Structural and morphotectonic evolution of the Sierras Pampeanas (Argentina) constrained by a multithermochronometer approach

Die Sierras Pampeanas in Zentral- und Nordwestargentinien stellen ein ausgeprägtes morphotektonisches Merkmal im Bereich der flach subduzierenden Nazca Platte unter die Südamerikanische Platte zwischen ~27° S und ~33° S dar. Diese flache Subduktion wurde bisher als Ursache für die Heraushebung und D...
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Autor*in:	Löbens, Stefan [verfasserIn] Siegesmund, Siegfried, [betreuer] Siegesmund, Siegfried, [gutachter] Sobel, Edward [gutachter]
Hochschulschrift:	Göttingen, Univ., Diss., 2012

Format:	E-Book
Sprache:	Englisch

Erschienen:	2012

Formangabe:	Hochschulschrift

Umfang:	Online-Ressource (PDF-Datei: 645 MB)

Weitere Ausgabe:	Erscheint auch als Druck-Ausgabe Löbens, Stefan: Structural and morphotectonic evolution of the Sierras Pampeanas (Argentina) constrained by a multithermochronometer approach - 2012

Links:	Link aufrufen jump-off jump-off Volltext Volltext

DOI / URN:	urn:nbn:de:gbv:7-11858/00-1735-0000-0015-A35E-A-2

Katalog-ID:	746434480

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Auf Basis von Apatit Spaltspurendatierungen, Zirkon und Apatit (U-Th)/He Thermochronometern sowie K-Ar Datierungen von Störungsletten werden in der vorliegenden Arbeit neue thermochronologische Daten vorgest... The Sierras Pampeanas in central and northwestern Argentina constitute a distinct morphotectonic feature above the shallow subducting Nazca Plate beneath the South American Plate between ~27 ° S and ~33° S. Uplift and deformation of the mountain ranges within this area are interpreted to be closely related to this flat-slab subduction during the Neogene. New thermochronological data, derived from application of the apatite fission-track, zircon and apatite (U-Th)/He thermochronometers as well as from K-Ar dating of fault gouges, presented in this thesis, reveal new and improved insights of ... Langzeitarchivierung gewährleistet pdager Hochschulschrift (DE-588)4113937-9 (DE-627)105825778 (DE-576)209480580 gnd-content Siegesmund, Siegfried, betreuer oth Siegesmund, Siegfried, gutachter oth Sobel, Edward gutachter oth Göttingen uvp Erscheint auch als Druck-Ausgabe Löbens, Stefan Structural and morphotectonic evolution of the Sierras Pampeanas (Argentina) constrained by a multithermochronometer approach 2012 v, 167 Bl. 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spelling	13,O12 dnb 104430667X DE-101 urn:nbn:de:gbv:7-11858/00-1735-0000-0015-A35E-A-2 urn (DE-627)746434480 (DE-576)9746434489 (DE-599)GBV746434480 (OCoLC)864735224 DE-627 ger DE-627 rakwb eng XA-DE-NI 910 550 22 Löbens, Stefan verfasserin aut Structural and morphotectonic evolution of the Sierras Pampeanas (Argentina) constrained by a multithermochronometer approach vorgelegt von Stefan Löbens 2012 Online-Ressource (PDF-Datei: 645 MB) Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Göttingen, Univ., Diss., 2012 Die Sierras Pampeanas in Zentral- und Nordwestargentinien stellen ein ausgeprägtes morphotektonisches Merkmal im