大兴安岭索伦地区哲斯组碎屑岩地球化学特征和锆石U-Pb年龄对沉积物源属性约束

doi:10.13278/j.cnki.jjuese.20190324

Abstract

Abstract: This paper focused on the clastic rocks of the Middle Permian Zhesi Formation, well exposed in the Haoren Town, Suolun region of Inner Mongolia. Geochemistry and zircon geochronology analyses were conducted, in order to constrain the ages and origins of sediment provenance. The dating results show that the U-Pb ages of detrital zircons from the Zhesi Formation sandstone can be divided into six groups, i.e., 282-244 Ma, 352-294 Ma, 468-379 Ma, 513-482 Ma, 802-580 Ma, and 2 500-1 800 Ma, respectively. Geochemically, the sandstone samples have high SiO₂, and low Fe₂O₃, FeO, and MgO contents, indicating they were mainly deposited from felsic rocks. Rare earth elements and trace elements characteristics and tectonic distinguished diagrams suggest the sediment source region of the Middle Permian Zhesi Formation dominantly displays similar features with those of continental arc and active continental margin, with minor corresponding to passive continental margin. The former setting is the results of the amalgamation-collision of the Jiamusi-Mongolia block and northwards subduction of the south branch of the Paleo-Asian Ocean during different stages, while the later one probably reflects the tectonic setting of the generation of some basement rocks. Considering the facts that:1) the study region is located in the southeastern Xing'an block, far away form the North China craton; 2) the Zhesi Formation clastic rocks mainly consist of feldspar lithic sandstone, lithic feldspar sandstone, and lithic sandstone with relatively low structure and ingredient maturity, suggesting characteristics of near-source deposition; and 3) the coeval igneous rocks in the surrounding regions were all formed in subduction-related settings, it is proposed here that the Zhesi Formation was most likely deposited in a back-arc or inter-arc basin related with the northwards subduction of the south branch of the Paleo-Asian Ocean beneath the Jiamusi-Mongolia block, and their provenance was dominantly from the subduction-related igneous rocks in the southern margin of the Jiamusi-Mongolia block, with little contributions from ancient basement of the Jiamusi-Mongolia block.

Key words: detrital zircon ages, geochemistry, provenance analyses, Zhesi Formation, Suolun region of Inner Mongolia

CLC Number:

P588.2

He Zhonghua, Wang Qizhi, Wang Qiang. Geochemistry and Zircon U-Pb Ages of Clastic Rocks of Zhesi Formation in Suolun Region, Great Xing’an Range: Constraints on Origins of Sediment Provenance[J].Journal of Jilin University(Earth Science Edition), 2020, 50(2): 405-424.

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Geochemistry and Zircon U-Pb Ages of Clastic Rocks of Zhesi Formation in Suolun Region, Great Xing’an Range: Constraints on Origins of Sediment Provenance

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