AN EARLY PERMIAN GARNET-BEATING PERALUMINOUS GRANITIC PLUTON IN THE SOUTH TIANSHAN OROGENIC BELT, NW CHINA: PETROLOGICAL, MINERALOGICAL AND GEOCHEMICAL CONSTRAINTS
https://doi.org/10.5800/GT-2017-8-3-0284
Abstract
The Ku’erchu granitic pluton (283±4 Ma) was exposed in the eastern part of the South Tianshan Orogenic Belt. The granites from the intrusion are mainly composed of orthoclase (~45 vol. %), plagioclase (~15 vol. %), quartz (~20 vol. %), muscovite (~10 vol. %) and biotite (~5 vol. %), with accessory minerals including garnet, zircon and Fe-Ti oxide.
About the Authors
Qie Qin
Institute of Geology, Chinese Academy of Geological Sciences
China
Beijing 100037
China
Beijing 100037
He Huang
Institute of Geology, Chinese Academy of Geological Sciences
China
Beijing 100037
China
Beijing 100037
Tao Wang
Institute of Geology, Chinese Academy of Geological Sciences
China
Beijing 100037
China
Beijing 100037
Zhaochong Zhang
China University of Geosciences
China
China
State Key Laboratory of Geological Processes and Mineral Resources,
Beijing 100083
Review
For citations:
Qin Q., Huang H., Wang T., Zhang Zh. AN EARLY PERMIAN GARNET-BEATING PERALUMINOUS GRANITIC PLUTON IN THE SOUTH TIANSHAN OROGENIC BELT, NW CHINA: PETROLOGICAL, MINERALOGICAL AND GEOCHEMICAL CONSTRAINTS. Geodynamics & Tectonophysics. 2017;8(3):537-538. https://doi.org/10.5800/GT-2017-8-3-0284
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