Bereich der flach subduzierenden Nazca Platte unter die Südamerikanische Platte zwischen ~27° S und ~33° S dar. Diese flache Subduktion wurde bisher als Ursache für die Heraushebung und Deformation von Höhenzügen innerhalb der Sierras Pampeanas während des Neogens angenommen. Auf Basis von Apatit Spaltspurendatierungen, Zirkon und Apatit (U-Th)/He Thermochronometern sowie K-Ar Datierungen von Störungsletten werden in der vorliegenden Arbeit neue thermochronologische Daten vorgest... The Sierras Pampeanas in central and northwestern Argentina constitute a distinct morphotectonic feature above the shallow subducting Nazca Plate beneath the South American Plate between ~27 ° S and ~33° S. Uplift and deformation of the mountain ranges within this area are interpreted to be closely related to this flat-slab subduction during the Neogene. New thermochronological data, derived from application of the apatite fission-track, zircon and apatite (U-Th)/He thermochronometers as well as from K-Ar dating of fault gouges, presented in this thesis, reveal new and improved insights of ... Langzeitarchivierung gewährleistet pdager Hochschulschrift (DE-588)4113937-9 (DE-627)105825778 (DE-576)209480580 gnd-content Siegesmund, Siegfried, betreuer oth Siegesmund, Siegfried, gutachter oth Sobel, Edward gutachter oth Göttingen uvp Erscheint auch als Druck-Ausgabe Löbens, Stefan Structural and morphotectonic evolution of the Sierras Pampeanas (Argentina) constrained by a multithermochronometer approach 2012 v, 167 Bl. (DE-627)755690079 http://hdl.handle.net/11858/00-1735-0000-0015-A35E-A text/html Resolving-System jump-off kostenfrei Volltext http://nbn-resolving.de/urn:nbn:de:gbv:7-11858/00-1735-0000-0015-A35E-A-2 text/html Resolving-System jump-off Volltext http://nbn-resolving.de/urn:nbn:de:gbv:7-11858/00-1735-0000-0015-A35E-A-2 2013-12-04 Resolving-System Volltext http://d-nb.info/104430667X/34 2013-12-04 Langzeitarchivierung Nationalbibliothek Volltext GBV-ODiss GBV_ILN_20 ISIL_DE-84 SYSFLAG_1 GBV_KXP SSG-OPC-GEO 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_105 ISIL_DE-841 GBV_ILN_110 ISIL_DE-Luen4 GBV_ILN_132 ISIL_DE-959 GBV_ILN_161 ISIL_DE-960 GBV_ILN_293 ISIL_DE-960-3 GBV_ILN_370 ISIL_DE-1373 GBV_ILN_2403 ISIL_DE-LFER BO 045F 910 20 01 0084 1461957575 x 08-03-14 21 01 0046 1462023363 z 08-03-14 22 01 0018 1462089054 SUBolrd xu 08-03-14 23 01 0830 1787697614 olr-d x 26-07-18 30 01 0104 1787776506 z 26-07-18 40 01 0007 1391058321 ediss xsn 22-05-13 60 01 0705 1462254179 OLRD z 08-03-14 63 01 3401 1787879119 ORD x 26-07-18 105 01 0841 1596281545 z 21-01-16 110 01 3110 1462310931 x 08-03-14 132 01 0959 1591397146 OLR-DISS x 19-12-15 161 01 0960 1597609951 ORD x 28-01-16 293 01 3293 1598108026 ORD xf 28-01-16 370 01 4370 1788112997 x 26-07-18 2403 01 DE-LFER 3495056211 00 --%%-- --%%-- n --%%-- l01 19-07-19 20 01 0084 http://nbn-resolving.de/urn:nbn:de:gbv:7-11858/00-1735-0000-0015-A35E-A-2 21 01 0046 http://nbn-resolving.de/urn:nbn:de:gbv:7-11858/00-1735-0000-0015-A35E-A-2 22 01 0018 http://nbn-resolving.de/urn:nbn:de:gbv:7-11858/00-1735-0000-0015-A35E-A-2 23 01 0830 