湖北大冶铜山口铜(钼)矿床中钨矿化特征及其地质意义
|
摘要
为了查明鄂东矿集区内铜山口矽卡岩-斑岩型铜(钼)矿床中钨矿化作用的地质特征.对该矿床中的钨矿(化)体开展了系统的矿床地质特征、岩石学和矿物学研究,并探讨基底对区内钨矿在空间上分布的影响.钨矿体主要产出于花岗闪长斑岩与碳酸盐岩地层的接触部位及其附近,其产状受接触面形态的控制;钨既可形成独立的钨矿体,也可作为铜和钼矿体的伴生组分;钨矿物主要为含Mo的白钨矿.铜山口矿床中的钨矿化与矽卡岩化有着密切的时间、空间和成因联系,具有典型的氧化性矽卡岩型钨矿特征,钨和铜矿化是同一岩浆-热液事件不同阶段的产物,但钨矿体的产出位置比铜矿化相对更深;鄂东矿集区南部的钨矿化岩体具有很多相似性,他们很可能在一定程度上受富含铜和钨的江南式基底控制,江南式和董岭式基底在鄂东矿集区的结合部位可能位于阳新岩体附近.
The Tongshankou deposit is a typical skarn-porphyry Cu(Mo)deposit in the East Hubei Province,thick tungsten ore bodies have been discovered in deep part of this deposit recently.In this paper,systematic researches on geological characteristics,petrology,and mineralogy were carried out on tungsten mineralization from the Tongshankou deposit.It is found that tungsten ore bodies were mainly produced at or near the contact zone between sedimentary rocks and granodioritic porphyry.Therefore,their occurrences are controlled by the shape of contact surface.Tungsten can be produced either as a separate tungsten ore body or as a byproduct element in Cu and Mo ore bodies.Scheelite is the mainly tungsten-bearing mineral,and is characterized by a significant enrichment of Mo.Tungsten mineralization process of the Tongshankou deposit is temporally,spatially and genetically associated with skarn alteration,and these features are consistent with those of oxidized W skarns.Tungsten and Cu mineralization are the product of different stages from the same magmatic-hydrothermal process,but the location of W ore bodies are relatively deeper than that of Cu.The Tongshankou porphyry stock shears a lot of similarities with stocks associ-ated with W mineralization in East Hubei Province,suggesting that they were probably partly controlled by Cu and W fertile Jiangnan basement,and the connect part of Jiangnan and Dongling basement under the East Hubei Province probably located nearby the Yangxinpluton.
The Tongshankou deposit is a typical skarn-porphyry Cu(Mo)deposit in the East Hubei Province,thick tungsten ore bodies have been discovered in deep part of this deposit recently.In this paper,systematic researches on geological characteristics,petrology,and mineralogy were carried out on tungsten mineralization from the Tongshankou deposit.It is found that tungsten ore bodies were mainly produced at or near the contact zone between sedimentary rocks and granodioritic porphyry.Therefore,their occurrences are controlled by the shape of contact surface.Tungsten can be produced either as a separate tungsten ore body or as a byproduct element in Cu and Mo ore bodies.Scheelite is the mainly tungsten-bearing mineral,and is characterized by a significant enrichment of Mo.Tungsten mineralization process of the Tongshankou deposit is temporally,spatially and genetically associated with skarn alteration,and these features are consistent with those of oxidized W skarns.Tungsten and Cu mineralization are the product of different stages from the same magmatic-hydrothermal process,but the location of W ore bodies are relatively deeper than that of Cu.The Tongshankou porphyry stock shears a lot of similarities with stocks associ-ated with W mineralization in East Hubei Province,suggesting that they were probably partly controlled by Cu and W fertile Jiangnan basement,and the connect part of Jiangnan and Dongling basement under the East Hubei Province probably located nearby the Yangxinpluton.
引文
Bi,C.S.,1987.Basic Geological Characteristics of Skarn-Type Scheelite Deposit in China.Journal of the Chinese Academy of Geological Sciences,17(3):49-64(in Chinese with English abstract).
