安徽庐枞盆地井边铜(金)矿床成矿特征及控矿地质因素探讨
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摘要
井边矿床位于庐枞盆地中部,为中低温热液脉型铜(金)矿床。矿体沿断裂和构造破碎带呈陡倾脉状产出。矿石构造主要为细(网)脉状、晶洞(簇)状,次为角砾状;矿石结构为交代和结晶作用形成的各种结构。黄铁矿成分标型Co/Ni、Fe/(S+As)、S/Se等比值特征显示成矿热液主要为中低温岩浆热液。黄铜矿单矿物、巴家滩岩浆岩的稀土元素特征与盆地砖桥旋回火山-次火山岩的稀土元素特征总体类似,矿石稀土元素继承或保存了含矿岩浆岩的源区信息。结合区域地质年代学资料以及矿体和正长斑岩脉均产于与火山-次火山安山玢岩相同的构造体系中等现象,推测成矿热液可能来源于火山喷发之后的次火山-侵入岩的岩浆期后热液。断裂构造是控制井边矿床的重要因素。本区构造与中国东部中生代新华夏体系一致,在区域南北左行对扭力场中,发生了强烈的断裂构造活动。"应变菱形解析"显示:第一序次的NE向、NW向与第二序次NW向、EW向、NNW向断裂共同控制矿床的产出。井边矿化区的分布呈现出从虎栈—张榜总体沿NE40°成带、NW310°成行的特点。
The Jingbian ore deposit is a medium-low temperature hydrothermal type Cu (Au) deposit lying in central Luzong basin. The ores are mainly in the veinlet,stockwork,crystal aggregate forms with subordinate brecciated structure. The textures of the ore are complex,resulting from metasomatism and crystallization. The ore bodies are commonly steeply-dipping veins,controlled by fault structure and tectonic shatter zone. The typomorphic values of Co/Ni,Fe/(S+As),and S/Se of pyrite show that the hydrothermal ore-forming solution mainly came from medium-low temperature magmatic hydrothermal fluids. The overall REE characteristics are similar to those of chalcopyrite from the Jingbian copper (gold) deposit,Bajiatan intrusive rock and volcanic rock and subvolcanic rocks of Zhuanqiao Formation. The REE characteristics of chalcopyrite inherited or retained source characteristics of ore-bearing magmatic rocks. In addition,regional geochronology and the phenomenon that the same tectonic system controls ore bodies and syenite porphyry veins indicate that the hydrothermal ore-forming solution probably came from magmatic hydrothermal solution of the intrusive rocks subsequent to volcanic rock and subvolcanic rocks. Fracture structure is an important factor controlling the Jingbian ore deposit,and the structure in this area is consistent with the Neo-cathaysian tectonic system of Mesozoic in eastern China. The fault structural activity is strong in Luzong area,controlled by regional NS-trending sinistral shear force field and rotational action. Using the means of "Analysis of Diamond in Stress Action" ,the authors reveal that the formation of the Jingbian ore deposit was controlled by the structures which consisted mainly of NE-and NW-striking faults and subordinately of NW-,EW-and NNW-trending faults. It is inferred that the mining areas of Zhangban and Huzhan in the ore deposit constitute a NE-trending metallogenic belt,and that the two ends and two sides of the belt are promising areas for ore exploration.
The Jingbian ore deposit is a medium-low temperature hydrothermal type Cu (Au) deposit lying in central Luzong basin. The ores are mainly in the veinlet,stockwork,crystal aggregate forms with subordinate brecciated structure. The textures of the ore are complex,resulting from metasomatism and crystallization. The ore bodies are commonly steeply-dipping veins,controlled by fault structure and tectonic shatter zone. The typomorphic values of Co/Ni,Fe/(S+As),and S/Se of pyrite show that the hydrothermal ore-forming solution mainly came from medium-low temperature magmatic hydrothermal fluids. The overall REE characteristics are similar to those of chalcopyrite from the Jingbian copper (gold) deposit,Bajiatan intrusive rock and volcanic rock and subvolcanic rocks of Zhuanqiao Formation. The REE characteristics of chalcopyrite inherited or retained source characteristics of ore-bearing magmatic rocks. In addition,regional geochronology and the phenomenon that the same tectonic system controls ore bodies and syenite porphyry veins indicate that the hydrothermal ore-forming solution probably came from magmatic hydrothermal solution of the intrusive rocks subsequent to volcanic rock and subvolcanic rocks. Fracture structure is an important factor controlling the Jingbian ore deposit,and the structure in this area is consistent with the Neo-cathaysian tectonic system of Mesozoic in eastern China. The fault structural activity is strong in Luzong area,controlled by regional NS-trending sinistral shear force field and rotational action. Using the means of "Analysis of Diamond in Stress Action" ,the authors reveal that the formation of the Jingbian ore deposit was controlled by the structures which consisted mainly of NE-and NW-striking faults and subordinately of NW-,EW-and NNW-trending faults. It is inferred that the mining areas of Zhangban and Huzhan in the ore deposit constitute a NE-trending metallogenic belt,and that the two ends and two sides of the belt are promising areas for ore exploration.