http://nbn-resolving.de/urn:nbn:de:gbv:7-11858/00-1735-0000-0015-A35E-A-2 30 01 0104 http://nbn-resolving.de/urn:nbn:de:gbv:7-11858/00-1735-0000-0015-A35E-A-2 60 01 0705 http://nbn-resolving.de/urn:nbn:de:gbv:7-11858/00-1735-0000-0015-A35E-A-2 63 01 3401 E-Book http://nbn-resolving.de/urn:nbn:de:gbv:7-11858/00-1735-0000-0015-A35E-A-2 LF 105 01 0841 http://nbn-resolving.de/urn:nbn:de:gbv:7-11858/00-1735-0000-0015-A35E-A-2 110 01 3110 http://nbn-resolving.de/urn:nbn:de:gbv:7-11858/00-1735-0000-0015-A35E-A-2 132 01 0959 http://nbn-resolving.de/urn:nbn:de:gbv:7-11858/00-1735-0000-0015-A35E-A-2 161 01 0960 http://nbn-resolving.de/urn:nbn:de:gbv:7-11858/00-1735-0000-0015-A35E-A-2 293 01 3293 http://nbn-resolving.de/urn:nbn:de:gbv:7-11858/00-1735-0000-0015-A35E-A-2 370 01 4370 http://nbn-resolving.de/urn:nbn:de:gbv:7-11858/00-1735-0000-0015-A35E-A-2 2403 01 DE-LFER http://hdl.handle.net/11858/00-1735-0000-0015-A35E-A 40 00 DE-7 00 (DE-627)625047834 VBN 500 Geochronologie einzelner Regionen 40 00 DE-7 01 (DE-627)625046226 VAE 811 Alpidische Orogene {Tektonik} 40 00 DE-7 02 (DE-627)625052684 VEX 200 Argentinien {Geologie} 60 01 0705 10 ho 20 01 0084 OLRD 110 01 3110 OLRD 370 01 4370 OLRD 22 01 0018 SUBolrd 23 01 0830 olr-d 40 01 0007 ediss 60 01 0705 OLRD 63 01 3401 ORD 132 01 0959 OLR-DISS 161 01 0960 ORD 293 01 3293 ORD 23 01 0830 2018-07-26:10:53:10
allfields_unstemmed	13,O12 dnb 104430667X DE-101 urn:nbn:de:gbv:7-11858/00-1735-0000-0015-A35E-A-2 urn (DE-627)746434480 (DE-576)9746434489 (DE-599)GBV746434480 (OCoLC)864735224 DE-627 ger DE-627 rakwb eng XA-DE-NI 910 550 22 Löbens, Stefan verfasserin aut Structural and morphotectonic evolution of the Sierras Pampeanas (Argentina) constrained by a multithermochronometer approach vorgelegt von Stefan Löbens 2012 Online-Ressource (PDF-Datei: 645 MB) Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Göttingen, Univ., Diss., 2012 Die Sierras Pampeanas in Zentral- und Nordwestargentinien stellen ein ausgeprägtes morphotektonisches Merkmal im Bereich der flach subduzierenden Nazca Platte unter die Südamerikanische Platte zwischen ~27° S und ~33° S dar. Diese flache Subduktion wurde bisher als Ursache für die Heraushebung und Deformation von Höhenzügen innerhalb der Sierras Pampeanas während des Neogens angenommen. Auf Basis von Apatit Spaltspurendatierungen, Zirkon und Apatit (U-Th)/He Thermochronometern sowie K-Ar Datierungen von Störungsletten werden in der vorliegenden Arbeit neue thermochronologische Daten vorgest... The Sierras Pampeanas in central and northwestern Argentina constitute a distinct morphotectonic feature above the shallow subducting Nazca Plate beneath the South American Plate between ~27 ° S and ~33° S. Uplift and deformation of the mountain ranges within this area are interpreted to be closely related to this flat-slab subduction during the Neogene. New thermochronological data, derived from application of the apatite fission-track, zircon and apatite (U-Th)/He thermochronometers as well as from K-Ar dating of fault gouges, presented in this thesis, reveal new and improved insights of ... Langzeitarchivierung