Blevin,P.L.,1995.Chemistry,Origin,and Evolution of Mineralized Granites in the Lachlan Fold Belt,Australia:The Metallogeny of I-and S-Type Granites.Economic Geology,90(6):1604-1619.https://doi.org/10.2113/gsecongeo.90.6.1604
Chang,Y.F.,Dong,S.W.,Huang,D.Z.,1996.On Tectonics of“Poly-Basement with One Cover”in Middle-Lower Yangtze Craton China.Volcanology&Mineral Resources,17(1-2):1-15(in Chinese with English abstract).
Chang,Y.F.,Liu,X.P.,Wu,Y.C.,1991.Metallogenic Belt of the Middle and Lower Yangtze River.Geological Publishing House,Beijing(in Chinese).
Ding,L.X.,Huang,G.C.,Xia,J.L.,2014.Petrogenesis of the Longjiaoshan-Fujiashan Porphyritic Intrusion in Southeastern Hubei Province and Implications for Cu-W Mineralization.Acta Geologica Sinica,88(8):1513-1527(in Chinese with English abstract).
Ding,L.X.,Huang,G.C.,Xia,J.L.,2018.Age and Petrogenesis of the Echeng Intrusion in Southeastern Hubei Province:Implications for Iron Mineralization.Earth Science,43(7):2350-2369(in Chinese with English abstract).
Einaudi,M.T.,Meinert,L.D.,Newberry,R.J.,1981.Skarn Deposits.In:Skinner,B.J,ed.,Economic Geology Seventy-Fifth Anniversary Volume.Economic Geology Publishing Company,Lancaster,317-391.https://doi.org/10.5382/AV75.11
Hart,C.J.R.,Mair,J.L.,Goldfarb,R.J.,et al.,2004.Source and Redox Controls on Metallogenic Variations in IntrusionRelated Ore Systems,Tombstone-Tungsten Belt,Yukon Territory,Canada.Transactions of the Royal Society of Edinburgh Earth Sciences,95(1-2):339-356.https://doi.org/10.1017/S0263593300001115
Hsu,L.C.,Galli,P.E.,1973.Origin of the Scheelite-Powellite Series of Minerals.Economic Geology,68(5):681-696.http://doi.org/10.2113/gsecongeo.68.5.681
Li,J.W.,Zhao,X.F.,Zhou,M.F.,et al.,2008.Origin of the Tongshankou Porphyry-Skarn Cu-Mo Deposit,Eastern Yangtze Craton,Eastern China:Geochronological,Geochemical,and Sr-Nd-Hf Isotopic Constraints.Mineralium Deposita,43(3):315-336.https://doi.org/10.1007/s00126-007-0161-3
Liang,X.T.,Quan,H.L.,Ma,X.L.,et al.,2012.Geophysical Deep Ore-Prospecting Model for Tongshankou Area of Daye,Hubei Province.Geophysical&Geochemical Exploration,36(4):697-704(in Chinese with English abstract).
Liu,Y.J.,Ma,D.S.,1987.Tungsten Geochemistry.Science Press,Beijing(in Chinese).
Lü,X.B.,Yao,S.Z,Lin,X.D.,1992.The Geological Characteristics and Ore-Forming Mechanism of Tongshankou Skarn-Porphyry Composite Type of Copper(Molybdenum)Ore Deposit,Hubei.Earth Science,(2):171-180(in Chinese with English abstract).
Lü,X.B.,Yao,S.Z,Lin,X.D.,1993.Alteration-Mineralization Zoning of the Tongshankou Copper(Molybdenum)Deposit in Daye Hubei and Its Prospecting Significance.Mining Geology,(2):97-106(in Chinese with English abstract).
Ma,Z.D.,Shan,G.X.,1997.Geological-Geochemical Studies of the Formation Mechanism of“Integral Whole of Multiplaces”Large and Superlarge Copper Deposits in the Middle and Lower Reaches of the Yangtze River.Mineral Deposits,16(3):225-234(in Chinese with English abstract).
Mao,J.W.,Xie,G.Q.,Duan,C.,et al.,2011.A TectonoGenetic Model for Porphyry-Skarn-Strata Bound CuAu-Mo-Fe and Magnetite-Apatite Deposits along the Middle-Lower Yangtze River Valley,Eastern China.Ore Geology Reviews,43(1):294-314.https://doi.org/10.1016/j.oregeorev.2011.07.010
Meinert,L.D.,1995.Compositional Variation of Igneous Rocks Associated with Skarn Deposits-Chemical Evidence for a Genetic Connection between Petrogenesis and Mineralization.In:Thompson,J.F.H.,ed.,Magmas,Fluids,and Ore Deposits.Victoria,Mineralogical Association of Canada Short Course Series,23:401-408.