引文
[1]曾键年,等.2009.长江中下游重要矿集区成矿地球动力学背景及构造-成矿响应(庐枞盆地2008年度阶段性报告).中国地质大学(武汉)地调院.
[2]冶金部华东地质勘查局八一五队.1994.安徽枞阳虎栈铜矿普查报告.
[1]曾键年,等.2009.长江中下游重要矿集区成矿地球动力学背景及构造-成矿响应(庐枞盆地2008年度阶段性报告).中国地质大学(武汉)地调院.
[1]冶金部华东地质勘查局八一五队.1994.安徽枞阳虎栈铜矿普查报告.
[1]冶金部华东地质勘查局八一五队.1994.安徽枞阳虎栈铜矿普查报告.
[1]曾键年,等.2009.长江中下游重要矿集区成矿地球动力学背景及构造-成矿响应(庐枞盆地2008年度阶段性报告).中国地质大学(武汉)地调院.
[2]冶金部华东地质勘查局八一五队.1994.安徽枞阳虎栈铜矿普查报告.
[1]王思源.2008.构造解构.内部资料.
Bralia A,Sabatini Gand Troja F.1979.Arevaluation of the Co/Ni ra-tioin pyrite as geochemical tool in ore genesis problems[J].Minera-lium Deposita,14(3):353-374.
Cai YJ,Ma C Aand Jiang Y C.1999.The experi mental study onther-mal electricitty forming mechanismof pyritein Au deposit andits ex-plorating practice[J].Volcanology and Mineralresources,20(3):218-224(in Chinese).
Cao Y.2008.Studies on Mesozoic A-type granitoids and their rock xeno-lithsin Lujiang-Zongyang area,Anhui Province(master candidate pa-per)[D].Supervisor:Du YS.Beijing:China University of Geosciences(in Chinese).
Сммрнова C Kидр.1983.Применне типоморфных особснностей минсралов оценки рудолроявлсний Востчного Уэбскстана и орсдслсния уровня их зрозионного среэа,ВКН,Новые идеи в генетической минералогии[M].Москва:Наука.108-113(inRussia).
Chen G Y,Sun D S and Yin HA.1988.Genetiemineralo-gyandprogyand prospecting mineralogy[M].Chongqing:Chongqing PublishingHouse.880p(in Chinese).
Duan C.2009.Geological and geochemical characteristics and genesis ofLongqiaoiron deposit in Luzong Basin,Anhui,China(master candi-date paper)[D].Supervisor:Zhou T F.Hefei:Hefei university ofTechnology.5(in Chinese).
Fan Y,Zhou T F,Yuan F,Qian C C,Lu S Mand Cooke D.2008.LA-ICP-MS zircon U-Pb age of the A-type granites in the Lu-Zong(Lujiang-Zongyang)area andtheir geological significances[J].Acta Petrologica Sinica,24(8):1715-1724(in Chinese with Eng-lish abstract).
Новгородова М И идр.1986.Использование типоморфизма минералов и минералов и минеральных ассоциаций при минералогическо мкартировании полиформациои Ных месторождени,В обтипоморфизм минерфлов и минеральных ассоциаций[M].Москва:Наука.88-95(in Russia).
Li H M,Wang D H,Zhang C Qand Chen Y C.2009.Characteristicsof trace and rare earth elementsin minerals fromsome typical lead-zinc deposits of Shaanxi Province[J].Mineral Deposits,28(4):434-448(in Chinese with English abstract).
Liu H,Qiu J S H,Luo Q H,Xu X S,Ling WLand Wang D Z.2002.Petrogenesis of the Mesozoic potash-rich volcanic rocks in the Lu-zong basin Anhui Province:Geochemical constraints[J].Geochi mi-ca,31(2):129-140(in Chinese with English abstract).
Liu J.2005.Geology and geochemical characteristice and mineraliztionpotential esti mation of Bajiatan intrusion in Luzong volcanic basin,Anhui Province(master candidate paper)[D].Hefei:Hefei Univer-sity of Technology(in Chinese).
Liu J,Zhou T F,Fan Y,Wu M A,Lu S Mand Qian C C.2007.Rockgeochemistry and genesis of the Bajiatan intrusion in the Lujiang-Zongyang volcaninc basin,Anhui[J].Acta Petrologica Sinica,23(10):2615-2622(in Chinese with English abstract).