gewährleistet pdager Hochschulschrift (DE-588)4113937-9 (DE-627)105825778 (DE-576)209480580 gnd-content Siegesmund, Siegfried, betreuer oth Siegesmund, Siegfried, gutachter oth Sobel, Edward gutachter oth Göttingen uvp Erscheint auch als Druck-Ausgabe Löbens, Stefan Structural and morphotectonic evolution of the Sierras Pampeanas (Argentina) constrained by a multithermochronometer approach 2012 v, 167 Bl. (DE-627)755690079 http://hdl.handle.net/11858/00-1735-0000-0015-A35E-A text/html Resolving-System jump-off kostenfrei Volltext http://nbn-resolving.de/urn:nbn:de:gbv:7-11858/00-1735-0000-0015-A35E-A-2 text/html Resolving-System jump-off Volltext http://nbn-resolving.de/urn:nbn:de:gbv:7-11858/00-1735-0000-0015-A35E-A-2 2013-12-04 Resolving-System Volltext http://d-nb.info/104430667X/34 2013-12-04 Langzeitarchivierung Nationalbibliothek Volltext GBV-ODiss GBV_ILN_20 ISIL_DE-84 SYSFLAG_1 GBV_KXP SSG-OPC-GEO 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_105 ISIL_DE-841 GBV_ILN_110 ISIL_DE-Luen4 GBV_ILN_132 ISIL_DE-959 GBV_ILN_161 ISIL_DE-960 GBV_ILN_293 ISIL_DE-960-3 GBV_ILN_370 ISIL_DE-1373 GBV_ILN_2403 ISIL_DE-LFER BO 045F 910 20 01 0084 1461957575 x 08-03-14 21 01 0046 1462023363 z 08-03-14 22 01 0018 1462089054 SUBolrd xu 08-03-14 23 01 0830 1787697614 olr-d x 26-07-18 30 01 0104 1787776506 z 26-07-18 40 01 0007 1391058321 ediss xsn 22-05-13 60 01 0705 1462254179 OLRD z 08-03-14 63 01 3401 1787879119 ORD x 26-07-18 105 01 0841 1596281545 z 21-01-16 110 01 3110 1462310931 x 08-03-14 132 01 0959 1591397146 OLR-DISS x 19-12-15 161 01 0960 1597609951 ORD x 28-01-16 293 01 3293 1598108026 ORD xf 28-01-16 370 01 4370 1788112997 x 26-07-18 2403 01 DE-LFER 3495056211 00 --%%-- --%%-- n --%%-- l01 19-07-19 20 01 0084 http://nbn-resolving.de/urn:nbn:de:gbv:7-11858/00-1735-0000-0015-A35E-A-2 21 01 0046 http://nbn-resolving.de/urn:nbn:de:gbv:7-11858/00-1735-0000-0015-A35E-A-2 22 01 0018 http://nbn-resolving.de/urn:nbn:de:gbv:7-11858/00-1735-0000-0015-A35E-A-2 23 01 0830 http://nbn-resolving.de/urn:nbn:de:gbv:7-11858/00-1735-0000-0015-A35E-A-2 30 01 0104 http://nbn-resolving.de/urn:nbn:de:gbv:7-11858/00-1735-0000-0015-A35E-A-2 60 01 0705 http://nbn-resolving.de/urn:nbn:de:gbv:7-11858/00-1735-0000-0015-A35E-A-2 63 01 3401 E-Book http://nbn-resolving.de/urn:nbn:de:gbv:7-11858/00-1735-0000-0015-A35E-A-2 LF 105 01 0841 http://nbn-resolving.de/urn:nbn:de:gbv:7-11858/00-1735-0000-0015-A35E-A-2 110 01 3110 http://nbn-resolving.de/urn:nbn:de:gbv:7-11858/00-1735-0000-0015-A35E-A-2 132 01 0959 http://nbn-resolving.de/urn:nbn:de:gbv:7-11858/00-1735-0000-0015-A35E-A-2 161 01 0960 http://nbn-resolving.de/urn:nbn:de:gbv:7-11858/00-1735-0000-0015-A35E-A-2 293 01 3293 http://nbn-resolving.de/urn:nbn:de:gbv:7-11858/00-1735-0000-0015-A35E-A-2 370 01 4370 http://nbn-resolving.de/urn:nbn:de:gbv:7-11858/00-1735-0000-0015-A35E-A-2 2403 01 DE-LFER http://hdl.handle.net/11858/00-1735-0000-0015-A35E-A 40 00 DE-7 00 (DE-627)625047834 VBN 500 Geochronologie einzelner Regionen 40 00 DE-7 01 (DE-627)625046226 VAE 811 Alpidische Orogene {Tektonik} 40 00 DE-7 02 (DE-627)625052684 VEX 200 Argentinien {Geologie} 60 01 0705 10 ho 20 01 0084 OLRD 110 01 3110 OLRD 370 01 4370 OLRD 22 01 0018 SUBolrd 23 01 0830 olr-d 40 01 0007 ediss 60 01 0705 OLRD 63 01 3401 ORD 132 01 0959 OLR-DISS 161 01 0960 ORD 293 01 3293 ORD 23 01 0830 2018-07-26:10:53:10
