蚀变-流体地质填图研究现状及方法探讨:兼论九瑞矿集区海西期喷流沉积流体系统
|
摘要
蚀变-流体地质填图是对区域流体进行地质调查研究,了解热液流体系统和指导矿产勘查的一种工作方法,为在重要矿集区开展深部、边部找矿提供了新思路。本文结合前人的研究成果,探讨了蚀变-流体地质填图的含义、理论依据、国内外研究现状、填图的要素、工作方法等,并将填图单元划分为流体系统-流体子系统-流体单元三级等级体系。九瑞矿集区是我国重要的铜金铅锌矿集区,根据蚀变-流体地质填图方法,对九瑞矿集区开展了系统的野外观测与综合研究。结果显示,九瑞矿集区存在海西期喷流沉积流体系统、燕山期岩浆流体系统和燕山期中低温热流体系统,详细阐述了海西期喷流沉积系统的特征、空间分布等情况。
Alteration-fluid geological mapping is an investigation of the regional fluid geology,and also is a way to understand the hydrothermal fluid system and guide the mineral exploration,which provide a new thinking for deeper and outer prospecting in important ore concentration area.Based on the previous studies,this paper discusses the meaning,theory,current research,mapping factors,and technique request of alteration-fluid geological mapping.And establish 3-grade mapping unit system,i.e.,fluid system,fluid subsystem,and fluid unit.Jiujiang-Ruichang is an very important lead,zinc,copper,gold ore concentration area in China.According to alteration-fluid geological mapping,it carries out field investigation and comprehensive study in Jiujiang-Ruichang.The study results show that,there three fluid systems in Jiujiang-Ruichang,i.e.,Hercynian exhalative-sedimentary fluid system,Yanshanian magmatic fluid and Yanshanian low temperature termal fluid system.It describes the characteristics and spatial distribution of Hercynian exhalative-sedimentary fluid system.
Alteration-fluid geological mapping is an investigation of the regional fluid geology,and also is a way to understand the hydrothermal fluid system and guide the mineral exploration,which provide a new thinking for deeper and outer prospecting in important ore concentration area.Based on the previous studies,this paper discusses the meaning,theory,current research,mapping factors,and technique request of alteration-fluid geological mapping.And establish 3-grade mapping unit system,i.e.,fluid system,fluid subsystem,and fluid unit.Jiujiang-Ruichang is an very important lead,zinc,copper,gold ore concentration area in China.According to alteration-fluid geological mapping,it carries out field investigation and comprehensive study in Jiujiang-Ruichang.The study results show that,there three fluid systems in Jiujiang-Ruichang,i.e.,Hercynian exhalative-sedimentary fluid system,Yanshanian magmatic fluid and Yanshanian low temperature termal fluid system.It describes the characteristics and spatial distribution of Hercynian exhalative-sedimentary fluid system.
引文
[1]翟裕生.地史中成矿演化的趋势和阶段性[J].地学前缘,1997,4(3-4):197-202.
[2]马东升.地壳中流体的大规模流动系统及其成矿意义[J].高校地质学报,1998,4(3):250-260.
[3]Crosta A,Sabine C,Taranik JV.Hydrothermal alteration mapping at Bodie,California,using AVIRIS hyperspectral data[J].Remote Secsing of Environment,1998,65(3):309-319.
[4]Thompson AJB,Hauff PL,Robitaille JA.Alteration mapping in exploration:application of short wave infrared(SWIR)spectroscopy[J].SEG Newsletter,1999,39(1):16-27.
[5]Tapia CH,Crosta AP,et al.Hydrothermal alteration mapping at the Quellaveco porphyry copper deposit,southern Peru:implications for regional exploration using remote sensing[C]//Proceedings of the international conference on applied geologic remote sensing,2000.
[6]董方浏,莫宣学,王勇,等.云南省巍山-永平矿集区成矿流体地质填图试验的重要进展[J].地学前缘,2001,8(3):52.
[7]邓晋福,戴圣潜,赵海玲,等.铜陵Cu-Au(Ag)成矿区岩浆-流体-成矿系统和亚系统的识别[J].矿床地质,2002,21(4):317-322.
[8]王勇,莫宣学,董方浏,等.云南巍山-永平矿集区流体地质填图的理论与实践[J].中国地质,2003,30(1):73-83.
