Please wait a minute...
E-mail Alert Rss
 
物探与化探  2010, Vol. 34 Issue (4): 415-421    
  综述 本期目录 | 过刊浏览 | 高级检索 |
SEDEX型矿床地质地球化学特征及研究趋势
 王炜1,鲍征宇1,李璇2,徐争启3
1.中国地质大学 地质过程与矿产资源国家重点实验室,湖北 武汉430074;2.成都理工大学 地球科学学院,四川 成都610059;3.成都理工大学 核技术与自动化工程学院,四川 成都610059
GEOLOGICAL AND GEOCHEMICAL CHARACTERISTICS AND RESEARCH TRENDS OF THE SEDEX DEPOSITS
WANG Wei 1,BAO Zhengyu 1,LI Xuan 2,XU Zhengqi 3
1. State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Wuhan430074, China;2. College of Earth Sciences, Chengdu University of Technology, Chengdu610059, China;3. College of Nuclear Technology and Automation Engineering, Chengdu University of Technology, Chengdu610059, China
全文: PDF(981 KB)  
输出: BibTeX | EndNote (RIS)      
摘要 

沉积喷流型矿床(SEDEX)是很重要的一类矿床,在世界范围内广泛分布,是Zn和Pb的重要来源,分别超过世界储量的50%和60%。笔者通过参阅前人研究成果以及相关文献,概述了沉积喷流矿床的构造背景、地质及地球化学特征、成矿模式以及勘探进展、找矿特征等,并列举出关于SEDEX矿床今后研究的几个方向。

服务
把本文推荐给朋友
加入引用管理器
E-mail Alert
RSS
作者相关文章
Abstract

Sedimentary exhalative deposits (SEDEX) widely distributed in the world constitute an important type of ore deposits. They are major sources of Zn and Pb and possess more than 50% and 60% of world Zn and Pb reserves, respectively. In this paper, based on consulting various research achievements and vast literatures concerning this type of ore deposits, the authors provide an overview of several aspects of the sedimentary exhalative deposits, such as their tectonic settings, geological and geochemical characteristics, oreforming model, progress of exploration, and prospecting characteristics, and point out several directions in the further study of  SEDEX deposits.

收稿日期: 2009-08-29      出版日期: 2010-08-10
: 

 

 
  P632

 
通讯作者: 王炜(1986- ),男,现正攻读地球化学专业硕士学位,主要从事勘查地球化学研究。
引用本文:   
王炜, 鲍征宇, 李璇, 徐争启. SEDEX型矿床地质地球化学特征及研究趋势[J]. 物探与化探, 2010, 34(4): 415-421.
WANG Wei, BAO Zheng-Yu, LI Xuan, XU Zheng-Qi. GEOLOGICAL AND GEOCHEMICAL CHARACTERISTICS AND RESEARCH TRENDS OF THE SEDEX DEPOSITS. Geophysical and Geochemical Exploration, 2010, 34(4): 415-421.
链接本文:  
https://www.wutanyuhuatan.com/CN/      或      https://www.wutanyuhuatan.com/CN/Y2010/V34/I4/415

[1]颜文.喷流矿床研究综述[J].地质地球化学,1993(6):18-23.

[2]刘继顺.喷流沉积成矿作用研究的若干问题[J].矿产与地质,1996,10(51):6-10.

[3]Huchinson R W.层控矿床在地质历史中的地位[J].国外矿床志,1988(3):19-57.

[4]Goodfellow W D. Geology, genesis and exploration of SEDEX deposits, with emphasis on the Selwyn Basin, Canada[G]//Deb M, Goodfellow W D.Sedimenthosted LeadZinc Sulphide Deposits: Attributes and Models of Some Major Deposits of India, Australia and Canada. Narosa Publishing House, Delhi, India, 2004:24-99.

[5]田毓龙,秦德先,林幼斌,等.喷流热水沉积矿床研究的现状与进展[J].昆明理工大学学报,1999,24(1):150-156.

[6]赵化琛.我国若干裂谷构造特征及其成矿作用[J].矿产与地质,1995,9(1):10-15.

[7]Karen Lund. Geometry of the neoproterozoic and paleozoic rift margin of western Laurentia: Implications for mineral deposit settings[J].Geosphere,2008,4(2):429-444.

[8]Heinrich D H. Sedimentary mineral deposits and the evolution of earth's nearsurface environments[J]. Economic Geology,2005,100:1489-1509.

