摘要
红河断裂是我国境内主要的区域性活动断裂之一,根据地震地质特征,它被分为南北两段。本文引入一种新的分段法—地球化学分段法,依据断裂上温泉的密度、热储温度、循环深度和CO_2、F、Li、Sr、B的含量等特征,把红河断裂北段进一步划分为四个亚段。笔者认为断裂带中的流体对断裂各亚段弱化程度的不同,是引起各个亚段地震活动性差异的主要原因。
The Red River fault is one of the major regioal active faults in China,it had been divided into the southern and northernsegments according to the feature of seismogeology,A new segmentation method,geochenmical segmentation method,is introduced in this paper. Based on the features of densities. reservoir temperatures,circulating depths and concentrations ofCO_2,F,Li,Sr and B of the worm spring along the fault,the northem segment is further divided into four sub-segments,The seismic activities along these sub segments of the fault differ from each other,which is thought to be mainlycaused by the difference in weakness degreeof each sub-segment due to the fluids in the fautl zone.
出处
《西北地震学报》
CSCD
1994年第4期91-98,共8页
Northwestern Seismological Journal
关键词
红河断裂
地球化学分段
地震活动性
Red River fault,Geochemical segmentation,Warm spring,Seismic activity.Fluid-weakness