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ZHAN Junyan, QIN Xiaofeng, WANG Zongqi, CAO Jie, PANG Baocheng, ZHAO Guoying, SHI Hao, WANG Zhen. 2020. Detrital zircon U-Pb geochronology of Late Paleozoic sandstone intercalations of siliceous rock sequences in Bancheng area, southern Guangxi: Constraint on depositional provenance[J]. Geology in China, 47(3): 839-852. doi: 10.12029/gc20200320
Citation: ZHAN Junyan, QIN Xiaofeng, WANG Zongqi, CAO Jie, PANG Baocheng, ZHAO Guoying, SHI Hao, WANG Zhen. 2020. Detrital zircon U-Pb geochronology of Late Paleozoic sandstone intercalations of siliceous rock sequences in Bancheng area, southern Guangxi: Constraint on depositional provenance[J]. Geology in China, 47(3): 839-852. doi: 10.12029/gc20200320
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Detrital zircon U-Pb geochronology of Late Paleozoic sandstone intercalations of siliceous rock sequences in Bancheng area, southern Guangxi: Constraint on depositional provenance

  • 1.

    College of Earth Science, Guilin University of Technology, Guilin 541004, Guangxi, China

  • 2.

    Guangxi Key Laboratory of Hidden Metallic Ore Deposits Exploration, Guilin University of Technology, Guilin 541004, Guangxi, China

  • 3.

    Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing 100037, China

  • 4.

    Center of Oil & Gas Survey, China Geological Survey, Beijing 100029, China

    • Fund Project: Supported by the National Natural Science Foundation of China(No.41362006), the National Natural Science Foundation of Guangxi(No.2013GXNSFAA019272), Talent Introduction Research Start- up Funds of Guilin University of Technology (No.002401003364), the Program of China Geological Survey (No.12120114039501, No.1212011085408, No.DD20160124)
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  • Author Bio: ZHAN Junyan, male, born in 1991, master candidate, majors in geology; E-mail: 332088985@qq.com
  • Corresponding author: QIN Xiaofeng, male, born in 1969, professor, supervisor of master candidates, engages in structural geology and petrology; E-mail:qxf@glut.edu.cn 
Received Date:  05 January 2017
Revised Date:  15 January 2018
Publish Date:  25 June 2020
    Abstract

  • Situated in the southwestern segment of Qinzhou-Hangzhou joint belt, Bancheng area of southern Guangxi is a pivotal area in understanding the geological tectonic evolution history of South China since the Paleozoic. Late Devonian to late Permian siliceous rock sequences are outcropped in this area. In recent years, the authors conducted systematic field geological survey and found that there exist a series of siltstone intercalations in late Paleozoic siliceous rock sequences of the Shiti reservoir in Bancheng Town, Qinzhou City. In this paper, LA-MC-ICP-MS U-Pb isotopic dating was performed for detrital zircons from two siltstone intercalation samples of the lower and upper late Paleozoic siliceous rock sequences. Detrital zircon U-Pb age spectra shows that there are four main age groups of 407-573 Ma (early Paleozoic), 644-954 Ma (Neoproterozoic), 1124-1636 Ma (Mesoproterozoic) and 2368-2548 Ma (Early Paleoproterozoic-late Neoarchean), which recorded four major tectonic thermal events in this area. These four periods of tectonic thermal events are consistent with the ages of widely developed magmatic rocks in Yunkai area of the Cathaysia Block, indicating that Yunkai area might have been major depositional provenance for the siltstone intercalations of late Paleozoic siliceous rock sequences. The depositional provenances of the lower and upper late Paleozoic siliceous rock sequences are significantly different, and there is a general tendency toward increasing complex and relatively older age of detrital zircon from the lower to the upper of late Paleozoic siliceous rock sequences, indicating that the Yunkai Block has experienced rapidly erosion and uplift process after Caledonian orogeny in the southwestern segment of Qinzhou-Hangzhou joint belt. Detrital zircon U-Pb age spectra of the sandstone intercalations of late Paleozoic siliceous rock sequences imply that the Qinzhou-Fangchang Basin was in an extension tectonic setting in Late Paleozoic period.

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