The calcite deposits are derived from the recrystallization of the carbonatite as a result of the weathering, eluviation of the fault, and the thermal contact activity and the metamorphism.
方解石矿有三个显著特征：
、块大、致密。
The calcite deposits are derived from the recrystallization of the carbonatite as a result of the weathering, eluviation of the fault, and the thermal contact activity and the metamorphism.
方解石矿有三个显著特征：、块大、致密。
Under to the rainy season, salinity along with moisture content to under movement, the saline-alkali soil is in the eluviation time ;
到了雨季，盐分又随着水分的下渗，处于下行状
，为淋溶期；
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