| 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 |
| 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 |
| Geological characteristics and prospecting potential and of the lead-zinc copper polymetallic deposit in the HuGang area, YongDing Country, Fujian Province |
| 投稿时间：2015-03-27 修订日期：2015-10-13 |
| DOI： |
| 中文关键词: 铅锌多金属矿 地质特征 找矿新进展 永定 福建省 |
| 英文关键词: lead-zinc multi-metal ore, geological characteristics, new ore-finding progress, Yongding city, Fujiang province |
| 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。 |
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| 中文摘要: |
| 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进行了初步总结，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指明了找矿方向。 |
| 英文摘要: |
| 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. |
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