由震源机制解资料研究川滇地区构造应力场*

(1.云南省地震局,云南 昆明 650224; 2.云南大学 资源环境与地球科学学院,云南 昆明 650091)

震源机制解; 构造应力场; 震源断错性质; 川滇地区

Research on Structural Stress Field Basing on Focal Mechanism Solutions Data in Sichuan-Yunan Area
CAO Ying1, WU Xiao-ping2, SHEN Ya-hong1, LI Zhao-long1

(1.Earthquake Administration of Yunnan Province, Kunming 650224, Yunnan, China)(2. School of Resource Environment and Earth Sciences, Yunnan University, Kunming 650091, Yunnan, China)

focal mechanism solution; tectonic stress field; focal rupture characteristics; Sichuan-Yunnan area

备注

利用1978~2009年川滇地区的124个地震震源机制解资料,采用对震源机制参数统计的方法,详细分析了地震断层类型和川滇地区的现代构造应力场特征。结果 表明,云南地区(21°~28°N,97°~108.8°E)主要受近N-S向的水平挤压力影响,区域应力场背景以水平作用力为主; 四川地区(28°~34.5°N,97°~108.8°E)由于平均P,T轴的仰角接近水平,构造应力场接近水平,主要受近E-W向挤压力作用,断层面较陡,受水平剪切力作用。川滇地区走滑型地震较多,主要分布于云南地区,四川地区内发生的地震类型较为分散且每种类型都有。

Basing on 124 focal mechanisms data from 1978 to 2009 in Sichuan-Yunan area, we analyzed the fault type of earthquake and the characteristic of modern tectonic stress field in Yunnan-Sichuan area by the statistic method of focal mechanisms parameters. The results showed that it was influenced by horizontal compression in nearly NS direction in Yunnan area(21°~28°N, 97°~108.8°E), and the main characteristic of regional stress field background is characterized by horizontal compression. Because of the average plunges of P-axis and T-axis were close to horizontal, the tectonic stress field which is close to horizontal mainly influenced by compression in nearly EW direction in Sichuan area(28°~34.5°N, 97°~108.8°E). The fault plane which was influenced by horizontal shear tress is stepper. The main type of fault is strike-slipe in Sichuan-Yunnan area, and mainly distributed in Yunnan. The earthquake occurred in Sichuan area had many types and scattering distribution.