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黄陵背斜东南边缘北东向线性构造特征及其与地震活动的关系
引用本文:韩晓光,徐卓民.黄陵背斜东南边缘北东向线性构造特征及其与地震活动的关系[J].华南地震,1992,12(4):42-45.
作者姓名:韩晓光  徐卓民
作者单位:国家地震局地震研究所,国家地震局地震研究所 武汉 43007,武汉 43007
摘    要:黄陵背斜东北,西北及西南三边为大断裂所切割,唯其东南边缘仅在卫星影象上有一线性构造。经实地考察研究,该线性构造地表以张性裂隙带的形式出现,其深部部分地段以主断面形式出现,从而在几何形态上组成一个完整的黄陵菱形断块构造。在断块的顶角处,是该地区中强地震的主要发生地带。

关 键 词:黄陵背斜  线性构造  地震活动性

FEATURES OF LINEAR STRUCTURE ON THE SOUTHEASTERNEDGE OF HUANG LING ANTICLINE ANDITS SEISMOTECTONIC SIGNIFICANCE
Han Xiaoguang and Xu Zuomin.FEATURES OF LINEAR STRUCTURE ON THE SOUTHEASTERNEDGE OF HUANG LING ANTICLINE ANDITS SEISMOTECTONIC SIGNIFICANCE[J].South China Journal of Seismology,1992,12(4):42-45.
Authors:Han Xiaoguang and Xu Zuomin
Abstract:Althought three big faults obviously exist separately on the northeastern , northwestern and southwestern edges of Huangling anticline, the southeastern edge of the anticline merely shows a linear structure on satellite image. Field investigation and study indicate that the linear structure represents a consisting of a series of tensile cracks on the surface and shows a main fault plane in depth beneath its some sections .Geometrically these faults and the linear structure constitute a complete Huangling rhombic block. Moderate - strong earthquakes mainly occur in the tip areas of the block.
Keywords:Huangling anticline  Linear structure  Tensile crack
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