张连增. 辽宁省综合地球物理解释断裂构造的方法和依据[J]. 地质与资源, 2015, 24(5): 483-488. DOI: 10.13686/j.cnki.dzyzy.2015.05.014
    引用本文: 张连增. 辽宁省综合地球物理解释断裂构造的方法和依据[J]. 地质与资源, 2015, 24(5): 483-488. DOI: 10.13686/j.cnki.dzyzy.2015.05.014
    ZHANG Lian-zeng. METHODS AND BASIS OF INTEGRATED GEOPHYSICAL INTERPRETATION OF FAULT STRUCTURES IN LIAONING PROVINCE[J]. Geology and Resources, 2015, 24(5): 483-488. DOI: 10.13686/j.cnki.dzyzy.2015.05.014
    Citation: ZHANG Lian-zeng. METHODS AND BASIS OF INTEGRATED GEOPHYSICAL INTERPRETATION OF FAULT STRUCTURES IN LIAONING PROVINCE[J]. Geology and Resources, 2015, 24(5): 483-488. DOI: 10.13686/j.cnki.dzyzy.2015.05.014

    辽宁省综合地球物理解释断裂构造的方法和依据

    METHODS AND BASIS OF INTEGRATED GEOPHYSICAL INTERPRETATION OF FAULT STRUCTURES IN LIAONING PROVINCE

    • 摘要: 通过研究辽宁省布格重力异常Δg及其位场转换场、航磁ΔT异常及其位场转换场、地震波场、大地电磁场,结合地貌以及钻探等资料,综合解释出了区内断裂构造.展示出了辽宁省断裂构造平面分布特征.配合地球物理解释剖面,可以了解区内主要断裂构造的垂向发育特征.分析认为郯庐断裂带为左行走滑断层带,划分出了表壳断裂、中-下地壳断裂、超岩石圈断裂.

       

      Abstract: With study on the Bouguer gravity anomaly Δg and its potential field conversion field,aeromagnetic anomaly ΔT and its potential field conversion,seismic wave field and magnetotelluric field,combined with the topography and drilling data of Liaoning Province,the author comprehensively interprets the fault structures,which show the plane distribution characteristics of faults in the province.Together with the geophysical interpretation section,the vertical development characteristics of main fault structures can be recognized.The analysis reveals that the Tan-Lu fault zone is of left lateral strike slip.The faults can be divided into supracrustal fault,middle-lower crust fault and translithospheric fault.

       

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