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Геодинамика и тектонофизика

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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

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Аннотация

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.

Об авторах

Qie Qin
Institute of Geology, Chinese Academy of Geological Sciences
Китай
Beijing 100037


He Huang
Institute of Geology, Chinese Academy of Geological Sciences
Китай
Beijing 100037


Tao Wang
Institute of Geology, Chinese Academy of Geological Sciences
Китай
Beijing 100037


Zhaochong Zhang
China University of Geosciences
Китай

State Key Laboratory of Geological Processes and Mineral Resources, 

Beijing 100083



Для цитирования:


Qin Q., Huang H., Wang T., Zhang Z. AN EARLY PERMIAN GARNET-BEATING PERALUMINOUS GRANITIC PLUTON IN THE SOUTH TIANSHAN OROGENIC BELT, NW CHINA: PETROLOGICAL, MINERALOGICAL AND GEOCHEMICAL CONSTRAINTS. Геодинамика и тектонофизика. 2017;8(3):537-538. https://doi.org/10.5800/GT-2017-8-3-0284

For citation:


Qin Q., Huang H., Wang T., Zhang Z. 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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ISSN 2078-502X (Online)