内蒙古西乌旗迪彦庙蛇绿岩带内辉长岩地球化学及年代学

doi:10.13278/j.cnki.jjuese.20200011

Abstract

Abstract: The Diyanmiao ophiolite in the west Ujimqin Banner, Inner Mongolia, which tectonically belongs to the Xilinhaote Late Paleozoic fold belt in the southeastern Central Asian orogenic belt, is located between the Erlianhot-Hegenshan ophiolite belt and the Jiaoqier-Xilinhaote ophiolite belt. This study focuses on the geochemical and geochronological characteristics of the gabbros from the Diyanmiao ophiolite. Whole-rock geochemical data show that the gabbros are high Al, lower K, lower Na, and tholeiitic in nature, with w(SiO₂) of 45.49%~50.48%, w(Al₂O₃) of 13.31%~17.05%, w(K₂O) of 0.01%~0.65%, w(Na₂O) of 0.30%~4.15%, w(CaO) of 8.00%~19.54%, w(MgO) of 5.22%~10.92%, and w(P₂O₅) of 0.03%~0.23%. These rocks have low total REE contents and relatively enriched HREE. They also show enrichments in K, Ta, and Sr, and depletions in Nb, Zr, Hf, and Ti. La-ICP-MS zircon U-Pb dating results suggest that the gabbros were formed at Early Carboniferous ((345.3±2.3) Ma). In combination with previously works and regional geology, the authors propose that the gabbros in the Diyanmiao ophiolite were possibly formed by fluids metasomatism in an island arc setting during oceanic subduction, rather than crystallization and differentiation processes.

Key words: Diyanmiao, geochemistry, zircon U-Pb dating, ophiolite, gabbro

CLC Number:

P588.12

Xiong Guangqiang, Liu Min, Zhang Da, Wang Zhong. Geochemistry and Geochronology of Gabbro in Diyanmiao Ophiolite Belt, West Ujimqin Banner, Inner Mongolia[J].Journal of Jilin University(Earth Science Edition), 2020, 50(5): 1599-1614.

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Geochemistry and Geochronology of Gabbro in Diyanmiao Ophiolite Belt, West Ujimqin Banner, Inner Mongolia

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