The deformation record of olivine in mylonitic peridotites from the Finero Complex, Ivrea Zone: Separate deformation cycles during exhumation-Reference-Cited by-同舟云学术

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The deformation record of olivine in mylonitic peridotites from the Finero Complex, Ivrea Zone: Separate deformation cycles during exhumation

Published:2015-12 Issue:12 Volume:34 Page:2514-2533
ISSN:0278-7407
Container-title:Tectonics
language:en
Short-container-title:Tectonics

Author:

Matysiak Agnes K.¹,Trepmann Claudia A.²

Affiliation:

1. Department of Geology, Institute of Earth and Environmental SciencesAlbert‐Ludwigs‐Universität Freiburg Freiburg Germany

2. Department of Earth and Environmental Sciences, Faculty of GeosciencesLudwig‐Maximilians‐Universität München Munich Germany

Funder

German science foundation (DFG)

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1002/2015TC003904

Reference112 articles.

1. Fluidaktivierte plastische Deformation in hochtemperierten Scherzonen;Altenberger U.;Eur. J. Mineral. Beih.,1990

2. Long-term deformation and fluid-enhanced mass transport in a Variscan peridotite shear zone in the Ivrea Zone, northern Italy: a microtextural, petrological and geochemical study of a reactivated shear zone

3. Subgrain rotation and dynamic recrystallization of olivine, upper mantle diapirism, and extension of the basin-and-range province

4. Dislocations, kink bands, and room-temperature plasticity of Ti3SiC2

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