内蒙古阿巴嘎旗地区宝力高庙组火山岩特征及对古亚洲洋东段演化的制约

刘博; 靳胜凯; 马明; 李利阳; 谢志远; 王建民

doi:10.3799/dqkx.2022.381

Volume 48 Issue 9

Sep. 2023

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Liu Bo, Jin Shengkai, Ma Ming, Li Liyang, Xie Zhiyuan, Wang Jianmin, 2023. Petrogenesis of the Baoligaomiao Volcanic Rocks in the Abaga Banner, Inner Mongolia: Implications for Evolution of the Eastern Paleo Asian Ocean. Earth Science, 48(9): 3312-3326. doi: 10.3799/dqkx.2022.381

Citation:

Liu Bo, Jin Shengkai, Ma Ming, Li Liyang, Xie Zhiyuan, Wang Jianmin, 2023. Petrogenesis of the Baoligaomiao Volcanic Rocks in the Abaga Banner, Inner Mongolia: Implications for Evolution of the Eastern Paleo Asian Ocean. Earth Science, 48(9): 3312-3326. doi: 10.3799/dqkx.2022.381

Citation:

Liu Bo, Jin Shengkai, Ma Ming, Li Liyang, Xie Zhiyuan, Wang Jianmin, 2023. Petrogenesis of the Baoligaomiao Volcanic Rocks in the Abaga Banner, Inner Mongolia: Implications for Evolution of the Eastern Paleo Asian Ocean. Earth Science, 48(9): 3312-3326. doi: 10.3799/dqkx.2022.381

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Petrogenesis of the Baoligaomiao Volcanic Rocks in the Abaga Banner, Inner Mongolia: Implications for Evolution of the Eastern Paleo Asian Ocean

doi: 10.3799/dqkx.2022.381

Liu Bo^{1
,
,},
Jin Shengkai^{1, 2
,
,},
Ma Ming¹,
Li Liyang¹,
Xie Zhiyuan¹,
Wang Jianmin¹

1.
Langfang Comprehensive Natural Resources Survey Center, China Geological Survey, Langfang 065000, China
2.
State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Beijing 100083, China

Received Date: 2022-06-13
Available Online: 2023-10-07
Publish Date: 2023-09-25

Abstract

Abstract

To investigate the tectonic evolution process of the Paleo-Asian Ocean in the Abaga Banner, Inner Mongolia, this paper presents detailed petrological, zircon U⁃Pb chronological, and whole-rock geochemical studies of the volcanic rocks of the Baoligaomiao Formation. We redefine the Baoligaomiao Formation into four members. Zircon U⁃Pb ages of the second member amphibole andesite, the third member rhyolite and the fourth member rhyolitic crystal tuff yield a U⁃Pb age of 320.1±5.7 Ma, 315.1±4.1 Ma and 304.8±2.3 Ma, respectively. The Baoligaomiao volcanic rocks are characterized by high-K and weak peraluminous rocks affinities, belonging to sub-alkaline series, and they are interpreted to be formed by the product of partial melting of the thickened lower crust formed by mantle-derived magma underplating. The study area evolved from the continental margin arc tectonic environment recorded by the second member of the Baoligaomiao Formation to the collision by the third member of the volcanic rocks, until to post-collision environment by the fourth member of the volcanic rocks. Combined with the previous research results of the Early Permian magmatic activity in this area (product of the post-collision extensional stage), it is suggested that the Erenhot-Hegenshan oceanic basin of the Paleo Asian Ocean was in the process of oceanic slab destruction characterized by intra-oceanic subduction during the Late Carboniferous. A synthetic study of the geochemical characteristics of the Baoligaomiao volcanic rocks and the regional geological data reveals that the study area was in the setting of micro-continents collision during the late Late Carboniferous.
- Paleo-Asian Ocean,
- Xingmeng orogenic belt,
- Erenhot-Hegenshan oceanic,
- Baoligaomiao Formation,
- volcanic rocks,
- petrology,
- geochemistry

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Petrogenesis of the Baoligaomiao Volcanic Rocks in the Abaga Banner, Inner Mongolia: Implications for Evolution of the Eastern Paleo Asian Ocean

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