威宁小赛—耿家屯地区铅锌矿成矿规律及成矿预测
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摘要
[中文摘要]威宁小赛-耿家屯地区位于“昭通—六盘水古生代燕山期铅、锌、铜、银、锰成矿带(Ⅲ28)”中的赫威水铅锌铜银成矿带(Ⅳ8)及黑石头—盘县铅锌银成矿带(Ⅳ9)两带上,铅锌矿点多,但中-大型矿床相对较少,研究区内工作程度较低,资金投入较少,没有开展系统的详细调查工作,近年来随着资源的需求及成矿理论的重新认识,以中国地质调查局为代表对区内铜铅锌矿进行了初步调查与综合研究；其中1992年至今,关于黔西北地区铅锌矿有很多论文发表,并从矿床地质特征及控矿因素和成矿规律进行分析。
本文以国土资源大调查项目《贵州小赛-耿家屯地区矿产远景调查》为依托,通过系统收集有关地质矿产资料和1:5万地质测量成果,采用“点面结合、重点突破、以点代面的原则”,从地、物、化、探矿工程等方面对威宁小赛-耿家屯地区铅锌矿进行控矿地质因素研究、对各种成矿信息进行综合分析和矿化信息的提取,从铅锌矿地质特征及成矿元素分布规律、物探异常分布规律、地层控矿规律、构造控矿规律、火成岩与铅锌矿的关系、矿床空间分布、成矿时间演化规律等几方面对铅锌的成矿规律进行了探索,认为研究区内铅锌矿成矿具多期性,主要成矿期为海西期,次为燕山-喜山期(改造期)：并从大地构造条件控矿因素分析、区域构造控制分析、断陷盆地控矿分析、构造控矿分析、地层岩性控矿分析以及铅锌矿找矿标志分析,初步建立了研究区内铅锌矿的找矿模型。
为打开区内寻找中大型站矿的新局面,为小赛-耿家屯地区寻找中大型铅锌矿矿提供理论基础。本次通过对铅锌矿成矿规律进行系统的分析研究,并结合前人的研究成果,将小赛-耿家屯地区进行了成矿预测,将研究区划分了六个找矿远景区及七个找矿靶区。
Pb-Zn Deposit Metallogenic Regularities and Metallogenic Prediction in The Areas of Xiaozai-Gengjiatun in Weiling CountyAbstract
The areas of Xiaozai-Gengjiatun in Weiling County located in Hezhang-Weining-Shuicheng Pb, Zn, Cu and Ag metallogenic belt (Ⅳ8Ⅲ) and Heshitou-Panxian Pb, Zn, Cu and Ag metallogenic belt (Ⅳ9Ⅲ) of Zhaotong-Liupanshui Pb, Zn, Cu and Ag metallogenic belt (Ⅲ28) of Paleozoic Phase of Yanshan. But the middle-large deposits are relatively few, The research area Capital investment less and have not carried detailed investigation. In recent years, with resources needs and the metallogeny theory rediscove, the China geological survey carrieda preliminary investigation and study. Since 1992, Published many papers about northwestern guizhou Pb-Zn deposit geology characteristics, ore-controlling factors and metallogenic regularities.
Based on the project which investigation of land and resources in Xiaozai-Gengjiatun areas of mineral vision investigation. Through collecting the data of geology and mineral resources and the related geological measurement results of 1/50,000. Using the principle of focal point of the entire area. We conducted ore-control factors of metallogenetic information research, analysis and mineralization information extraction for Xiaozai-Gengjiatun deposits in Weiling County. From Pb-Zn deposit geological characteristics, ore-forming elements distribution, geophysical anomalies distributions, ore-controlling structure, mine, igneous and relationships, ore deposits space distribution and metallogenic time evolution regularity of zinc in such aspects as the ore-forming regularity is explored. To believed there are many ore-forming period, the main ore-forming period of hercynian, and the yanshan-Himalayan(alter period) is secondary. And the tectonic conditions, the ore-controlling factors, regional tectonic control ore-controlling factors, fault basin ore-controlling factors, ore-controlling factors, lithological ore-controlling factors and lead-zinc deposit prospecting marks are analyzed, initially established a research area Pb-Zn deposit prospecting model.
For offer a theoretical basis for middle-large deposits in Xiaozai-Gengjiatun deposits in Weiling County. Through the system researched, combining the deposits of metallogenic regularities of previous research achievements, We divided into six ore-hunting prospect areas and seven oreprospecting target areas.
