龙门山和成都地震构造区的划分  

Seismo-tectonic Zonation of Longmengshan and Chengdu Region

作　　者：孔军[1] 周荣军[1] 

机构地区：[1]四川省地震局,成都610041

出　　处：《震灾防御技术》2014年第1期64-73,共10页Technology for Earthquake Disaster Prevention

基　　金：中国地震局芦山7.0级地震科学考察资助项目

摘　　要：新编制的地震动参数区划图采用了潜在震源区三级划分方案,以体现背景地震活动空间分布的不均匀性,并在地震构造区内归纳出统一的地震构造模型。本文根据西南地区潜在震源区三级划分的成果,分析了龙门山地震统计区内的龙门山和成都地震构造区的基本特征,历史地震活动强度及频度,主要活动构造的构造变形样式,建立了地震构造区的发震构造模型,确定了构造区的本底地震及划分构造源的地震构造标志。同时,提出了确定背景源空间分布函数的简单方法。The principle of three-level delineation is adopted in determination of potential seismic source for the new national seismic zoning map of China,in order to embody the inhomogeneity of the spatial distribution of background seismic activity,and to induct an uniform seismotectonic model for each seismotectonic province.Based on achievements of determining potential seismic source in southwestern China,we analyzed the basic characteristics,historical earthquakes magnitude and frequency,deformation mechanism of main active tectonics structure of Longmenshan and Chengdu seismotectonic province in Longmenshan seismic region,and established the seismogenic model for each seismotectonic province,and identified the upper limit of background earthquake.A simple method is also put forward for calculating the spatial distribution function of background seismic source in this paper.

关 键 词：潜在震源区 地震构造区 空间分布函数 

分 类 号：P315[天文地球—地震学]