胶东范家庄地区晚侏罗世低镁埃达克质花岗岩成因及构造背景

刘晓阳; 谭俊; 王怀洪; 王勇军; 甘觐荣; 王治华; 张铭

doi:10.3799/dqkx.2018.376

Volume 45 Issue 2

Feb. 2020

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Liu Xiaoyang, Tan Jun, Wang Huaihong, Wang Yongjun, Gan Jinrong, Wang Zhihua, Zhang Ming, 2020. Petrogenesis and Tectonic Setting of the Late Jurassic Low-Mg Adakitic Granites in the Fanjiazhuang Area, Jiaodong Peninsula. Earth Science, 45(2): 451-466. doi: 10.3799/dqkx.2018.376

Citation:

Liu Xiaoyang, Tan Jun, Wang Huaihong, Wang Yongjun, Gan Jinrong, Wang Zhihua, Zhang Ming, 2020. Petrogenesis and Tectonic Setting of the Late Jurassic Low-Mg Adakitic Granites in the Fanjiazhuang Area, Jiaodong Peninsula. Earth Science, 45(2): 451-466. doi: 10.3799/dqkx.2018.376

Citation:

Liu Xiaoyang, Tan Jun, Wang Huaihong, Wang Yongjun, Gan Jinrong, Wang Zhihua, Zhang Ming, 2020. Petrogenesis and Tectonic Setting of the Late Jurassic Low-Mg Adakitic Granites in the Fanjiazhuang Area, Jiaodong Peninsula. Earth Science, 45(2): 451-466. doi: 10.3799/dqkx.2018.376

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Petrogenesis and Tectonic Setting of the Late Jurassic Low-Mg Adakitic Granites in the Fanjiazhuang Area, Jiaodong Peninsula

doi: 10.3799/dqkx.2018.376

1.
Faculty of Earth Resources, China University of Geosciences, Wuhan 430074, China
2.
Shandong Provincial Research Institute of Coal Geology Planning and Exploration, Jinan 250100, China
3.
Key Laboratory of Coalfield Geophysics, Geophysical Society of China, Jinan 250100, China
4.
The First Prospecting Team of Shandong Coal Geology Bureau, Zaozhuang 277000, China

Received Date: 2018-12-03
Publish Date: 2020-02-15

Abstract

Abstract

A series of late Jurassic adakitic rocks are widely developed in the Jiaodong Peninsula, eastern China, and their petrogenesis and tectonic setting provide important evidence for Mesozoic tectonic evolution in Jiaodong area. In this study, we investigate the bulk-rock major element, trace element and Sr-Nd-Pb isotopes of the granitoid exposed in the Fanjiazhuang area. LA-ICP-MS zircon U-Pb dating results yield a weighted mean ²⁰⁶Pb/²³⁸U age of 161±2 Ma for the Fanjiazhuang granitoid. Geochemical data indicate that the intrusion is characterized by high SiO₂(68.94%-71.00%), Al₂O₃(>15.17%), Sr but low MgO(0.32%-0.41%), Y and Yb contents, and high Sr/Y and La/Yb ratios. The rocks exhibit high initial ⁸⁷Sr/⁸⁶Sr ratios (0.709 28 to 0.711 41), low ε_Nd(t) (-20.5 to -14.1) and they are characterized by high radiogenic Pb isotopic compositions with (²⁰⁶Pb/²⁰⁴Pb)_t=16.853-17.207, (²⁰⁷Pb/²⁰⁴Pb)_t=15.436-15.495, (²⁰⁸Pb/²⁰⁴Pb)_t=37.340-37.629. The elemental and isotopic data suggest that the late Jurassic low-Mg adakitic granites in Fanjiazhuang area were derived from the partial melting of the thickened lower crust. The results show that the magma sources were dominated by lower crust of the Yangtze Block and with subordinate lower crust of the North China Block. The Izanagi plate subduction was the most likely geodynamic force for formation of the Jurassic Fanjiazhuang low-Mg adakatic granite in the Jiaodong Peninsula.
- geochemistry,
- Sr-Nd-Pb isotopes,
- low-Mg adakitic,
- Late Jurassic,
- Fanjiazhuang,
- Jiaodong Peninsula

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References(90)

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