Luan S W.1987.Gold geology and direction of prospecting[M].Chengdu:Sichuan Science and Technology Publishing House.78-84(in Chinese).
Mao J Wand Wang Zh L.2004.Apreli minarystudyonti meli mits andgeody-namic setting of large-scale metallogeny in east China[J].Mineral De-posits,19(4):91-99(in Chinese with English abstract).
Nie FJ,translated.1976.The distributed of the REE and other traceelement in magnetite[A].Foreign mining geology[M].1993.Insti-tute of Geology and Mineral Resources.26(2):119-133.
Qing R Q,Liu Z P,Qian L P,Wang S and Zhou W Y.2001.Study ofmode of occurrence of golg in the Jianbing gold deposit,ZongyangCounty[J].J.Hefei University of Technology,24(4):523-528(in Chinese with English abstract).
Qin YJ,Zeng J N,Zeng Y,Ma Z D,Chen J Hand Jin X.2010.ZirconLA-ICP-MS U-Pb dating of ore-bearing pyroxene-trachyan-desite porphyry and its geological significance in Luohe-Nihe ironore field in Luzong basin,sourthern Anhui,China[J].GeologicalBulletinof China,29(6):851-862(in Chinese with English ab-stract).
Ren QJ,Wang D Z,Xu Z W,Dong S G,Pan L Q,Yang R Y,Fang C Qand Hu J A.1993.Formation and development of the Mesozoic Lu-jiang-Zongyang volcanic-Structural depression in Anhui Provinceand their relation to mineralization[J].Acta Geologica Sinica,62(2):121-136(in Chinese with English abstract).
Sun Y D,Yang R Y,Ren QJ and Liu X S.1994.Discussion on thecharacteristics and tectonic setting of the Mesozoic volcanic sequencesin Lujiang-Zongyang area[J].Acta Petrologica Sinica,10(1):94-103.(in Chinese with English abstract).
ShaoJ L.1988.Prospecting mineralogyof golddeposit[M].Wuhan:China U-niversity of Geosciences Publishing House.158p(in Chinese).
Taylor S Rand Mclennan S M.1985.The continental cruct:Its compo-sition and evolution[M].Londeon:Blackwell Scientific Pubications.312.
Wang D Z,Ren QJ,Qiu J S,Chen K R,Xu Z Wand Zen J H.1996.Characteritics of volvanic rocks in the shoshonite province,easternChina,and their metallogenesis[J].Acta Geologica Sinica,70:23-34(in Chinese with English abstract).
Wang Q,Zhao Z H,Xiong X L and Xu J F.2001.Melting of the un-derplated basaltic lower crust:Evidence fromthe Shaxi adakitic sodicquartz diorte-porphyrites,Anhui Province,China[J].Geochi mica,30(4):353-363(in Chinese with English abstract).
Wang Q,Derek A Wand Xu J F.2006.Petrogenesis of Cretaceousadakitic and shoshonitic igneous rocks in the Luzong area,AnhuiProvince(eastern China):I mplications for geodynamics and Cu-Aumineralization[J].Lithos,89(3-4):424-446.
Wang S Y.1990.Metallotectonic analysis for tin-multi metal depositsof strata-bound type[J].Earth Science,15(4):421-430(inChinese with English abstract).
Wang S Y.1993.Metallogenic tectonic analysis of eruptive-sedi menta-ry-transformed type silver-polymetallic deposit in Yindongzi,Shanxi Province[J].Geoscience,7(3):73-82(in Chinese withEnglish abstract).
Wang Z Tand Qin K Z.1991.The typer and metallogence mettings oflarge scale depositsin China andthe potential of metellogenic concen-trated area[J].Mineral Deposits,10(3):119-120(in Chinese withEnglish abstract).
Wu L R,Qi J Y,Wang T D,Zhang X Yand Xu YS.1982.Mesozoicvolcanic rocks in eastern part of China[J].Acta Geologica Sinica,(3):223-235(in Chinese with English abstract).
Wu MA,Hong MJ and Zhao WG.2007.Mineralizationregularity andexploration direction in Luzong area,Anhui[J].Resources Surveyand Envonmennt[J].28(4):269-278(in Chinese with Englishabstract).
Xu Z W,Ren QJ,Yang R Yand Wang S.1992.Distribution regulari-ties and metallogenic patterns of veinlike Cu(Au)-deposits in Lu-jiang-Zhongyang area[J].Geology and Prospecting,28(1):8-16(in Chinese with English abstract).
Yang X Y.2006.40Ar-39Ar dating and geological significance onthe Cu-bearing porpyrite of Shaxi fromsouthern Tan-Lu fault belt[J].J.mineral Petrol.,26(4):34-39(in Chinese with English abstract).
Yu X Y and Bai Z G.1981.Latitic series in Lujiang-Zongyang region[J].Geochi mica,10(1):57-65(in Chinese with Englishabstract).
