Fluid immiscibility, continuous influxing of meteoric water and water-rock exchange are very important factors that caused gold and stibnite to deposit.
流体不混溶、大气降水的不断加入以及水-岩交换作用是导致本区成矿流体中金、锑淀积成矿的主要因素。
Among them, leaching of meteoric water has contributed less to the formation of anomalously high porosity zones compared to other factors.
其中大气水淋滤形成的次生孔隙对异常高孔隙的贡献较小。
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