紫金山整装勘查区内生金属矿产成矿地质特征及找矿方向  

Metallogenic geologic feature and prospecting direction of endogenetic metallic ore in Zijinshan integrated prospecting area

作　　者：李雪平[1] 

机构地区：[1]福建省121地质大队,福建龙岩364021

出　　处：《企业技术开发》2013年第12期64-66,88,共4页Technological Development of Enterprise

摘　　要：紫金山整装勘查区是福建省内生金属矿产的主要产地,已发现有铜、金等矿床(点)10余处。紫金山整装勘查区内生金属矿产成矿受地层、构造、岩浆岩的综合控制,岩浆岩侵入在成矿中起主导作用,成矿时期主要为燕山期。根据区内地质特点及以往地质工作情况,文章从控矿层位、控矿构造、岩浆活动、矿化范围、成矿时期与成矿环境入手探讨了紫金山整装勘查区的内生金属矿产成矿地质特征。提出了紫金山整装勘查区内生金属矿产找矿方向。Zijinshan integrated prospecting area which has explored more than 10 deposits, such as copper, golden and so on is a main producing area of endogenetic metallic ore in Fujian Province.The mineralizing of endogenetic metallic ore in Zijinshan integrated prospecting area is comprehensively controlled by stratum,structure and magmatic rock,and the invading of magmatie rock plays a leading role in the ore-forming period in yanshanian.based on the geological feature and the geological work before, this paper analyses geologic feature of endogenetic metallic ore in Zijinshan integrated prospecting area from aspects as follows：ore-controlling stratum, ore-controlling structure,ore-forming period,metallogenic environment.At last,prospecting direction of endogenetic metallic ore in Zijinshan integrated prospecting area is also put forward.

关 键 词：紫金山整装勘查区 内生金属矿 成矿地质特征 找矿方向 

分 类 号：P618[天文地球—矿床学]