绿泥石片岩和斜长角闪岩在高温高压下的物理力学性质及其应用  

THE PHYSOCAL AND MECHANICAL PROPERTIES OF CHLORITE-SCHIST AND PLAGIOCHASE AMPHIBOLITE AT HIGH P T CONDITIONS AND ITS APPLICATION

作　　者：高平[1] 刘若新[1] 马宝林[1] 李彪[1] 母润昌 

机构地区：[1]国家地震局地质研究所

出　　处：《地震地质》1994年第1期83-88,共6页Seismology and Geology

摘　　要：在高温高压下绿泥石片岩和斜长角闪岩中含水矿物的脱水作用可以引起岩石物理力学性质的异常变化。在半封闭条件下，含水矿物的脱水温度有随压力增加而降低的趋势。脱水作用可能是华北地区壳内低速高导层（体）的形成原因之一。这一低速高导层（体）同时也是低强度的软弱层（体），有利于地震在其上覆脆性岩层中的孕育与发生。The conductivity，P-wave velocity and the strengh of chlorite-schist and plagiochase amphi-bolite were measured at high P T conditions.It has been shown that the dehydration of water-bearing minerals wolild lend to abnormal changes of physical and mechanical properties．The de-hydrating temperature decreased with increasing pressure at semi-sealed condition. It has beenpresented that the dehydration of water-bearing minerals in chlorite-schist and plagichase amphi-bolite should be the cause of the low-velocity ／ high conductivity layer（or body）in North Chinacrust，This layer（body）should also be a soft layer（body）with low strgngth，favourable to theoccurrence of earthquake.

关 键 词：绿泥石 片岩 角闪岩 波速 电导率 

分 类 号：P584[天文地球—岩石学]