The geological surfaces in the joint of the Guizhong depression with the peripheral geological structure units are the favorable districts of the mineralization of the MVT type lead-zinc deposits.
桂中凹陷与周边地质构造单元接合处的地质界面是“mvt型”铅锌矿床形成的有利地段。
The geological surfaces in the joint of the Guizhong depression with the peripheral geological structure units are the favorable districts of the mineralization of the MVT type lead-zinc deposits.
桂中凹陷与周边地质构造单元接合处的地质界面是“mvt型”铅锌矿床形成的有利地段。
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