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BI Chengbin, YU Niuben, LU Guansong, NIJIATI·Abuduxun, PAN Fei, MABI Awei. 2019. Redetermination and disintegration of the continental volcanic strata of the former Santanghu Formation in Oetonggar area, Eastern Junggar Basin[J]. Geology in China, 46(6): 1384-1395. doi: 10.12029/gc20190610
Citation: BI Chengbin, YU Niuben, LU Guansong, NIJIATI·Abuduxun, PAN Fei, MABI Awei. 2019. Redetermination and disintegration of the continental volcanic strata of the former Santanghu Formation in Oetonggar area, Eastern Junggar Basin[J]. Geology in China, 46(6): 1384-1395. doi: 10.12029/gc20190610
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Redetermination and disintegration of the continental volcanic strata of the former Santanghu Formation in Oetonggar area, Eastern Junggar Basin

  • 1.

    Northwestern Jiangxi Geological Party, Bureau of Geology and Exploration and Development of Mineral Researches of Jiangxi Province, Jiujiang 332000, Jiangxi, China

  • 2.

    Xinjiang Key Laboratory of Orogenic Belts, Continental Dynamics and Metallogenic Prediction, Urumqi 830047, Xinjiang, China

  • 3.

    Xinjiang University, Urumqi 830047, Xinjiang, China

  • 4.

    Chengdu University of Technology, Chengdu 610059, Sichuan, China

    • Fund Project: Supported by the Xinjiang Uygur Autonomous Region for Central Government Return of Two Rights Price Items (A15-1-LQ04)
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  • Author Bio: BI Chengbin, male, born in 1963, senior engineer, majors in the study of geology and mineral resources; E-mail: bcb715@qq.com
  • Corresponding author: YU Niuben, male, born in 1990, engineer, majors in the research on geological resources and geological engineering; E-mail:820707631@qq.com 
Received Date:  29 July 2018
Revised Date:  21 April 2019
Publish Date:  25 December 2019
    Abstract

  • In this paper,the authors studied the comparison between lithologic assemblage and lithofacies assemblage SHIRIMP zircon U-Pb dating results and fossil chronology,and believed that the continental volcanic rocks of the former Santanghu Formation in Oetonggar area of Eastern Junggar Basin should be redefined as the Batamayineishan Formation. It is suggested that the widely distributed continental volcanic rocks at the northeast edge of Junggar Basin should be decomposed into the Batamayineishan Formation and the Santanghu Formation according to the geological age. The Santanghu Formation only represents the early Permian continental volcanic rocks. The study of chronology shows that the age of the Batamayineishan Formation in Oetolanagar is time-penetrating. The age of the first lithologic segment is (335.6±6.5)Ma,and the age of the second lithologic segment is (320.5±7.1)Ma,suggesting that the rocks belong to the late lower Carboniferous period to the upper Carboniferous period. Thus,the dispute over the lower and upper Carboniferous system for the Batamayineishan Formation has been solved. According to the comprehensive study,this set of continental volcanic rocks belongs to tectono-magmatic activities in the East Junggar tectonic belt from west to east under the background of chain suture. The residual ocean basin disappeared until the beginning of continental volcanic activity; in addition,it was affected by the tension environment on the western side and the island arc environment on the eastern side. Volcanic mechanisms,structures,and intermittent eruptions of the Batamayineishan Formation in the Oetanagar region suggest that it has petroleum geological significance.

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