allfieldsGer	13,O12 dnb 104430667X DE-101 urn:nbn:de:gbv:7-11858/00-1735-0000-0015-A35E-A-2 urn (DE-627)746434480 (DE-576)9746434489 (DE-599)GBV746434480 (OCoLC)864735224 DE-627 ger DE-627 rakwb eng XA-DE-NI 910 550 22 Löbens, Stefan verfasserin aut Structural and morphotectonic evolution of the Sierras Pampeanas (Argentina) constrained by a multithermochronometer approach vorgelegt von Stefan Löbens 2012 Online-Ressource (PDF-Datei: 645 MB) Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Göttingen, Univ., Diss., 2012 Die Sierras Pampeanas in Zentral- und Nordwestargentinien stellen ein ausgeprägtes morphotektonisches Merkmal im Bereich der flach subduzierenden Nazca Platte unter die Südamerikanische Platte zwischen ~27° S und ~33° S dar. Diese flache Subduktion wurde bisher als Ursache für die Heraushebung und Deformation von Höhenzügen innerhalb der Sierras Pampeanas während des Neogens angenommen. Auf Basis von Apatit Spaltspurendatierungen, Zirkon und Apatit (U-Th)/He Thermochronometern sowie K-Ar Datierungen von Störungsletten werden in der vorliegenden Arbeit neue thermochronologische Daten vorgest... The Sierras Pampeanas in central and northwestern Argentina constitute a distinct morphotectonic feature above the shallow subducting Nazca Plate beneath the South American Plate between ~27 ° S and ~33° S. Uplift and deformation of the mountain ranges within this area are interpreted to be closely related to this flat-slab subduction during the Neogene. New thermochronological data, derived from application of the apatite fission-track, zircon and apatite (U-Th)/He thermochronometers as well as from K-Ar dating of fault gouges, presented in this thesis, reveal new and improved insights of ... Langzeitarchivierung gewährleistet pdager Hochschulschrift (DE-588)4113937-9 (DE-627)105825778 (DE-576)209480580 gnd-content Siegesmund, Siegfried, betreuer oth Siegesmund, Siegfried, gutachter oth Sobel, Edward gutachter oth Göttingen uvp Erscheint auch als Druck-Ausgabe Löbens, Stefan Structural and morphotectonic evolution of the Sierras Pampeanas (Argentina) constrained by a multithermochronometer approach 2012 v, 167 Bl. (DE-627)755690079 http://hdl.handle.net/11858/00-1735-0000-0015-A35E-A text/html Resolving-System jump-off kostenfrei Volltext http://nbn-resolving.de/urn:nbn:de:gbv:7-11858/00-1735-0000-0015-A35E-A-2 text/html Resolving-System jump-off Volltext http://nbn-resolving.de/urn:nbn:de:gbv:7-11858/00-1735-0000-0015-A35E-A-2 2013-12-04 Resolving-System Volltext http://d-nb.info/104430667X/34 2013-12-04 Langzeitarchivierung Nationalbibliothek Volltext GBV-ODiss GBV_ILN_20 ISIL_DE-84 SYSFLAG_1 GBV_KXP SSG-OPC-GEO 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_105 ISIL_DE-841 GBV_ILN_110 ISIL_DE-Luen4 GBV_ILN_132 ISIL_DE-959 GBV_ILN_161 ISIL_DE-960 GBV_ILN_293 ISIL_DE-960-3 GBV_ILN_370 ISIL_DE-1373 GBV_ILN_2403 