mountain range is one of the longest on Earth and hosts the second largest orogenic plateau in the world, the Altiplano-Puna plateau. The Andes are known as a non-collisional subduction-type orogen which developed as a result of the interaction between the subducted oceanic Nazca plate and the South American continental plate. The different Andean segments exhibit along-strike variations of morphotectonic provinces characterized by different elevations, volcanic activity, deformation styles, crustal thickness, shortening magnitude and oceanic plate geometry. Most of the present-day elevation can be explained by crustal shortening in the last ~50 Ma, with the shortening magnitude decreasing from ~300 km in the central (15°S-30°S) segment to less than half that in the southern part (30°S-40°S). Several factors were proposed that might control the magnitude and acceleration of ... Archivierung/Langzeitarchivierung gewährleistet pdager DE-101 Hochschulschrift (DE-588)4113937-9 (DE-627)105825778 (DE-576)209480580 gnd-content Sobolev, Stephan akademischer betreuerin (DE-588)116719490X (DE-627)1030884366 (DE-576)511032412 dgs Krüger, Frank akademischer betreuerin dgs Čížková, Hanna akademischer betreuerin dgs Le Breton, Eline akademischer betreuerin dgs Universität Potsdam Grad-verleihende Institution (DE-588)2120681-8 (DE-627)101653735 (DE-576)193975041 dgg Potsdam (DE-588)4046948-7 (DE-627)106196332 (DE-576)209071575 uvp Erscheint auch als Druck-Ausgabe Pons, Michaël The nature of the tectonic shortening in Central Andes Potsdam, 2023 xvi Seiten, Seite 17-160 (DE-627)1859837158 https://doi.org/10.25932/publishup-60089 Resolving-System kostenfrei https://nbn-resolving.org/urn:nbn:de:kobv:517-opus4-600892 Resolving-System kostenfrei https://d-nb.info/1300440473/34 Langzeitarchivierung Nationalbibliothek kostenfrei https://publishup.uni-potsdam.de/frontdoor/index/index/docId/60089 application/pdf Verlag kostenfrei GBV-ODiss GBV_ILN_20 ISIL_DE-84 SYSFLAG_1 GBV_KXP 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_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_285 ISIL_DE-517 GBV_ILN_293 ISIL_DE-960-3 GBV_ILN_370 ISIL_DE-1373 GBV_ILN_2027 ISIL_DE-105 GBV_ILN_2403 ISIL_DE-LFER BO 20 01 0084 4376357804 x 15-09-23 21 01 0046 4376410934 z 15-09-23 22 01 0018 4376466352 SUBolrd xu 15-09-23 23 01 0830 4376488046 olr-d x 15-09-23 30 01 0104 4376505293 z 15-09-23 40 01 0007 4376524816 xsn 15-09-23 60 01 0705 4376545864 OLRD z 15-09-23 63 01 3401 4376557064 ORD x 15-09-23 70 01 0089 4376571075 zdo 15-09-23 105 01 0841 4376701645 z 15-09-23 110 01 3110 4376588342 x 15-09-23 132 01 0959 4376620998 OLR-DISS x 15-09-23 151 01 0546 4376630322 OLR-ODISS z 15-09-23 161 01 0960 4376642320 ORD z 15-09-23 285 01 0517 437628162X 00 9300 --%%-- s --%%-- ACQ Das E-Book steht unter einer CC-Lizenz. 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allfieldsSound	23,O09 dnb 1300440473 DE-101 urn:nbn:de:kobv:517-opus4-600892 urn 10.25932/publishup-60089 doi (DE-627)185898985X (DE-599)DNB1300440473 DE-627 ger DE-627 rda eng XA-DE-BB 551.8 DE-101 550 DE-101 Pons, Michaël verfasserin (DE-588)1302565532 (DE-627)185957095X aut The nature of the tectonic shortening in Central Andes = Die Beschaffenheit der tektonischen Verkürzung in den Zentralanden Michaël Pons ; Gutachter*in(nen): Stephan Sobolev, Hanna Čížková, Eline le Breton ; Betreuer: Stephan Sobolev, Frank Krüger Übersetzung des Haupttitels Die Beschaffenheit der tektonischen Verkürzung in den Zentralanden Die Beschaffenheit der tektonischen Verkürzung in den Zentralanden Potsdam [2023?] 1 Online-Ressource (xvi Seiten, Seite 17-160, 41699 KB) Illustrationen, Diagramme, Karten Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Volltext: PDF kumulative Dissertation Literaturverzeichnis: Seite 139-160 Ort und Tag der Disputation: Potsdam, 17.03.2023 Dissertation Universität Potsdam 2023 kumulative Dissertation The Andean Cordillera is a mountain range located at the western South American margin and is part of the Eastern- Circum-Pacific orogenic Belt. The ~7000 km long mountain range is one of the longest on Earth and hosts the second largest orogenic plateau in the world, the Altiplano-Puna plateau. The Andes are known as a non-collisional subduction-type orogen which developed as a result of the interaction between the subducted oceanic Nazca plate and