Yuan F,Zhou T F,Fan Y,Lu S M,Qian C C,Zhang L J,Duan C andTang H M.2009.Source,evolution andtectonic setting of Mesozoicvolcanic rocks in Luzong basin,Anhui Province[J].Acta Petrologica Sinica,24(8):1691-1702(in Chinese with English abstract).
Zhan S Qand Li HC.1986.Causes of introductionto mineralogy(Vol.1and2)[M].Changchun:Jilin University Press(in Chinese).
Zhao Z Hand Tu G C.2003.Super-large depositsin china(Ⅱ)[M].Beijing:Science Press.235p(in Chinese).
Zhou T F,Fan Y,Yuan F,Lu S M,Shang S G,Cooke D,Meffre S andZhao G C.2008.Geochronology of volcanic rocks andits significanceof Luzong Basin,Anhui Provice[J].Science in China(Series D:Earth Sciences),18(32):1342-1353(in Chinese).
Zhou X W,Li S R,Lu Land Ling WB.2005.Reseach onthe compo-sition typomorphismof pyrite from Longkeng gold-siliver mineral-ization district in Wuyi,Zhejiang Province,China[J].Bulletin of Mi-neralogy,Petrology and Geochemistry,24(4):317-327(in Chi-nese with English abstract).
Zeng J N,Qin YJ,Guo K Y,Chen G Gand Zeng Y.2010.Zircon U-Pb dating of ore-bearing magmatic rocks and its constraint on theformation ti me of the ore deposits in Luzong Basin,Anhui Province[J].Acta Geologica Sinica,84(4):465-478(in Chinese with Eng-lish abstract).
蔡元吉,马承安,蒋永才.1999.金矿床黄铁矿热电性质形成机理实验研究及其找矿应用[J].火山地质与矿产,20(3):218-224.
曹毅.2008.安徽庐枞盆地中生代A型花岗岩类及其岩石包体研究(硕士论文)[D].导师:杜杨松.北京:中国地质大学.
陈光远,孙岱生,殷辉安.1988.成因矿物学与找矿矿物学[M].重庆:重庆出版社.880.
段超.2009.安徽庐枞盆地龙桥铁矿床地质地球化学特征和矿床成因研究(硕士论文)[D].导师:周涛发.合肥:合肥工业大学.5.
范裕,周涛发,袁峰,钱存超,陆三明,DAVID Cooke.2008.安徽庐江-枞阳地区A型花岗岩的LA-ICP-MS定年及其地质意义[J].岩石学报,24(8):1715-1724.
李厚民,王登红,张长青,陈毓川,李立兴.2009.陕西几类重要铅锌矿床的矿物微量元素和稀土元素特征[J].矿床地质,28(4):434-448.
刘洪,邱检生,罗清华,徐夕生,凌文黎,王德滋.2002.安徽庐枞中生代富钾火山岩成因的地球化学制约[J].地球化学,31(2):129-140.
刘珺.2005.安徽庐极火山岩盆地中巴家滩岩体的地质地球化学特征和成矿潜力评价(硕士论文)[D].导师:周涛发.合肥:合肥工业大学.
刘珺,周涛发,袁峰,范裕,吴明安,陆三明,钱存超.2007.安徽庐枞地区中巴家滩岩体的岩石地球化学特征及成因[J].岩石学报,23(10):2615-2622.
毛景文,王志良.2004.中国东部大规模成矿时限及其动力学背景的初步探讨[J].矿床地质,19(4):91-99.
聂凤军(译).1976.磁铁矿中稀土元素及其它痕量元素的分布[A].见:外国矿产地质[M].1993地质矿产研究所.26(2):119-133.
钱让清,刘中平,钱立平,王实,周文雅.2001.枞阳井边金矿金的赋存状态研究[J].合肥工业大学学报(自然科学版),24(4):253-258.
覃永军,曾键年,曾勇,马振东,陈津华,金希.2010.安徽庐枞盆地罗河-泥河铁矿田含矿辉石粗安玢岩的锆石LA-ICP-MSU-Pb定年及其地质意义[J].地质通报,29(6):851-862.
任启江,王德滋,徐兆文,董火根,潘龙泉,杨荣勇,方长泉,胡进安.1993.安徽庐枞火山-构造洼地的形成、演化及成矿[J].地质学报,62(2):121-136.
孙冶东,杨荣勇,任启江,刘孝善.1994.安徽庐枞中生代火山岩系的特征及其形成的构造背景[J].岩石学报,10(1):94-103.
邵洁涟.1988.金矿找矿矿物学[M].武汉:中国地质大学出版社.158.
王德滋,任启江,邱检生,陈克荣,徐兆文,曾家湖.1996.中国东部橄榄安粗岩省的火山岩特征及其成矿作用[J].地质学报,70:23-34.
