安徽省东至县神龙山白云岩、石灰岩矿床地质特征及其开发探讨  

Geological characteristics and development of Shenlongshan dolomite and limestone deposits in Dongzhi County, Anhui Province

作　　者：王慧 吴苑 WANG Hui;WU Yuan(No.321 Geological Team of Anhui Geological and Mineral Exploration Bureau,Tongling 244033,Anhui,China)

机构地区：[1]安徽省地质矿产勘查局321地质队,安徽铜陵244033

出　　处：《资源信息与工程》2023年第1期20-23,共4页Resource Information and Engineering

摘　　要：神龙山白云岩、石灰岩矿床位于安徽省池州市境内。本文对神龙山白云岩、石灰岩矿床的地质特征、矿床成因类型进行了分析,探讨了矿床开采的技术条件和找矿方向。研究认为:神龙山白云岩、石灰岩矿床主要出露晚寒武系团山组至早奥陶系红花园组地层,共圈定矿体8个;矿床属于海相碳酸盐岩沉积形成的沉积型白云岩和石灰岩矿床,达到超大型规模;矿山投资开发经济社会效益较好;未来找矿方向主要集中在奥陶系仑山组、红花园组等地层。Shenlongshan dolomite and limestone deposits are located in Dongzhi County, Chizhou City, Anhui Province. In this paper, the geological characteristics and genetic types of the dolomite and limestone deposits in Shenlongshan were analyzed, and the prospecting technical conditions and direction of the deposits were discussed. The results showed that the dolomite and limestone deposits in Shenlongshan mainly show strata from Late Cambrian Tuanshan Formation to Early Ordovician Honghuayuan Formation, and a total of 8 ore bodies were delineated. The deposit belongs to the sedimentary dolomite and limestone deposits formed from Marine carbonate rock sediment, which reach super-large scale. Mine investment development has good economic and social benefits. The future prospecting direction will mainly focus on the Ordovician Lunshan Formation, Honghuayuan Formation and other strata.

关 键 词：白云岩 石灰岩 地质特征 找矿方向 矿床开发 东至县 

分 类 号：P619[天文地球—矿床学]