矿区山前钾化带是钾化蚀变的产物，局部地段构成矿体。
Piedmont potassic alteration zone is the product of potash feldspathization, part of the zone is ore body.
蚀变类型主要有硅化、绢云母化、钾化、黄铁矿化。
The alteration are mainly silicification, sericitization, k feldspathization and pyritization.
蚀变以钾化与硅化和成矿关系最为密切。
Potassic and silicification in all alteration type are most close to mineralization.
蚀变以钾化与硅化和成矿关系最为密切。
Potassic and silicification in all alteration type are most close to mineralization.
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