[9]蒙义峰,侯增谦,杨竹森,等.安徽铜陵地区蚀变-流体填图方法的探讨[J].地学前缘,2003,10(1):105-110.
[10]蒙义峰,侯增谦,杨竹森,等.铜陵矿集区蚀变-流体填图与成矿流体系统[J].矿产地质,2004,23(3):261-270.
[11]贾丽琼,徐文艺,杨丹,等.江西九瑞地区宝山斑岩型铜多金属矿床锆石U-Pb和辉钼矿Re-Os年龄及其地质意义[J].矿床地质,2015,34(1):63-80.
[12]常印佛,刘湘培,吴言昌.长江中下游铜铁成矿带[M].北京:地质出版社,1991:71-76.
[13]翟裕生,姚书振,林新多.长江中下游地区铁铜矿床[M].北京:地质出版社,1992:12-35.
[14]李伟源.欧洲共同体国家地壳流体研究的概况和进展[J].地学前缘,1996,3(3-4):313-323.
[15]Wyllie PJ.Petrology:Materials sciences of the universe[C]//The National Symp.At the Ann.,Con.,G S,India,Veranas.Souvenir Publication,2000:1-6.
[16]贾跃明.流体成矿系统于成矿作用研究[J].地学前缘,1996,3(3-4):253-258.
[17]李兆麟,杨荣勇,孙晓明,等.地质作用中的流体形成演化及成矿作用[J].地学前缘,1996,3(3-4):237-244.
[18]李院生,卢焕章,陈晓枫,等.流体作用在地球动力学演化过程中的意义[J].地球科学进展,1997,12(2):138-143.
[19]迟国祥,薛春纪.成矿流体动力学的原理、研究方法及应用[J].地学前缘,2011,18(5):1-18.
[20]翟裕生.论成矿系统[J].地学前缘,1999,6(1):13-27.
[21]Miyataki S and Lee K.Mapping alteration minerals in northern Cuprite and Goldfield,Nevada,with JERS-1 OPS data[C]//Proceedings of the thematic conference on geologic remote sensing,1997:473-484.
[22]Miyatake S,Sanga T,Hayashi T,et al.Regional alteration mapping with JERS-1 OPS data,La Rioja and San Juan Province,Argentine Repulic[C]//Proceedings of the international conference on applied geologic remote sensing,2000;385-394.
[23]Wendell P and Nusbaum R.Hydrothermal alteration mapping and ground trothing using hypspectral data,Virginia City,Nevada[C]//Proceedings of the fourteenth international conference on applied geologic remote sensing,Las Vegas,NV,United States,2000;200-205.
[24]Yamaguchi Y and Naito C.Spectral indices for lithologic discrimination and mapping by using the ASTER SWIR bands[J].International Journal of Remote Sensing,2003,24(22):4311-4323.
[25]Rowan LC and Mars JC.Lithologic mapping in the Mountain Pass,California area using Advanced Spaceborne Thermal Emission and Reflection Radiometer(ASTER)data[J].Remote Sensing of Environment,2003,84(3):350-366.
[26]Ninomiya Y.Lithologic mapping with multispectral ASTER TIR and SWIR data[J].Proceedings of SPIE,2004,5234:180-190.
[27]Tommaso ID and Rubinstein N.Hydrothermal alteration mapping using ASTER data in the Infiernillo porphyry deposit,Argentina[J].Ore Geology Reviews,2007,32(1-2):275-290.
[28]Farrand WH.Mapping alteration mineralogy in the Tushar Mountains and Marysvale mining district,Utah using AVIRIS data[C]//Proceedings of the fourteenth international conference on applied geologic remote sensing.Las Vegas,NV,United States,2000:62-69.
[29]Verdel CS,Knepper DJ,Livo KE,et al.Mapping minerals at the Copper Flat porphyry,New Mexico,using AVIRIS data[C]//JPL Publication.California Institute of Technology,Jet Propulsion Laboratory.Pasadena,CA,United States,2001:427-433.
[30]Guinnness EA,Arvidson RE,Jolliff BL,et al.Mapping alteration minerals exposed on the summit of Mauna Kea volcano using ACIRIS data:implications for mapping Mars mineralogy[C]//Abstracts of papers submitted to the lunar and planetary science Conference.abstr.no.2001:1659.
