|本期目录/Table of Contents|

[1]宋谢炎,康 健,隆廷茂,等.甘肃金川超大型Ni-Cu-PGE硫化物矿床岩浆通道分枝构造及其深部找矿意义[J].地球科学与环境学报,2023,45(05):1049-1062.[doi:10.19814/j.jese.2023.05063]
 SONG Xie-yan,KANG Jian,LONG Ting-mao,et al.Bifurcate Magma Conduit of Jinchuan Super-large Ni-Cu-PGE Sulfide Deposit in Gansu, China and Its Implications for Deep Ore Prospecting[J].Journal of Earth Sciences and Environment,2023,45(05):1049-1062.[doi:10.19814/j.jese.2023.05063]
点击复制

甘肃金川超大型Ni-Cu-PGE硫化物矿床岩浆通道分枝构造及其深部找矿意义(PDF)
分享到:

《地球科学与环境学报》[ISSN:1672-6561/CN:61-1423/P]

卷:
第45卷
期数:
2023年第05期
页码:
1049-1062
栏目:
庆贺汤中立院士从事地质工作七十周年专辑
出版日期:
2023-09-15

文章信息/Info

Title:
Bifurcate Magma Conduit of Jinchuan Super-large Ni-Cu-PGE Sulfide Deposit in Gansu, China and Its Implications for Deep Ore Prospecting
文章编号:
1672-6561(2023)05-1049-14
作者:
宋谢炎1康 健1隆廷茂12李晓栋12王永才3李德贤3艾启兴3卢建全3
(1. 中国科学院地球化学研究所 矿床地球化学国家重点实验室,贵州 贵阳 550081; 2. 中国科学院大学,北京 101408; 3. 金川集团股份有限公司,甘肃 金昌 737100)
Author(s):
SONG Xie-yan1 KANG Jian1 LONG Ting-mao12 LI Xiao-dong12 WANG Yong-cai3 LI De-xian3 AI Qi-xing3 LU Jian-quan3
(1. State Key Laboratory of Ore Deposit Geochemistry, Institute of Geochemistry, Chinese Academy of Sciences, Guiyang 550081, Guizhou, China; 2. University of Chinese Academy of Sciences, Beijing 101408, China; 3. Jinchuan Group Co., Ltd., Jinchang 737100, Gansu, China)
关键词:
小岩体成大矿 Ni-Cu-PGE硫化物矿床 岩浆通道分枝 成矿后断裂 深部找矿 甘肃
Keywords:
small intrusion forming large deposit Ni-Cu-PGE sulfide deposit bifurcate magma conduit post-mineralization fault deep ore prospecting Gansu
分类号:
P611
DOI:
10.19814/j.jese.2023.05063
文献标志码:
A
摘要:
甘肃金川超大型Ni-Cu-PGE硫化物矿床经过50多年的开采,在深边部寻找新的矿体,特别是富矿,以保持生产效率,已经成为当务之急,首先需要解决找矿方向问题。金川矿床的4个主要矿体不仅在空间上是相互独立的,空间分布格局还与矿区的成矿后断裂系统关系密切。在前人对各个主要矿体地质和地球化学特征、矿区断裂构造的系统分析和研究基础上,提出金川矿床的岩浆通道系统存在多个岩浆通道分枝,且每个分枝的启动时间不同,因此,每个矿体不仅成矿过程存在差异,也存在先后次序。在分析成矿后断裂对金川岩体和矿体空间分布状态的影响基础上,还对深部找矿潜力进行了分析,提出了深部找矿方向和策略。
Abstract:
After more than 50 years mining activities, deep prospecting for new orebodies rich in Ni and Cu become more and more important in Jinchuan super-large Ni-Cu-PGE sulfide deposit of Gansu, China. The 4 major orebodies of Jinchuan deposit are not connected each other, and location patterns of the orebodies have been affected by movement of the faults. On the basis of the studies on geology and geochemistry of these orebodies and the associated faults of Jinchuan deposit, the bifurcate magma conduit during the formation of Jinchuan deposit was identified. Branches of the bifurcate magma conduit develop and form the four major orebodies successively. Therefore, each individual orebody is formed by following a time sequence and has distinguishable features. The influence of post-mineralization faults on the spatial distribution of Jinchuan pluton and ore bodies was discussed; subsequently, potential and deep prospecting targets were also discussed.

