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众所周知,与沉积岩或火山岩围岩呈整合产出的层状及透镜状矿体具有重要的工业价值。属于此种类型的有外生,还有很多内生矿床,其中以铅、铜、汞及铀的热液矿床最为特征。正如沃里弗松(1952)及克列特尔(1956)等人文章中多次指出的那样,在强变形的沉积岩层中,内生矿床一般受构造控制表现的非常明显。矿田范围内分布有大的断裂及与之伴生的陡倾断层。矿体发育于陡斜褶皱转折端及翼部的片理化和层间滑动带,还发育于紧密褶曲
It is well-known that layered and lenticular ore bodies that are integrated with sedimentary or volcanic rocks have important industrial value. This type of exogenous, there are many endogenous deposits, of which lead, copper, mercury and uranium hydrothermal deposits most characterized. As many times in Warriorson’s (1952) and Chrettell (1956) et al. Articles point out, endogenic deposits are generally structurally controlled in strongly deformed sedimentary formations. There are large faults and associated steeply dipping faults in the ore field. Ore body developed in steeply folded folds and wings of the fragment of the physical and chemical sliding between the layers, but also developed in tight folds