漠河盆地二十二站组砂岩形成时代及物源区构造环境判别

李良; 孙丰月; 李碧乐; 许庆林; 张雅静; 兰理实

doi:10.3799/dqkx.2017.003

Volume 42 Issue 1

Jan. 2017

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Li Liang, Sun Fengyue, Li Bile, Xu Qinglin, Zhang Yajing, Lan Lishi, 2017. Geochronology of Ershi'erzhan Formation Sandstone in Mohe Basin and Tectonic Environment of Its Provenance. Earth Science, 42(1): 35-52. doi: 10.3799/dqkx.2017.003

Citation:

Li Liang, Sun Fengyue, Li Bile, Xu Qinglin, Zhang Yajing, Lan Lishi, 2017. Geochronology of Ershi'erzhan Formation Sandstone in Mohe Basin and Tectonic Environment of Its Provenance. Earth Science, 42(1): 35-52. doi: 10.3799/dqkx.2017.003

Citation:

Li Liang, Sun Fengyue, Li Bile, Xu Qinglin, Zhang Yajing, Lan Lishi, 2017. Geochronology of Ershi'erzhan Formation Sandstone in Mohe Basin and Tectonic Environment of Its Provenance. Earth Science, 42(1): 35-52. doi: 10.3799/dqkx.2017.003

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Geochronology of Ershi'erzhan Formation Sandstone in Mohe Basin and Tectonic Environment of Its Provenance

doi: 10.3799/dqkx.2017.003

1.
College of Earth Sciences, Jilin University, Changchun 130061, China
2.
College of Earth Science and Engineering, Shandong University of Science and Technology, Qingdao 266590, China
3.
No.1 Gold Geological Party of CAPF, Mudanjiang 157021, China

Received Date: 2016-07-25
Publish Date: 2017-01-15

Abstract

Abstract

o address the controversy of the Ershi'erzhan Formation sandstone formation ages in the Mohe basin of the northern Great Khingan Range, this study presents an accurate limit to its formation ages using the LA-ICP-MS detrital zircon U-Pb dating for the first time in this paper, and discusses its provenance and tectonic setting combined with the geochemistry of major and trace elements. The results show that the fragmental material in sandstone has poor psephicity and sorting, indicating that source region is relatively unstable with characteristics of rapid denudation, transportation and sedimentation. The grains of detrital zircons are big with clear oscillatory zoning, and Th/U values range from 0.35-1.07, which is indicative of a magmatic origin. Zircon U-Pb dating results show that 90 dating data are distributed in the following three periods, namely, 152-170Ma with the peak of 158Ma, standing for the lower limit of Ershi'erzhan Formation sedimentary rocks at Late Jurassic; 179-193Ma with the peak of 190Ma and 205-214Ma with the peak of 210Ma. The three peak ages are the evolution records of the Mongolia-Okhotsk ocean. The peak ages of 210Ma and 190Ma are consistent with the Late Triassic and Early Jurassic magmatic events of south margin of the basin in the Erguna massif, the peak age of 158Ma fits the Late Jurassic magmatic event of north margin of the basin. The geochemical diagrams of major and trace elements reveal that the provenance has the background of active continental margin. Meanwhile, the zircon dating shows that there is no Pre-Mesozoic clastics in the Ershi'erzhan Formation. It suggest that these were generated within an active continental margin setting at the north margin of the Erguna massif in Mesozoic, and provided the most clastics for the Ershi'erzhan Formation. Combining with the previous studies, it is concluded that the Ershi'erzhan Formation sandstone was formed in Late Jurassic under the environment of rapid denudation, transportation and sedimentation, controlled by the uplift of the Mongolia-Okhotsk orogenic belt, indicating that the eastern Mongolia-Okhotsk ocean has already closed in Late Jurassic.
- Mohe basin,
- Ershi'erzhan Formation,
- sandstone,
- detrital zircon,
- geochemistry,
- active continental margin,
- Mongolia-Okhotsk ocean

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References(85)

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沈阳化工大学材料科学与工程学院沈阳 110142

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Geochronology of Ershi'erzhan Formation Sandstone in Mohe Basin and Tectonic Environment of Its Provenance

doi: 10.3799/dqkx.2017.003

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