内蒙古温都尔庙地区早二叠世岛弧型花岗闪长岩的发现:对古亚洲洋闭合的时限约束

高征西; 王继春; 周路路; 赵鑫; 秦江东; 王沛东; 吴艳君; 汪岩; 宝音乌力吉

doi:10.3799/dqkx.2019.239

Volume 44 Issue 10

Nov. 2019

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Article Navigation > Earth Science > 2019 > 44(10): 3178-3192

Gao Zhengxi, Wang Jichun, Zhou Lulu, Zhao Xin, Qin Jiangdong, Wang Peidong, Wu Yanjun, Wang Yan, Baoyin Wuliji, 2019. Discovery of Early Permian Island-Arc Type Granodiorites in Wenduermiao Area, Inner Mongolia: Constraints on Timing of Closure of PaleoAsian Ocean. Earth Science, 44(10): 3178-3192. doi: 10.3799/dqkx.2019.239

Citation:

Gao Zhengxi, Wang Jichun, Zhou Lulu, Zhao Xin, Qin Jiangdong, Wang Peidong, Wu Yanjun, Wang Yan, Baoyin Wuliji, 2019. Discovery of Early Permian Island-Arc Type Granodiorites in Wenduermiao Area, Inner Mongolia: Constraints on Timing of Closure of PaleoAsian Ocean. Earth Science, 44(10): 3178-3192. doi: 10.3799/dqkx.2019.239

Citation:

Gao Zhengxi, Wang Jichun, Zhou Lulu, Zhao Xin, Qin Jiangdong, Wang Peidong, Wu Yanjun, Wang Yan, Baoyin Wuliji, 2019. Discovery of Early Permian Island-Arc Type Granodiorites in Wenduermiao Area, Inner Mongolia: Constraints on Timing of Closure of PaleoAsian Ocean. Earth Science, 44(10): 3178-3192. doi: 10.3799/dqkx.2019.239

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Discovery of Early Permian Island-Arc Type Granodiorites in Wenduermiao Area, Inner Mongolia: Constraints on Timing of Closure of PaleoAsian Ocean

doi: 10.3799/dqkx.2019.239

Gao Zhengxi^{1,2,3
,},
Wang Jichun^{2,3
,
,},
Zhou Lulu⁴,
Zhao Xin^2,3,
Qin Jiangdong^2,3,
Wang Peidong^2,3,
Wu Yanjun^2,3,
Wang Yan⁵,
Baoyin Wuliji^2,3

1.
School of Earth Resources, China University of Geosciences, Wuhan 430074, China
2.
Inner Mongolia Key Laboratory of Magmatic Mineralization and Ore-Prospecting, Huhhot 010020, China
3.
Geological Survey Institute of Inner Mongolia Autonomous Region, Huhhot 010020, China
4.
Anhui Natural Gas Development Co., Ltd., Hefei 230051, China
5.
Shenyang Center of Geological Survey, China Geological Survey, Shenyang 110034, China

Received Date: 2019-09-24
Publish Date: 2019-11-11

Abstract

Abstract

The study area is located in the key part between the North China and the Siberia plates, which may represent the final closure of the Paleo-Asian Ocean. Granodiorites were recognized in the Gashun area for the first time. According to petrogeochemistry, zircon U-Pb geochronology and Lu-Hf isotope analysis, the granodiorites yield an LA-MC-ICP-MS zircon UPb age of 294.8±2.7 Ma, suggesting that they were formed in the Early Permian. The rocks have SiO₂=64.69%-67.64%, Al₂O₃=15.00%-15.52%, MgO=1.14%-1.77%, Na₂O=1.41%-3.61%, and K₂O=3.25%-3.98%. The content of ∑ REE varies from 157.89×10^-6 to 174.43×10^-6, the content of LREE varies from 147.86×10^-6 to 149.55×10^-6, and the content of HREE vary from 9.34×10^-6 to 11.8×10^-6. The rocks display rightly-inclined REE distribution curves, slightly negative Eu anomalies, highly fractionated LREE/HREE, and more enriched LREE relative to HREE. In the rocks, Rb and K were obviously enriched, and Ba and Sr (LILE) were depleted; Th was enriched and Nb, Ta and Ti etc. (HFSE) were depleted. Zircon ¹⁷⁶Hf/¹⁷⁷Hf changes from 0.282 673 to 0.282 791, and ε_Hf(t) varies from 2.7 to 7.0. The two-stage model ages (T_DM2) vary from 861 Ma to 1 129 Ma, and ¹⁷⁶Lu/¹⁷⁷Hf ranges from 0.000 486 to 0.000 734. Combined with petrogeochemical characteristics, this set of granodiorites is considered to be formed by island-arc magmatism, confirming that the Paleo-Asian Ocean was still open in the Early Permian.
- island-arc type granodiorite,
- Paleo-Asian Ocean,
- Wenduermiao area,
- petrology

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References(80)

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Discovery of Early Permian Island-Arc Type Granodiorites in Wenduermiao Area, Inner Mongolia: Constraints on Timing of Closure of PaleoAsian Ocean

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