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Геодинамика и тектонофизика

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GEOCHEMICAL CHARACTERISTICS OF TIANMENSHAN COMPOSITE PLUTON, SOUTH CHINA

https://doi.org/10.5800/GT-2017-8-3-0255

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Аннотация

The southern Jiangxi province is located at east Nanling range, which is an important W-Sn metallogenic province of China. The Early Yanshanian Tianmenshan is composed of the main-phase porphyritic biotite granite and the highly differentiated fine-gained biotite granite, intruding in the Lower Cambrian Niujiaohe Formation. The main-phase granite and the late-stage highly differentiated granite emplaced at 152–158 Ma and 152–151 Ma, respectively. The later was in the center of the pluton as a ovalize shape, with a transitional contact with the main-phase granite.

Об авторах

Yanjiao Chen
Hefei University of Technology
Китай

School of Resources and Environment Engineering, 

Hefei 230009



Bin Chen
Hefei University of Technology
Китай

School of Resources and Environment Engineering, 

Hefei 230009



Xiaoxia Duan
Hefei University of Technology
Китай

School of Resources and Environment Engineering, 

Hefei 230009



Для цитирования:


Chen Y., Chen B., Duan X. GEOCHEMICAL CHARACTERISTICS OF TIANMENSHAN COMPOSITE PLUTON, SOUTH CHINA. Геодинамика и тектонофизика. 2017;8(3):433-434. https://doi.org/10.5800/GT-2017-8-3-0255

For citation:


Chen Y., Chen B., Duan X. GEOCHEMICAL CHARACTERISTICS OF TIANMENSHAN COMPOSITE PLUTON, SOUTH CHINA. Geodynamics & Tectonophysics. 2017;8(3):433-434. https://doi.org/10.5800/GT-2017-8-3-0255

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ISSN 2078-502X (Online)