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Basement Structure and Properties of the Western Junggar Basin, China
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  • 英文篇名:Basement Structure and Properties of the Western Junggar Basin, China
  • 作者:Junmeng ; Zhao ; Shuze ; Chen ; Gong ; Deng ; Xuezhong ; Shao ; Heng ; Zhang ; Jamshed ; Aminov ; Xinfa ; Chen ; Zongjin ; Ma
  • 英文作者:Junmeng Zhao;Shuze Chen;Gong Deng;Xuezhong Shao;Heng Zhang;Jamshed Aminov;Xinfa Chen;Zongjin Ma;Chinese Academy of Sciences(CAS)Center for Excellence in Tibetan Plateau Earth Sciences;Key Laboratory of Continental Collision and Plateau Uplift,Institute of Tibetan Plateau Research,Chinese Academy of Sciences;University of Chinese Academy of Sciences;Institute of Geology,China Earthquake Administration;Xinjiang Oilfield Company;
  • 英文关键词:Junggar Basin;;seismically-converted wave;;joint inversion of gravity and geomagnetism;;basement structure
  • 中文刊名:Journal of Earth Science
  • 英文刊名:地球科学学刊(英文版)
  • 机构:Chinese Academy of Sciences(CAS)Center for Excellence in Tibetan Plateau Earth Sciences;Key Laboratory of Continental Collision and Plateau Uplift,Institute of Tibetan Plateau Research,Chinese Academy of Sciences;University of Chinese Academy of Sciences;Institute of Geology,China Earthquake Administration;Xinjiang Oilfield Company;
  • 出版日期:2019-04-11
  • 出版单位:Journal of Earth Science
  • 年:2019
  • 期:02
  • 基金:supported by the Major Program of the National Natural Science Foundation of China (No. 41490611);; the Joint Research Projects between the Pakistan Science Foundation and the National Natural Science Foundation of China (No. 41661144026);; the Detailed Lithospheric Structure and Deep Processes of the Tibetan Main Collision Zone (No. 2016YFC0600301)
  • 语种:英文;
  • 页:5-17
  • 页数:13
  • CN:42-1788/P
  • ISSN:1674-487X
  • 分类号:P631.4;P548
摘要
A comprehensive geophysical profile stretching from Qingyijing at the southern edge of the Junggar Basin to Ubara on the northern margin of the Junggar Basin was conducted in an attempt to probe the crustal structure of the western Junggar Basin(hereafter referred to simply as ‘the Basin'), and, in particular, the structure and property of the Basin's crystalline basement. A survey using seismically converted waves was conducted along this profile to determine the characteristics of the P-and Swave velocities typical of the crust and uppermost mantle. A joint inversion of gravitation and aeromagnetic data was also performed to acquire the density and magnetization intensity values found beneath the western Basin. This research revealed that the Basin is composed of the so-called Manasi terrain in the south, and the Wulungu terrain in the north. Their boundary is located along the WNW-trending Dishuiquan-Sangequan suture, linking the NE-striking Da'erbute suture(DS) in the west, and the WNWtrending Kalameili suture(KS) in the east. In its northern part, the Wulungu-type terrain has a doublelayered basement, of which the upper layer is a folded basement of Hercynian orogenic origin, and the lower layer is a crystalline basement of Middle–Upper Proterozoic age. The southern part of the Basin, i.e., the Manasi terrain, has a single-layered crystalline basement. The folded basement here is too thin to be clearly distinguished.
        A comprehensive geophysical profile stretching from Qingyijing at the southern edge of the Junggar Basin to Ubara on the northern margin of the Junggar Basin was conducted in an attempt to probe the crustal structure of the western Junggar Basin(hereafter referred to simply as ‘the Basin'), and, in particular, the structure and property of the Basin's crystalline basement. A survey using seismically converted waves was conducted along this profile to determine the characteristics of the P-and Swave velocities typical of the crust and uppermost mantle. A joint inversion of gravitation and aeromagnetic data was also performed to acquire the density and magnetization intensity values found beneath the western Basin. This research revealed that the Basin is composed of the so-called Manasi terrain in the south, and the Wulungu terrain in the north. Their boundary is located along the WNW-trending Dishuiquan-Sangequan suture, linking the NE-striking Da'erbute suture(DS) in the west, and the WNWtrending Kalameili suture(KS) in the east. In its northern part, the Wulungu-type terrain has a doublelayered basement, of which the upper layer is a folded basement of Hercynian orogenic origin, and the lower layer is a crystalline basement of Middle–Upper Proterozoic age. The southern part of the Basin, i.e., the Manasi terrain, has a single-layered crystalline basement. The folded basement here is too thin to be clearly distinguished.
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