大兴安岭中北段老道口闪长岩锆石U-Pb年龄、地球化学特征及构造意义

doi:10.13278/j.cnki.jjuese.201602115

Abstract

Abstract:

Laodaokou unit is located in Oroqen Autonomous Banner, Inner Mongolia, the east of Xing'an Mongolian orogenic belt, northern Great Xing'an Range. The unit is mainly composed of diorite, adamellite, and dioritic porphyrite. SIMS U-Pb dating of zircon of the diorite provides the age of (126.09±0.95) Ma, indicating that the plution was formed in Early Cretaceous instead of Cambrian as thought before. The major element data show that the diorites contains 56.13%-57.91% of SiO₂, 0.97%-0.99% of TiO₂, 2.00%-2.12% of MgO, 6.73%-7.41% of TFe₂O₃, 36.00-38.00 of Mg^#, 4.29%-4.53% of Na₂O, 1.38%-1.59% of K₂O, 17.95%-18.36% of Al₂O₃. The K₂O/Na₂O ratios range from 0.31 to 0.37. The diorites are rich in alumina and sodium relatively. The rare earth elements chondrite standardized curves show that they are rich in light REE and depleted of heavy REE with weak negative δEu (0.85-0.87). Laodaokou plution is rich in large ion lithophile element (LILE)(e.g., Ba、K、Rb、Th、U), but depleted of high field strength elements (HFSE) (e. g., Nb、Ta、Ti、and P). The geochemical signatures above imply a characteristic related to subduction, and this suggests that the magmatic source of Laodaokou diorites were from the lithospheric mantle, which was metasomatosed by subduction fluid. Combining with the geochemical characteristics of Laodaokou plution and its regional tectonic settings, we conclude that the plution might be formed under a lithospheric extension after the closure of Mongolia-Okhotsk Ocean.

Key words: SIMS ziron U-Pb dating, Mongolia-Okhotsk suture zone, diorite, lithospheric mantle, Laodaokou diorites, Xing'an Mongolian orogenic belt

CLC Number:

P588.12

Liu Yongjiang, Liu Binqiang, Feng Zhiqiang, Wen Quanbo, Li Weimin, Zhang Tiean, Li Xiaoyu, Du Bingying. SIMS Zircon U-Pb Age, Petrogeochemistry and Its Tectonic Implication of Laodaokou Diorite in the Mid-North Part of Great Xing'an Range[J].Journal of Jilin University(Earth Science Edition), 2016, 46(2): 482-498.

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SIMS Zircon U-Pb Age, Petrogeochemistry and Its Tectonic Implication of Laodaokou Diorite in the Mid-North Part of Great Xing'an Range

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