Pseudotachylytes Generated During Seismic Faulting and Eclogitization of the Deep Crust
Author:
Affiliation:
1. Mineralogisk-Geologisk Museum, Sarsgt. 1, N-0562 Oslo, Norway
2. Department of Geological Sciences, University of Michigan, Ann Arbor, MI 48109-2143, USA.
Publisher
American Association for the Advancement of Science (AAAS)
Subject
Multidisciplinary
Reference26 articles.
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2. AUSTRHEIM, H, ECLOGITIZATION OF LOWER CRUSTAL GRANULITES BY FLUID MIGRATION THROUGH SHEAR ZONES, EARTH AND PLANETARY SCIENCE LETTERS 81: 221 (1987).
3. AUSTRHEIM, H, THE GRANULITE ECLOGITE FACIES TRANSITION - A COMPARISON OF EXPERIMENTAL WORK AND A NATURAL OCCURRENCE IN THE BERGEN ARCS, WESTERN NORWAY, LITHOS 25: 163 (1990).
4. AUSTRHEIM, H, TERRA NOVA 3: 492 (1991).
5. BOUNDY, T.M., STRUCTURAL DEVELOPMENT AND PETROFABRICS OF ECLOGITE FACIES SHEAR ZONES, BERGEN ARCS, WESTERN NORWAY - IMPLICATIONS FOR DEEP CRUSTAL DEFORMATIONAL PROCESSES, JOURNAL OF METAMORPHIC GEOLOGY 10: 127 (1992).
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