ISIL_DE-LFER BO 045F 910 20 01 0084 1461957575 x 08-03-14 21 01 0046 1462023363 z 08-03-14 22 01 0018 1462089054 SUBolrd xu 08-03-14 23 01 0830 1787697614 olr-d x 26-07-18 30 01 0104 1787776506 z 26-07-18 40 01 0007 1391058321 ediss xsn 22-05-13 60 01 0705 1462254179 OLRD z 08-03-14 63 01 3401 1787879119 ORD x 26-07-18 105 01 0841 1596281545 z 21-01-16 110 01 3110 1462310931 x 08-03-14 132 01 0959 1591397146 OLR-DISS x 19-12-15 161 01 0960 1597609951 ORD x 28-01-16 293 01 3293 1598108026 ORD xf 28-01-16 370 01 4370 1788112997 x 26-07-18 2403 01 DE-LFER 3495056211 00 --%%-- --%%-- n --%%-- l01 19-07-19 20 01 0084 http://nbn-resolving.de/urn:nbn:de:gbv:7-11858/00-1735-0000-0015-A35E-A-2 21 01 0046 http://nbn-resolving.de/urn:nbn:de:gbv:7-11858/00-1735-0000-0015-A35E-A-2 22 01 0018 http://nbn-resolving.de/urn:nbn:de:gbv:7-11858/00-1735-0000-0015-A35E-A-2 23 01 0830 http://nbn-resolving.de/urn:nbn:de:gbv:7-11858/00-1735-0000-0015-A35E-A-2 30 01 0104 http://nbn-resolving.de/urn:nbn:de:gbv:7-11858/00-1735-0000-0015-A35E-A-2 60 01 0705 http://nbn-resolving.de/urn:nbn:de:gbv:7-11858/00-1735-0000-0015-A35E-A-2 63 01 3401 E-Book http://nbn-resolving.de/urn:nbn:de:gbv:7-11858/00-1735-0000-0015-A35E-A-2 LF 105 01 0841 http://nbn-resolving.de/urn:nbn:de:gbv:7-11858/00-1735-0000-0015-A35E-A-2 110 01 3110 http://nbn-resolving.de/urn:nbn:de:gbv:7-11858/00-1735-0000-0015-A35E-A-2 132 01 0959 http://nbn-resolving.de/urn:nbn:de:gbv:7-11858/00-1735-0000-0015-A35E-A-2 161 01 0960 http://nbn-resolving.de/urn:nbn:de:gbv:7-11858/00-1735-0000-0015-A35E-A-2 293 01 3293 http://nbn-resolving.de/urn:nbn:de:gbv:7-11858/00-1735-0000-0015-A35E-A-2 370 01 4370 http://nbn-resolving.de/urn:nbn:de:gbv:7-11858/00-1735-0000-0015-A35E-A-2 2403 01 DE-LFER http://hdl.handle.net/11858/00-1735-0000-0015-A35E-A 40 00 DE-7 00 (DE-627)625047834 VBN 500 Geochronologie einzelner Regionen 40 00 DE-7 01 (DE-627)625046226 VAE 811 Alpidische Orogene {Tektonik} 40 00 DE-7 02 (DE-627)625052684 VEX 200 Argentinien {Geologie} 60 01 0705 10 ho 20 01 0084 OLRD 110 01 3110 OLRD 370 01 4370 OLRD 22 01 0018 SUBolrd 23 01 0830 olr-d 40 01 0007 ediss 60 01 0705 OLRD 63 01 3401 ORD 132 01 0959 OLR-DISS 161 01 0960 ORD 293 01 3293 ORD 23 01 0830 2018-07-26:10:53:10
allfieldsSound	13,O12 dnb 104430667X DE-101 urn:nbn:de:gbv:7-11858/00-1735-0000-0015-A35E-A-2 urn (DE-627)746434480 (DE-576)9746434489 (DE-599)GBV746434480 (OCoLC)864735224 DE-627 ger DE-627 rakwb eng XA-DE-NI 910 550 22 Löbens, Stefan verfasserin aut Structural and morphotectonic evolution of the Sierras Pampeanas (Argentina) constrained by a multithermochronometer approach vorgelegt von Stefan Löbens 2012 Online-Ressource (PDF-Datei: 645 MB) Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Göttingen, Univ., Diss., 2012 Die Sierras Pampeanas in Zentral- und Nordwestargentinien stellen ein ausgeprägtes morphotektonisches Merkmal im Bereich der flach subduzierenden Nazca Platte unter die Südamerikanische Platte zwischen ~27° S und ~33° S dar. Diese flache Subduktion wurde bisher als Ursache für die Heraushebung und Deformation von Höhenzügen innerhalb der Sierras Pampeanas