Under supergene process influencing, kaolinites invered dickites, siderite were been ferritization, part of carbonate mineral have been dissoluted producing calcite.
在生作用的影响下,高岭石向地开石转,菱铁矿褐铁矿,部分碳酸盐矿物溶解生成方解石。
Under supergene process influencing, kaolinites invered dickites, siderite were been ferritization, part of carbonate mineral have been dissoluted producing calcite.
在生作用的影响下,高岭石向地开石转,菱铁矿褐铁矿,部分碳酸盐矿物溶解生成方解石。
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