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川滇构造带及其邻区的地壳结构与地震分布
引用本文:傅维洲,贺日政,邱虎.川滇构造带及其邻区的地壳结构与地震分布[J].吉林大学学报(地球科学版),1999(4).
作者姓名:傅维洲  贺日政  邱虎
作者单位:长春科技大学地球探测与信息技术学院!长春130026(傅维洲,贺日政),天津市地震局!天津300201(邱虎)
摘    要:综合前人资料分析了川—滇构造带及其邻区地壳-上地幔速度结构与地震分布的关系。结果表明,川—滇构造带具有同青藏高原地壳-上地幔结构相似的某些特征;地震活动主要沿安宁河断裂带和小江断裂带分布。震源以永仁、渡口和会理三地所在区域最浅,向四周渐深

关 键 词:川滇构造带  地壳结构  地震分布  震源深度

CRUSTAL STRUCTURE AND EARTHQUAKE DISTRIBUTION OF THE TECTONIC ZONE IN EASTERN SICHUAN AND WESTERN YUNNAN PROVINCES
Fu Weizhou,He Rizheng.CRUSTAL STRUCTURE AND EARTHQUAKE DISTRIBUTION OF THE TECTONIC ZONE IN EASTERN SICHUAN AND WESTERN YUNNAN PROVINCES[J].Journal of Jilin Unviersity:Earth Science Edition,1999(4).
Authors:Fu Weizhou  He Rizheng
Abstract:In this paper, the date of predecessors has been used to analyse relation between the structure of the crust-upper mantle and earthquake distribution in tectonic zone of western Sichuan and eastern Yunnan provinces. The results show that some characteristics of crust-upper mantle structure of tectonic zone of western Sichuan and eastern Yunnan provinces are similar to Qinghai-Xizang plateau. The earthquake active mainly distributes along the An'ning River fault zone and Xiaojiang fault zone. Its hypocenter in the field of Yongren, Dukou and Huili is more shallow than its circumference.
Keywords:tectonic zone of western Sichuan and eastern Yunnan Provinces  crustal structure  earthquake distribution  depth of seismic focus
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