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繁昌盆地张家冲铅锌矿地质特征及成矿规律
引用本文:洪东良,段留安,赵磊,邓江洪,陈四新. 繁昌盆地张家冲铅锌矿地质特征及成矿规律[J]. 安徽地质, 2014, 0(2): 103-107,118
作者姓名:洪东良  段留安  赵磊  邓江洪  陈四新
作者单位:[1]华东冶金地质勘查局综合地质大队,安徽马鞍山243000 [2]中国科学技术大学地球和空间科学学院,安徽合肥230026 [3]武警黄金第七支队,山东烟台264004 [4]鑫诚矿业有限责任公司,安徽池州247116
基金项目:致谢:本文在成文过程中得到了华东冶金地质勘查局综合地质大队刘心兵等、池州市鑫诚矿业赵磊等同志的帮助,在此一并致以感谢.
摘    要:长江中下游成矿带铜陵矿集区,长期以来为国内外研究的热点地区之一,但大都集中于研究Cu、Au、S、Fe等矿产,而铅锌矿的相关报道或科研工作相对较少。铜陵张家冲铅锌矿位于长江中下游成矿带繁昌盆地内,属次火山口控制的铅锌矿,是繁昌火山岩盆地内发现的第一个有色金属矿床,同时也是通过对盆地内硅化带的系统解剖发现的矿床,有着较高的科研和生产价值。笔者近年来组织了对该区的施工,提交(332+333)铅锌矿石资源量675.87×104t,Pb+Zn金属量11.90×104t。本文旨在通过对该区铅锌矿地质特征、矿床成因、找矿标志及成矿规律等进行总结,进一步丰富该地区成矿模式和理论,为本区乃至整个繁昌盆地下步找矿提供参考和借鉴。

关 键 词:铅锌矿  地质特征  成矿规律  繁昌盆地  张家冲

GEOLOGICAL FEATURES AND ORE-FORMING PATTERN OF THE ZHANGJIACHONG PB-ZN ORE DEPOSIT IN THE FANCHANG BASIN
HONG Dong-liang,DUAN Liu-an,ZHAO Lei,DEN Jang-hong,CHEN Si-xin. GEOLOGICAL FEATURES AND ORE-FORMING PATTERN OF THE ZHANGJIACHONG PB-ZN ORE DEPOSIT IN THE FANCHANG BASIN[J]. Geology of Anhui, 2014, 0(2): 103-107,118
Authors:HONG Dong-liang  DUAN Liu-an  ZHAO Lei  DEN Jang-hong  CHEN Si-xin
Affiliation:1. Comprehensive Geological Brigade of East China Metallurgical Geological Prospecting Bureau, Maanshan, Anhui 243000, China; 2. School of Earth and Space Sciences, University of Science and Technology of China, Hefei, Anhui 230026, China;3 Armed Police Gold-Prospecting Branch 7, Yantai, Shandong 264004, China;4 Xiehen mining Corporation Ltd. , Chizhou,Anhui 247166, China)
Abstract:The Tongling mining camp in the mid-lower Yangtze River metallogenic zone has been one of hot spots for study at home and abroad for a long time, which mostly focused on minerals of Cu, Au, S and Fe, with less report on Pb and Zn. The Zhangjiachong Pb-Zn ore deposit, Tongling is situated in the Fanchang basin of the mid-lower Yangtze River metallogenic zone. Controlled by a subvolcanc crater, it is the first non-ferrous ore deposit ever found in the Fanchang volcanic rock basin, and is also a result of systematic analysis of silicified zone in the basin, bearing higher scientific research and production values. In recent years, the author organized work in the area and presented a resource 332+333of Pb-Zn ore at 675.87×10^4t, and Pb+Zn metal at 11.90×10^4t. This paper aimed to summarize geological features, ore genesis, ore-prospecting indicators and ore-forming pattern of Pb-Zn deposits in the area, further enrich metallogenic model and theory for the area and provide a reference for ore prospecting in the area and even the whole Fanchang basin in the future.
Keywords:Pb-Zn ore  geological features  ore-forming pattern  Zhangjiachong  Fnachang basin
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