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云南兰坪盆地北部东缘铅锌矿床喷流沉积成因的厘定——来自矿物学和硫同位素证据
引用本文:黄玉凤,曹殿华,王志军,李以科,王安建.云南兰坪盆地北部东缘铅锌矿床喷流沉积成因的厘定——来自矿物学和硫同位素证据[J].地质力学学报,2011,17(1):91-102.
作者姓名:黄玉凤  曹殿华  王志军  李以科  王安建
作者单位:1. 中国地质科学院矿产资源研究所,北京,100037
2. 罕王傲牛矿业股份有限公司,辽宁抚顺,113001
基金项目:国家科技支撑计划课题(2006BAB01A07)资助
摘    要:通过详细的野外地质工作和显微镜下观察,对云南兰坪盆地东北部维西-乔后断裂带上三叠统石钟山组(T3s)中产出的铅锌矿床成因进行厘定.研究结果表明,测区内存在大量典型的同生沉积矿床标志,如:纹层构造、条纹条带构造、网脉构造、黄铁矿条带软沉积构造、黄铁矿草莓状结构、黄铁矿胶状构造、闪锌矿同心环状构造等.青甸湾矿床金属硫化物硫...

关 键 词:兰坪盆地  喷流沉积  同生沉积  矿物学  硫同位素
收稿时间:2010/10/26 0:00:00

SEDEX DEPOSIT GENESIS OF THE Pb-Zn DEPOSITS IN THE NORTHEASTERN MARGIN OF LANPING BASIN IN YUNAN: EVIDENCE FROM MINERALOGICAL AND SULFUR ISOTOPIC STUDIES
HUANG Yu-feng,CAO Dian-hu,WANG Zhi-jun,LI Yi-ke and WANG An-jian.SEDEX DEPOSIT GENESIS OF THE Pb-Zn DEPOSITS IN THE NORTHEASTERN MARGIN OF LANPING BASIN IN YUNAN: EVIDENCE FROM MINERALOGICAL AND SULFUR ISOTOPIC STUDIES[J].Journal of Geomechanics,2011,17(1):91-102.
Authors:HUANG Yu-feng  CAO Dian-hu  WANG Zhi-jun  LI Yi-ke and WANG An-jian
Affiliation:HUANG Yu-feng1,CAO Dian-hua1,WANG Zhi-jun2,LI Yi-ke1,WANG An-jian1(1.Institute of Mineral Resources,Chinese Academy of Geological Sciences,Beijing 100037,China,2.Hanwang Aoniu Mining Corporation Ltd.,Fushun 113001,China)
Abstract:A series of lead-zinc deposits such as Qingdianwan,Caizidi,Jinshantao and so on,which are situated in the Upper Triassic Shizhongshan Formation(T3s) at the Weixi-Qiaohou fault belt,northeast of Lanping Basin.The genesis studies of these lead-zinc deposits are relatively superficial..In this paper,through detailed field geological survey and studies under the microscope,authors found a large number of typical signs of the synsedimentary deposit such as laminated structure,striped band structure,vein net stru...
Keywords:Lanping Basin  Sedimentary Exhalative deposit(SEDEX)  synsedimentary  mineralogy  sulfur isotope  
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