[31]Merry N and Pontual S.Rapid alteration mapping using field portable infrared spectrometers[C]//Publication Series Australasian Institute of Mining and Metallurgy,4-99.1999:693-698.
[32]Forster CB and Evans JP.Impact of a permeable thrust fault on thermal and hydrologic regimes:Regional scale numerical modeling result[J].Geophysical Research Letters,1991,18:979-982.
[33]Huston DL,Brauhart CW,Wellman P,et al.Gamma ray spectrometric and oxygen isotope mapping of regional alteration halos in massive sulphide districts:an example from Panorama,central Pilbara Craton:PartⅠ,Remote alteration mapping by gamma ray spectrometry;PartⅡ,Alteration mapping by oxygen isotopes[J].AGSO Research Newsletter,1998,29:14-16.
[34]国家辉.滩间山金龙沟金矿区找矿矿物学填图应用效果[J].贵金属地质,1998,7(4):258-268.
[35]任英忱,杜长学.找矿矿物学在山东招远-掖县地区金矿深部预测中的应用[J].矿物岩石地球化学通讯,1992,1:17-19;
[36]吕古贤,邓军,郭涛,等.玲珑-焦家式金矿构造变形岩相形迹大比例尺填图与构造成矿研究[J].地球学报,1998,19(2):177-186.
[37]郭涛,吕古贤.阜山金矿区构造变形岩相填图与成矿流体构造物理化学特征研究[J].地质找矿论丛,1999,14(3):50-56.
[38]修连存,郑志忠,俞正奎,等.近红外光谱分析技术在蚀变矿物鉴定中的应用[J].地质学报,2007,81(11):1584-1590.
[39]修连存,郑志忠,俞正奎,等.近红外光谱仪测定岩石中蚀变矿物方法研究[J].岩矿测试,2009,28(6):519-523.
[40]方维萱,杨新雨,柳玉龙,等.岩相学填图技术在云南东川白锡腊铁铜矿段深部应用试验与找矿预测[J].矿物学报,2012,32(1):101-114.
[41]石得凤,张术根,韩世礼.矿物学填图在福建丁家山铅锌矿成因研究中的应用[J].岩石矿物学杂志,2012,31(2):243-251.
[42]魏爱英,薛传东,洪托,等.滇东北毛坪铅锌矿床的蚀变-矿化分带模式——蚀变-岩相填图证据[J].岩石矿物学杂志,2012,31(5):723-735.
[43]要梅娟,申俊峰,李胜荣,等.石英流体包裹体的岩相学和热爆参数填图在前河金矿中的应用[J].地质与勘探,2008,44(6):56-61.
[44]邓晋福,莫宣学,赵海玲,等.中国东部燕山期岩石圈-软流圈系统大灾变与成矿环境[J].矿床地质,1999,18(4):309-315.
[45]季绍新,王文斌,邢文臣.赣西北铜矿[M].北京:地质出版社,1990:1-167.
[46]Mao J W,Wang Y T,Lehmann B,et al.Molybdenite Re-Os and albite 40 Ar/39 Ar dating of Cu-Au-Mo and magnetite porphyry systems in the Yangtze River valley nd metallogenic implications[J].Ore Geology Reviews,2006,29:307-324.
[47]李进文,李旭辉,裴荣富,等.江西武山铜矿南矿带辉钼矿Re-Os同位素年龄及其地质意义[J].地质学报,2007,81(6):801-806.
[48]蒋少涌,李亮,朱碧,等.江西武山铜矿区花岗闪长斑岩的地球化学和Sr-Nd-Hf同位素组成及成因探讨[J].岩石学报,2008,24(8):1679-1690.
[49]蒋少涌,孙岩,孙明志,等.长江中下游成矿带九瑞矿集区叠合断裂系统和叠加成矿作用[J].岩石学报,2010,26(9):2751-2761.
[50]陈志洪,邢光福,郭坤一,等.长江中下游成矿带九瑞矿集区(北部)含矿岩体的锆石U-Pb定年及其地质意义[J].地质学报,2011,85(7):1146-1158.
[51]文春华,徐文艺,钟宏,等.九瑞矿集区城门山斑岩型钼铜矿床流体包裹体研究[J].地质学报,2012,86(10):1604-1620.
