Dynamic evolution of deformation microstructures in rocks. Physical conditions for deformation. Estimate of the physical conditions for deformation based on c-axis fabric transitions in naturally deformed quartzite.
نویسندگان
چکیده
منابع مشابه
Evolution of recorded microstructures in minerals during cooling of Zarrin intrusion, evidence for dynamic deformation
The Zarrin granitoids is located in the west of Yazd block, Central Iran. Zarrin granitoids exhibit mylonitic rocks ranging from protomylonitic to mylontic. In Zarrin granitoids examples of sub-magmatic, microstructures are represented by chessboard patterns in quartz and sub-magmatic fractures in plagioclase, indicating deformation at high-temperature conditions (T > 650º C) and the presence o...
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ژورنال
عنوان ژورنال: The Journal of the Geological Society of Japan
سال: 1996
ISSN: 0016-7630,1349-9963
DOI: 10.5575/geosoc.102.211