Newberry,R.J.,1982.Tungsten-Bearing Skarns of Sierra Nevada I.The Pine Creek Mine,California.Economic Geology,77(4):823-844.https://doi.org/10.2113/gsecongeo.77.4.823
Newberry,R.J.,1998.W-and Sn-Skarn Deposits:A 1998Status Report.In:Lentz,D.R.,ed.,Mineralized IntrusionRelated Skarn Systems.Mineralogical Association of Canada Short Course Series.Ottawa,26:289-335.
Newberry,R.J.,Swanson,S.E.,1986.Scheelite Skarn Granitoids:An Evaluation of the Roles of Magmatic Source and Process.Ore Geology Reviews,1(1):57-81.https://doi.org/10.1016/0169-1368(86)90005-3
Nie,L.Q.,Zhou,T.F.,Fan,Y.,et al.,2016.LA-ICPMS U-Pb Zircon Age and Molybdenite Re-Os Dating of Donggushan,the First Tungsten Deposit Found in the Luzong Orefield,Middle-Lower Yangtze River Valley Metallogenic Belt.Acta Petrologica Sinica,32(2):303-318(in Chinese with English abstract).
Rasmussen,K.L.,Lentz,D.R.,Falck,H.,et al.,2011.Felsic Magmatic Phases and the Role of Late-Stage Aplitic Dykes in the Formation of the World-Class Cantung Tungsten Skarn Deposit,Northwest Territories,Canada.Ore Geology Reviews,41(1):75-111.https://doi.org/10.1016/j.oregeorev.2011.06.011
Sato,K.,1980.Tungsten Skarn Deposit of the Fujigatani Mine,Southwest Japan.Economic Geology,75(7):1066-1082.
Shu,Q.A.,Chen,P.L.,Cheng,J.R.,1992.Geology of Fe-Cu Ore Deposits in Eastern Hubei Province.Press of Metallurgical Industry,Beijing(in Chinese).
Sillito,R.H.,2010.Porphyry Copper Systems.Economic Geology,105:3-41.https://doi.org/10.2113/gsecongeo.105.1.3
Song S.W.,Mao J.W.,Zhu Y.F.,et al.,2018.Partial-Melting of Fertile Metasedimentary Rocks Controlling the Ore Formation on the Jiangnan Porphyry-Skarn Tungsten Belt,South China:A Case Study at the Giant Zhuxi W-Cu Skarn Deposit.Lithos,304-307:180-199.https://doi.org/10.1016/j.lithos.2018.02.002
Sun,J.F.,1984.Characteristics of the Tungsten Skarn Deposits from Daye-Yangxin Area.Geology and Prospecting,(8):11-13,31(in Chinese).
Sun,Y.,Ma,C.Q.,Liu,B.,2017.Record of Late Yanshanian Mafic Magmatic Activity in the Middle-Lower Yangtze River Metallogenic Belt.Earth Science,42(6):891-908(in Chinese with English abstract).
Wang,D.H.,Chen,Z.H.,Huang,G.C.,et al.2012.Northwards and Westwards Prospecting for Tungsten and Its Significance in South China.Geotectonica et Metallogenia,36(3):322-329(in Chinese with English abstract).
Wang,Q.,Zhao,Z.H.,Bao,Z.W.,et al.,2004.Geochemistry and Petrogenesis of the Tongshankou and Yinzu Adakitic Intrusive Rocks and the Associated Porphyry Copper-Molybdenum Mineralization in Southeast Hubei,East China.Resource Geology,54(2):137-152.|https://doi.org/10.1111/j.1751-3928.2004.tb00195.x
Xie,G.Q.,Li,R.L.,Jiang,G.H.,et al.,2008.Geochemistry and Petrogenesis of Late Mesozoic Granitoids in Southeastern Hubei Province and Constrains on the Timing of Lithospheric Thinning,Middle-Lower Reaches of the Yangtze River,Eastern China.Acta Petrologica Sinica,24(8):1703-1714(in Chinese with English abstract).
