Biostratigraphy and structure of the Voirons Flysch: Gurnigel Nappe, Haute-Savoie, France

The Voirons Flysch (Haute-Savoie, France) is the subject of the present research. In this study we propose (i) a refined age model based on planktonic foraminiferal biostratigraphy, (ii) the extension of the reworking process and (iii) a structural study suggesting an updated tectonic model for this...

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Bibliographic Details
Main Author: Ospina Ostios, Lina Maria
Other Authors: Kindler, Pascal, Sartori, Mario
Format: Doctoral or Postdoctoral Thesis
Language:French
Published: Université de Genève 2016
Subjects:
Online Access:https://archive-ouverte.unige.ch/unige:93352
https://doi.org/10.13097/archive-ouverte/unige:93352
id ftunivgeneve:oai:unige.ch:unige:93352
record_format openpolar
spelling ftunivgeneve:oai:unige.ch:unige:93352 2023-05-15T18:00:50+02:00 Biostratigraphy and structure of the Voirons Flysch: Gurnigel Nappe, Haute-Savoie, France Ospina Ostios, Lina Maria Kindler, Pascal Sartori, Mario 2016 https://archive-ouverte.unige.ch/unige:93352 https://doi.org/10.13097/archive-ouverte/unige:93352 fre fre Université de Genève info:eu-repo/semantics/altIdentifier/urn/urn:nbn:ch:unige-933528 unige:93352 https://archive-ouverte.unige.ch/unige:93352 doi:10.13097/archive-ouverte/unige:93352 Free access / Restricted access until 2018-03-22 info:eu-repo/semantics/embargoedAccess info:eu-repo/classification/ddc/550 Voirons Flysch Planktonic foraminifera Reworking Conical fold Haute-Savoie Text info:eu-repo/semantics/doctoralThesis Thesis Thèse 2016 ftunivgeneve https://doi.org/10.13097/archive-ouverte/unige:93352 2022-02-08T22:36:18Z The Voirons Flysch (Haute-Savoie, France) is the subject of the present research. In this study we propose (i) a refined age model based on planktonic foraminiferal biostratigraphy, (ii) the extension of the reworking process and (iii) a structural study suggesting an updated tectonic model for this flysch. Based on the determination of isolated specimens, ages for each member of the Voirons Flysch have been suggested. It could be deposited between the late-Middle Eocene and Late Eocene or Early Oligocene. The extension of the reworking suggests one (or more) rock (s) source (s) of Early Cretaceous to early Middle Eocene age. The structural analysis shows that the Voirons Flysch forms an open conical fold (suggesting fold amplitude attenuation) with dip variations about 20º. The relative homogeneity in stratification orientations observed suggests that no major tectonic disturbance can be recognized between the members of this flysch. Doctoral or Postdoctoral Thesis Planktonic foraminifera Université de Genève: Archive ouverte UNIGE
institution Open Polar
collection Université de Genève: Archive ouverte UNIGE
op_collection_id ftunivgeneve
language French
topic info:eu-repo/classification/ddc/550
Voirons Flysch
Planktonic foraminifera
Reworking
Conical fold
Haute-Savoie
spellingShingle info:eu-repo/classification/ddc/550
Voirons Flysch
Planktonic foraminifera
Reworking
Conical fold
Haute-Savoie
Ospina Ostios, Lina Maria
Biostratigraphy and structure of the Voirons Flysch: Gurnigel Nappe, Haute-Savoie, France
topic_facet info:eu-repo/classification/ddc/550
Voirons Flysch
Planktonic foraminifera
Reworking
Conical fold
Haute-Savoie
description The Voirons Flysch (Haute-Savoie, France) is the subject of the present research. In this study we propose (i) a refined age model based on planktonic foraminiferal biostratigraphy, (ii) the extension of the reworking process and (iii) a structural study suggesting an updated tectonic model for this flysch. Based on the determination of isolated specimens, ages for each member of the Voirons Flysch have been suggested. It could be deposited between the late-Middle Eocene and Late Eocene or Early Oligocene. The extension of the reworking suggests one (or more) rock (s) source (s) of Early Cretaceous to early Middle Eocene age. The structural analysis shows that the Voirons Flysch forms an open conical fold (suggesting fold amplitude attenuation) with dip variations about 20º. The relative homogeneity in stratification orientations observed suggests that no major tectonic disturbance can be recognized between the members of this flysch.
author2 Kindler, Pascal
Sartori, Mario
format Doctoral or Postdoctoral Thesis
author Ospina Ostios, Lina Maria
author_facet Ospina Ostios, Lina Maria
author_sort Ospina Ostios, Lina Maria
title Biostratigraphy and structure of the Voirons Flysch: Gurnigel Nappe, Haute-Savoie, France
title_short Biostratigraphy and structure of the Voirons Flysch: Gurnigel Nappe, Haute-Savoie, France
title_full Biostratigraphy and structure of the Voirons Flysch: Gurnigel Nappe, Haute-Savoie, France
title_fullStr Biostratigraphy and structure of the Voirons Flysch: Gurnigel Nappe, Haute-Savoie, France
title_full_unstemmed Biostratigraphy and structure of the Voirons Flysch: Gurnigel Nappe, Haute-Savoie, France
title_sort biostratigraphy and structure of the voirons flysch: gurnigel nappe, haute-savoie, france
publisher Université de Genève
publishDate 2016
url https://archive-ouverte.unige.ch/unige:93352
https://doi.org/10.13097/archive-ouverte/unige:93352
genre Planktonic foraminifera
genre_facet Planktonic foraminifera
op_relation info:eu-repo/semantics/altIdentifier/urn/urn:nbn:ch:unige-933528
unige:93352
https://archive-ouverte.unige.ch/unige:93352
doi:10.13097/archive-ouverte/unige:93352
op_rights Free access / Restricted access until 2018-03-22
info:eu-repo/semantics/embargoedAccess
op_doi https://doi.org/10.13097/archive-ouverte/unige:93352
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