北山造山带公婆泉岩浆弧的组成、时代及其大地构造意义

李敏; 辛后田; 田健; 孟宪锋; 潘志龙; 陈超; 梁国庆

doi:10.3799/dqkx.2020.123

Volume 45 Issue 7

Jul. 2020

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Article Navigation > Earth Science > 2020 > 45(7): 2393-2412

Li Min, Xin Houtian, Tian Jian, Meng Xianfeng, Pang Zhilong, Chen Chao, Liang Guoqing, 2020. Composition, Age and Polarity of Gongpoquan Arc and Its Tectonic Significance in Beishan Orogen. Earth Science, 45(7): 2393-2412. doi: 10.3799/dqkx.2020.123

Citation:

Li Min, Xin Houtian, Tian Jian, Meng Xianfeng, Pang Zhilong, Chen Chao, Liang Guoqing, 2020. Composition, Age and Polarity of Gongpoquan Arc and Its Tectonic Significance in Beishan Orogen. Earth Science, 45(7): 2393-2412. doi: 10.3799/dqkx.2020.123

Citation:

Li Min, Xin Houtian, Tian Jian, Meng Xianfeng, Pang Zhilong, Chen Chao, Liang Guoqing, 2020. Composition, Age and Polarity of Gongpoquan Arc and Its Tectonic Significance in Beishan Orogen. Earth Science, 45(7): 2393-2412. doi: 10.3799/dqkx.2020.123

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Composition, Age and Polarity of Gongpoquan Arc and Its Tectonic Significance in Beishan Orogen

doi: 10.3799/dqkx.2020.123

Li Min^{1, 2
,
,},
Xin Houtian^{1, 2},
Tian Jian^{1, 2},
Meng Xianfeng³,
Pang Zhilong³,
Chen Chao³,
Liang Guoqing³

1.
Tianjin Center of Geological Survey, China Geological Survey, Tianjin 300170, China
2.
North China Geological Science and Technology Innovation Center, Tianjin 300170, China
3.
Regional Geological Survey Institute of Hebei Province, Langfang 065000, China

Received Date: 2020-05-20
Publish Date: 2020-07-15

Abstract

Abstract

Gongpoquan arc extends nearly east-west in Gongpoquan-Shibanjing-Xiaohuangshan area on the north side of Niuquanzi-Xichangjing ophiolite mèlange belt in Beishan orogen. Its material composition, formation age of different rocks and spatial distribution pattern are very important for studying the Early Paleozoic tectonic evolution of Beishan orogen. Based on the study and analysis of data from more than 30 pieces of 1:50 000 regional geological mapping, It's made clear that the Gongpoquan arc is mainly composed of three stages of strong tectono-magmatism, which are gabbro-diorite assemblages and basalts of 510-470 Ma, gneissic tonalites-granodiorite assemblages and a small amount of diorite-quartz diorite assemblages as well as large-scale andesite of 470-430 Ma, syenogranite-monzogranite assemblage of 430-410 Ma.Combined with the regional geological knowledge and the geochemical data of the above rock assemblages, they were formed in three different stages of tectonic evolution:initial subduction, main subduction and post collision periods. The spatial distribution of granite assemblages in the main subduction period has a distribution pattern from south to north. The variations of lithology indicates that the Yueyashan-Xichangjing Ocean has a polarity of northward subduction.
- Gongpoquan arc,
- Early Paleozoic,
- island arc accretion,
- subduction,
- Beishan orogen,
- tectonics

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References(51)

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