安徽省庐枞盆地高岭土矿的成矿规律、找矿方向及开发应用问题探讨

摘要

庐枞盆地是以中、下侏罗统陆相碎屑岩建造为基底，经燕山运动而发育起来的陆相继承性火山岩盆地，是长江中下游地区重要的矿产地之一。盆地北部高岭土矿化普遍且强烈，具有很好的找矿远景。本文初步探讨了庐枞盆地高岭土成矿规律、矿床成因及找矿方向，提出了下一步开发利用的建议。%The Lu-Zong basin is a continental inherited basin, which has been developed through the Yanshanian Movement, with mid and lower Jurassic land facies clastic rock formation being the basement, and is one of important ore fields in the mid-lower Yangtze River reaches. The northern part of the basin is widely and strongly kaolinized having a good prospect for kaolin exploration. This paper made an initial discussion on the ore-forming law, origin of ore deposit and range of exploration of kaolin in the basin, and gave suggestions for further development and utilization.