内蒙古索伦地区上二叠统林西组碎屑岩地球化学特征及其对物源的指示意义

doi:10.13278/j.cnki.jjuese.201606114

Abstract

Abstract: The provenanceof the Linxi Formation in Solonker area was greatly influenced by the closure of the Paleo-Asian Ocean occurred in the Late Paleozoic. A comprehensive analysis of the element geochemical characteristics of the clastic rock has been done to study the source rock types and the tectonic setting of the Linxi Formation in the Solonker area. The major elements compositions indicated that the early sediments was of low weathering degree from the first depositional cycle and the latter sediments was of moderate weathering degree from the first depositional cycle or recycled deposition, and the igneous rock was the primary source rock. The trace elements and rare earth elements characteristics demonstrated a dissected magmatic arc dominated tectonic setting for the source rock of Linxi Formation. The intermediate and alkaline igneous rocks from the upper crust were the primary source rocks, with lower content of sedimentary rock. The indicator (Gd/Yb)_n showed the early sediments was from the Archean alkaline igneous rocks. Comprehensive analysis showed that the provenances of the Linxi Formation were jointly derived from the north margin of the North China plate in the south and the Sonid Zuoqi-Xilinhot-sourthern Xiwuqi magma arc in the north.

Key words: geochemical, provenance, tectonic setting, Linxi Formation, Solonker area

CLC Number:

P588.21

Li Fulai, Xiao Fei, Meng Fanchao, Ren Zeying. Geochemical Characteristics and Implication for Provenance of Upper Permian Linxi Formation Clastic Rocks in Solonker Area, Inner Mongolia[J].Journal of Jilin University(Earth Science Edition), 2016, 46(6): 1769-1780.

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Geochemical Characteristics and Implication for Provenance of Upper Permian Linxi Formation Clastic Rocks in Solonker Area, Inner Mongolia

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