Detrital composition of Tiesiao Formation and Liangjiehe Formation of Nanhua System in Songtao Highland of the northeastern Guizhou Province and tectonic setting of its source regions
LONG Jianxi1, ZHOU Qi1, ZHANG Sui2, ZHU Luyan3, YANG Zhongqin1
1. Guizhou Geology Institution, Guizhou Guiyang 550081, China; 2. No.103 Geology Team, Guizhou Geology and Mineral Development Bureau, Guizhou Tongren 554300, China; 3. Guizhou Geology and Mineral Center, Guizhou Guiyang 550018, China
Abstract：The tectonic properties of Xuefeng movement has significant controversies. This study anglyzed the terrigenous detrital composition of Tiesiao Formation and Liangjiehe Formation of Nanhua System in Songtao Highland of the northeastern Guizhou Province, using Dickinson triangle diagrams theory. The results show that the terrigenous detrital source mainly comes from arc orogen sources and recycled orogen provenances, accompanied by volcanic activities. The maturity of the detrital components in Tiesiao Formation is relatively low, and the components mainly landed around the volcanic arc source area, showing the characteristics of near erosion and transporting accumulation. The quartz content in Liangjiehe Formation is higher than that in Tiesiao Formation, which lands in the recycled orogen provenances. The detrital composition contains basalt, andesitic basalt, trachyte, tuff, ignimbrite, rhyolite, felsic mylonites and so on, indicating that intracontinental rift and intraplate orogenic mechanism occurred during or before the sedimentation of Tiesiao Formation and Liangjiehe Formation in the study area. This research could provide some microscopic evidence for tectonic attribute of Xuefeng movement.
龙建喜, 周琦, 张遂, 朱路艳, 杨忠琴. 黔东北松桃高地南华系铁丝坳组和两界河组碎屑组分及源区背景[J]. 中国地质调查, 2024, 11(4): 42-49.
LONG Jianxi, ZHOU Qi, ZHANG Sui, ZHU Luyan, YANG Zhongqin. Detrital composition of Tiesiao Formation and Liangjiehe Formation of Nanhua System in Songtao Highland of the northeastern Guizhou Province and tectonic setting of its source regions. , 2024, 11(4): 42-49.
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