关于中国西部龙首山、祁连山成矿区（带）进一步找矿问题的思考

doi:10.11867/j.issn.1001-8166.2005.01.0036

地球科学进展 ›› 2005, Vol. 20 ›› Issue (1): 36 -041. doi: 10.11867/j.issn.1001-8166.2005.01.0036

白云来 ^1，2，范育新 ³，汤中立 ⁴，江荣伏 ⁵

1.中国石油勘探开发研究院西北分院，甘肃兰州 730020；;
2.中国地质大学，北京 100083；;
3.兰州大学资源环境学院，甘肃兰州 730000；;
4.甘肃省地质勘查局，甘肃兰州;
5.金川公司，甘肃兰州

收稿日期:2003-08-08 修回日期:2004-05-11 出版日期:2005-01-25
通讯作者: 白云来 E-mail:baiyl6666@sina.com
基金资助:
原地质矿产部“九五”前沿科技项目华北古陆成矿系统成矿构造动力学(编号：9501107)；甘肃省科技攻关项目“华北古陆西南边缘(龙首山—祁连山)成矿系统及成矿构造动力学”（编号：GS002-B25-062）资助.

Pondering upon the Problem of Further Exploration in the Longshoushan Qilianshan Ore Belt, Western China

BAI Yunlai ^{1 ,2}，FAN Yuxin ³, TANG Zhongli ⁴ , JIANG Rongfu ⁵

1. China University of Geosciences, Beijing 100083,China；
2. Petrochina Exploration & Development Research Institute(Northwest), Lanzhou 730020,China；
3. College of Earth and Envienment, Lanzhou University, Lanzhou 730000,China;
4.Gansu Bureauof Geological Exploration, Lanzhou 730000,China;
5. Jinchuan Company, Gansu Jinchang 745000,China

Received:2003-08-08 Revised:2004-05-11 Online:2005-01-25 Published:2005-01-25

下载PDF ( 1025 )

进入21世纪以来，我国许多矿山都面临着后备资源危机问题，西部地区甘肃境内的龙首山、祁连山成矿区（带）里的矿山也不例外。从"成矿系统"的观念出发，深入分析了区域成矿构造背景，认为区内存在华北古陆西南和柴达木-中祁连北部两种大陆边缘；提出应利用非传统矿产理念进行新一轮矿产勘查，在龙首山、祁连山成矿区（带）不仅要加强传统矿种的勘查，也要注意新类型矿产的开发，同时注意环境保护；最后，还强调矿产资源的勘查和开发工作离不开既有较高理论水平又具有丰富勘查经验的高素质勘查人才，也离不开强有力的资金保证。

关键词: 龙首山, 祁连山, 成矿区（带）, 成矿系统

Many mines in China have been confronting with crisis of reserved resources since the 21st century. The mines, which situated in the LongshoushanQilianshan ore belt in Gansu province can not run away from such a fate. From the idea of metallogenic systems, We analyzed regional metallogenic tectonic settings of the Longshoushan-Qilianshan ore belt, and considered that there are two continental margins of Southwestern North-China paleocontinent and Northern Qitam-Mid-Qilianshan plate. We think it very necessary to carry out a new circle of mineral exploration under the guidance of nontraditional-mineral-resources-theory. In the Longshoushan-Qilianshan ore belt, we should not only strengthen the exploration of traditional minerals but also pay more attention to new type of mineral resources. At the same time environment protection should also be emphasized. Minerals exploration is based on talents who have advanced theory, abundant exploration experiences and large amount of capitals.

Key words: Longshoushan-Qilianshan, Ore belt, Crisis of resources

中图分类号:

