内蒙古北山造山带北部早二叠世末期高镁辉长岩地球化学特征及构造意义

张国震; 辛后田; 段连峰; 牛文超; 田健; 张永

doi:10.3799/dqkx.2021.203

Volume 47 Issue 9

Sep. 2022

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Article Navigation > Earth Science > 2022 > 47(9): 3258-3269

Zhang Guozhen, Xin Houtian, Duan Lianfeng, Niu Wenchao, Tian Jian, Zhang Yong, 2022. Geochemical Characteristics and Tectonic Implications of the End Early Permian High Magnesium Gabbro from Northern Beishan Orogenic Belt, Inner Mongolia. Earth Science, 47(9): 3258-3269. doi: 10.3799/dqkx.2021.203

Citation:

Zhang Guozhen, Xin Houtian, Duan Lianfeng, Niu Wenchao, Tian Jian, Zhang Yong, 2022. Geochemical Characteristics and Tectonic Implications of the End Early Permian High Magnesium Gabbro from Northern Beishan Orogenic Belt, Inner Mongolia. Earth Science, 47(9): 3258-3269. doi: 10.3799/dqkx.2021.203

Citation:

Zhang Guozhen, Xin Houtian, Duan Lianfeng, Niu Wenchao, Tian Jian, Zhang Yong, 2022. Geochemical Characteristics and Tectonic Implications of the End Early Permian High Magnesium Gabbro from Northern Beishan Orogenic Belt, Inner Mongolia. Earth Science, 47(9): 3258-3269. doi: 10.3799/dqkx.2021.203

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Geochemical Characteristics and Tectonic Implications of the End Early Permian High Magnesium Gabbro from Northern Beishan Orogenic Belt, Inner Mongolia

doi: 10.3799/dqkx.2021.203

Zhang Guozhen^{1, 2
,
,},
Xin Houtian^{3
,
,},
Duan Lianfeng^{1, 2
,
,},
Niu Wenchao^{1, 2},
Tian Jian^{1, 2},
Zhang Yong^{1, 2}

1.
Tianjin Center, China Geological Survey, Tianjin 300170, China
2.
North China Center for Geoscience Innovation, Tianjin 300170, China
3.
Shenyang Center, China Geological Survey, Shengyang 110034, China

Received Date: 2021-11-03
Publish Date: 2022-09-25

Abstract

Abstract

A suite of high-magnesium gabbro is located in the Qinghegou-Hongliuxia area in the southern part of the Baiheshan ophillite mélange belt in the northern Beishan orogenic belt. Based on LA-ICP-MS zircon U-Pb dating, whole-rock geochemical and Sr-Nd isotopic analyses, the gabbro was intruded at 278.2±1.3 Ma and they show high magnesium geochemical characteristic, belonging to low-tholeiite to calc-alkaline series. They are enriched in large-ion lithophile elements of Rb, Ba, Sr and depleted in high field strength elements of Nb, Ta, Ti. The values of ε_Nd(t) of the gabbro vary from 5.64 to 6.77, with high Sm/Yb, implying magma originates from depleted mantle. Relatively high Mg^#, Cr, Ni and negative Zr and Hf indicate that the primary magma has undergone limited fractional crystallization and crustal contamination. Combined with regional geological material, it is suggested that the end of the accretionary orogeny is Early to Middle Permian in the northern Beishan orogenic belt. The Paleo-Asian Ocean in the Beishan orogenic belt may have been lasted until or after Middle Permian.
- high magnesium gabbro,
- Sr-Nd isotope,
- latest Early Permian,
- accretionary orogenic time limit,
- Beishan orogenic belt,
- geochemistry

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References(61)

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Geochemical Characteristics and Tectonic Implications of the End Early Permian High Magnesium Gabbro from Northern Beishan Orogenic Belt, Inner Mongolia

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