Unusual transition in quartzite dislocation creep regimes and crystal slip systems in the aureole of the Eureka Valley–Joshua Flat–Beer Creek pluton, California: a case for anhydrous conditions created by decarbonation reactions-Reference-Cited by-同舟云学术

Unusual transition in quartzite dislocation creep regimes and crystal slip systems in the aureole of the Eureka Valley–Joshua Flat–Beer Creek pluton, California: a case for anhydrous conditions created by decarbonation reactions

Published:2004-06 Issue:1-4 Volume:384 Page:209-231
ISSN:0040-1951
Container-title:Tectonophysics
language:en
Short-container-title:Tectonophysics

Author:

Morgan Sven S.,Law Richard D.

Publisher

Elsevier BV

Subject

Earth-Surface Processes,Geophysics

Reference91 articles.

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4. Secondary lineation in a high-T quartzite (Galicia, Spain): an explanation for an abnormal fabric;Bouchez;J. Struct. Geol.,1984

5. The evolution of a late-Variscan high-T/low-P region: the southeastern margin of the Bohemian massif;Büttner;Geol. Rundsch.,1997

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