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笔者在苏皖南部地区观察过数十处金属和非金属矿床,发现层控矿床中断裂活动异常活跃,其中对层控矿床起控制作用的是由层间滑动发育起来的层滑断裂。它受到岩层的界限制约,其构造部位、形成机制和力学性质等均具有明显的特点,并与层控矿床的发育有着内在的联系。层滑断裂的研究,可以追溯到十九世纪中叶伊塞尔(A·Eseker,1846)发现阿尔卑斯的推覆体和伊文思(J.Evans,1866)发表地壳层圈滑动的理论,涉及问题颇广。到本世纪七十年
The author observed dozens of metal and nonmetallic deposits in the southern part of Jiangsu and Anhui Provinces and found that the active faults in the stratiformized ore deposit are extremely active. Among them, the stratiform slip developed by interlayer sliding is controlled by the stratabound control. It is restricted by the boundaries of strata. Its structural parts, formation mechanism and mechanical properties all have obvious characteristics and are intrinsically linked with the development of stratabound mineral deposits. The study of slip-shear faults can be traced back to the mid-nineteenth century when A. Eseker (1846) found that alpine nappe and J. Evans (1866) published the theory of crustal slip, wide. Seventy years of this century