[9]翟裕生.同生断层对层控超大型矿床的控制[J].中国科学:D辑,1998,28(3):214-218.

[10] 古志宏,赵俊兴,周永章,等.西秦岭厂坝—李家沟铅锌矿矿床地质特征和成因分析[J].中山大学研究生学刊:自然科学、医学版,2007,28(3):40-46.

[11] 彭润民,翟裕生,韩雪峰,等.内蒙古狼山造山带构造演化与成矿响应[J].岩石学报,2007,23(3):679-688.

[12] Goodfellow W D, Lydon J W, Turner R W, et al. Geology and genesis of stratiform sedimenthosted (SEDEX) ZnPbAg sulphide deposits[J].Geological Association of Canada Special Paper,1993,40:203-251.

[13] 池三川.非火山环境海底沉积—喷流(“SEDEX”)矿床[J].地学前缘,1994,1(3-4):183.

[14] 徐克勤,王鹤年,周建平,等.论华南喷流—沉积块状硫化物矿床[J].高校地质学报,1996,2(3):241-256.

[15] 颜文,李朝阳.热水喷流沉积成矿与地学思维[J].地球科学进展,1993,8(2):40-46.

[16] David L K, Karen D K, William B C, et al. Beyond the obvious limits of ore deposits: the use of mineralogical, geochemical, and biological features for the remote detection of mineralization[J]. Economic Geology,2006,101:729-752.

[17] Goodfellow W D, Lydon J W. Sedimentary exhalative(SEDEX) deposits[EB/OL]. http:// gsc.nrcan.gc.ca/mindep/synth_dep/sedex/index_e.php, 2008-09-23/2009-05-05.

[18] 韩发,孙海田.Sedex型矿床成矿系统[J].地学前缘,1999,6(1):139-163.

[19] 王长明,张寿庭,邓军,等.内蒙古黄岗梁锡铁多金属矿床层状夕卡岩的喷流沉积成因[J].岩石矿物学杂志,2007,26(5):409-417.

[20] 田朝江.塔卡矿区MVT、Sedex型矿床特征及成因探讨[J].新疆有色金属,2008(6):6-8.

[21] 坚润堂,李峰,徐国端.锡铁山SEDEX型铅锌矿床成矿物质来源综述[J].矿产与地质,2007,21(6):642-648.

[22] 祝朝辉,张乾,朱笑青,等.中国SEDEX型矿床成矿流体硼、硅、氦氩同位素组成研究评述[J].矿物岩石地球化学通报,2006,25(3):279-284.

[23] 李贶,胡凯,蒋少涌,等.粤西大降坪黄铁矿矿床HeAr同位素和稀土元素组成及成矿物质来源探讨[J].南京大学学报:自然科学,2006,42(6):611-620.

[24] 胡瑞忠,钟宏,叶造军,等.金顶超大型铅锌矿床氦、氩同位素地球化学[J].中国科学:D辑,1998,28(3):208-213.

[25]Jiang Shaoyong, John F S, Martin R P. SmNd dating of the giant Sullivan PbZnAg deposit, British Columbia[J].Geology,2000,28(8):751-754.

[26]  Franklin J M. Volcanicassociated massive sulfide deposits[J]. Economic Geology,1981,75:567-573.

[27] Cooke D R, Bull S W, Large R R, et al.The importance of oxidized brines for the formation of Australian Proterozoic stratiform sedimenthosted PbZn (Sedex) deposits[J]. Economic Geology,2000,95:1-18.

[28] John F S, Julie A D, Jeanine M S, et al. Paleozoic sedimentary rocks in the Red Dog ZnPbAg district and vicinity, western Brooks Range, Alaska: provenance, deposition, and metallogenic significance[J].Economic Geology,2004,99:1385-1414.

[29] Goodfellow W D. Anoxic stratified oceans as a source of sulphur in sedimenthosted stratiform ZnPb deposits (Selwyn Basin, Yukon, Canada)[J].Chemical Geology,1987,65:359-382.

[30] Goodfellow W D. Anoxic conditions in the Aldridge Basin during formation of the Sullivan ZnPb deposit: implications for the genesis of massive sulphides and distal hydrothermal sediments[G]//Lydon J W, Hy T, Slack J F, et.al. The Geological Environment of the Sullivan Deposit, British Columbia. Mineral Deposits Division of the Geological Association of Canada,2000: 218-250.

[31] 赵准.兰坪金顶铅锌矿——陆相SEDEX型矿床[J].云南地质,2007,26(1):1-14.

