Geochronological evidence for continuous exhumation through the ductile‐brittle transition along a crustal‐scale low‐angle normal fault: Simplon Fault Zone, central Alps-Reference-Cited by-同舟云学术

Geochronological evidence for continuous exhumation through the ductile‐brittle transition along a crustal‐scale low‐angle normal fault: Simplon Fault Zone, central Alps

Published:2010-05-08 Issue:3 Volume:29 Page:
ISSN:0278-7407
Container-title:Tectonics
language:en
Short-container-title:Tectonics

Author:

Campani M.¹²,Mancktelow N.¹,Seward D.¹,Rolland Y.³,Müller W.⁴,Guerra I.⁵

Affiliation:

1. Department of Earth Sciences ETH Zurich Zurich Switzerland

2. Now at Institut für Geologie, Leibniz Universität Hannover, Hannover, Germany.

3. Géosciences Azur Université de Nice Sophia Antipolis, CNRS, IRD Nice France

4. Department of Earth Sciences Royal Holloway, University of London Egham UK

5. IMG Quartier UNIL‐Dorigny Lausanne Switzerland

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2009TC002582

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3. Zur Geologie der Wurzelzone östlich des Ossolatales;Bearth P.;Eclogae Geol. Helv.,1956

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