首页|宿州符离集打鼓山白云岩矿地质特征及成因类型

宿州符离集打鼓山白云岩矿地质特征及成因类型

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安徽宿州市符离集地区赋存多个白云岩矿床,产于中上寒武系,风化面常呈黑褐色,新鲜面为灰、灰白色带肉红色,可与其它基岩区别.本文以该区打鼓山白云岩矿床为例,三个矿层对应矿石类型为鲕状白云岩、结晶质白云岩和泥质白云岩三种.白云石占 95%以上,MgO平均含量 20.72%,为深海相白云岩,物质来源于南部淮阳地盾长期剥蚀的Ca、Mg等以胶体方式搬运沉积而成.
GEOLOGICAL CHARACTERISTICS AND GENETIC TYPES OFTHE DAGUSHAN DOLOSTONE DEPOSIT INFULIJI,SUZHOU
There are multiple dolomite deposits in the Fuliji area in Suzhou City,Anhui Province,which occur in the middle to upper Cambrian strata.The weathered surface of them is often black brown,and the fresh surface is gray,grayish white with flesh red color,which can be distinguished from other bedrocks.The ore types corresponding to the three ore layers of the Dagushan dolomite deposit are oolitic dolomite,crystalline dolomite and argillaceous dolomite.Dolomite accounts for over 95%,with an average MgO content of 20.72%.They are deep-sea dolomites derived from the long-term erosion of Ca and Mg,which were transported and deposited in a colloidal manner,in the southern Huaiyang Shield.

Middle-Upper CambrianDolomiteErosionSedimentationFuliji Dolomite DepositSuzhou,Anhui

郝琴华

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安徽省地质矿产勘查局325地质队,安徽 淮北 235037

寒武系中上统 白云岩 剥蚀 沉积 符离集白云岩矿 安徽宿州

2024

云南地质
云南省地矿总公司 云南省地质矿产勘查院

云南地质

影响因子:0.259
ISSN:1004-1885
年,卷(期):2024.43(3)