The mineral-bearing hydrotherm which separated from the granodiorite porphyry magma entered into the fissures of the top part of the diorite or granodiorite porphyry. In this process, the atmospheric water dissolving formation minerals in infiltration process mixed with the original magma, and formed the mixed-mineralization fluids.

  • 从花岗闪长斑岩岩浆中分离出来的含矿热液,进入闪长玢岩或花岗闪长斑岩顶部的裂隙带后,与下渗的大气降水及溶解其中的部分成矿物质混合,形成混合流体。

  • 互联网摘选 2025-02-24 14:56:10

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