während des Neogens angenommen. Auf Basis von Apatit Spaltspurendatierungen, Zirkon und Apatit (U-Th)/He Thermochronometern sowie K-Ar Datierungen von Störungsletten werden in der vorliegenden Arbeit neue thermochronologische Daten vorgest... The Sierras Pampeanas in central and northwestern Argentina constitute a distinct morphotectonic feature above the shallow subducting Nazca Plate beneath the South American Plate between ~27 ° S and ~33° S. Uplift and deformation of the mountain ranges within this area are interpreted to be closely related to this flat-slab subduction during the Neogene. New thermochronological data, derived from application of the apatite fission-track, zircon and apatite (U-Th)/He thermochronometers as well as from K-Ar dating of fault gouges, presented in this thesis, reveal new and improved insights of ... Langzeitarchivierung gewährleistet pdager Hochschulschrift (DE-588)4113937-9 (DE-627)105825778 (DE-576)209480580 gnd-content Siegesmund, Siegfried, betreuer oth Siegesmund, Siegfried, gutachter oth Sobel, Edward gutachter oth Göttingen uvp Erscheint auch als Druck-Ausgabe Löbens, Stefan Structural and morphotectonic evolution of the Sierras Pampeanas (Argentina) constrained by a multithermochronometer approach 2012 v, 167 Bl. 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hochschulschrift_txt_mv	Göttingen, Univ., Diss., 2012
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authorswithroles_txt_mv	Löbens, Stefan @@aut@@ Siegesmund, Siegfried, @@oth@@ Sobel, Edward @@oth@@
publishDateDaySort_date	2012-01-01T00:00:00Z
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title_sort	structural and morphotectonic evolution of the sierras pampeanas (argentina) constrained by a multithermochronometer approach
title_auth	Structural and morphotectonic evolution of the Sierras Pampeanas (Argentina) constrained by a multithermochronometer approach
abstract	Die Sierras Pampeanas in Zentral- und Nordwestargentinien stellen ein ausgeprägtes morphotektonisches Merkmal im Bereich der flach subduzierenden Nazca Platte unter die Südamerikanische Platte zwischen ~27° S und ~33° S dar. Diese flache Subduktion wurde bisher als Ursache für die Heraushebung und Deformation von Höhenzügen innerhalb der Sierras Pampeanas während des Neogens angenommen. Auf Basis von Apatit Spaltspurendatierungen, Zirkon und Apatit (U-Th)/He Thermochronometern sowie K-Ar Datierungen von Störungsletten werden in der vorliegenden Arbeit neue thermochronologische Daten vorgest... The Sierras Pampeanas in central and northwestern Argentina constitute a distinct morphotectonic feature above the shallow subducting Nazca Plate beneath the South American Plate between ~27 ° S and ~33° S. Uplift and deformation of the mountain ranges within this area are interpreted to be closely related to this flat-slab subduction during the Neogene. New thermochronological data, derived from application of the apatite fission-track, zircon and apatite (U-Th)/He thermochronometers as well as from K-Ar dating of fault gouges, presented in this thesis, reveal new and improved insights of ...