P42
TP79

［1］Song Shuhe.The characteristics of pyrite-type copper deposit in the Qilianshan mountains,China[J].Acta Geologica Sinic,1995，35(1)：34-46.[宋叔和.祁连山一带黄铁矿型铜矿的特征及成矿规律[J].地质学报，1995，35(1)：34-46.]
［2］Tang Zhongli,Bai Yunlai.The tectonics frame and metallogenic systems[J].Earth Science Frontiers，1999，6（2）：271-284. [汤中立,白云来.华北古大陆西南边缘构造格架与成矿系统[J].地学前缘，1999，6（2）：271-284.]
［3］Tang Zhongli,Bai Yunlai.The Metallogenic Systems and the Metallogenic Dynamics[M].Beijing: Geological Publishing House,2002.[汤中立，白云来.华北西南边缘（龙首山—祁连山）成矿系统及成矿动力学[M].北京：地质出版社,2002.]
［4］Tang Zhongli,Bai Yunlai.The two types of the tectonic foundation block and its metallogenic systems in the northern Qinlian orogenic belt[J].Acta Geologica Gansu,2001,10(2):1-11.[汤中立,白云来.北祁连造山带两种构造基地岩块及成矿系统[J].甘肃地质学报,2001,10(2):1-11.]
［5］Tang Zhongli,Bai Yunlai,Li Zhilin.Geotectonic Setting of Large and Superlarge Mineral Deposits on the Southwestern Margin of the North China Plate[J].Acta Geologica Sinica，Journal of the Geological Society of China，2002，76 (3):367-377.
［6］Yang Yu, Fan Guolin ,Yao Guojin,et al. Gansu Rock Stratum[M].Wuhan: China University of Geosciences Publishing House,1997.[杨雨，范国琳，姚国金，等.甘肃省岩石地层[M].武汉:中国地质大学出版社,1997.]
［7］Feng Yimin. Investigatory summary of the Qilian orogenic belt,China:History,presence and prospect[J].Advances in Earth Science,1997, 12(4): 307-314.[冯益民.祁连造山带研究概况——历史、现状及展望[J].地球科学进展，1997,12(4): 307-314.]
［8］Xia Linqin,Xia Zuchun, Xu Xueyi.The dynamics of tectonic-volcanics magma evolvement [J].Xibei Geological Science,1995，16：1-28.[夏林圻，夏祖春，徐学义.北祁连构造—火山岩岩浆演化动力学[J].西北地质科学，1995，16：1-28.] 
［9］Tang Zhongli,Li Wenyuan. Metallogenic Regularities and Geological Correlation on Jinchuan Copper-Nickel Deposit, China[M].Beijing: Geological Publishing House,1995.1-20.[汤中立,李文渊.金川铜镍硫化物（含铂）矿床成矿规律及地质对比[M].北京：地质出版社,1995.1-20.]
［10］Zhai Yusheng. Regional Metallogeny[M].Beijing: Geological Publishing House,1999.[翟裕生.区域成矿学[M].北京：地质出版社，1999.]

[1]	李琼,王姣姣,潘保田. 构造和降水对祁连山北麓冲积扇演化影响的数值模拟研究[J]. 地球科学进展, 2020, 35(6): 607-617.
[2]	陈京华, 贾文雄 , 赵珍, 张禹舜, 刘亚荣. 1982—2006年祁连山植被覆盖的时空变化特征研究[J]. 地球科学进展, 2015, 30(7): 834-845.
[3]	胡凯, 方小敏, 赵志军. 宇宙成因核素 ¹⁰Be揭示的北祁连山侵蚀速率特征[J]. 地球科学进展, 2015, 30(2): 268-275.
[4]	郑国光，陈跃，陈添宇，陈乾，朱君鉴，李照荣. 祁连山夏季地形云综合探测试验[J]. 地球科学进展, 2011, 26(10): 1057-1070.
[5]	由伟丰,张海清,校培喜,曹宣铎,胡云绪,谢从瑞. 北祁连山—阿拉善地区寒武纪构造—岩相古地理[J]. 地球科学进展, 2011, 26(10): 1092-1100.
[6]	余吉远，李向民，马中平，孙吉明，王建强. 青海省祁连县清水沟-白柳沟矿田含矿火山岩系年代学研究[J]. 地球科学进展, 2010, 25(1): 55-60.
[7]	张鸿翔. 我国特色成矿系统的研究进展与重点关注的科学问题[J]. 地球科学进展, 2009, 24(5): 563-570.
[8]	武震,刘时银,张世强. 祁连山老虎沟12号冰川冰下形态特征分析[J]. 地球科学进展, 2009, 24(10): 1149-1158.
[9]	王建平，翟裕生，刘家军，柳振江，刘俊. 矿床变化与保存研究的裂变径迹新途径[J]. 地球科学进展, 2008, 23(4): 421-427.
[10]	王宝鉴,黄玉霞,王劲松,陶健红. 祁连山云和空中水汽资源的季节分布与演变[J]. 地球科学进展, 2006, 21(9): 948-955.
[11]	宋述光. 北祁连山俯冲杂岩带的构造演化[J]. 地球科学进展, 1997, 12(4): 351-365.
[12]	张德会. 浅成热液成矿系统模型研究评述[J]. 地球科学进展, 1996, 11(6): 563-568.

阅读次数

全文

摘要