本文以国土资源大调查项目《贵州小赛-耿家屯地区矿产远景调查》为依托,通过系统收集有关地质矿产资料和1:5万地质测量成果,采用“点面结合、重点突破、以点代面的原则”,从地、物、化、探矿工程等方面对威宁小赛-耿家屯地区铅锌矿进行控矿地质因素研究、对各种成矿信息进行综合分析和矿化信息的提取,从铅锌矿地质特征及成矿元素分布规律、物探异常分布规律、地层控矿规律、构造控矿规律、火成岩与铅锌矿的关系、矿床空间分布、成矿时间演化规律等几方面对铅锌的成矿规律进行了探索,认为研究区内铅锌矿成矿具多期性,主要成矿期为海西期,次为燕山-喜山期(改造期)：并从大地构造条件控矿因素分析、区域构造控制分析、断陷盆地控矿分析、构造控矿分析、地层岩性控矿分析以及铅锌矿找矿标志分析,初步建立了研究区内铅锌矿的找矿模型。
为打开区内寻找中大型站矿的新局面,为小赛-耿家屯地区寻找中大型铅锌矿矿提供理论基础。本次通过对铅锌矿成矿规律进行系统的分析研究,并结合前人的研究成果,将小赛-耿家屯地区进行了成矿预测,将研究区划分了六个找矿远景区及七个找矿靶区。
Pb-Zn Deposit Metallogenic Regularities and Metallogenic Prediction in The Areas of Xiaozai-Gengjiatun in Weiling CountyAbstract
The areas of Xiaozai-Gengjiatun in Weiling County located in Hezhang-Weining-Shuicheng Pb, Zn, Cu and Ag metallogenic belt (Ⅳ8Ⅲ) and Heshitou-Panxian Pb, Zn, Cu and Ag metallogenic belt (Ⅳ9Ⅲ) of Zhaotong-Liupanshui Pb, Zn, Cu and Ag metallogenic belt (Ⅲ28) of Paleozoic Phase of Yanshan. But the middle-large deposits are relatively few, The research area Capital investment less and have not carried detailed investigation. In recent years, with resources needs and the metallogeny theory rediscove, the China geological survey carrieda preliminary investigation and study. Since 1992, Published many papers about northwestern guizhou Pb-Zn deposit geology characteristics, ore-controlling factors and metallogenic regularities.
Based on the project which investigation of land and resources in Xiaozai-Gengjiatun areas of mineral vision investigation. Through collecting the data of geology and mineral resources and the related geological measurement results of 1/50,000. Using the principle of focal point of the entire area. We conducted ore-control factors of metallogenetic information research, analysis and mineralization information extraction for Xiaozai-Gengjiatun deposits in Weiling County. From Pb-Zn deposit geological characteristics, ore-forming elements distribution, geophysical anomalies distributions, ore-controlling structure, mine, igneous and relationships, ore deposits space distribution and metallogenic time evolution regularity of zinc in such aspects as the ore-forming regularity is explored. To believed there are many ore-forming period, the main ore-forming period of hercynian, and the yanshan-Himalayan(alter period) is secondary. And the tectonic conditions, the ore-controlling factors, regional tectonic control ore-controlling factors, fault basin ore-controlling factors, ore-controlling factors, lithological ore-controlling factors and lead-zinc deposit prospecting marks are analyzed, initially established a research area Pb-Zn deposit prospecting model.
For offer a theoretical basis for middle-large deposits in Xiaozai-Gengjiatun deposits in Weiling County. Through the system researched, combining the deposits of metallogenic regularities of previous research achievements, We divided into six ore-hunting prospect areas and seven oreprospecting target areas.
引文
[1]贵州省地质矿产局.盘县幅区域地质调查报告.1973.
[2]贵州省地质矿产局.水城幅区域地质调查报告.1978.
[3]贵州省地质局.威宁幅区域地质调查报告.1982.
