Crystallographic preferred orientations of exhumed subduction channel rocks from the Eclogite Zone of the Tauern Window (Eastern Alps, Austria), and implications on rock elastic anisotropies at great depths-Reference-Cited by-同舟云学术

Crystallographic preferred orientations of exhumed subduction channel rocks from the Eclogite Zone of the Tauern Window (Eastern Alps, Austria), and implications on rock elastic anisotropies at great depths

Published:2015-04 Issue: Volume:647-648 Page:89-104
ISSN:0040-1951
Container-title:Tectonophysics
language:en
Short-container-title:Tectonophysics

Author:

Keppler Ruth,Ullemeyer Klaus,Behrmann Jan H.,Stipp Michael,Kurzawski Robert M.,Lokajíček Tomas

Funder

German Federal Ministry of Education and Research (BMBF)

Publisher

Elsevier BV

Subject

Earth-Surface Processes,Geophysics

Reference91 articles.

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5. Franciscan subduction off to a slow start: evidence from high-precision Lu–Hf garnet ages on high grade-blocks;Anczkiewicz;Earth Planet. Sci. Lett.,2004

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