摘要
江西省莲花县江下垅粉石英矿,赋存于二叠系上统狮子形组,系硅质灰岩、硅质岩风化而成。矿体严格受地层控制,岩石硅质成分是成矿的先决条件,温暖湿润的气候是成矿的后天条件。
Jiangxialong konilite deposit in Lianhua county,Jiangxi province occurrences in the lion formation of Permian system,which is weathering from siliceous limestone & siliceous rock.,Ore is controlled strictly by stratum,the siliceous component of rock is the precondition of mineralization,warm and moist climate is the postnatal conditions of mineralization.
引文
[1]江西省地质矿产局.江西地质志[M].北京:地质出版社,1985
[2]江西省地质矿产局赣西地质调查大队.江西省萍乡市荷家塘粉石英矿区初步勘探地质报告[R].1986.
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