Mylonitic ductile shear zones within tectonites and cumulates as evidence for an oceanic transform fault in the Antalya ophiolite, S.W. Turkey
- 1 January 1984
- journal article
- Published by Geological Society of London in Geological Society, London, Special Publications
- Vol. 17 (1) , 319-334
- https://doi.org/10.1144/gsl.sp.1984.017.01.23
Abstract
No abstract availableKeywords
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