额尔古纳地块韩家园子‒富林地区中生代火成岩的成因及其对蒙古‒鄂霍茨克洋演化的启示

刘博; 王一丁; 文韵琪; 韩宝福

doi:10.3799/dqkx.2022.065

Volume 47 Issue 9

Sep. 2022

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Liu Bo, Wang Yiding, Wen Yunqi, Han Baofu, 2022. Geochronology and Geochemistry of Mesozoic Igneous Rocks in the Hanjiayuanzi⁃Fulin Area of the Erguna Massif: Constraints on the Tectonic Evolution of the Mongol⁃Okhotsk Ocean. Earth Science, 47(9): 3316-3333. doi: 10.3799/dqkx.2022.065

Citation:

Liu Bo, Wang Yiding, Wen Yunqi, Han Baofu, 2022. Geochronology and Geochemistry of Mesozoic Igneous Rocks in the Hanjiayuanzi⁃Fulin Area of the Erguna Massif: Constraints on the Tectonic Evolution of the Mongol⁃Okhotsk Ocean. Earth Science, 47(9): 3316-3333. doi: 10.3799/dqkx.2022.065

Citation:

Liu Bo, Wang Yiding, Wen Yunqi, Han Baofu, 2022. Geochronology and Geochemistry of Mesozoic Igneous Rocks in the Hanjiayuanzi⁃Fulin Area of the Erguna Massif: Constraints on the Tectonic Evolution of the Mongol⁃Okhotsk Ocean. Earth Science, 47(9): 3316-3333. doi: 10.3799/dqkx.2022.065

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Geochronology and Geochemistry of Mesozoic Igneous Rocks in the Hanjiayuanzi⁃Fulin Area of the Erguna Massif: Constraints on the Tectonic Evolution of the Mongol⁃Okhotsk Ocean

doi: 10.3799/dqkx.2022.065

1.
Key Laboratory of Ministry of Education on Safe Mining of Deep Metal Mines, College of Resources and Civil Engineering, Northeastern University, Shenyang 110819, China
2.
Key Laboratory of Orogenic Belts and Crustal Evolution of Ministry of Education, School of Earth and Space Sciences, Peking University, Beijing 100871, China

Received Date: 2022-02-21
Publish Date: 2022-09-25

Abstract

Abstract

The Hanjiayuanzi-Fulin area in the eastern Erguna Massif, located adjacent to the Mongol-Okhotsk suture zone, is characterized by numerous Early Jurassic to Early Cretaceous igneous rocks, which is important to reconstruct the subduction and closure history of the Mongol-Okhotsk Ocean. In this study, we present new petrology, LA-ICP-MS zircon U-Pb ages and whole-rock geochemical data for the Mesozoic igneous rocks from the Hanjiayuanzi-Fulin area. Zircon U-Pb ages of Hanjiayuanzi K-feldspar granite and Fulin trachyandesite are 196±2 Ma and 122±2 Ma, corresponding to the Early Jurassic and Early Cretaceous, respectively. The K-feldspar granite belongs to metaluminous Ⅰ-type granite, with low Mg^# value (36) and Nb/Ta ratios (16.55-17.05) close to the primitive mantle, which could be derived from partial melting of the juvenile lower crust. It is enriched in large ion lithophile elements (LILEs, e.g., Rb, Ba, K), and depleted in high field strength elements (HFSEs, e.g., Nb, Ta, Ti), showing the geochemical characteristics of typical arc igneous rocks. Combined with the spatial distribution of contemporary metaluminous-weakly peraluminous Ⅰ-type granites, we propose that the Early Jurassic Hanjiayuanzi K-feldspar granite may be related to the southward subduction of the Mongol-Okhotsk Ocean beneath the Erguna massif. By contrast, the trachyandesite has lower SiO₂ contents (59.67%-59.93%), higher Mg^# values (42-43), and is also enriched in LILEs and depleted in HFSEs. Besides, it has an enrichment of Sr and depletion of Th, suggesting an origin from the enriched lithospheric mantle. Based on the regional distribution of Early Cretaceous calc-alkaline volcanic rocks, A-type granites and metamorphic core complexes, we suggest that the Early Cretaceous trachyandesite was formed in an extensional environment after the closure of the Mongol-Okhotsk Ocean. Combined with published data from igneous and sedimentary rocks, the closure time of the Mongol-Okhotsk Ocean in the northern Great Xing'an Range is suggested to be between latest Late Jurassic and earliest Early Cretaceous (~150-140 Ma).
- Mongol-Okhotsk Ocean,
- Erguna massif,
- Early Jurassic,
- Early Cretaceous,
- igneous rocks,
- geochemistry

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致谢: 感谢主编和三位匿名审稿人所提出的修改意见.感谢自然资源部东北亚矿产资源评价重点实验室郝宇杰博士在实验过程中给予的帮助.中山大学博士研究生吴宜翰参与了野外工作，论文修改过程中河北地质大学唐宗源博士给予了修改意见，在此一并感谢！

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Geochronology and Geochemistry of Mesozoic Igneous Rocks in the Hanjiayuanzi⁃Fulin Area of the Erguna Massif: Constraints on the Tectonic Evolution of the Mongol⁃Okhotsk Ocean

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