[52]贾丽琼,徐文艺,杨丹,等.江西九瑞地区东雷湾矽卡岩型铜多金属矿床流体包裹体特征及稳定同位素地球化学研究[J].岩石矿物学杂志,2015,34(2):184-204.
[53]贾丽琼,杨丹,徐文艺,等.江西九瑞地区东雷湾矽卡岩型铜多金属矿床锆石U-Pb和辉钼矿Re-Os年龄及其地质意义[J].地球学报,2015,36(2):177-186.
[54]崔彬,李忠文,等.江西九瑞地区铜金成矿系列[M].武汉:中国地质大学出版社,1992:130.
[55]王文斌,李文达,董平,等.论长江中下游地区含铜黄铁矿型矿床成因[J].火山地质与矿床,1994,15(2):25-34.
[56]翟裕生,邓军,宋鸿林,等.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.
[57]Gu LX,Zaw Kin,Hu W X,et al.Distinctive features of Late Palaeozioc massive sulphide deposits in South China[J].Ore Geology Review,2007,31(1-4):107-138.
[58]殷鸿福,吴顺宝,杜远生,等.华南是特提斯多岛洋体系的一部分[J].地球科学,1999,24(1):1-12.
[59]方维萱,胡瑞忠,苏文超,等.扬子地块南缘及邻区大陆动力成矿系统、成矿系列特征与找矿方向[J].矿物学报,2001,21(4):561-570.
[60]杨竹森,侯增谦,蒙义峰,等.安徽铜陵矿集区海西期喷流沉积流体系统时空结构[J].矿床地质,2004,23(3):281-297.
[2]马东升.地壳中流体的大规模流动系统及其成矿意义[J].高校地质学报,1998,4(3):250-260.
[3]Crosta A,Sabine C,Taranik JV.Hydrothermal alteration mapping at Bodie,California,using AVIRIS hyperspectral data[J].Remote Secsing of Environment,1998,65(3):309-319.
[4]Thompson AJB,Hauff PL,Robitaille JA.Alteration mapping in exploration:application of short wave infrared(SWIR)spectroscopy[J].SEG Newsletter,1999,39(1):16-27.
[5]Tapia CH,Crosta AP,et al.Hydrothermal alteration mapping at the Quellaveco porphyry copper deposit,southern Peru:implications for regional exploration using remote sensing[C]//Proceedings of the international conference on applied geologic remote sensing,2000.
[6]董方浏,莫宣学,王勇,等.云南省巍山-永平矿集区成矿流体地质填图试验的重要进展[J].地学前缘,2001,8(3):52.
[7]邓晋福,戴圣潜,赵海玲,等.铜陵Cu-Au(Ag)成矿区岩浆-流体-成矿系统和亚系统的识别[J].矿床地质,2002,21(4):317-322.
[8]王勇,莫宣学,董方浏,等.云南巍山-永平矿集区流体地质填图的理论与实践[J].中国地质,2003,30(1):73-83.
[9]蒙义峰,侯增谦,杨竹森,等.安徽铜陵地区蚀变-流体填图方法的探讨[J].地学前缘,2003,10(1):105-110.
[10]蒙义峰,侯增谦,杨竹森,等.铜陵矿集区蚀变-流体填图与成矿流体系统[J].矿产地质,2004,23(3):261-270.
[11]贾丽琼,徐文艺,杨丹,等.江西九瑞地区宝山斑岩型铜多金属矿床锆石U-Pb和辉钼矿Re-Os年龄及其地质意义[J].矿床地质,2015,34(1):63-80.
[12]常印佛,刘湘培,吴言昌.长江中下游铜铁成矿带[M].北京:地质出版社,1991:71-76.
[13]翟裕生,姚书振,林新多.长江中下游地区铁铜矿床[M].北京:地质出版社,1992:12-35.
[14]李伟源.欧洲共同体国家地壳流体研究的概况和进展[J].地学前缘,1996,3(3-4):313-323.
[15]Wyllie PJ.Petrology:Materials sciences of the universe[C]//The National Symp.At the Ann.,Con.,G S,India,Veranas.Souvenir Publication,2000:1-6.
[16]贾跃明.流体成矿系统于成矿作用研究[J].地学前缘,1996,3(3-4):253-258.
[17]李兆麟,杨荣勇,孙晓明,等.地质作用中的流体形成演化及成矿作用[J].地学前缘,1996,3(3-4):237-244.