Xie,G.Q.,Mao,J.W.,Li,R.L.,et al.,2007.Re-Os Molybdenite and Ar-Ar Phlogopite Dating of Cu-Fe-Au-Mo(W)Deposits in Southeastern Hubei,China.Mineralogy&Petrology,90(3-4):249-270.https://doi.org/10.1007/s00710-006-0176-y
Xie,G.Q.,Mao,J.W.,Li,X.W.,et al.,2011a.Late Mesozoic Bimodal Volcanic Rocks in the Jinniu Basin,MiddleLower Yangtze River Belt(YRB),East China:Age,Petrogenesis and Tectonic Implications.Lithos,127:144-164.https://doi.org/10.1016/j.lithos.2011.08.012
Xie,G.Q.,Mao,J.W.,Zhao,H.J.,2011b.Zircon U-Pb Geochronological and Hf Isotopic Constraints on Petrogenesis of Late Mesozoic Intrusions in the Southeast Hubei Province,Middle-Lower Yangtze River Belt(MLYRB),East China.Lithos,125:693-710.https://doi.org/10.1016/j.lithos.2011.04.001
Xie,G.Q.,Mao,J.W.,Zhao,H.J.,et al.,2012.Zircon U-Pb and Phlogopite 40 Ar-39 Ar Age of the Chengchao and Jinshandian Skarn Fe Deposits,Southeast Hubei Province,Middle-Lower Yangtze River Valley Metallogenic Belt,China.Mineralium Deposita,47(6):633-652.https://doi.org/10.1007/s00126-011-0367-2
Yan,D.R.,Deng,X.D.,Hu,H.,et al.,2012.U-Pb Age and Petrogenesis of the Ruanjiawan Granodiorite Pluton and Xiniushan Granodiorite Porphyry,Southeast Hubei Province:Implications for Cu-Mo Mineralization.Acta Petrologica Sinica,28(10):3373-3388(in Chinese with English abstract).
Zhao,X.F.,Li,J.W.,Ma,C.Q.,2006.40 Ar/39 Ar Geochronology of the Tongshankou Cu(Mo)Deposit in the Southeastern Hubei Fe-Cu Province:Implications for Regional Metallogeny.Acta Geologica Sinica,80(6):849-862(in Chinese with English abstract).
Zhou,T.F.,Fan,Y.,Wang,S.W.,et al.,2017.Metallogenic Regularity and Metallogenic Model of the Middle-Lower Yangtze River Valley Metallogenic Belt.Acta Petrologica Sinica,33(11):3353-3372(in Chinese with English abstract).
Zhu,Q.Q.,Xie,G.Q.,Han,Y.X.,2017.SHRIMP Zircon U-Pb Dating of Quartz Diorite Porphyry from the Shizilishan Sr(Pb-Zn)Deposit in Hubei Province and Its Geological Significance.Acta Petrologica Sinica,33(11):3484-3494(in Chinese with English abstract).
Zhu,Z.Q.,1987.Discussion of Skarn Scheelite Deposit from Middle-Lower Yangtze River.Jiangsu Geology,(3):8-11(in Chinese).
毕承思,1987.中国矽卡岩型白钨矿矿床成矿基本地质特征.中国地质科学院院报,17(3):49-64.
常印佛,董树文,黄德志,1996.论中-下扬子“一盖多底”格局与演化.火山地质与矿产,17(1-2):1-15.
常印佛,刘湘培,吴言昌,1991.长江中下游铜铁成矿带.地质出版社,北京.
丁丽雪,黄圭成,夏金龙,2014.鄂东南地区龙角山-付家山斑岩体成因及其对成矿作用的指示.地质学报,88(8):1513-1527.
丁丽雪,黄圭成,夏金龙,2018.鄂东南地区鄂城岩体的时代、成因及其对成矿作用的指示.地球科学,43(7):2350-2369.
梁学堂,全浩理,马玄龙,等,2012.湖北大冶铜山口地区地球物理深部找矿模式.物探与化探,36(4):697-704.
刘英俊,马东升,1987.钨的地球化学.科学出版社,北京.
吕新彪,姚书振,林新多,1992.湖北大冶铜山口矽卡岩-斑岩复合型铜(钼)矿床地质特征和成矿机制.地球科学,(2):171-180.
