SEISMOLOGY AND GEOLOGY ›› 1984, Vol. 6 ›› Issue (3): 23-28.

• Brief Report • Previous Articles     Next Articles

CHARACTERISTICS OF THE EARTHQUAKE-GENERATING STRUCTURES FOR MAGNITUDE 8.0 PINGLUO EARTHQUAKE OF 1739 AND THE PROCESS OF ITS PREPARATION

Li Mengluan, Wan Zicheng   

  1. Institute of Seismology, Ningsia Hui Autonomous Region
  • Received:1983-11-30 Online:1984-09-05 Published:2009-11-25

1739年平罗8.0级地震的发震构造及其孕育特征

李孟銮, 万自成   

  1. 宁夏回族自治区地震局

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。