侯争,郭增长,杜久升,康育鹏,黄晓东

• 1:河南理工大学
• 2:河南测绘职业学院

摘要(Abstract)：

为获取芦山地震前后川滇地区地壳的形变特征,利用陆态网2009—2013年和2014—2016年两期全球卫星导航系统(GNSS)水平速度场资料分别计算并对比分析了地震发生前后主应变率场、最大剪应变率场、面膨胀率场及基线长度的变化情况。结果显示芦山地震之前龙门山断裂带主要以压缩应变为主,面压缩应变和最大剪应变均处于高值区,震后能量部分释放,压缩形变程度减弱,但其西南方向的安宁河断裂带和鲜水河断裂带南段出现明显的压缩应变高值区,同时南汀河断裂带附近也呈现较明显的压缩应变。岷江断裂带附近区域的压缩应变虽然减弱,但仍然没有改变它的应变状态,这可能促使了2017年九寨沟M_s7.0地震的发生。

关键词(KeyWords)： 地壳形变;主应变率场;面膨胀率场;最大剪应变率场;基线

Abstract:

Keywords:

基金项目(Foundation): 国家自然科学基金项目（41774041）;; 教育部人文社会科学青年基金项目（17YJCZH041）;; 煤炭工业协会科学技术研究指导性计划项目（MTKJ2016-212）;; 河南省自然科学基金项目（182300410111,182300410115）;; 河南省高校基本科研业务费专项资金资助项目（NSFRF170906）

作者(Author): 侯争,郭增长,杜久升,康育鹏,黄晓东

DOI: 10.16251/j.cnki.1009-2307.2021.02.001

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