摘要
埋藏史模拟技术已经在油气地质研究领域中被广泛应用,但是在金属矿床中却鲜有探索者。随着对金属需求的日益增加,迫切需要把类似埋藏史模拟技术等在石油行业已经运用成熟的技术引入到金属矿产的相应研究中。恢复了晴隆地区埋藏史,结合流体包裹体均一温度,确定晴隆锑矿成矿深度范围为2 587~4982 m,成矿时间可能为早三叠世到晚三叠世中期。
Currently,the modeling technology of burial history has applied in the research of oil—gas geology,however,this technology has not yet been applied in the research of the metal deposit geology.With the increasing demand for metals,it is necessary to introduce the modeling technology of burial history that has been used maturely in the oil industry into the metal mineral in the corresponding research technique.Maps for the burial history of Qinglong area were drawn in combination with the homogenization temperature of fluid inclusions,and it reveals that Qinglong Antimony deposit took place during early Triassic Period and Middle of late Triassic Period with the range of metallogenic depth 2 587~4 982 m.
出处
《江西科学》
2011年第2期200-206,共7页
Jiangxi Science
基金
国家危机矿山接替资源勘查项目(200453001)
全国危机矿山西南层控矿床成矿规律总结研究项目(20089943)
昆明理工大学成矿动力学与隐伏矿预测创新团队联合资助
关键词
晴隆锑矿
流体包裹体
埋藏史
成矿时代
均一温度
Qinglong antimony deposit
Fluid inclusion
Burial history
Metallogenic epoch
Homogenization temperature
