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2019 Vol. 46, No. 4
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Article navigation > Geology in China > 2019 > 46(4): 690-703
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YAN Jiayong, LÜ Qintian, LUO Fan, CHEN Anguo, YE Gaofeng, ZHANG Yongqian, ZHANG Kun, ZHAO Jinhua, ZHANG Chong, LIU Zhendong, LIU Yan. 2019. Where is Qinzhou-Hangzhou juncture belt? Evidence from integrated geophysical exploration[J]. Geology in China, 46(4): 690-703. doi: 10.12029/gc20190402
Citation: YAN Jiayong, LÜ Qintian, LUO Fan, CHEN Anguo, YE Gaofeng, ZHANG Yongqian, ZHANG Kun, ZHAO Jinhua, ZHANG Chong, LIU Zhendong, LIU Yan. 2019. Where is Qinzhou-Hangzhou juncture belt? Evidence from integrated geophysical exploration[J]. Geology in China, 46(4): 690-703. doi: 10.12029/gc20190402
shu

Where is Qinzhou-Hangzhou juncture belt? Evidence from integrated geophysical exploration

  • 1.

    Chinese Academy of Geological Sciences, Beijing, 100037, China

  • 2.

    China Deep Exploration Center, China Geological Survey & Chinese Academy of Geological Sciences, Beijing, 100037, China

  • 3.

    School of Geophysics and Measurement-control Technology, East China Institute of Technology, Nanchang 330013, Jiangxi, China

  • 4.

    Geological Survey of Anhui Province, Hefei 230001, Anhui, China

  • 5.

    School of Geophysics and Information Technology, China University of Geosciences, Beijing 100083, China

    • Fund Project: Supported by China Geological Survey Program (No. DD20160082, DD20190012), National Key R&D Program of China (No. 2016YFC0600201) and National Natural Science Foundation (No. 41574133, No. 41630320)
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  • Author Bio: YAN Jiayong, male, born in 1977, doctor, senior engineer, majors in mineral detecting and deep earth exploration; E-mail: yanjy@163.com
  • Corresponding author: LÜ Qingtian, male, born in 1964, doctor, professor, majors in deep earth exploration; E-mail:lqt@cags.ac.cn 
Received Date:  05 March 2019
Revised Date:  30 July 2019
Publish Date:  25 August 2019
    Abstract

  • The suture zone between the Yangtze Paleoplate and the Cathaysia Paleoplate (called Qin-Hang junction belt) is one of the most important tectonic-magmatic-metallogenic belts in southeastern China. There is still considerable controversy over the method of dividing the location and boundary of the western section of the Qin-Hang junction belt. In order to identify and determine the boundaries of the Qin-Hang junction belt, the authors employed the large-scale satellite gravity and magnetic data in combination with the integrated processing and analysis of regional magnetotelluric and broadband seismic data. The comprehensive evaluation shows that the Qin-Hang junction belt is the southern boundary of the Jiangnan orogenic belt. The authors hold that the border is Ningbo-Jinhua-Shangrao-Ganzhou-Chenzhou-Beihai in the south and Shanghai-Huzhou-Yingtan-LinchuanPingxiang-Hengyang-Yongzhou-Guilin-Wuzhou-Qinzhou in the north. On both sides of the joint belt, both the gravity field and the magnetic field have distinct characteristics, indicating the different material compositions and basements between the Yangtze and Cathaysia plates. There are also local differences in the geophysical fields of the Qin-Hang junction belt, suggesting that the tectonic belt has undergone multiple stage magmatism and formed different combinations of metal deposits in different sections, forming a unique metallogenic belt, i.e., the Qin-Hang metallogenic belt.

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