Abstract In this study, the sandstone samples obtained from two profiles including the Jinsuoguan of Tongchuan and the Liuye river of Zhouzhi area, are selected as the research object. It aims at understanding the Middle-Late Triassic source composition and transformation in the southern margin of Ordos Basin and the coupling mechanism of basin and mountain. By means of the petrography, detrital zircon U-Pb geochronology and geochemistry analysis, the changes of the source composition in the southern margin of the Ordos Basin are investigated, and tectonic coupling mechanism between the basin and mountain are explored. It shows that five groups of ages for the Upper Triassic detrital zircons in the Jinsuoguan profile are found: 237-330 Ma, 390-480 Ma, 870-1230 Ma, 1740-1980 Ma, 2070-2732 Ma. Four groups of age are found in the Middle Triassic detrital zircon: 240-290 Ma, 1760-1840 Ma, 2250-2300 Ma, 2350-2700 Ma. Five groups of age are discovered in the Upper Triassic detrital zircon found in the northern Ordos Basin: 244-310 Ma, 360-600 Ma, 800-1300 Ma, 1700-2100 Ma and 2450-2550 Ma. Based on the comparison of sediment source, it confirms that the Middle Triassic sediment provenance of the south margin of the Ordos Basin is from the North China Craton, Xing’anling-Mongolian Orogenic Belt and the Alxa region. The Late Triassic provenance of the sand bodies is from the North China Craton, Alxa region, West Qinling, the Northern Qinling and Qilianshan Orogenic Belt. The deduction is also supported by petrological characteristics and the transformation of the tectonic setting in the source area. The Middle Triassic provenance transformation is related to the activation of the Qinling Orogenic Belt in the south margin of Ordos Basin and the transformation of the basin pattern.
Fund:Co-funded by the Central University Basic Scientific Research Operating Expenses(No.2652017458),National Science and Technology Major Projects of China(No. 2017ZX05005-002)
Corresponding Authors:
Ruan Zhuang,born in 1983,is an associate professor and master tutor. He is mainly engaged in researches on petroleum geology and sedimentary geology. E-mail: ruanz0103@cugb.edu.cn.
About author: Liu Shuai,born in 1993,is a master candidate. He majors in sedimentary geology. E-mail: 1181234277@qq.com.
Cite this article:
Liu Shuai,Ruan Zhuang,Yang Zhi-Hui et al. Provenance evolution of southern margin of Ordos Basin during the Middle-Later Triassic and its geological implication[J]. JOPC, 2019, 21(6): 939-958.
Liu Shuai,Ruan Zhuang,Yang Zhi-Hui et al. Provenance evolution of southern margin of Ordos Basin during the Middle-Later Triassic and its geological implication[J]. JOPC, 2019, 21(6): 939-958.
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