Metamorphic P-T Path of High-Pressure Mafic Granulite (Retrograded Eclogite) from Dinggye of Tibet and Its Tectonic Implication
Ding Zigeng
Tong Laixi
Liu Xiaohan
Liu Zhao
Zhou Xuejun
Abstract:Dinggye is located in the central part of the Greater Himalayan crystalline complex (GHC) in southern Tibet.It is essential to investigate the metamorphic P-T path of granulite in this area to better understand the collision and uplifting process of the Tibetan plateau.The petrological study of the high-pressure mafic granulite (retrograded eelogite) from the region indicates four stages:(1) peak eclogite facies mineral assemblage (M1) consists of garnet (core)+omphacite (psedomorph)+ quartz + rutile;(2) high-pressure granulite facies mineral assemblage (M2) comprises garnet (mantle) +clinopyroxene+ plagioclase+ilmenite + amphibole + biotite;(3) medium-pressure granulite facies assemblage (M3) is composed of garnet (rim) + orthopyroxene + plagioclase + biotite;(4) amphibolite facies mineral assemblage (M4) consists of amphibole+plagioclase.Using the THERMOCALC program,the thermodynamic modeling in the NCFMASHTO system has been undertaken for the high-pressure mafic granulite.Combined with the conventional thermobarometers and the average P-T estimates,the P-T conditions of the different metamorphic stages are estimated to be 786-826 ℃,0.78-0.96 GPa (M2);798-850 ℃,0.71-0.75 GPa (M3);and 610-666 ℃,0.51-0.60 GPa (M4),respectively,indicating a post-peak clockwise P-T path characterized by nearly isothermal decompression.Combined with geological data available,we propose that the highpressure mafic granulite (retrograded eclogite) of the Dinggye formed during the Himalayan collisional orogeny,and underwent a post-peak tectonic uplift process of nearly isothermal decompression.
Keywords:high-pressure mafic granuliteP-T pathcollisional orogenesisGreater HimalayaDinggyepetrology
Publication Date:2018-01-01
Online Publishing Date:2025-08-15(First online date of this platform, not the publication date of the document)
Pages:16( 220-235 )
