最近,湖北省地质实验研究所在湖北省随州市附近上第三系地层中首次发现凹凸棒石,并经油浸薄片鉴定、Ⅹ光衍射分析、红外光谱分析、差热分析以及单矿物化学分析等多种测试方法所证实。现将该矿物初步研究成果报导如下: 一、凹凸棒石地质产状随州凹凸棒石产于上第三系凤凰镇组,该组岩性上部为含砂粘土石灰岩夹膨润土,中部为方解石化隐晶质白云岩,下部为隐晶质白云岩。含矿岩石主要为隐晶质白云岩,上覆紫红 Recently, Hubei Institute of Geology and Experimental Research discovered the first attapulgite in the Tertiary strata near Suizhou, Hubei Province, and was identified by oil immersion flake, X-ray diffraction analysis, infrared spectroscopy, differential thermal analysis and single mineral chemical analysis Confirmed by a variety of test methods. Now the mineral preliminary research results reported as follows: First, the attapulgite geological production Suizhou Attapulgite produced in the Upper Triassic Fenghuangzhen Formation, the upper part of the lithology sandstone bentonite bentonite limestone, the central calcite Hidden Crystal dolomite, the lower part of cryptocrystalline dolomite. Ore-bearing rocks are mainly cryptocrystalline dolomite, overlying purple