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临川高岭(俗称滑石子)是一种地质储量不大的优质瓷用原料。它主要是由高岭石组成。本矿床位于中国大地构造——南华准地台,北武夷山台穹的赛阳关背斜中(即1:20万区域地质测量东乡幅测区南部的临川县溪南一带)矿区出露地层是上侏罗统“武夷群”(旧称)岩系。矿体就是产于该群中鹅湖岭组深灰,紫灰色的厚层粗粒流纹岩中,矿脉大小、形状、延伸方向完全受流纹岩中的裂隙大小,形状和延伸方向的控制。是一个典型风化充填淋积型矿床。从物化性能的初步研究表明本矿床是窑业性能很好的高岭土。
Linchuan Kaolin (commonly known as talc) is a high quality porcelain with little geological reserves of raw materials. It is mainly composed of kaolinite. The deposit is located in the outcrop formation of China’s tectonic tectonics - South China Quasi-platform and the Saiyangguan anticline in the dome of the platform of the North Wuyi Mountain (ie 1: 200,000 regional geological survey in the south of Linxiang County in Dongxiang area) Is the Upper Jurassic “Wuyi group ” (formerly known) rock series. The ore body is produced in the thick gray rhyolite of thick gray and purple gray in the Ehulhuling Formation of this group. The size, shape and direction of the vein are totally controlled by the size, shape and direction of the crack in rhyolite . Is a typical weathered filling mineral deposits. Preliminary studies from the physical and chemical properties show that the deposit is a good kaolin clay industry performance.