首页> 中文期刊>地质找矿论丛 >产于层间构造带中的新型萤石矿体地质特征——以浙江常山县高坞山矿段ⅩⅣ号矿体为例

产于层间构造带中的新型萤石矿体地质特征——以浙江常山县高坞山矿段ⅩⅣ号矿体为例

     

摘要

浙江常山八面山萤石矿床是浙江省首次发现的新类型萤石矿床,其中高坞山矿段ⅩⅣ号矿体为矿田中受寒武系碳酸盐岩层间构造带控制的似层状矿体的典型代表.萤石矿体厚度大,品位较高,资源储量规模达中型.通过矿体地质特征和控矿因素的研究,认为矿床属低温热液成因,受岩浆岩、构造和地层因素的共同控制;成矿作用以充填作用为主,伴有交代作用;成矿物质氟主要来源于岩浆期后热液,而非寒武系碳酸盐岩地层,据此提出了直接和间接的找矿标志.%The Bamianshan deposit located in Changshan county, Zhejiang province is a new type of fluo-rite deposit and firstly discovered in Zhejiang province. Ore body ⅩⅣ of Gaowushan ore domain is a typical representative of layered ore body with big thickness, high grade and large mineral resources volume. Study on its geological characteristics and ore-controlling factors show that it is jointly controlled by intrusion, wall rock and structure. The ore is dominated by filling and acompanied by replacement. The ore materials are mainly derived from the post-magma hydrothermal fluid rather than the Cambrian carbonate rocks. Then direct and indirect prospecting indicators are put forward.

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