학술논문
Petrological and fluid inclusion studies of pelitic schists from Bodonch area, western Mongolian Altai
Document Type
Journal Article
Source
Abstracts for Annual Meeting of Japan Association of Mineralogical Sciences. 2011, :102
Subject
Language
English
Abstract
The Altai Orogen in the southwestern margin of the Central Asian Orogenic Belt contains various volcano-sedimentary rocks that were deformed and metamorphosed under various P-T conditions Geothermobarometric and mineral equilibrium modelling studies on the rocks obtained peak P-T condition of 640-690C /6.3-10.7 kbar and clockwise path from the area. Such high-pressure amphibolite-facies event is related to the activity of CO2-rich fluid.