福建省麟厚锰矿属风化型氧化锰矿床，多呈土状、粉状， 密度小，含水率高。
Mn ores of linhou Mn Mine belong to weathering-type Mn oxide, shaped like earth and powder, with small specific gravity and large moisture content.
古潜山主要发育风化壳岩溶带储层和内幕储层。 下古生界碳酸盐岩裂缝-溶蚀型储集层的发育特征以有无上古覆盖是岩溶发育的前提；
The buried-hills mainly develope two kinds of reservoir, one is related to the crust of weathering and karst zone, the other is to lithology.
矿床成因属风化残积型，受地层、岩性的控制。
Genetically, it is an eluvial deposit produced by weathering, controlled by the stratigraphy and lithology.
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