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个旧锡矿印支中晚期海底基性火山-沉积Sn-Cu-Zn(Au)矿床成矿雏议

个旧锡矿印支中晚期海底基性火山-沉积Sn-Cu-Zn(Au)矿床成矿雏议

ISSN:0495-5331
2006年第42卷第1期
地质·矿床
谈树成[1],秦德先[2],赵筱青[1],李俊[2],夏既胜[1],蒋顺德[2],崔银亮[2],张学书[2] TAN Shu-cheng[1],QIN De-xian[2],ZHAO Xiao-qing[1],LI Jun[2],XIA Ji-sheng[1],JIANG Shun-de[2],CUI Yin-liang[2],ZHANG Xue-shu[2]
  1. 云南大学资源环境与地球科学学院,昆明,650091
  2. 昆明理工大学矿产地质研究所,昆明,650093

个旧锡矿长期以来在花岗岩成因模式指导下进行找矿,曾取得了显著的找矿效果.近年来,随着研究和勘查工作的深入,个旧锡矿的非花岗岩成矿作用也日益受到了重视.在全面研究和总结个旧锡多金属矿区成矿理论的基础上,以系统论为指导,以成矿系列研究为切入点,探讨了印支中晚期海底基性火山-沉积Sn-Cu-Zn(Au)矿床成矿观点,并论述了该类型矿床的地质地球化学特征.

The ore-finding has been guided by the theory of granitic genesis and model for a long time in the Gejiu tin deposit,and remarkable prospecting results were once got.In recent years,theory of non-granitic genesis is paid more and more attention.After summarizing geological and geochemical characteristics at Gejiu,submarine basic volcano-sedimentary Sn-Cu-Zn(Au) deposit series of the medium-later Indo-Chinese epoch is established.

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ISSN:0495-5331
2006年第42卷第1期
地质·矿床

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