摘要
通过对地壳温度和力条件下岩石半脆性蠕变实验结果的微宏观分析,本文建立了地壳岩石半脆性蠕变本构方程.依据这一本构关系和从实验中得到相应蠕变参数,进一步估计了石英岩、花岗岩和辉卡岩在地壳温度压力条件下的流变特性。
The constitutive equation for inbomogeneou semibrittle creep of crustal rocks have been given through experimental researches on some typical crustal rocks at crustal conditions. On the basis of this constitutive equation and the creep parameters of rocks from a lot of creep experiments, We give some further discussions on the rheological behaviors of quartzite, granite and gabbro at crustal conditions.
出处
《岩石力学与工程学报》
EI
CAS
CSCD
1990年第2期164-173,共10页
Chinese Journal of Rock Mechanics and Engineering