[32] Yang Jianwen, Feng Zuohai, Luo Xianrong,et al.On the role of buoyancy force in the ore genesis of SEDEX deposits:Example from Northern Australia[J].Earth Sciences,2009,52(4):452-460.

[33] 刘建宏,张新虎,赵彦庆,等.西秦岭成矿系列、成矿谱系研究及其找矿意义[J].矿床地质,2006,25(6):727-734.

[34] 叶杰,刘建明,张安立.沉积喷流型矿化的岩石学证据——以大兴安岭南段黄岗和大井矿床为例[J].岩石学报,2002,18(4):585-592.

[35] 朱笑青,张乾,何玉良,等.地史早期岩石中的铅锌演化——狼山—渣尔泰山中元古代铅锌成矿的物质基础[J].矿物学报,2005,25(4):325-333.

[36] Garth E G, Karen D K, John F S, et al. Trace elements in ZnPbAg deposits and related stream sediments, Brooks Range Alaska, with implications for Tl as a pathfinder element[J].Geochemistry,2009,9:19-37.

[37] 涂光炽. 超大型矿床的探寻与研究的若干进展[J].地学前缘,1994,1(3):45-53.

[38] 彭润民,翟裕生,王志刚,等.内蒙古狼山炭窑口热水喷流沉积矿床钾质“双峰式”火山岩层的发现及其示踪意义[J].中国科学:D辑,2004,34(12):1135-1144.

[1] 徐新学. 大地电磁测深法在深部矿产资源调查中的应用[J]. 物探与化探, 2011, 35(1): 17-19.
[2] 赵君, 乔树岩, 戴慧敏. 水系沉积物测量在阿巴通德拉扎卡地区找矿应用[J]. 物探与化探, 2011, 35(1): 24-27.
[3] 吴富强, 赵培松, 李朝旭.  昆明东川区播卡金矿地球化学特征与成因[J]. 物探与化探, 2011, 35(1): 28-32.
[4] 张伟, 陈陵康. 西藏冲江地区地球化学异常信息的提取[J]. 物探与化探, 2011, 35(1): 33-36.
[5] 张秋, 谭志伟, 张作祥, 赵兰, 刘凤霞. 贝尔凹陷水文地球化学特征与油气藏的关系[J]. 物探与化探, 2011, 35(1): 37-41.
[6] 刘振军, 王德发, 范子梁, 刘英才. 高精度航空磁测在西藏一江两河地区找矿效果[J]. 物探与化探, 2011, 35(1): 47-51.
[7] 景小阳.
煤矿高密度电阻率仪的设计与实现
[J]. 物探与化探, 2011, 35(1): 52-57.
[8] 孟银生, 姚长利, 刘瑞德, 黄力军. 地热田温度预测的反演电阻率方法[J]. 物探与化探, 2011, 35(1): 58-60.
[9] 王星明, 郭栋, 李嘉.
水资源勘查中综合电法勘探方法技术与应用
[J]. 物探与化探, 2011, 35(1): 65-69.
[10] 王衍棠, 罗文造, 舒虎. 北黄海盆地地震主要采集参数模拟[J]. 物探与化探, 2011, 35(1): 70-74.
[11] 任政委, 武毅, 孙党生, 孙晟, 王璇. 高干扰环境下西安市地裂缝勘查新方法[J]. 物探与化探, 2011, 35(1): 75-79.
[12] 杨农合, 王辉, 徐小林, 吴朝俊, 杨宁宁, 王宝琛. 应用瞬变电磁法小线框大电流探测隐伏断层[J]. 物探与化探, 2011, 35(1): 80-85.
[13] 孙歧峰, 白清云. 转换横波阻抗的求取[J]. 物探与化探, 2011, 35(1): 93-96.
[14] 李强, 尚新民, 赵胜天, 王胜阁.
非一致性时移地震资料叠前互约束处理技术
[J]. 物探与化探, 2011, 35(1): 97-102.
[15] 李文杰, 宁俊瑞, 陈世军, 刘来详. 利用Burg反褶积提高地震资料处理质量[J]. 物探与化探, 2011, 35(1): 127-130.
Viewed
Full text


Abstract

Cited

  Shared   
  Discussed   
京ICP备05055290号-3
版权所有 © 2021《物探与化探》编辑部
通讯地址:北京市学院路29号航遥中心 邮编:100083
电话:010-62060192;62060193 E-mail:whtbjb@sina.com