吕新彪,姚书振,林新多,1993.大冶铜山口铜钼矿床蚀变-矿化分带找矿意义.矿山地质,(2):97-106.
马振东,单光祥,1997.长江中下游地区多位一体大型、超大型铜矿形成机制的地质、地球化学研究.矿床地质,16(3):225-234.
聂利青,周涛发,范裕,等,2016.长江中下游成矿带庐枞矿集区首例钨矿床成岩成矿时代及其意义.岩石学报,32(2):303-318.
舒全安,陈培良,程建荣,1992.鄂东铁铜矿产地质.冶金工业出版社,北京.
孙家福,1984.大冶-阳新地区夕卡岩型白钨矿床的成矿特点.地质与勘探,(8):11-13,31.
孙洋,马昌前,刘彬,2017.长江中下游地区燕山晚期基性岩浆活动的记录.地球科学,42(6):891-908.
王登红,陈郑辉,黄国成,等,2012.华南“南钨北扩”、“东钨西扩”及其找矿方向探讨.大地构造与成矿学,36(3):322-329.
谢桂青,李瑞玲,蒋国豪,等,2008.鄂东南地区晚中生代侵入岩的地球化学和成因及对岩石圈减薄时限的制约.岩石学报,24(8):1703-1714.
颜代蓉,邓晓东,胡浩,等,2012.鄂东南地区阮家湾和犀牛山花岗闪长岩的时代、成因及成矿和找矿意义.岩石学报,28(10):3373-3388.
赵新福,李建威,马昌前,2006.鄂东南铁铜矿集区铜山口铜(钼)矿床40 Ar/39 Ar年代学及对区域成矿作用的指示.地质学报,80(6):849-862.
周涛发,范裕,王世伟,等,2017.长江中下游成矿带成矿规律和成矿模式.岩石学报,33(11):3353-3372.
朱乔乔,谢桂青,韩颖霄,2017.湖北狮子立山锶(铅锌)矿区石英闪长玢岩锆石SHRIMP U-Pb定年及其意义.岩石学报,33(11):3484-3494.
朱增青,1987.长江中、下游矽卡岩型白钨矿床成矿特征浅析.江苏地质,(3):8-11.
Blevin,P.L.,1995.Chemistry,Origin,and Evolution of Mineralized Granites in the Lachlan Fold Belt,Australia:The Metallogeny of I-and S-Type Granites.Economic Geology,90(6):1604-1619.https://doi.org/10.2113/gsecongeo.90.6.1604
Chang,Y.F.,Dong,S.W.,Huang,D.Z.,1996.On Tectonics of“Poly-Basement with One Cover”in Middle-Lower Yangtze Craton China.Volcanology&Mineral Resources,17(1-2):1-15(in Chinese with English abstract).
Chang,Y.F.,Liu,X.P.,Wu,Y.C.,1991.Metallogenic Belt of the Middle and Lower Yangtze River.Geological Publishing House,Beijing(in Chinese).
Ding,L.X.,Huang,G.C.,Xia,J.L.,2014.Petrogenesis of the Longjiaoshan-Fujiashan Porphyritic Intrusion in Southeastern Hubei Province and Implications for Cu-W Mineralization.Acta Geologica Sinica,88(8):1513-1527(in Chinese with English abstract).
Ding,L.X.,Huang,G.C.,Xia,J.L.,2018.Age and Petrogenesis of the Echeng Intrusion in Southeastern Hubei Province:Implications for Iron Mineralization.Earth Science,43(7):2350-2369(in Chinese with English abstract).
