1927年古浪大震地质构造背景及其成因的初步探讨
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PRELIMINARY DISCUSSION OF GEOTECTONICAL BACKGROUND AND GENESIS OF GULANG STRONG EARTHQUAKE IN 1927
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    摘要:

    本文根据多年野外考察资料,在论述1927年古浪大震形变带及发震断裂带特征基础上,分析了地震发生的地质构造背景,认为这次大震是塔儿庄-皇城断裂带和武威-天祝断裂带同时活动的产物,同时对两组断裂破裂方式进行了初步分析,提出了断块错动力学模型。

    Abstract:

    In this paper,based on the data of virtual investigation,the author has discussed the characteristics of deformation band and earthquake frac-ture of Gulang earthquke in 1927 and analysed the geotectonical back-ground of this earthquake.The author helieves that the occurrence of Gulang earthquake in1927 Was the result that the fracture band of Tazhuang-Huangcheng andthat of Wuwei-Tianzhu were in activity at the sametime.And based no the analysis of their rupturing way,the mechanics model of fragmentation massif movement has been made.

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贾云鸿.1927年古浪大震地质构造背景及其成因的初步探讨[J].地震工程学报,1982,4(3):78-82. Jia Yun-hong. PRELIMINARY DISCUSSION OF GEOTECTONICAL BACKGROUND AND GENESIS OF GULANG STRONG EARTHQUAKE IN 1927[J]. China Earthquake Engineering Journal,1982,4(3):78-82.

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  • 收稿日期:1981-05-11
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  • 在线发布日期: 2017-07-04