参考文献/References:

[1] 金川集团股份有限公司.甘肃省金昌市白家嘴子矿区镍铜矿资源储量核实报告[R].金昌:金川集团股份有限公司,2017.
Jinchuan Group Co.,Ltd.Reserves of Ni-Cu Sulfide Deposit in Baijiazuizi Mining District,Jinchang,Gansu Province[R].Jinchang:Jinchuan Group Co.,Ltd.,2017.
[2] 宋谢炎.岩浆硫化物矿床研究现状及重要科学问题[J].矿床地质,2019,38(4):699-710.
SONG Xie-yan.Current Research Status and Important Issues of Magmatic Sulfide Deposits[J].Mineral Deposits,2019,38(4):699-710.
[3] 汤中立,李文渊.金川铜镍硫化物矿床(含铂)矿床成矿模式及地质对比[M].北京:地质出版社,1995.
TANG Zhong-li,LI Wen-yuan.Comparing Formation Model and Geology of Jinchuan Cu-Ni(Pt)Sulfide Deposit[M].Beijing:Geological Publishing House,1995.
[4] 汤中立,徐 刚,王泸文,等.小岩体成矿体系[J].矿物学报,2011,31(增):397-398.
TANG Zhong-li,XU Gang,WANG Lu-wen,et al.Ore-forming System in Small Intrusive Bodies[J].Acta Mineralogica Sinica,2011,31(S):397-398.
[5] 汤中立,闫海卿,焦建刚.中国岩浆硫化物矿床新分类与小岩体成矿作用[J].矿床地质,2006,25(1):1-9.
TANG Zhong-li,YAN Hai-qing,JIAO Jian-gang.New Classification of Magmatic Sulfide Deposits in China and Ore-forming Processes of Small Intrusive Bodies[J].Mineral Deposits,2006,25(1):1-9.
[6] CHAI G,NALDRETT A J.Characteristics of Ni-Cu-PGE Mineralization and Genesis of the Jinchuan Deposit,Northwest China[J].Economic Geology,1992,87(6):1475-1495.
[7] LI C S,XU Z H,DE WAAL S A,et al.Compositional Variations of Olivine from the Jinchuan Ni-Cu Sulfide Deposit,Western China:Implications for Ore Genesis[J].Mineralium Deposita,2004,39(2):159-172.
[8] RIPLEY E M,SARKAR A,LI C S.Mineralogic and Stable Isotope Studies of Hydrothermal Alteration at the Jinchuan Ni-Cu Deposit,China[J].Economic Geo-logy,2005,100(7):1349-1361.
[9] LI X H,SU L,CHUNG S L,et al.Formation of the Jinchuan Ultramafic Intrusion and the World's Third Largest Ni-Cu Sulfide Deposit:Associated with the ~825 Ma South China Mantle Plume?[J].Geoche-mistry,Geophysics,Geosystems,2005,6(11):2005-GC001006.
[10] YANG S H,QU W J,TIAN Y L,et al.Origin of the Inconsistent Apparent Re-Os Ages of the Jinchuan Ni-Cu Sulfide Ore Deposit,China:Post-segregation Diffusion of Os[J].Chemical Geology,2008,247(3/4):401-418.
[11] CHEN L M,SONG X Y,KEAYS R R,et al.Segregation and Fractionation of Magmatic Ni-Cu-PGE Sulfides in the Western Jinchuan Intrusion,Northwestern China:Insights from Platinum Group Element Geochemistry[J].Economic Geology,2013,108(8):1793-1811.
[12] DUAN J,LI C S,QIAN Z Z,et al.Geochronological and Geochemical Constraints on the Petrogenesis and Tectonic Significance of Paleozoic Dolerite Dykes in the Southern Margin of Alxa Block,North China Craton[J].Journal of Asian Earth Sciences,2015,111:244-253.
[13] KANG J,SONG X Y,LONG T M,et al.Lithologic and Geochemical Constraints on the Genesis of a Newly Discovered Orebody in the Jinchuan Intrusion,NW China[J].Economic Geology,2022,117(8):1809-1825.
