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哀牢山成矿带壳幔相互作用与金成矿关系探讨——以元阳大坪金矿床为例
引用本文:袁士松,葛良胜,路彦明,郭晓东,王美娟,王治华,邹依林.哀牢山成矿带壳幔相互作用与金成矿关系探讨——以元阳大坪金矿床为例[J].矿床地质,2010,29(2):253-264.
作者姓名:袁士松  葛良胜  路彦明  郭晓东  王美娟  王治华  邹依林
作者单位:1. 中国地质大学地球科学与资源学院,北京,100083;中国人民武装警察部队黄金地质研究所,河北,廊坊,065000
2. 中国人民武装警察部队黄金地质研究所,河北,廊坊,065000
基金项目:国家“十一·五”科技支撑项目(编号:2006BAB01B10);;国家重点基础研究发展计划(编号:2009CB42100)的联合资助
摘    要:哀牢山成矿带位于云南省中南部,带内相续发现了墨江金厂、镇沅老王寨和元阳大坪等一批大型-超大型金多金属矿床。滇西南地区的莫霍面等深度特征、大陆地温梯度和大地热流高异常特征以及地球深层次结构特征,一致表明哀牢山地区在新生代处于强烈的壳幔相互作用时期。以大坪超大型金矿床同位素组成为例开展了示踪学研究,结果表明,成矿物质及成矿流体均以上地幔或下地壳来源为主,成矿过程中有少量地壳浅部的大气饱和水、岩浆水或它们的混合流体的加入。区域地球物理场特征及同位素示踪学研究一致表明,在哀牢山成矿带内矿床形成过程中,伴随有强烈的深部岩浆活动,壳幔相互作用对该地区矿床的形成有重要贡献。

关 键 词:地质学  壳幔相互作用  哀牢山成矿带  超大型矿床  大坪金矿  云南  

Relationship between crust-mantle reaction and gold mineralization in Ailaoshan metallogenic belt: A case study of Daping gold deposit in Yuanyang
YUAN ShiSong,GE LiangSheng,LU YanMing,GUO XiaoDong,WANG MeiJuan,WANG ZhiHua,ZOU YiLin.Relationship between crust-mantle reaction and gold mineralization in Ailaoshan metallogenic belt: A case study of Daping gold deposit in Yuanyang[J].Mineral Deposits,2010,29(2):253-264.
Authors:YUAN ShiSong  GE LiangSheng  LU YanMing  GUO XiaoDong  WANG MeiJuan  WANG ZhiHua  ZOU YiLin
Institution:1 School of Earth Science and Resources/a>;China University of Geosciences/a>;Beijing 100083/a>;China/a>;2 Gold Geological Institute of CAPF/a>;Langfang 065000/a>;Hebei/a>;China
Abstract:The Ailaoshan metallogenic belt is located in the middle-south part of Yunnan Province, where there are several large-superlarge gold-polymetallic deposits such as Jinchang in Mojiang, Laowangzhai in Zhenyuan and Daping in Yuanyang. Regional geophysical characteristics show that the NW-striking Ailaoshan metallogenic belt has a complicated crust-mantle structure. The Moho discontinu-ity isobath features reveal that the crust in the northeast is thicker than that in the southwest and represents a mantle-slop...
Keywords:geology  crust-mantle reaction  Ailaoshan metallogenic belt  superlarge deposit  Daping gold deposit  Yunnan Province  
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