额尔古纳地块中生代火山岩盆地基底构造特征:来自灵泉盆地的启示

张丽; 刘永江; 冯志强; 李伟民; 温泉波; 梁琛岳; 郇恒飞; 孟婧瑶; 周建平; 阳正勇

doi:10.3799/dqkx.2017.141

Volume 42 Issue 12

Dec. 2017

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Article Navigation > Earth Science > 2017 > 42(12): 2229-2242

Zhang Li, Liu Yongjiang, Feng Zhiqiang, Li Weimin, Wen Quanbo, Liang Chenyue, Huan Hengfei, Meng Jingyao, Zhou Jianping, Yang Zhengyong, 2017. Basement Structural Features of Mesozoic Volcanic Basins in Erguna Massif: Implications from Lingquan Basin. Earth Science, 42(12): 2229-2242. doi: 10.3799/dqkx.2017.141

Citation:

Zhang Li, Liu Yongjiang, Feng Zhiqiang, Li Weimin, Wen Quanbo, Liang Chenyue, Huan Hengfei, Meng Jingyao, Zhou Jianping, Yang Zhengyong, 2017. Basement Structural Features of Mesozoic Volcanic Basins in Erguna Massif: Implications from Lingquan Basin. Earth Science, 42(12): 2229-2242. doi: 10.3799/dqkx.2017.141

Citation:

Zhang Li, Liu Yongjiang, Feng Zhiqiang, Li Weimin, Wen Quanbo, Liang Chenyue, Huan Hengfei, Meng Jingyao, Zhou Jianping, Yang Zhengyong, 2017. Basement Structural Features of Mesozoic Volcanic Basins in Erguna Massif: Implications from Lingquan Basin. Earth Science, 42(12): 2229-2242. doi: 10.3799/dqkx.2017.141

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Basement Structural Features of Mesozoic Volcanic Basins in Erguna Massif: Implications from Lingquan Basin

doi: 10.3799/dqkx.2017.141

1.
College of Earth Sciences, Jilin University, Changchun 130061, China
2.
Shenyang Institute of Geology and Mineral Resources, CGS, Shenyang 110034, China
3.
Department of Earth Science and Engineering, Taiyuan University of Technology, Taiyuan 030024, China
4.
Boome Pickens School of Geology, Oklahoma State University, Stillwater 74078, USA
5.
Geological Party No. 243, China National Nuclear Corporation, Chifeng 024006, China

Received Date: 2017-04-23
Publish Date: 2017-12-15

Abstract

Abstract

Characteristics of Bouguer gravity anomaly in the Lingquan basin indicate that lower gravity region on both sides of the basin is mainly the Jurassic-Cretaceous fault zone, the center is mainly a basement uplift. The upward continuation of the gravity anomaly is carried out, the results show that the upper surface of deep geological bodies has the characteristics of "east, west deep and center shallow"; the residual gravity anomaly also indicates that the local gravity of the central region mainly reflects the basement uplift, and the lower gravity of the eastern and western regions mainly reflects the fault of the Jurassic-Cretaceous. The basement faults of the Lingquan basin mainly are north and north-east, secondly is northwest, there are also early near north-south and east-west faults. The tectonic unit of the Lingquan basin is divided into the western fault zone, the central uplift zone and the eastern fault zone, we find that the Lingquan basin is actually an uplift rather than a graben basin, this is the result of tectonic inversion in the basin, other Mesozoic volcanic basins in the Erguna massif also have this model, and its basement is characterized by "shallow south deep north".
- Erguna massif,
- Lingquan basin,
- gravity anomaly,
- basement structure,
- geophysics

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References(37)

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