王强,赵振华,熊小林,许继峰.2001.底侵玄武质下地壳的熔融:来自安徽沙溪adakite质富钠石英闪长份岩的证据[J].地球化学,30(4):353-363.
王思源.1990.芒场矿田锡多金属成矿构造解析[J].地球科学,15(4):421-430.
王思源.1993.陕西银硐子喷溢沉积改造型银多金属矿床成矿构造解析[J].现代地质,7(3):73-82.
王之田,秦克章.1991.中国大型铜矿类型、成矿环境与成矿集中区的潜力[J].矿床地质,10(3):119-120.
栾世伟.1987.金矿地质与找矿方向[M].成都:四川科学技术出版社.78-84.
吴利仁,齐进英,王听渡,张秀棋,徐永生.1982.中国东部中生代火山岩[J].地质学报,(3):223-235.
吴明安,侯明金,赵文广.2007.安徽省庐枞地区成矿规律及找矿方向[J].资源调查与环境,28(4):269-278.
徐兆文,任启江,杨荣勇,王实.1992.安徽庐枞地区脉状铜矿、铜金矿化分布规律和矿床模式[J].地质与勘探,28(1):8-16.
杨晓勇.2006.郯庐断裂带南段沙溪含铜斑岩体的40Ar-39A:年代学研究及意义[J].矿物岩石,26(4):34-39.
于学元,白正华.1981.庐枞盆地安粗岩系[J].地球化学,10(1):57-65.
袁峰,周涛发,范裕,陆三明,钱存超,张乐骏,段超,唐敏慧.2009.庐枞盆地中生代火山岩的起源、演化及形成背景[J].岩石学报,24(8):1691-1702.
斩是琴,李鸿超.1986.成因矿物学概论(上、下)[M].长春:吉林大学出版社.
赵振华,涂光炽.2003.中国超大型矿床(Ⅱ)[M].北京:科学出版社.325页.
周涛发,范裕,袁峰,陆三明,尚世贵,David Cooke,Sebastien Mef-fre,赵国春.2008.安徽庐枞(庐江-枞阳)盆地火山岩的年代学及其意义[J].中国科学(D辑:地球科学),18(32):1342-1353.
周学武,李胜荣,鲁力,林卫兵.2005.浙江弄坑金银矿区黄铁矿成分标型研究[J].矿物岩石地球化学通报,24(4):317-327.
曾键年,覃永军,郭坤一,陈国光,曾勇.2010.安徽庐枞盆地含矿岩浆岩锆石U-Pb年龄及其对成矿时限的约束[J].地质学报,84(4):465-478.
[2]冶金部华东地质勘查局八一五队.1994.安徽枞阳虎栈铜矿普查报告.
[1]曾键年,等.2009.长江中下游重要矿集区成矿地球动力学背景及构造-成矿响应(庐枞盆地2008年度阶段性报告).中国地质大学(武汉)地调院.
[1]冶金部华东地质勘查局八一五队.1994.安徽枞阳虎栈铜矿普查报告.
[1]冶金部华东地质勘查局八一五队.1994.安徽枞阳虎栈铜矿普查报告.
[1]曾键年,等.2009.长江中下游重要矿集区成矿地球动力学背景及构造-成矿响应(庐枞盆地2008年度阶段性报告).中国地质大学(武汉)地调院.
[2]冶金部华东地质勘查局八一五队.1994.安徽枞阳虎栈铜矿普查报告.
[1]王思源.2008.构造解构.内部资料.
Bralia A,Sabatini Gand Troja F.1979.Arevaluation of the Co/Ni ra-tioin pyrite as geochemical tool in ore genesis problems[J].Minera-lium Deposita,14(3):353-374.
Cai YJ,Ma C Aand Jiang Y C.1999.The experi mental study onther-mal electricitty forming mechanismof pyritein Au deposit andits ex-plorating practice[J].Volcanology and Mineralresources,20(3):218-224(in Chinese).
Cao Y.2008.Studies on Mesozoic A-type granitoids and their rock xeno-lithsin Lujiang-Zongyang area,Anhui Province(master candidate pa-per)[D].Supervisor:Du YS.Beijing:China University of Geosciences(in Chinese).
Сммрнова C Kидр.1983.Применне типоморфных особснностей минсралов оценки рудолроявлсний Востчного Уэбскстана и орсдслсния уровня их зрозионного среэа,ВКН,Новые идеи в генетической минералогии[M].Москва:Наука.108-113(inRussia).
Chen G Y,Sun D S and Yin HA.1988.Genetiemineralo-gyandprogyand prospecting mineralogy[M].Chongqing:Chongqing PublishingHouse.880p(in Chinese).