[4]刘家铎、张成江等.扬子地台西南缘成矿规律及找矿方向[M].北京：地质出版社,2004
[5]四川、云南、贵州省地质局.川滇黔铅锌成矿区成矿远景区划—川滇黔铅锌成矿区成矿规律及找矿预测科研报告.[R]1983
[6]王华云、梁福谅、曾鼎权等.贵州铅锌矿地质[M].贵州：贵州科技出版社,1996
[7]贵州省地质矿产局.贵州省区域地质志[M].北京：地质出版社,1987
[8]毛德明、何家骏、廖朝贵.天桥铅锌矿床的沉积改造成矿特征[J]地质地球化学.2001年第29卷第1期
[9]张国平、刘丛强、杨元根、吴攀.碳酸盐岩地区铅锌矿山水系中铅锌铜的迁移及其硫同位素示踪[J].矿物学报.2002年9月第22卷第3期
[10]张启厚、毛健全、顾尚义.水城赫章铅锌矿成矿的金属物源研究[J].贵州工业大学学报.第27卷第6期1998年12月
[11]钱建平.黔西北威宁—水城铅锌矿带动力成矿作用研究[J].地质地球化学.2001年第29卷第3期
[12]朱德彬、胡从亮、王忠福、陈冲、沈大兴.黔西北水城—艾家坪地区化探异常及铅锌矿找矿前景分析[J]贵州地质.2007年24卷第3期(总第92期)
[13]顾尚义.黔西北铅锌矿稀土元素组成特征—兼论黔西北地区铅锌矿成矿与峨眉山玄武岩的关系[J].贵州地质.2006年23卷第4期(总第89期)
[14]郑传仑.黔西北铅锌矿区的控矿构造研究[J].矿产与地质.1992年第3期第6卷总第29期
[15]刘幼平、杭家华、张伦尉、曾道国.黔西北铅锌矿集区成矿条件及找矿潜力探讨[J].矿产与地质.2004年第6期第18卷总第106期
[16]王林江.黔西北铅锌矿床的地质地球化学特征[J].桂林冶金地质学院学报.第14卷第2期1994年4月
[17]毛德明.黔西北铅锌矿床REE特征及其意义[J].贵州地质.2001年18卷第1期(总第66期)
[18]顾尚义.黔西北地区铅锌矿硫同位素特征研究[J].贵州工业大学学报(自然科学版).第36卷第1期2007年2月
[19]金中国、张伦尉、叶静.黔西北地区铅锌矿床成矿物质来源探讨[J].地质与勘探.第43卷第6期2007年11月
[20]刘幼平.黔西北地区铅锌矿成矿规律及找矿模式初探[J].贵州地质.2002年19卷第3期(总第72期)
[21]余未来、范良伍.黔西北地区典型铅锌矿床地质特征分析及找矿思路[J].矿物学报.第27卷第3／4期2007年12月
[22]李文博、黄智龙、陈进、韩润生、张振亮、许成.会泽超大型铅锌矿床成矿时代研究[J].矿物学报.第24卷第2期2004年6月
[23]叶天竺、孙文珂等.战略性矿产远景调查综合研究培训班专家讲义.(中国地质调查 局2006)
[24]黄智龙、陈进、韩润生等.云南会泽超大型铅锌矿床地球化学及成因—兼论峨眉山玄武岩与铅锌成矿的关系[M].北京：地质出版社,2004
[25]李发源、顾雪祥、付绍洪、章明.MVT铅锌矿床定年方法评述[J].矿物学报.第24卷第2期2004年6月
[26]王东、杨德传、邓克勇、刘仕辉.贵州威宁耿家寨(钒)铅锌矿地质特征及找矿潜力分析[J].科园月刊.第60期2007年3月
[27]王东、杨德传、曺运祥、邓克勇.贵州省小赛-耿家屯地区铅锌矿控矿因素及找矿方向[J].科园月刊.第87期2008年5月
[28]Lesley Wyborn. at al. Using GIS for mineral potentialevaluation in areas with few known mineraloccurrences. Second National forum on GIS in the Geosciences, 1995,29-31.
[29]Cox D P, Singer D A. Mineral deposit models. United States Geological Survey Bulletin,1986.
[30]Hodgson C J and Clark A H. Giant Ore Deposits. Queen' s University, Kingston,1995.
[31]Xie Xuejing and Cheng Hangxin. The suitability of floodplain sediment as global sampling medium:evidence from China. J. Geochem. Explor,1997,58:51-62.
[32]DeVerle P. Harris, Frederik P. Agterberg. The Appraisal of Mineral Resources. Economic Geology, Seventy - Fifth Anniversary. Volume(1905 1980).1981:897-938.
[33]Barton P B and others. Recommendations for assess m ents of undiscovered mineral resources. U. S. Geological Survey Open File ort 1995, (82):139.
[34]Bliss J D, M enzie W D. Spatial m ineral deposit m odels and the prediction of undiscovered mineral deposits. Mineral deposit modeling Geological Association of Canada Special Paper,1983, (40):693
[35]Lesley Wyborn, at al. Using GIS for mineral potential evaluation in areas with few known mineral occurrences. Second National forum on GIS in the Geosciences,1995,29～31.
[2]贵州省地质矿产局.水城幅区域地质调查报告.1978.
[3]贵州省地质局.威宁幅区域地质调查报告.1982.
