SEISMOLOGY AND GEOLOGY ›› 1984, Vol. 6 ›› Issue (3): 23-28.
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Li Mengluan, Wan Zicheng
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李孟銮, 万自成
Abstract: Following the discussion of regional-geological characteristics of the northern part of Ningsia,it is indicated that the earthquake-generating structures for the Pingluo quake (M=8.0) of 1739 is held to be NNE-striking Huanghe River fault lying at the Yinchuang-Pingluo area.This paper is an analysis of the characterized preparation the shock in terms of a generalized focal model and an elucidation of the spatial position and characteristics for the structural elements.
摘要: 本文在讨论了宁夏北部区域地质基本特征的基础上,指出1739年平罗8.0级地震的发震构造是银川—平罗间呈北北东方向展布的断裂。利用“组合模式”就该地震的孕育特征进行了初步分析,阐述了积累单元和调整单元的空间位置及特征。
Li Mengluan, Wan Zicheng. CHARACTERISTICS OF THE EARTHQUAKE-GENERATING STRUCTURES FOR MAGNITUDE 8.0 PINGLUO EARTHQUAKE OF 1739 AND THE PROCESS OF ITS PREPARATION[J]. SEISMOLOGY AND GEOLOGY, 1984, 6(3): 23-28.
李孟銮, 万自成. 1739年平罗8.0级地震的发震构造及其孕育特征[J]. 地震地质, 1984, 6(3): 23-28.
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