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福建永定虎岗地区铅锌铜多金属矿地质特征及找矿前景分析
引用本文:沈莽庭.福建永定虎岗地区铅锌铜多金属矿地质特征及找矿前景分析[J].地质与勘探,2016,52(1):70-83.
作者姓名:沈莽庭
作者单位:1. 南京地质调查中心,江苏南京,210016;2. 福建地质调查研究院,福建福州,350013;3. 安徵省勘查技术院,安徵合肥,230031
基金项目:中国地质调查项目-福建永定虎岗地区铁锰多金属矿矿产远景调查(编号:1212011085465)资助。
摘    要:本文研究了福建永定虎岗地区铅锌多金属矿成矿的区域地质背景、矿化地质条件、矿石共生组合特征和矿物生成顺序,分析了控矿因素与矿床的时空分布.认为该区铅锌多金属矿成矿作用主要表现因岩浆活动受控于二叠系栖霞组、船山组灰岩、经畲组砂质泥岩形成的似层状矽卡岩型铅锌多金属矿化体.另外在矿化成因分析的基础上建立了成矿模式,指出了下一步勘查该类型矿床的方向.

关 键 词:铅锌多金属矿  地质特征  找矿新进展  永定  福建省
收稿时间:2015/3/27 0:00:00
修稿时间:2015/10/13 0:00:00

Geological characteristics and prospecting potential and of the lead-zinc copper polymetallic deposit in the HuGang area, YongDing Country, Fujian Province
Shen Mang-ting.Geological characteristics and prospecting potential and of the lead-zinc copper polymetallic deposit in the HuGang area, YongDing Country, Fujian Province[J].Geology and Prospecting,2016,52(1):70-83.
Authors:Shen Mang-ting
Abstract:In this paper, by summarized the regional geological background of lead-zinc ore mineralization and mineralization characteristics of the geological condition , features of ore symbiotic combination , generate order and analysis of the ore controlling factors, spatial and temporal distribution in HuGang area of YongDing Country, Fujian Province, This paper thought the lead-zinc polymetallic mineralization mainly stratiform Stratoid skarn body due to magmatic activity is controlled by the Permian Qixia, Chuanshan Formation limestone and sandy mudstone by Jingshe Formation . And based on the analysis of the causes of mineralization established metallogenic model for further exploration of the type of deposit indicates prospecting.
Keywords:lead-zinc multi-metal ore    geological characteristics    new ore-finding progress    Yongding city    Fujiang province
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