[14] SONG X Y,DANYUSHEVSKY L V,KEAYS R R,et al.Structural,Lithological,and Geochemical Constraints on the Dynamic Magma Plumbing System of the Jinchuan Ni-Cu Sulfide Deposit,NW China[J].Mineralium Deposita,2012,47(3):277-297.
[15] SONG X Y,KEAYS R R,ZHOU M F,et al.Siderophile and Chalcophile Elemental Constraints on the Origin of the Jinchuan Ni-Cu-(PGE)Sulfide Deposit,NW China[J].Geochimica et Cosmochimica Acta,2009,73(2):404-424.
[16] SONG X Y,ZHOU M F,WANG C Y,et al.Role of Crustal Contamination in Formation of the Jinchuan Intrusion and Its World-class Ni-Cu-(PGE)Sulfide Deposit,Northwest China[J].International Geological Review,2006,48(12):1113-1132.
[17] 甘肃省地质矿产勘查开发局第六地质队.白家咀子硫化铜镍矿床地质[M].北京:地质出版社,1984.
The Sixth Geological Team of Gansu Provincial Bureau of Geology and Mineral Exploration & Development.Geology of the Baijiaozuizi Cu-Ni Sulfide Deposit[M].Beijing:Geological Publishing House,1984.
[18] ZHANG M J,KAMO S L,LI C S,et al.Precise U-Pb Zircon-baddeleyite Age of the Jinchuan Sulfide Ore-bearing Ultramafic Intrusion,Western China[J].Mi-neralium Deposita,2010,45(1):3-9.
[19] TANG Z L,SONG X Y,SU S G.Ni-Cu Deposits Related to High-Mg Basaltic Magma,Jinchuan,Western China[M]∥LI C S,RIPLEY E M.New Developments in Magmatic Ni-Cu and PGE Deposits.Beijing:Geological Publishing House,2009:121-140.
[20] 李士彬,宋谢炎,胡瑞忠,等.甘肃金川Ⅱ号岩体岩相学特征及分离结晶过程探讨[J].岩石学报,2007,23(10):2553-2560.
LI Shi-bin,SONG Xie-yan,HU Rui-zhong,et al.Petrographic Features of Segment Ⅱ of the Jinchuan Intrusion,Gansu,and Its Fractional Crystallization[J].Acta Petrologica Sinica,2007,23(10):2553-2560.
[21] NALDRETT A J.Magmatic Sulphide Deposit:Geology,Geochemistry,and Exploration[M].New York:Springer,2004.
[22] LONG T M,SONG X Y,KANG J,et al.Genesis of No.2 Orebody of the Jinchuan Magmatic Ni-Cu-(PGE)Sulfide Deposit,NW China:New Constraints from the Newly Discovered Deep Extension[J].Mine-ralium Deposita,2023,58:1317-1332.
[23] 焦建刚,汤中立,闫海卿,等.金川铜镍硫化物矿床中富铜矿石铂族元素特征及矿床成因[J].西北地质,2012,45(4):242-253.
JIAO Jian-gang,TANG Zhong-li,YAN Hai-qing,et al.PGE Characteristics of Cu-rich Ores in the Jinchuan Cu-Ni Sulfide Deposit and Its Genesis[J].Northwestern Geology,2012,45(4):242-253.
[24] DUAN J,LI C S,QIAN Z Z,et al.Multiple S Isoto-pes,Zircon Hf Isotopes,Whole-rock Sr-Nd Isotopes,and Spatial Variations of PGE Tenors in the Jinchuan Ni-Cu-PGE Deposit,NW China[J].Mineralium Deposita,2016,51(4):557-574.
[25] SU S G,LI C S,ZHOU M F,et al.Controls on Variations of Platinum-group Element Concentrations in the Sulfide Ores of the Jinchuan Ni-Cu Deposit,Western China[J].Mineralium Deposita,2008,43(6):609-622.
[26] TONNELIER N J.Geology and Genesis of The Jinchuan Ni-Cu-(PGE)Deposit,China[D].Sudbury:Laurentian University,2010.
[27] 宋谢炎,肖家飞,朱 丹,等.岩浆通道系统与岩浆硫化物成矿研究新进展[J].地学前缘,2010,17(1):153-163.
