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中国航磁大地构造单元划分

熊盛青, 杨海, 丁燕云, 李占奎. 2018. 中国航磁大地构造单元划分[J]. 中国地质, 45(4): 658-680. doi: 10.12029/gc20180402
引用本文: 熊盛青, 杨海, 丁燕云, 李占奎. 2018. 中国航磁大地构造单元划分[J]. 中国地质, 45(4): 658-680. doi: 10.12029/gc20180402
XIONG Shengqing, YANG Hai, DING Yanyun, LI Zhankui. 2018. Subdivision of tectonic units in China based on aeromagnetic data[J]. Geology in China, 45(4): 658-680. doi: 10.12029/gc20180402
Citation: XIONG Shengqing, YANG Hai, DING Yanyun, LI Zhankui. 2018. Subdivision of tectonic units in China based on aeromagnetic data[J]. Geology in China, 45(4): 658-680. doi: 10.12029/gc20180402

中国航磁大地构造单元划分

  • 基金项目:
    中国地质调查局“中国陆域航磁特征及地质构造研究”项目(1212011087009)与国家863计划主题项目“航空地球物理遥感综合探测技术与解释系统研究”课题(2013AA063905)联合资助
详细信息
    作者简介: 熊盛青, 男, 1963年生, 教授级高级工程师, 博士生导师, 长期从事航空地球物理、遥感技术及其地学应用研究工作; E-mail:xsq@agrs.cn
  • 中图分类号: P544;P631.2+22

Subdivision of tectonic units in China based on aeromagnetic data

  • Fund Project: Supported by China Geological Survey Program (No. 1212011087009) and National High Technology Research and Development Program (No. 2013AA063905)
More Information
    Author Bio: XIONG Shengqing, male, born in 1963, senior engineer and supervisor of doctor candidates, mainly engages in application of aero geophysics, remote sensing technology in geosciences; Email: xsq@agrs.cn .
  • 本文以我国截止到2011年基本覆盖陆域及部分海域的航磁数据编制的全国航磁系列图为基础,以航磁反映的区域磁场和磁性基底起伏特征为依据,汲取主流大地构造观的划分理念,以板块构造理论及大陆动力学思想为指导,以磁场反映的构造特征为切入点,结合重力、遥感、地质资料对中国陆域构造单元进行划分。大地构造单元划分4个级别:一级构造单元为陆块区和造山系,共划分出8个;二级构造单元为陆块、弧盆系和地块,共划分出32个;三级构造单元为盆地、坳陷带(区)和隆起带(区),共划分出85个;四级构造单元为隆起和坳陷,共划分出332个。本划分方案旨在为油气地质构造背景研究及油气勘探提供一份地球物理资料。文中重点讨论了一、二级构造单元界线厘定的磁场依据及与前人划分存在的不同之处,而三、四级构造单元完全依据磁场及磁性基底起伏情况进行划分,并在盆地和坳陷区给出了深度信息,这为油气勘探者提供了必要的技术支撑。同时,借助丰富的航磁信息提示出一些地质构造方面难解现象,供同行专家参考与讨论。

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  • 图 1  中国陆域航磁划分大地构造单元在航磁化极图上的反映

    Figure 1. 

    图 2  中国陆域航磁划分大地构造简图

    Figure 2. 

    图 3  中国陆域大地构造单元简图

    Figure 3. 

    表 1  中国航磁大地构造单元划分

    Table 1.  Tectonic units of China revealed by aeromagnetic data

    下载: 导出CSV
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出版历程
收稿日期:  2017-07-12
修回日期:  2017-11-17
刊出日期:  2018-08-25

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