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将乐县何坑—际下矿段方解石-萤石矿床特征及控矿因素

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何坑—际下矿段位于福建省将乐县何坑—曹地矿区,系武夷成矿带中南段之将乐—蒲城矿集区的一部分.在简述区域地质背景的基础上,从矿体、矿石、围岩蚀变等方面对方解石-萤石矿床特征进行了分析,据此总结了何坑—际下矿段的控矿因素,并初步研究了该矿段的矿床成因.研究发现:矿段内发育3个接触变质型方解石矿体和4个萤石矿体(矽卡岩型+充填型矿床);主要的赋矿层位是早三叠世溪口组,也受控于晚侏罗世正长花岗岩或矽卡岩,其控矿、含矿构造以NE—NEE向逆断层性质的断裂带为主,且具硅化、方解石或萤石矿化、矽卡岩化的围岩蚀变特征.该研究对矿段外围寻找隐伏矿体或圈定类似矿区找矿靶区均具有一定参考意义.
Deposit Characteristics and Ore-controlling Factors of Calcite-fluorite Ore in Hekeng-Jixia Ore Section of Jiangle County
The Hekeng-Jixia ore section is located in the Hekeng-Caodi mining area in Jiangle Coun-ty,Fujian Province.It is part of the Jiangle-Pucheng ore concentration area in the central and southern sec-tion of the Wuyi metallogenic belt.On the basis of briefly describing the regional geological background,the characteristics of calcite-fluorite deposit are analyzed from the aspects of ore body,ore and wall rock altera-tion.Based on this,the ore-controlling factors of Hekeng-Jixia ore section are summarized,and the genesis of the ore section is preliminarily studied.It is found that three contact metamorphic calcite ore bodies and four fluorite ore bodies(skarn type+filling type deposits)are developed in the ore section.The main ore-bearing strata are the early Triassic Xikou Formation,which is also controlled by the late Jurassic syenogran-ite or skarn.The ore-controlling and ore-bearing structures are dominated by NE-NEE reverse fault zones,and have silicification,calcite or fluorite mineralization,and skarnization.This study has certain reference significance for finding concealed ore bodies in the periphery of the ore section or delineating the prospect-ing target area of similar mining areas.

deposit characteristicsore-controlling factorscalcite-fluorite ore

郑清伟

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福建省197地质大队

矿床特征 控矿因素 方解石-萤石矿

2024

现代矿业
中钢集团马鞍山矿山研究院有限公司

现代矿业

影响因子:0.33
ISSN:1674-6082
年,卷(期):2024.40(12)