Duan C.2009.Geological and geochemical characteristics and genesis ofLongqiaoiron deposit in Luzong Basin,Anhui,China(master candi-date paper)[D].Supervisor:Zhou T F.Hefei:Hefei university ofTechnology.5(in Chinese).
Fan Y,Zhou T F,Yuan F,Qian C C,Lu S Mand Cooke D.2008.LA-ICP-MS zircon U-Pb age of the A-type granites in the Lu-Zong(Lujiang-Zongyang)area andtheir geological significances[J].Acta Petrologica Sinica,24(8):1715-1724(in Chinese with Eng-lish abstract).
Новгородова М И идр.1986.Использование типоморфизма минералов и минералов и минеральных ассоциаций при минералогическо мкартировании полиформациои Ных месторождени,В обтипоморфизм минерфлов и минеральных ассоциаций[M].Москва:Наука.88-95(in Russia).
Li H M,Wang D H,Zhang C Qand Chen Y C.2009.Characteristicsof trace and rare earth elementsin minerals fromsome typical lead-zinc deposits of Shaanxi Province[J].Mineral Deposits,28(4):434-448(in Chinese with English abstract).
Liu H,Qiu J S H,Luo Q H,Xu X S,Ling WLand Wang D Z.2002.Petrogenesis of the Mesozoic potash-rich volcanic rocks in the Lu-zong basin Anhui Province:Geochemical constraints[J].Geochi mi-ca,31(2):129-140(in Chinese with English abstract).
Liu J.2005.Geology and geochemical characteristice and mineraliztionpotential esti mation of Bajiatan intrusion in Luzong volcanic basin,Anhui Province(master candidate paper)[D].Hefei:Hefei Univer-sity of Technology(in Chinese).
Liu J,Zhou T F,Fan Y,Wu M A,Lu S Mand Qian C C.2007.Rockgeochemistry and genesis of the Bajiatan intrusion in the Lujiang-Zongyang volcaninc basin,Anhui[J].Acta Petrologica Sinica,23(10):2615-2622(in Chinese with English abstract).
Luan S W.1987.Gold geology and direction of prospecting[M].Chengdu:Sichuan Science and Technology Publishing House.78-84(in Chinese).
Mao J Wand Wang Zh L.2004.Apreli minarystudyonti meli mits andgeody-namic setting of large-scale metallogeny in east China[J].Mineral De-posits,19(4):91-99(in Chinese with English abstract).
Nie FJ,translated.1976.The distributed of the REE and other traceelement in magnetite[A].Foreign mining geology[M].1993.Insti-tute of Geology and Mineral Resources.26(2):119-133.
Qing R Q,Liu Z P,Qian L P,Wang S and Zhou W Y.2001.Study ofmode of occurrence of golg in the Jianbing gold deposit,ZongyangCounty[J].J.Hefei University of Technology,24(4):523-528(in Chinese with English abstract).
Qin YJ,Zeng J N,Zeng Y,Ma Z D,Chen J Hand Jin X.2010.ZirconLA-ICP-MS U-Pb dating of ore-bearing pyroxene-trachyan-desite porphyry and its geological significance in Luohe-Nihe ironore field in Luzong basin,sourthern Anhui,China[J].GeologicalBulletinof China,29(6):851-862(in Chinese with English ab-stract).
Ren QJ,Wang D Z,Xu Z W,Dong S G,Pan L Q,Yang R Y,Fang C Qand Hu J A.1993.Formation and development of the Mesozoic Lu-jiang-Zongyang volcanic-Structural depression in Anhui Provinceand their relation to mineralization[J].Acta Geologica Sinica,62(2):121-136(in Chinese with English abstract).
Sun Y D,Yang R Y,Ren QJ and Liu X S.1994.Discussion on thecharacteristics and tectonic setting of the Mesozoic volcanic sequencesin Lujiang-Zongyang area[J].Acta Petrologica Sinica,10(1):94-103.(in Chinese with English abstract).
ShaoJ L.1988.Prospecting mineralogyof golddeposit[M].Wuhan:China U-niversity of Geosciences Publishing House.158p(in Chinese).
Taylor S Rand Mclennan S M.1985.The continental cruct:Its compo-sition and evolution[M].Londeon:Blackwell Scientific Pubications.312.
Wang D Z,Ren QJ,Qiu J S,Chen K R,Xu Z Wand Zen J H.1996.Characteritics of volvanic rocks in the shoshonite province,easternChina,and their metallogenesis[J].Acta Geologica Sinica,70:23-34(in Chinese with English abstract).
Wang Q,Zhao Z H,Xiong X L and Xu J F.2001.Melting of the un-derplated basaltic lower crust:Evidence fromthe Shaxi adakitic sodicquartz diorte-porphyrites,Anhui Province,China[J].Geochi mica,30(4):353-363(in Chinese with English abstract).
