河北水门寺瓷石矿床地质特征及成因初探
Nonferrous Metals Abstract(2016)
Abstract
水门寺瓷石矿位于河北省秦皇岛市抚宁县水门寺村一带,本文在综合分析该矿床地质特征的基础上,对矿床成因进行了初步探讨,认为该矿床由呈岩床状沿龙山组底部的石英砂岩与泥质砂页岩的层间裂隙顺层侵入的石英斑岩在侵位和冷凝过程中发生自变质作用,产生强烈的绢云母化、高岭土化而形成.
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