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黄金科学技术 ›› 2013, Vol. 21 ›› Issue (5): 21-27.

• 矿产勘查与资源评价 • 上一篇    下一篇

秦岭造山带卡林型—类卡林型金矿勘查与研究回顾

张复新1,王立社2   

  1. 1.西北大学大陆动力国家重点实验室,陕西  西安   710069;
    2.西安地质调查中心,陕西  西安   710054
  • 出版日期:2013-10-28 发布日期:2014-04-02
  • 作者简介:张复新(1945-),男,河北张家口人,教授,从事矿床地质与地球化学研究工作.zhangfux@nwu.edu.cn
  • 基金资助:

    国家青年科学基金项目“英格里克和清水泉镁铁质—超镁铁质岩成因成因研究”(编号:41103021)和国家自然科学基金项目“甘肃阳山超大微细浸染型金矿成因研究”(编号:40572065)联合资助.

Exploration and Research Review of Carlin and Carlin-like Type Gold Deposits in Qinling Moutains Orogenic Belt

ZHANG Fuxin1,WANG Lishe2   

  1. 1.State Key Laboratory of Continental Dynamics,Northwest University,Xi’an   710069,Shaanxi,China;
    2.Xi’an Geological Survey Center,Xi’an   710054,Shaanxi,China
  • Online:2013-10-28 Published:2014-04-02

摘要:

20世纪70年代初,卡林型金矿理论传入中国,并与中国地质实际相结合,很快在西北和西南地区发现找矿线索并勘查出经典的卡林型小型金矿,至此拉开了中国大陆寻找卡林型金矿的序幕。20世纪70—80年代是我国学者对卡林型金矿研究和勘查比较系统的认识阶段,矿床理论得到深化,更加明确了卡林型金矿的内涵,并发现和勘查出数例经典卡林型金矿。20世纪90年代和21世纪之交,我国卡林型金矿勘查与研究步入收获阶段,在完善卡林型金矿内涵的基础上,根据已发现的一些大—中型卡林型金矿厘定出类卡林型金矿新亚类。在中国已经发现成群、成带集中分布的卡林型—类卡林型金矿,其控矿因素突显,成矿规律趋同,并构成西北和西南2个世界级规模的卡林型—类卡林型金三角金矿带。21世纪以来,我国卡林型金矿勘查与研究工作步入理性阶段,接连成功勘查几例超大型卡林型金矿,其中阳山金矿属于卡林型—类卡林型的复合类型。至此,对该类型金矿产出地质背景、形成地质条件与控矿因素、矿床类型、矿床成因和成矿规律的认识更加系统、完善和成熟。

关键词: 卡林型金矿, 类卡林型金矿, 勘查与研究阶段, 秦岭&mdash, 昆仑造山成矿带

Abstract:

In the early 1970’s,Carlin-type gold deposits theory was introduced into China from the United States of America.Soon,geological workers found clues and explored some small classical Carlin type gold deposits in the northwest and southwest regions by combining this theory with Chinese geological reality.From that time on,the prelude for Carlin type gold deposits was opened in mainland China.1970s to 1980s is the stage of cognition about the Carlin type gold deposits,during this period,the scholars did more systematic research on the deposits,the deepening of deposit theory and cognition were promoted obviously.Through gold exploration and research,workers became more and more clear and established the connotation of Carlin type gold deposits,improved the understanding and correct ideas,several cases of classic Carlin type gold deposits were found and explored.The turn from the 1990s to the beginning of 21 centuries,exploration and research of Carlin type gold deposits got into the harvest time.And then,on the basis of improving connotation of Carlin type gold deposits,some large,medium-sized Carlin type gold deposits had discovered which were redefined as the Carlin-like type gold deposits.At that time,there are Carlin and Carlin-like type gold deposits in China,which distribute in groups or belts,with clear ore control factors and stability metallogenic regularity,and constituted the northwest,southwest two world scale Carlin and Carlin-like type Golden Triangle ore belt.The research and exploration have gone into rational stage since 21 century,some super-large Carlin type gold deposits were explored successfully in succession,Yangshan deposit is a sign of it,which belongs to Carlin and Carlin-like composite type.At this time,study on the geological background,formation conditions,control factors,origin and metallogenic regularity of the type deposits has become more systemic,perfect and well-rounded.

Key words: Carlin type gold deposits, Carlin-like type gold deposits, exploration and research stage, Qinling-Kunlun orogenic and metallogenic belt

中图分类号: 

  • P618.51

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