[4]刘家铎、张成江等.扬子地台西南缘成矿规律及找矿方向[M].北京：地质出版社,2004
[5]四川、云南、贵州省地质局.川滇黔铅锌成矿区成矿远景区划—川滇黔铅锌成矿区成矿规律及找矿预测科研报告.[R]1983
[6]王华云、梁福谅、曾鼎权等.贵州铅锌矿地质[M].贵州：贵州科技出版社,1996
[7]贵州省地质矿产局.贵州省区域地质志[M].北京：地质出版社,1987
[8]毛德明、何家骏、廖朝贵.天桥铅锌矿床的沉积改造成矿特征[J]地质地球化学.2001年第29卷第1期
[9]张国平、刘丛强、杨元根、吴攀.碳酸盐岩地区铅锌矿山水系中铅锌铜的迁移及其硫同位素示踪[J].矿物学报.2002年9月第22卷第3期
[10]张启厚、毛健全、顾尚义.水城赫章铅锌矿成矿的金属物源研究[J].贵州工业大学学报.第27卷第6期1998年12月
[11]钱建平.黔西北威宁—水城铅锌矿带动力成矿作用研究[J].地质地球化学.2001年第29卷第3期
[12]朱德彬、胡从亮、王忠福、陈冲、沈大兴.黔西北水城—艾家坪地区化探异常及铅锌矿找矿前景分析[J]贵州地质.2007年24卷第3期(总第92期)
[13]顾尚义.黔西北铅锌矿稀土元素组成特征—兼论黔西北地区铅锌矿成矿与峨眉山玄武岩的关系[J].贵州地质.2006年23卷第4期(总第89期)
[14]郑传仑.黔西北铅锌矿区的控矿构造研究[J].矿产与地质.1992年第3期第6卷总第29期
[15]刘幼平、杭家华、张伦尉、曾道国.黔西北铅锌矿集区成矿条件及找矿潜力探讨[J].矿产与地质.2004年第6期第18卷总第106期
[16]王林江.黔西北铅锌矿床的地质地球化学特征[J].桂林冶金地质学院学报.第14卷第2期1994年4月
[17]毛德明.黔西北铅锌矿床REE特征及其意义[J].贵州地质.2001年18卷第1期(总第66期)
[18]顾尚义.黔西北地区铅锌矿硫同位素特征研究[J].贵州工业大学学报(自然科学版).第36卷第1期2007年2月
[19]金中国、张伦尉、叶静.黔西北地区铅锌矿床成矿物质来源探讨[J].地质与勘探.第43卷第6期2007年11月
[20]刘幼平.黔西北地区铅锌矿成矿规律及找矿模式初探[J].贵州地质.2002年19卷第3期(总第72期)
[21]余未来、范良伍.黔西北地区典型铅锌矿床地质特征分析及找矿思路[J].矿物学报.第27卷第3／4期2007年12月
[22]李文博、黄智龙、陈进、韩润生、张振亮、许成.会泽超大型铅锌矿床成矿时代研究[J].矿物学报.第24卷第2期2004年6月
[23]叶天竺、孙文珂等.战略性矿产远景调查综合研究培训班专家讲义.(中国地质调查 局2006)
[24]黄智龙、陈进、韩润生等.云南会泽超大型铅锌矿床地球化学及成因—兼论峨眉山玄武岩与铅锌成矿的关系[M].北京：地质出版社,2004
[25]李发源、顾雪祥、付绍洪、章明.MVT铅锌矿床定年方法评述[J].矿物学报.第24卷第2期2004年6月
[26]王东、杨德传、邓克勇、刘仕辉.贵州威宁耿家寨(钒)铅锌矿地质特征及找矿潜力分析[J].科园月刊.第60期2007年3月
[27]王东、杨德传、曺运祥、邓克勇.贵州省小赛-耿家屯地区铅锌矿控矿因素及找矿方向[J].科园月刊.第87期2008年5月
[28]Lesley Wyborn. at al. Using GIS for mineral potentialevaluation in areas with few known mineraloccurrences. Second National forum on GIS in the Geosciences, 1995,29-31.
[29]Cox D P, Singer D A. Mineral deposit models. United States Geological Survey Bulletin,1986.
[30]Hodgson C J and Clark A H. Giant Ore Deposits. Queen' s University, Kingston,1995.
[31]Xie Xuejing and Cheng Hangxin. The suitability of floodplain sediment as global sampling medium:evidence from China. J. Geochem. Explor,1997,58:51-62.
[32]DeVerle P. Harris, Frederik P. Agterberg. The Appraisal of Mineral Resources. Economic Geology, Seventy - Fifth Anniversary. Volume(1905 1980).1981:897-938.
[33]Barton P B and others. Recommendations for assess m ents of undiscovered mineral resources. U. S. Geological Survey Open File ort 1995, (82):139.
[34]Bliss J D, M enzie W D. Spatial m ineral deposit m odels and the prediction of undiscovered mineral deposits. Mineral deposit modeling Geological Association of Canada Special Paper,1983, (40):693
[35]Lesley Wyborn, at al. Using GIS for mineral potential evaluation in areas with few known mineral occurrences. Second National forum on GIS in the Geosciences,1995,29～31.