abstractGer	Die Sierras Pampeanas in Zentral- und Nordwestargentinien stellen ein ausgeprägtes morphotektonisches Merkmal im Bereich der flach subduzierenden Nazca Platte unter die Südamerikanische Platte zwischen ~27° S und ~33° S dar. Diese flache Subduktion wurde bisher als Ursache für die Heraushebung und Deformation von Höhenzügen innerhalb der Sierras Pampeanas während des Neogens angenommen. Auf Basis von Apatit Spaltspurendatierungen, Zirkon und Apatit (U-Th)/He Thermochronometern sowie K-Ar Datierungen von Störungsletten werden in der vorliegenden Arbeit neue thermochronologische Daten vorgest... The Sierras Pampeanas in central and northwestern Argentina constitute a distinct morphotectonic feature above the shallow subducting Nazca Plate beneath the South American Plate between ~27 ° S and ~33° S. Uplift and deformation of the mountain ranges within this area are interpreted to be closely related to this flat-slab subduction during the Neogene. New thermochronological data, derived from application of the apatite fission-track, zircon and apatite (U-Th)/He thermochronometers as well as from K-Ar dating of fault gouges, presented in this thesis, reveal new and improved insights of ...
abstract_unstemmed	Die Sierras Pampeanas in Zentral- und Nordwestargentinien stellen ein ausgeprägtes morphotektonisches Merkmal im Bereich der flach subduzierenden Nazca Platte unter die Südamerikanische Platte zwischen ~27° S und ~33° S dar. Diese flache Subduktion wurde bisher als Ursache für die Heraushebung und Deformation von Höhenzügen innerhalb der Sierras Pampeanas während des Neogens angenommen. Auf Basis von Apatit Spaltspurendatierungen, Zirkon und Apatit (U-Th)/He Thermochronometern sowie K-Ar Datierungen von Störungsletten werden in der vorliegenden Arbeit neue thermochronologische Daten vorgest... The Sierras Pampeanas in central and northwestern Argentina constitute a distinct morphotectonic feature above the shallow subducting Nazca Plate beneath the South American Plate between ~27 ° S and ~33° S. Uplift and deformation of the mountain ranges within this area are interpreted to be closely related to this flat-slab subduction during the Neogene. New thermochronological data, derived from application of the apatite fission-track, zircon and apatite (U-Th)/He thermochronometers as well as from K-Ar dating of fault gouges, presented in this thesis, reveal new and improved insights of ...
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title_short	Structural and morphotectonic evolution of the Sierras Pampeanas (Argentina) constrained by a multithermochronometer approach
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Diese flache Subduktion wurde bisher als Ursache für die Heraushebung und Deformation von Höhenzügen innerhalb der Sierras Pampeanas während des Neogens angenommen. Auf Basis von Apatit Spaltspurendatierungen, Zirkon und Apatit (U-Th)/He Thermochronometern sowie K-Ar Datierungen von Störungsletten werden in der vorliegenden Arbeit neue thermochronologische Daten vorgest...</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">The Sierras Pampeanas in central and northwestern Argentina constitute a distinct morphotectonic feature above the shallow subducting Nazca Plate beneath the South American Plate between ~27 ° S and ~33° S. Uplift and deformation of the mountain ranges within this area are interpreted to be closely related to this flat-slab subduction during the Neogene. 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Structural and morphotectonic evolution of the Sierras Pampeanas (Argentina) constrained by a multithermochronometer approach

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