Wang Q,Derek A Wand Xu J F.2006.Petrogenesis of Cretaceousadakitic and shoshonitic igneous rocks in the Luzong area,AnhuiProvince(eastern China):I mplications for geodynamics and Cu-Aumineralization[J].Lithos,89(3-4):424-446.
Wang S Y.1990.Metallotectonic analysis for tin-multi metal depositsof strata-bound type[J].Earth Science,15(4):421-430(inChinese with English abstract).
Wang S Y.1993.Metallogenic tectonic analysis of eruptive-sedi menta-ry-transformed type silver-polymetallic deposit in Yindongzi,Shanxi Province[J].Geoscience,7(3):73-82(in Chinese withEnglish abstract).
Wang Z Tand Qin K Z.1991.The typer and metallogence mettings oflarge scale depositsin China andthe potential of metellogenic concen-trated area[J].Mineral Deposits,10(3):119-120(in Chinese withEnglish abstract).
Wu L R,Qi J Y,Wang T D,Zhang X Yand Xu YS.1982.Mesozoicvolcanic rocks in eastern part of China[J].Acta Geologica Sinica,(3):223-235(in Chinese with English abstract).
Wu MA,Hong MJ and Zhao WG.2007.Mineralizationregularity andexploration direction in Luzong area,Anhui[J].Resources Surveyand Envonmennt[J].28(4):269-278(in Chinese with Englishabstract).
Xu Z W,Ren QJ,Yang R Yand Wang S.1992.Distribution regulari-ties and metallogenic patterns of veinlike Cu(Au)-deposits in Lu-jiang-Zhongyang area[J].Geology and Prospecting,28(1):8-16(in Chinese with English abstract).
Yang X Y.2006.40Ar-39Ar dating and geological significance onthe Cu-bearing porpyrite of Shaxi fromsouthern Tan-Lu fault belt[J].J.mineral Petrol.,26(4):34-39(in Chinese with English abstract).
Yu X Y and Bai Z G.1981.Latitic series in Lujiang-Zongyang region[J].Geochi mica,10(1):57-65(in Chinese with Englishabstract).
Yuan F,Zhou T F,Fan Y,Lu S M,Qian C C,Zhang L J,Duan C andTang H M.2009.Source,evolution andtectonic setting of Mesozoicvolcanic rocks in Luzong basin,Anhui Province[J].Acta Petrologica Sinica,24(8):1691-1702(in Chinese with English abstract).
Zhan S Qand Li HC.1986.Causes of introductionto mineralogy(Vol.1and2)[M].Changchun:Jilin University Press(in Chinese).
Zhao Z Hand Tu G C.2003.Super-large depositsin china(Ⅱ)[M].Beijing:Science Press.235p(in Chinese).
Zhou T F,Fan Y,Yuan F,Lu S M,Shang S G,Cooke D,Meffre S andZhao G C.2008.Geochronology of volcanic rocks andits significanceof Luzong Basin,Anhui Provice[J].Science in China(Series D:Earth Sciences),18(32):1342-1353(in Chinese).
Zhou X W,Li S R,Lu Land Ling WB.2005.Reseach onthe compo-sition typomorphismof pyrite from Longkeng gold-siliver mineral-ization district in Wuyi,Zhejiang Province,China[J].Bulletin of Mi-neralogy,Petrology and Geochemistry,24(4):317-327(in Chi-nese with English abstract).
Zeng J N,Qin YJ,Guo K Y,Chen G Gand Zeng Y.2010.Zircon U-Pb dating of ore-bearing magmatic rocks and its constraint on theformation ti me of the ore deposits in Luzong Basin,Anhui Province[J].Acta Geologica Sinica,84(4):465-478(in Chinese with Eng-lish abstract).
蔡元吉,马承安,蒋永才.1999.金矿床黄铁矿热电性质形成机理实验研究及其找矿应用[J].火山地质与矿产,20(3):218-224.
曹毅.2008.安徽庐枞盆地中生代A型花岗岩类及其岩石包体研究(硕士论文)[D].导师:杜杨松.北京:中国地质大学.
陈光远,孙岱生,殷辉安.1988.成因矿物学与找矿矿物学[M].重庆:重庆出版社.880.
段超.2009.安徽庐枞盆地龙桥铁矿床地质地球化学特征和矿床成因研究(硕士论文)[D].导师:周涛发.合肥:合肥工业大学.5.
范裕,周涛发,袁峰,钱存超,陆三明,DAVID Cooke.2008.安徽庐江-枞阳地区A型花岗岩的LA-ICP-MS定年及其地质意义[J].岩石学报,24(8):1715-1724.
