吉林省下三叠统卢家屯组LA-ICP-MS锆石U-Pb定年及其地质意义

doi:10.13278/j.cnki.jjuese.201502110

Abstract

Abstract:

According to the associated lithologic feature, the Lujiatun Formation is divided into Yingbeishan conglomerate section, Loudoushan variegated rock section, and Yangshuhezi black rock section. Based on the fossil assemblages, such as Palaeanodonta-Palaeomutela fauna, Pleuroneia? sp. and the conchostracan, it was formed in Permian. A systematic U-Pb isotopic chronology of the detrital zircon is studied for the Bottom, Middle, and Upper Section of the construction profiles of Lujiatun Formation in Yingbeishan-Shuangdingshan in Jiutai. The results show three minimum zircon age peaks at (283.4±7.9) Ma, (262.4±3.9) Ma, and (255.5±5.8) Ma from the bottom to the top. It can be confirmed that the top section of the formation belonged to the Late Permian. The detrital zircon ages of 1 800 Ma and 2 500 Ma in the Lujiantun Group are typical for the base plate age of North China Plate. In conclusion, the plate closure happened probably during P₃-T₁ between the northern margin of North China Plate and the group of plates to its north.

Key words: Lujiatun Formation, Lower Triassic, detrital zircon, zircon LA-ICP-MS U-Pb age, Jilin Province

CLC Number:

Nie Lijun, Yu Hongbin, Zhang Jianze, Wang Cong, Li Dong, Li Yang. Zircons LA-ICP-MS U-Pb Ages of the Lower Triassic Lujiatun Group and Its Geological Significance in Jilin Province[J].Journal of Jilin University(Earth Science Edition), 2015, 45(2): 453-470.

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Zircons LA-ICP-MS U-Pb Ages of the Lower Triassic Lujiatun Group and Its Geological Significance in Jilin Province

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