摘要
自然界绝大多数控矿断裂均具明显的多期活动特征，对其多期活动性及其力学性质的研究，尤其是成矿期力学性质的判析，是控矿构造区域应力场分析和构造控矿规律研究的关键所在。本文就控矿断裂力学性质研究中常用的却又易产生误判的若干判析标志，进行初步分析和探讨。
In nature,the most of ore controlling faults have experienced repeated movement.Identification of their activity and mechanical properties especially during mineralization,is the key to revealing the tectonic stress field and the structures leading to the control of the ores.This paper has a preliminary discussion of these problems.
出处
《地质力学学报》
CSCD
1997年第3期68-73,共6页
Journal of Geomechanics