SONG Xie-yan,XIAO Jia-fei,ZHU Dan,et al.New Insights on the Formation of Magmatic Sulfide Deposits in Magma Conduit System[J].Earth Science Frontiers,2010,17(1):153-163.
[28] LIGHTFOOT P C,KEAYS R R,EVANS-LAMSWOOD D,et al.S Saturation History of Nain Plutonic Suite Mafic Intrusions:Origin of the Voisey's Bay Ni-Cu-Co Sulfide Deposit,Labrador,Canada[J].Mineralium Deposita,2012,47:23-50.
[29] SONG X Y,DENG Y F,XIE W,et al.Prolonged Basaltic Magmatism and Short-lived Magmatic Sulfide Mineralization in Orogenic Belts[J].Lithos,2021,390/391:106114.
[30] DENG Y F,SONG X Y,XIE W,et al.The Role of External Sulfur in Triggering Sulfide Immiscibility at Depth:Evidence from the Huangshan-Jing'erquan Ni-Cu Metallogenic Belt,NW China[J].Economic Geology,2022,117(8):1867-1879.
[31] 宋谢炎,邓宇峰,颉 炜,等.新疆黄山—镜儿泉铜镍硫化物成矿带岩浆通道成矿特征及其找矿意义[J].矿床地质,2022,41(6):1108-1123.
SONG Xie-yan,DENG Yu-feng,XIE Wei,et al.Ore-forming Processes in Magma Plumbing Systems and Significances for Prospecting of Huangshan-Jing'er-quan Ni-Cu Sulfide Metallogenetic Belt,Xinjiang,NW China[J].Mineral Deposits,2022,41(6):1108-1123.
[32] 苏尚国,汤中立,周 岱.金川含矿超镁铁岩侵入体侵位序列[J].地学前缘,2010,17(2):118-126.
SU Shang-guo,TANG Zhong-li,ZHOU Dai.Empla-cement Sequence in the Jinchuan Sulfide Ore-bearing Ultramafic Intrusion,Western China[J].Earth Scien-ce Frontiers,2010,17(2):118-126.
[33] 闫海卿,王 强,胡彦强,等.金川铜镍硫化物岩浆矿床前锋岩浆与岩浆通道[J].中国地质,2013,40(3):807-819.
YAN Hai-qing.WANG Qiang,HU Yan-qiang,et a1.Striker Magma and Magma Channel in the Jinchuan Copper-nickel Sulfide Magmatic Deposit[J].Geology in China,2013,40(3):807-819.
[34] SAUMUR B M,CRUDEN A R,BOUTELIER D.Sul-fide Liquid Entrainment by Silicate Magma:Implications for the Dynamics and Petrogenesis of Magmatic Sulfide Deposits[J].Journal of Petrology,2016,56(12):2473-2490.
[35] 宋谢炎,胡瑞忠,陈列锰.铜、镍、铂族元素地球化学性质及其在幔源岩浆起源、演化和岩浆硫化物矿床研究中的意义[J].地学前缘,2009,16(4):287-305.
SONG Xie-yan,HU Rui-zhong,CHEN Lie-meng.Geochemical Natures of Copper,Nickel and PGE and Their Significance for the Study of Origin and Evolution of Mantle-derived Magmas and Magmatic Sulfide Deposits[J].Earth Science Frontiers,2009,16(4):287-305.

相似文献/References:

[1]李文渊,高永宝,张照伟,等.镁铁—超镁铁质岩与花岗岩-伟晶岩“小岩体成大矿”对比——以昆仑成矿带夏日哈木和大红柳滩超大型矿床为例[J].地球科学与环境学报,2023,45(05):1036.[doi:10.19814/j.jese.2023.05049]
 LI Wen-yuan,GAO Yong-bao,ZHANG Zhao-wei,et al.Comparison of Mafic-ultramafic and Granite-pegmatite “Small Intrusion Forming Large Deposit”—Taking Xiarihamu and Dahongliutan Super-large Deposits in Kunlun Metallogenic Belt, China as Examples[J].Journal of Earth Sciences and Environment,2023,45(05):1036.[doi:10.19814/j.jese.2023.05049]

备注/Memo

备注/Memo:
收稿日期:2023-05-30; 修回日期:2023-07-22投稿网址:http:∥jese.chd.edu.cn/
基金项目:国家自然科学基金项目(42330807,42121003)
作者简介:宋谢炎(1962-),男,河北丰宁人,研究员,博士研究生导师,理学博士,E-mail:songxieyan@vip.gyig.ac.cn。
更新日期/Last Update: 2023-10-15