李厚民,王登红,张长青,陈毓川,李立兴.2009.陕西几类重要铅锌矿床的矿物微量元素和稀土元素特征[J].矿床地质,28(4):434-448.
刘洪,邱检生,罗清华,徐夕生,凌文黎,王德滋.2002.安徽庐枞中生代富钾火山岩成因的地球化学制约[J].地球化学,31(2):129-140.
刘珺.2005.安徽庐极火山岩盆地中巴家滩岩体的地质地球化学特征和成矿潜力评价(硕士论文)[D].导师:周涛发.合肥:合肥工业大学.
刘珺,周涛发,袁峰,范裕,吴明安,陆三明,钱存超.2007.安徽庐枞地区中巴家滩岩体的岩石地球化学特征及成因[J].岩石学报,23(10):2615-2622.
毛景文,王志良.2004.中国东部大规模成矿时限及其动力学背景的初步探讨[J].矿床地质,19(4):91-99.
聂凤军(译).1976.磁铁矿中稀土元素及其它痕量元素的分布[A].见:外国矿产地质[M].1993地质矿产研究所.26(2):119-133.
钱让清,刘中平,钱立平,王实,周文雅.2001.枞阳井边金矿金的赋存状态研究[J].合肥工业大学学报(自然科学版),24(4):253-258.
覃永军,曾键年,曾勇,马振东,陈津华,金希.2010.安徽庐枞盆地罗河-泥河铁矿田含矿辉石粗安玢岩的锆石LA-ICP-MSU-Pb定年及其地质意义[J].地质通报,29(6):851-862.
任启江,王德滋,徐兆文,董火根,潘龙泉,杨荣勇,方长泉,胡进安.1993.安徽庐枞火山-构造洼地的形成、演化及成矿[J].地质学报,62(2):121-136.
孙冶东,杨荣勇,任启江,刘孝善.1994.安徽庐枞中生代火山岩系的特征及其形成的构造背景[J].岩石学报,10(1):94-103.
邵洁涟.1988.金矿找矿矿物学[M].武汉:中国地质大学出版社.158.
王德滋,任启江,邱检生,陈克荣,徐兆文,曾家湖.1996.中国东部橄榄安粗岩省的火山岩特征及其成矿作用[J].地质学报,70:23-34.
王强,赵振华,熊小林,许继峰.2001.底侵玄武质下地壳的熔融:来自安徽沙溪adakite质富钠石英闪长份岩的证据[J].地球化学,30(4):353-363.
王思源.1990.芒场矿田锡多金属成矿构造解析[J].地球科学,15(4):421-430.
王思源.1993.陕西银硐子喷溢沉积改造型银多金属矿床成矿构造解析[J].现代地质,7(3):73-82.
王之田,秦克章.1991.中国大型铜矿类型、成矿环境与成矿集中区的潜力[J].矿床地质,10(3):119-120.
栾世伟.1987.金矿地质与找矿方向[M].成都:四川科学技术出版社.78-84.
吴利仁,齐进英,王听渡,张秀棋,徐永生.1982.中国东部中生代火山岩[J].地质学报,(3):223-235.
吴明安,侯明金,赵文广.2007.安徽省庐枞地区成矿规律及找矿方向[J].资源调查与环境,28(4):269-278.
徐兆文,任启江,杨荣勇,王实.1992.安徽庐枞地区脉状铜矿、铜金矿化分布规律和矿床模式[J].地质与勘探,28(1):8-16.
杨晓勇.2006.郯庐断裂带南段沙溪含铜斑岩体的40Ar-39A:年代学研究及意义[J].矿物岩石,26(4):34-39.
于学元,白正华.1981.庐枞盆地安粗岩系[J].地球化学,10(1):57-65.
袁峰,周涛发,范裕,陆三明,钱存超,张乐骏,段超,唐敏慧.2009.庐枞盆地中生代火山岩的起源、演化及形成背景[J].岩石学报,24(8):1691-1702.
斩是琴,李鸿超.1986.成因矿物学概论(上、下)[M].长春:吉林大学出版社.
赵振华,涂光炽.2003.中国超大型矿床(Ⅱ)[M].北京:科学出版社.325页.
周涛发,范裕,袁峰,陆三明,尚世贵,David Cooke,Sebastien Mef-fre,赵国春.2008.安徽庐枞(庐江-枞阳)盆地火山岩的年代学及其意义[J].中国科学(D辑:地球科学),18(32):1342-1353.
周学武,李胜荣,鲁力,林卫兵.2005.浙江弄坑金银矿区黄铁矿成分标型研究[J].矿物岩石地球化学通报,24(4):317-327.
曾键年,覃永军,郭坤一,陈国光,曾勇.2010.安徽庐枞盆地含矿岩浆岩锆石U-Pb年龄及其对成矿时限的约束[J].地质学报,84(4):465-478.
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