这些高侵位体是寻找和评价斑岩铜(钼)矿的有利对象。
These high emplacement intrusive bodies are favourable targets for the investigation and evaluation of porphyry copper deposits.
岩石属于大陆板内张性构造环境下高侵位形成的壳源重熔型花岗岩类。
The rocks are crustal remelting, shall level granites formed in a within-plate tensional tectonic environment.
此外，主断裂坡折带在低水位期和湖侵期，控制了沉积体系类型，而在高水位期控制了沉积体系的规模。
In addition, the main fault slop-break zone affected on the sedimentary system types during lower stand and lake transgression and on the sedimentary scale during high stand.
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