漠河盆地绣峰组形成时代及物源分析：对蒙古‒鄂霍茨克洋东段演化的启示

陈龙; 梁琛岳; 刘永江; 贾祥鹤; 张骞; 宋志伟; 李冬雪; 段东

doi:10.3799/dqkx.2021.159

Volume 47 Issue 9

Sep. 2022

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Article Navigation > Earth Science > 2022 > 47(9): 3334-3353

Chen Long, Liang Chenyue, Liu Yongjiang, Jia Xianghe, Zhang Qian, Song Zhiwei, Li Dongxue, Duan Dong, 2022. Geochronology and Provenance Analysis of the Xiufeng Formation in Mohe Basin: Implications for the Evolution of the Eastern Mongol-Okhotsk Ocean. Earth Science, 47(9): 3334-3353. doi: 10.3799/dqkx.2021.159

Citation:

Chen Long, Liang Chenyue, Liu Yongjiang, Jia Xianghe, Zhang Qian, Song Zhiwei, Li Dongxue, Duan Dong, 2022. Geochronology and Provenance Analysis of the Xiufeng Formation in Mohe Basin: Implications for the Evolution of the Eastern Mongol-Okhotsk Ocean. Earth Science, 47(9): 3334-3353. doi: 10.3799/dqkx.2021.159

Citation:

Chen Long, Liang Chenyue, Liu Yongjiang, Jia Xianghe, Zhang Qian, Song Zhiwei, Li Dongxue, Duan Dong, 2022. Geochronology and Provenance Analysis of the Xiufeng Formation in Mohe Basin: Implications for the Evolution of the Eastern Mongol-Okhotsk Ocean. Earth Science, 47(9): 3334-3353. doi: 10.3799/dqkx.2021.159

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Geochronology and Provenance Analysis of the Xiufeng Formation in Mohe Basin: Implications for the Evolution of the Eastern Mongol-Okhotsk Ocean

doi: 10.3799/dqkx.2021.159

Chen Long^{1
,
,},
Liang Chenyue^{1, 2
,
,
,},
Liu Yongjiang^{3, 4},
Jia Xianghe¹,
Zhang Qian¹,
Song Zhiwei¹,
Li Dongxue¹,
Duan Dong¹

1.
College of Earth Sciences, Jilin University, Changchun 130061, China
2.
Key Laboratory of Mineral Resources Evaluation in Northeast Asia, Ministry of Natural Resources, Jilin University, Changchun 130061, China
3.
Frontiers Science Center for Deep Ocean Multispheres and Earth System, Key Lab of Submarine Geosciences and Prospecting Techniques, MOE and College of Marine Geosciences, Ocean University of China, Qingdao 266100, China
4.
Laboratory for Marine Mineral Resources, Qingdao National Laboratory for Marine Science and Technology, Qingdao 266237, China

Received Date: 2021-09-24
Publish Date: 2022-09-25

Abstract

Abstract

The Mohe basin is located in the southern margin of the eastern Mongol-Okhotsk suture zone (MOSB), which is an excellent window for studying the evolution of the eastern Mongol-Okhotsk Ocean. In this paper, four sandstone samples from the Xiufeng Formation in the eastern margin of the Mohe basin were analyzed by petrography, chronology and geochemistry. The results show that the sandstone debris of the Xiufeng Formation has poor roundness and sorting, and shows the characteristics of near-source denudation. A total of 217 concordant ages were obtained from U-Pb zircon dating, divided into three age groups, and the peak ages of all concordant ages correspond identically to the regional magmatic activities on the Erguna Block. LA‐ICP‐MS U-Pb zircon dating yields the youngest concordant ages of 158±2 Ma (N=5) for the Xiufeng Formation. Based on the previous research results, we try to limit the evolution of the Mongol-Okhotsk Ocean and even the eastern part of the Central Asian Orogenic Belt. All samples are enriched in large ion lithophile elements (LILEs) and light rare earth elements (LREEs), depleted in high field strength elements (HFSEs) and heavy rare earth elements (HREEs), and have obvious negative Eu anomalies. The lithology of the source rocks is mainly felsic from the upper crust and is situated in active continental margins. The continental island arc provides the sediments in the Xiufeng Formation in the south of the Mohe basin, the Erguna block and the old basement of the basin. The provenance is located in the tectonic environment of the continental island arc, which is related to the southward subduction, collision and closure of the Mongol-Okhotsk Ocean in the Late Jurassic. Based on all the evidence above, we can infer that the Mongol-Okhotsk Ocean was still in the subduction stage and did not close during the sedimentation of the Xiufeng Formation (ca. 158 Ma). Combined with previous data, it is inferred that the final closure of the Mongol-Okhotsk Ocean may be limited between the Late Jurassic and Early Cretaceous.
- Mohe basin,
- Mongol-Okhotsk Ocean,
- Central Asian Orogenic Belt,
- Xiufeng Formation,
- Zircon U-Pb age,
- geochemistry

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References(79)

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Geochronology and Provenance Analysis of the Xiufeng Formation in Mohe Basin: Implications for the Evolution of the Eastern Mongol-Okhotsk Ocean

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