摘要
本文利用高温高压多功能三轴实验装置 ,以NaCl为固体围压传压介质 ,在围压为 45 0MPa~ 80 0MPa ,温度区间为 6 0 0℃~ 1 1 5 0℃和应变速率为 1× 1 0 - 4~3 1 2 5× 1 0 - 6 s条件下 ,对攀枝花辉长岩进行了流变学实验研究。实验结果表明 ,辉长岩围压在 45 0MPa~ 80 0MPa条件下 ,温度在 6 0 0℃时为脆性变形 ,70 0℃~ 85 0℃时为半塑性流动 ,含微破裂 ,大于 90 0℃时为塑性流动。辉长岩的脆 塑性转化温度为 70 0℃~ 90 0℃ ,主要影响因素为温度、围压和应变速率 ,同时存在双相流变学问题。
In this paper,an experimental study of brittle ductile transition in Panzhihua fine grained gabbro was performed under a Griggs type apparatus with NaCl as the confining pressure medium. Experiments were conducted in conditions of:450MPa~800MPa confining pressure,600℃~1150℃ temperature,and 1×10 -4 ~3 125×10 -6 /s strain rate.The results of experiments show that the deformation of the gabbro is brittle fractures at temperature 600℃,semibrittle flow at 700℃~850℃,and plastic flow at temperature higher than 900℃.The temperature of brittle plastic transition is 700℃~900℃ at the confining pressure 450MPa~800MPa.The major factors that influence the brittle plastic transition in the gabbro are temperature and strain rate,and the influence of confining pressure is secondary.
出处
《地质力学学报》
CSCD
2001年第2期130-138,共9页
Journal of Geomechanics
基金
国家自然科学基金项目!(编号 :496 3312 0 )
国家重点基础发展规划项目! (编号 :G19980 40 70 4)
中国地震局构造物理开放实验室项