上海地质
上海地質
상해지질
2010年
B11期
184~186
,共null页
硅质灰岩 粉石英
硅質灰巖 粉石英
규질회암 분석영
siliceous limestone; konilite
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。
江西省蓮花縣江下垅粉石英礦，賦存于二疊繫上統獅子形組，繫硅質灰巖、硅質巖風化而成。礦體嚴格受地層控製，巖石硅質成分是成礦的先決條件，溫暖濕潤的氣候是成礦的後天條件。
강서성연화현강하롱분석영광，부존우이첩계상통사자형조，계규질회암、규질암풍화이성。광체엄격수지층공제，암석규질성분시성광적선결조건，온난습윤적기후시성광적후천조건。
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.