[18]李院生,卢焕章,陈晓枫,等.流体作用在地球动力学演化过程中的意义[J].地球科学进展,1997,12(2):138-143.
[19]迟国祥,薛春纪.成矿流体动力学的原理、研究方法及应用[J].地学前缘,2011,18(5):1-18.
[20]翟裕生.论成矿系统[J].地学前缘,1999,6(1):13-27.
[21]Miyataki S and Lee K.Mapping alteration minerals in northern Cuprite and Goldfield,Nevada,with JERS-1 OPS data[C]//Proceedings of the thematic conference on geologic remote sensing,1997:473-484.
[22]Miyatake S,Sanga T,Hayashi T,et al.Regional alteration mapping with JERS-1 OPS data,La Rioja and San Juan Province,Argentine Repulic[C]//Proceedings of the international conference on applied geologic remote sensing,2000;385-394.
[23]Wendell P and Nusbaum R.Hydrothermal alteration mapping and ground trothing using hypspectral data,Virginia City,Nevada[C]//Proceedings of the fourteenth international conference on applied geologic remote sensing,Las Vegas,NV,United States,2000;200-205.
[24]Yamaguchi Y and Naito C.Spectral indices for lithologic discrimination and mapping by using the ASTER SWIR bands[J].International Journal of Remote Sensing,2003,24(22):4311-4323.
[25]Rowan LC and Mars JC.Lithologic mapping in the Mountain Pass,California area using Advanced Spaceborne Thermal Emission and Reflection Radiometer(ASTER)data[J].Remote Sensing of Environment,2003,84(3):350-366.
[26]Ninomiya Y.Lithologic mapping with multispectral ASTER TIR and SWIR data[J].Proceedings of SPIE,2004,5234:180-190.
[27]Tommaso ID and Rubinstein N.Hydrothermal alteration mapping using ASTER data in the Infiernillo porphyry deposit,Argentina[J].Ore Geology Reviews,2007,32(1-2):275-290.
[28]Farrand WH.Mapping alteration mineralogy in the Tushar Mountains and Marysvale mining district,Utah using AVIRIS data[C]//Proceedings of the fourteenth international conference on applied geologic remote sensing.Las Vegas,NV,United States,2000:62-69.
[29]Verdel CS,Knepper DJ,Livo KE,et al.Mapping minerals at the Copper Flat porphyry,New Mexico,using AVIRIS data[C]//JPL Publication.California Institute of Technology,Jet Propulsion Laboratory.Pasadena,CA,United States,2001:427-433.
[30]Guinnness EA,Arvidson RE,Jolliff BL,et al.Mapping alteration minerals exposed on the summit of Mauna Kea volcano using ACIRIS data:implications for mapping Mars mineralogy[C]//Abstracts of papers submitted to the lunar and planetary science Conference.abstr.no.2001:1659.
[31]Merry N and Pontual S.Rapid alteration mapping using field portable infrared spectrometers[C]//Publication Series Australasian Institute of Mining and Metallurgy,4-99.1999:693-698.
[32]Forster CB and Evans JP.Impact of a permeable thrust fault on thermal and hydrologic regimes:Regional scale numerical modeling result[J].Geophysical Research Letters,1991,18:979-982.
[33]Huston DL,Brauhart CW,Wellman P,et al.Gamma ray spectrometric and oxygen isotope mapping of regional alteration halos in massive sulphide districts:an example from Panorama,central Pilbara Craton:PartⅠ,Remote alteration mapping by gamma ray spectrometry;PartⅡ,Alteration mapping by oxygen isotopes[J].AGSO Research Newsletter,1998,29:14-16.
[34]国家辉.滩间山金龙沟金矿区找矿矿物学填图应用效果[J].贵金属地质,1998,7(4):258-268.
[35]任英忱,杜长学.找矿矿物学在山东招远-掖县地区金矿深部预测中的应用[J].矿物岩石地球化学通讯,1992,1:17-19;
[36]吕古贤,邓军,郭涛,等.玲珑-焦家式金矿构造变形岩相形迹大比例尺填图与构造成矿研究[J].地球学报,1998,19(2):177-186.
[37]郭涛,吕古贤.阜山金矿区构造变形岩相填图与成矿流体构造物理化学特征研究[J].地质找矿论丛,1999,14(3):50-56.
