文章摘要
吴珍汉,杨玉东.燕山地区中元古界金多金属矿床类型及其时空分布规律[J].地质与勘探,1998,(3):10-15
燕山地区中元古界金多金属矿床类型及其时空分布规律
CLASSIFICATION AND TIME-SPATIAL DISTRIBUTION OF GOLD AND MULTIMETAL DEPOSITS BORN IN MIDDLE PROTEROZOIC STRATA OF YANSHAN AREA
  
DOI:
中文关键词: 金矿床 多金属矿床 矿床类型 时空分布规律
英文关键词: gold multimetal deposits,Middle Proterozoic strata,Yanshan area
基金项目:
吴珍汉  杨玉东
中国地质科学院地质力学研究所
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中文摘要:
      燕山地区中元古界碎屑岩-碳酸盐岩系内赋存着似层状金矿、古砾岩型金矿、似层状银多金属矿、层状铅锌矿、夕卡岩型铜多金属矿及火山岩型铜矿6种不同类型的矿术。古砾岩型金矿、火山岩型铜矿与层状铅锌矿分别形成于中元古宙常州沟期、大红峪期与高于庄期;似层状金矿、银多金属矿与夕卡岩型铜多金属矿则主要形成于中生代燕山期。中元古宙金多金属矿化的空间分布受同沉积构造、岩相古地理与古沉积环境等因素所制约,而燕山期金、银、
英文摘要:
      Many gold,silver and multimetal deposits,including the stratiform-like gold deposits,the palaeo-conglomerate-type gold deposits,the stratiform-like silver and multimetal deposits,the stratified lead-zinc deposits,the skarn-type copper and multimetal deposits and the marine volcanic copper deposits,are born in the Middle Proterozoic strata of Yanshan area.The palaeo-conglomerate-type gold deposits,the marine volcanic copper deposits and the stratified lead-zinc deposits were separately formed in the Changzhougou period,Dahongyu period and Gaoyuzhuang period of the Middle Proterozoic.The stratiform-like gold,silver and multimetal deposits and the skarn-type copper and multimetal deposits were mainly formed in the Mesozoic Yanshanian period.The Middle Proterozoic metallizations were mainly controlled by the syn-sedimentary faults,rock facies and palaeo-geography and the sedimentary environments.The spatial distribution of Yanshanian metallization and deposits was mainly controlled by the Middle Proterozoic stratigraphic sequence and the Yanshanian fault-magmatic activity.
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