Einaudi,M.T.,Meinert,L.D.,Newberry,R.J.,1981.Skarn Deposits.In:Skinner,B.J,ed.,Economic Geology Seventy-Fifth Anniversary Volume.Economic Geology Publishing Company,Lancaster,317-391.https://doi.org/10.5382/AV75.11
Hart,C.J.R.,Mair,J.L.,Goldfarb,R.J.,et al.,2004.Source and Redox Controls on Metallogenic Variations in IntrusionRelated Ore Systems,Tombstone-Tungsten Belt,Yukon Territory,Canada.Transactions of the Royal Society of Edinburgh Earth Sciences,95(1-2):339-356.https://doi.org/10.1017/S0263593300001115
Hsu,L.C.,Galli,P.E.,1973.Origin of the Scheelite-Powellite Series of Minerals.Economic Geology,68(5):681-696.http://doi.org/10.2113/gsecongeo.68.5.681
Li,J.W.,Zhao,X.F.,Zhou,M.F.,et al.,2008.Origin of the Tongshankou Porphyry-Skarn Cu-Mo Deposit,Eastern Yangtze Craton,Eastern China:Geochronological,Geochemical,and Sr-Nd-Hf Isotopic Constraints.Mineralium Deposita,43(3):315-336.https://doi.org/10.1007/s00126-007-0161-3
Liang,X.T.,Quan,H.L.,Ma,X.L.,et al.,2012.Geophysical Deep Ore-Prospecting Model for Tongshankou Area of Daye,Hubei Province.Geophysical&Geochemical Exploration,36(4):697-704(in Chinese with English abstract).
Liu,Y.J.,Ma,D.S.,1987.Tungsten Geochemistry.Science Press,Beijing(in Chinese).
Lü,X.B.,Yao,S.Z,Lin,X.D.,1992.The Geological Characteristics and Ore-Forming Mechanism of Tongshankou Skarn-Porphyry Composite Type of Copper(Molybdenum)Ore Deposit,Hubei.Earth Science,(2):171-180(in Chinese with English abstract).
Lü,X.B.,Yao,S.Z,Lin,X.D.,1993.Alteration-Mineralization Zoning of the Tongshankou Copper(Molybdenum)Deposit in Daye Hubei and Its Prospecting Significance.Mining Geology,(2):97-106(in Chinese with English abstract).
Ma,Z.D.,Shan,G.X.,1997.Geological-Geochemical Studies of the Formation Mechanism of“Integral Whole of Multiplaces”Large and Superlarge Copper Deposits in the Middle and Lower Reaches of the Yangtze River.Mineral Deposits,16(3):225-234(in Chinese with English abstract).
Mao,J.W.,Xie,G.Q.,Duan,C.,et al.,2011.A TectonoGenetic Model for Porphyry-Skarn-Strata Bound CuAu-Mo-Fe and Magnetite-Apatite Deposits along the Middle-Lower Yangtze River Valley,Eastern China.Ore Geology Reviews,43(1):294-314.https://doi.org/10.1016/j.oregeorev.2011.07.010
Meinert,L.D.,1995.Compositional Variation of Igneous Rocks Associated with Skarn Deposits-Chemical Evidence for a Genetic Connection between Petrogenesis and Mineralization.In:Thompson,J.F.H.,ed.,Magmas,Fluids,and Ore Deposits.Victoria,Mineralogical Association of Canada Short Course Series,23:401-408.
Newberry,R.J.,1982.Tungsten-Bearing Skarns of Sierra Nevada I.The Pine Creek Mine,California.Economic Geology,77(4):823-844.https://doi.org/10.2113/gsecongeo.77.4.823
Newberry,R.J.,1998.W-and Sn-Skarn Deposits:A 1998Status Report.In:Lentz,D.R.,ed.,Mineralized IntrusionRelated Skarn Systems.Mineralogical Association of Canada Short Course Series.Ottawa,26:289-335.
Newberry,R.J.,Swanson,S.E.,1986.Scheelite Skarn Granitoids:An Evaluation of the Roles of Magmatic Source and Process.Ore Geology Reviews,1(1):57-81.https://doi.org/10.1016/0169-1368(86)90005-3
Nie,L.Q.,Zhou,T.F.,Fan,Y.,et al.,2016.LA-ICPMS U-Pb Zircon Age and Molybdenite Re-Os Dating of Donggushan,the First Tungsten Deposit Found in the Luzong Orefield,Middle-Lower Yangtze River Valley Metallogenic Belt.Acta Petrologica Sinica,32(2):303-318(in Chinese with English abstract).
Rasmussen,K.L.,Lentz,D.R.,Falck,H.,et al.,2011.Felsic Magmatic Phases and the Role of Late-Stage Aplitic Dykes in the Formation of the World-Class Cantung Tungsten Skarn Deposit,Northwest Territories,Canada.Ore Geology Reviews,41(1):75-111.https://doi.org/10.1016/j.oregeorev.2011.06.011
Sato,K.,1980.Tungsten Skarn Deposit of the Fujigatani Mine,Southwest Japan.Economic Geology,75(7):1066-1082.