[38]修连存,郑志忠,俞正奎,等.近红外光谱分析技术在蚀变矿物鉴定中的应用[J].地质学报,2007,81(11):1584-1590.
[39]修连存,郑志忠,俞正奎,等.近红外光谱仪测定岩石中蚀变矿物方法研究[J].岩矿测试,2009,28(6):519-523.
[40]方维萱,杨新雨,柳玉龙,等.岩相学填图技术在云南东川白锡腊铁铜矿段深部应用试验与找矿预测[J].矿物学报,2012,32(1):101-114.
[41]石得凤,张术根,韩世礼.矿物学填图在福建丁家山铅锌矿成因研究中的应用[J].岩石矿物学杂志,2012,31(2):243-251.
[42]魏爱英,薛传东,洪托,等.滇东北毛坪铅锌矿床的蚀变-矿化分带模式——蚀变-岩相填图证据[J].岩石矿物学杂志,2012,31(5):723-735.
[43]要梅娟,申俊峰,李胜荣,等.石英流体包裹体的岩相学和热爆参数填图在前河金矿中的应用[J].地质与勘探,2008,44(6):56-61.
[44]邓晋福,莫宣学,赵海玲,等.中国东部燕山期岩石圈-软流圈系统大灾变与成矿环境[J].矿床地质,1999,18(4):309-315.
[45]季绍新,王文斌,邢文臣.赣西北铜矿[M].北京:地质出版社,1990:1-167.
[46]Mao J W,Wang Y T,Lehmann B,et al.Molybdenite Re-Os and albite 40 Ar/39 Ar dating of Cu-Au-Mo and magnetite porphyry systems in the Yangtze River valley nd metallogenic implications[J].Ore Geology Reviews,2006,29:307-324.
[47]李进文,李旭辉,裴荣富,等.江西武山铜矿南矿带辉钼矿Re-Os同位素年龄及其地质意义[J].地质学报,2007,81(6):801-806.
[48]蒋少涌,李亮,朱碧,等.江西武山铜矿区花岗闪长斑岩的地球化学和Sr-Nd-Hf同位素组成及成因探讨[J].岩石学报,2008,24(8):1679-1690.
[49]蒋少涌,孙岩,孙明志,等.长江中下游成矿带九瑞矿集区叠合断裂系统和叠加成矿作用[J].岩石学报,2010,26(9):2751-2761.
[50]陈志洪,邢光福,郭坤一,等.长江中下游成矿带九瑞矿集区(北部)含矿岩体的锆石U-Pb定年及其地质意义[J].地质学报,2011,85(7):1146-1158.
[51]文春华,徐文艺,钟宏,等.九瑞矿集区城门山斑岩型钼铜矿床流体包裹体研究[J].地质学报,2012,86(10):1604-1620.
[52]贾丽琼,徐文艺,杨丹,等.江西九瑞地区东雷湾矽卡岩型铜多金属矿床流体包裹体特征及稳定同位素地球化学研究[J].岩石矿物学杂志,2015,34(2):184-204.
[53]贾丽琼,杨丹,徐文艺,等.江西九瑞地区东雷湾矽卡岩型铜多金属矿床锆石U-Pb和辉钼矿Re-Os年龄及其地质意义[J].地球学报,2015,36(2):177-186.
[54]崔彬,李忠文,等.江西九瑞地区铜金成矿系列[M].武汉:中国地质大学出版社,1992:130.
[55]王文斌,李文达,董平,等.论长江中下游地区含铜黄铁矿型矿床成因[J].火山地质与矿床,1994,15(2):25-34.
[56]翟裕生,邓军,宋鸿林,等.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.
[57]Gu LX,Zaw Kin,Hu W X,et al.Distinctive features of Late Palaeozioc massive sulphide deposits in South China[J].Ore Geology Review,2007,31(1-4):107-138.
[58]殷鸿福,吴顺宝,杜远生,等.华南是特提斯多岛洋体系的一部分[J].地球科学,1999,24(1):1-12.
[59]方维萱,胡瑞忠,苏文超,等.扬子地块南缘及邻区大陆动力成矿系统、成矿系列特征与找矿方向[J].矿物学报,2001,21(4):561-570.
[60]杨竹森,侯增谦,蒙义峰,等.安徽铜陵矿集区海西期喷流沉积流体系统时空结构[J].矿床地质,2004,23(3):281-297.