辽东弓长岭—岫岩地区古元古界辽河群变沉积岩的物源及构造背景

doi:10.13278/j.cnki.jjuese.20190225

Abstract

Abstract: Gongchangling-Xiuyan area is located in the eastern part of the Jiao-Liao-Ji orogenic belt, where thick layers of the Paleoproterozoic metasedimentary rocks are developed. We studied on these metamorphic sedimentary rocks in petrography and zircon U-Pb chronology. The petrographic characteristics show that the metamorphic degree of these rocks is low, overall greenschist facies metamorphism with no highly metamorphosed minerals formed. Quartz is the main mineral in the rocks, and carbonate minerals are common in the North Liaohe Group. The distinct oscillatory zoning and high Th/U ratios (>0.3) of detrital zircons in the Paleoproterozoic metasedimentary rock suggest these zircons are of magmatic origin. Combining the data of U-Pb geochronology, we found that detrital zircons from the Li’eryu, Gaojiayu, Dashiqiao and Gaixian Formations yield age peaks at 2 159 Ma, 2 500 Ma, 2 189/2 530 Ma, and 2 044/2 197 Ma, respectively, indicating that their sediments are from the Liao-Ji Paleoproterozoic granitoids and the adjacent Archean complex. Combining the data of previous researches, We considered that the South and North Liaohe Groups formed in the same tectonic setting and underwent the same evolution process. Therefore, the Paleoproterozoic arc-continent collision model may be more applicable to interpret the evolution of the Jiao-Liao-Ji orogenic belt.

Key words: Liaodong Peninsula, Liaohe Group, detrital zircon, geochronology, provenance

CLC Number:

P588.3

Wang Chengzhi, Dong Yongsheng, Wang Pengsen, Chen Musen, Bai Xuerui. Provenance and Tectonic Setting of the Paleoproterozoic Metasedimentary Rocks from the Liaohe Group in Gongchangling-Xiuyan Area, East Liaoning Province[J].Journal of Jilin University(Earth Science Edition), 2020, 50(4): 941-956.

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Provenance and Tectonic Setting of the Paleoproterozoic Metasedimentary Rocks from the Liaohe Group in Gongchangling-Xiuyan Area, East Liaoning Province

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