Shu,Q.A.,Chen,P.L.,Cheng,J.R.,1992.Geology of Fe-Cu Ore Deposits in Eastern Hubei Province.Press of Metallurgical Industry,Beijing(in Chinese).
Sillito,R.H.,2010.Porphyry Copper Systems.Economic Geology,105:3-41.https://doi.org/10.2113/gsecongeo.105.1.3
Song S.W.,Mao J.W.,Zhu Y.F.,et al.,2018.Partial-Melting of Fertile Metasedimentary Rocks Controlling the Ore Formation on the Jiangnan Porphyry-Skarn Tungsten Belt,South China:A Case Study at the Giant Zhuxi W-Cu Skarn Deposit.Lithos,304-307:180-199.https://doi.org/10.1016/j.lithos.2018.02.002
Sun,J.F.,1984.Characteristics of the Tungsten Skarn Deposits from Daye-Yangxin Area.Geology and Prospecting,(8):11-13,31(in Chinese).
Sun,Y.,Ma,C.Q.,Liu,B.,2017.Record of Late Yanshanian Mafic Magmatic Activity in the Middle-Lower Yangtze River Metallogenic Belt.Earth Science,42(6):891-908(in Chinese with English abstract).
Wang,D.H.,Chen,Z.H.,Huang,G.C.,et al.2012.Northwards and Westwards Prospecting for Tungsten and Its Significance in South China.Geotectonica et Metallogenia,36(3):322-329(in Chinese with English abstract).
Wang,Q.,Zhao,Z.H.,Bao,Z.W.,et al.,2004.Geochemistry and Petrogenesis of the Tongshankou and Yinzu Adakitic Intrusive Rocks and the Associated Porphyry Copper-Molybdenum Mineralization in Southeast Hubei,East China.Resource Geology,54(2):137-152.|https://doi.org/10.1111/j.1751-3928.2004.tb00195.x
Xie,G.Q.,Li,R.L.,Jiang,G.H.,et al.,2008.Geochemistry and Petrogenesis of Late Mesozoic Granitoids in Southeastern Hubei Province and Constrains on the Timing of Lithospheric Thinning,Middle-Lower Reaches of the Yangtze River,Eastern China.Acta Petrologica Sinica,24(8):1703-1714(in Chinese with English abstract).
Xie,G.Q.,Mao,J.W.,Li,R.L.,et al.,2007.Re-Os Molybdenite and Ar-Ar Phlogopite Dating of Cu-Fe-Au-Mo(W)Deposits in Southeastern Hubei,China.Mineralogy&Petrology,90(3-4):249-270.https://doi.org/10.1007/s00710-006-0176-y
Xie,G.Q.,Mao,J.W.,Li,X.W.,et al.,2011a.Late Mesozoic Bimodal Volcanic Rocks in the Jinniu Basin,MiddleLower Yangtze River Belt(YRB),East China:Age,Petrogenesis and Tectonic Implications.Lithos,127:144-164.https://doi.org/10.1016/j.lithos.2011.08.012
Xie,G.Q.,Mao,J.W.,Zhao,H.J.,2011b.Zircon U-Pb Geochronological and Hf Isotopic Constraints on Petrogenesis of Late Mesozoic Intrusions in the Southeast Hubei Province,Middle-Lower Yangtze River Belt(MLYRB),East China.Lithos,125:693-710.https://doi.org/10.1016/j.lithos.2011.04.001
Xie,G.Q.,Mao,J.W.,Zhao,H.J.,et al.,2012.Zircon U-Pb and Phlogopite 40 Ar-39 Ar Age of the Chengchao and Jinshandian Skarn Fe Deposits,Southeast Hubei Province,Middle-Lower Yangtze River Valley Metallogenic Belt,China.Mineralium Deposita,47(6):633-652.https://doi.org/10.1007/s00126-011-0367-2
Yan,D.R.,Deng,X.D.,Hu,H.,et al.,2012.U-Pb Age and Petrogenesis of the Ruanjiawan Granodiorite Pluton and Xiniushan Granodiorite Porphyry,Southeast Hubei Province:