the South American continental plate. The different Andean segments exhibit along-strike variations of morphotectonic provinces characterized by different elevations, volcanic activity, deformation styles, crustal thickness, shortening magnitude and oceanic plate geometry. Most of the present-day elevation can be explained by crustal shortening in the last ~50 Ma, with the shortening magnitude decreasing from ~300 km in the central (15°S-30°S) segment to less than half that in the southern part (30°S-40°S). Several factors were proposed that might control the magnitude and acceleration of ... Archivierung/Langzeitarchivierung gewährleistet pdager DE-101 Hochschulschrift (DE-588)4113937-9 (DE-627)105825778 (DE-576)209480580 gnd-content Sobolev, Stephan akademischer betreuerin (DE-588)116719490X (DE-627)1030884366 (DE-576)511032412 dgs Krüger, Frank akademischer betreuerin dgs Čížková, Hanna akademischer betreuerin dgs Le Breton, Eline akademischer betreuerin dgs Universität Potsdam Grad-verleihende Institution (DE-588)2120681-8 (DE-627)101653735 (DE-576)193975041 dgg Potsdam (DE-588)4046948-7 (DE-627)106196332 (DE-576)209071575 uvp Erscheint auch als Druck-Ausgabe Pons, Michaël The nature of the tectonic shortening in Central Andes Potsdam, 2023 xvi Seiten, Seite 17-160 (DE-627)1859837158 https://doi.org/10.25932/publishup-60089 Resolving-System kostenfrei https://nbn-resolving.org/urn:nbn:de:kobv:517-opus4-600892 Resolving-System kostenfrei https://d-nb.info/1300440473/34 Langzeitarchivierung Nationalbibliothek kostenfrei https://publishup.uni-potsdam.de/frontdoor/index/index/docId/60089 application/pdf Verlag kostenfrei GBV-ODiss GBV_ILN_20 ISIL_DE-84 SYSFLAG_1 GBV_KXP 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_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_285 ISIL_DE-517 GBV_ILN_293 ISIL_DE-960-3 GBV_ILN_370 ISIL_DE-1373 GBV_ILN_2027 ISIL_DE-105 GBV_ILN_2403 ISIL_DE-LFER BO 20 01 0084 4376357804 x 15-09-23 21 01 0046 4376410934 z 15-09-23 22 01 0018 4376466352 SUBolrd xu 15-09-23 23 01 0830 4376488046 olr-d x 15-09-23 30 01 0104 4376505293 z 15-09-23 40 01 0007 4376524816 xsn 15-09-23 60 01 0705 4376545864 OLRD z 15-09-23 63 01 3401 4376557064 ORD x 15-09-23 70 01 0089 4376571075 zdo 15-09-23 105 01 0841 4376701645 z 15-09-23 110 01 3110 4376588342 x 15-09-23 132 01 0959 4376620998 OLR-DISS x 15-09-23 151 01 0546 4376630322 OLR-ODISS z 15-09-23 161 01 0960 4376642320 ORD z 15-09-23 285 01 0517 437628162X 00 9300 --%%-- s --%%-- ACQ Das E-Book steht unter einer CC-Lizenz. 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title	The nature of the tectonic shortening in Central Andes = Die Beschaffenheit der tektonischen Verkürzung in den Zentralanden
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physical	1 Online-Ressource (xvi Seiten, Seite 17-160, 41699 KB) Illustrationen, Diagramme, Karten
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title_short	The nature of the tectonic shortening in Central Andes
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GND_txt_mv	Pons, Michael Pons, Michaël Hochschulschrift Sobolev, S. Sobolev, Stephan V. Sobolev, S. V. Sobolev, Stephan Vladimir Sobolev, Stephan Uni Potsdam Potsdamer Universität Univ. Potsdam University of Potsdam Universität Potsdam Bostanium Postampium Poztupimi Potzdam Bostampium Potsdamum State Capital of Potsdam Stadtgemeinde Potsdam Residenzstadt Potsdam Potestampium Potsdam-Sanssouci Pozdam Potsdamm Landeshauptstadt Potsdam Potsdam
GND_txtF_mv	Pons, Michael Pons, Michaël Hochschulschrift Sobolev, S. Sobolev, Stephan V. Sobolev, S. V. Sobolev, Stephan Vladimir Sobolev, Stephan Uni Potsdam Potsdamer Universität Univ. Potsdam University of Potsdam Universität Potsdam Bostanium Postampium Poztupimi Potzdam Bostampium Potsdamum State Capital of Potsdam Stadtgemeinde Potsdam Residenzstadt Potsdam Potestampium Potsdam-Sanssouci Pozdam Potsdamm Landeshauptstadt Potsdam Potsdam
title_alt	Die Beschaffenheit der tektonischen Verkürzung in den Zentralanden
doi_str	10.25932/publishup-60089
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up_date	2024-07-04T13:26:29.426Z
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The nature of the tectonic shortening in Central Andes : = Die Beschaffenheit der tektonischen Verkürzung in den Zentralanden

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