内蒙古乌拉特中旗哈达呼舒基性岩体形成的构造背景与古亚洲洋的早期俯冲历史

刘金龙; 孙丰月; 王英德; 李良; 张宇婷; 辛未; 胡安新

doi:10.3799/dqkx.2016.141

Volume 41 Issue 12

Dec. 2016

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Liu Jinlong, Sun Fengyue, Wang Yingde, Li Liang, Zhang Yuting, Xin Wei, Hu Anxin, 2016. Tectonic Setting of Hadahushu Mafic Intrusion in Urad Zhongqi Area, Inner Mongolia: Implications for Early Subduction History of Paleo-Asian Ocean Plate. Earth Science, 41(12): 2019-2030. doi: 10.3799/dqkx.2016.141

Citation:

Liu Jinlong, Sun Fengyue, Wang Yingde, Li Liang, Zhang Yuting, Xin Wei, Hu Anxin, 2016. Tectonic Setting of Hadahushu Mafic Intrusion in Urad Zhongqi Area, Inner Mongolia: Implications for Early Subduction History of Paleo-Asian Ocean Plate. Earth Science, 41(12): 2019-2030. doi: 10.3799/dqkx.2016.141

Citation:

Liu Jinlong, Sun Fengyue, Wang Yingde, Li Liang, Zhang Yuting, Xin Wei, Hu Anxin, 2016. Tectonic Setting of Hadahushu Mafic Intrusion in Urad Zhongqi Area, Inner Mongolia: Implications for Early Subduction History of Paleo-Asian Ocean Plate. Earth Science, 41(12): 2019-2030. doi: 10.3799/dqkx.2016.141

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Tectonic Setting of Hadahushu Mafic Intrusion in Urad Zhongqi Area, Inner Mongolia: Implications for Early Subduction History of Paleo-Asian Ocean Plate

doi: 10.3799/dqkx.2016.141

1.
College of Earth Sciences, Jilin University, Changchun 130061, China
2.
Jiangxi Jiyuan Mining Corporation, Nanchang 330030, China

Received Date: 2016-04-15
Publish Date: 2016-12-15

Abstract

Abstract

The Urad Zhongqi area of western Inner Mongolia crosses the North China Plate margin and Xing'an-Mongolia Orogenic Belt, which distributed regional basic rock massif occurred as small stocks, and a lack of reliable data of intrusion age. This paper reports LA-ICP-MS zircon U-Pb dating, geochemical and Hf isotopic data of Hadahushu mafic intrusion in Urad Zhongqi area, with the aim of constraining its petrogenesis and the beginning time of subduction of the Paleo-Asian oceanic plate. LA-ICP-MS U-Pb dating results of zircons from the mafic intrusion indicate that the intrusion formed at the Late Cambrian (513±2 Ma). The geochemical characteristics of these rocks indicate that they are the calc-alkaline series, and are characterized by enrichment in LILE (such as K, Ba, Rb), relatively depleted in HFSE (such as Nb, Ta, Zr, Ti) and LREE. The ε_Hf(t) values and one-stage model ages (T_DM1) of zircons from the rock vary from 14.15 to 15.03 and from 518 to 556 Ma, respectively. These characteristics suggest that the primary magma was derived from the depleted lithospheric mantle source. Based on the previous study, we conclude that the formation of mafic intrusion was related to the subduction of the Paleo-Asian oceanic plate.
- geochronology,
- zircon Hf isotope,
- mafic intrusion,
- Urad Zhongqi,
- geochemistry

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References(92)

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Tectonic Setting of Hadahushu Mafic Intrusion in Urad Zhongqi Area, Inner Mongolia: Implications for Early Subduction History of Paleo-Asian Ocean Plate

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