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1931年南海西沙群岛北6 3/4级地震震中位置与震级的讨论

魏柏林

华南地震2001,Vol.21Issue(1):43-48,6.
华南地震2001,Vol.21Issue(1):43-48,6.

1931年南海西沙群岛北6 3/4级地震震中位置与震级的讨论

Discussion on epicenter and magnitude of earthquake (M=6 3/4) in the north of the Xisha Islands of S outh China Sea in 1931

魏柏林1

作者信息

  • 1. 广东省地震局,
  • 折叠

摘要

Abstract

Based on the seismogeological tectonic environment , the intensity record of historical earthquakes and so on, it is discussed on the epicenter and magni tude of the MS6 3/4 earthquake in the north of the Xisha I slands of South C hina Sea occurred on September 21,1931. This earthquake caused intensityⅤin Gu angzhou, Sanshui and Zhongshan , the long axis of isoseismic line with intensity about trends NW.According to the iso-intensity line roughly delineated,it is co njectured that the epicenter location should be moved 110 km to east (at 20°N, 114.1°E),and based on the statistical result of the maximum distance from the epicenter location to isoseismic line with intensityⅤ, the magnitude M S=7.1 of this earthquake determined by Xujiahui observatory in Shanghai should be more reasonable.

关键词

震中定位/地震烈度图/震级/发震断裂

分类

天文与地球科学

引用本文复制引用

魏柏林..1931年南海西沙群岛北6 3/4级地震震中位置与震级的讨论[J].华南地震,2001,21(1):43-48,6.

基金项目

广东省自然科学基金项目(粤科基[1997]23) (粤科基[1997]23)

华南地震

OACSCD

1001-8662

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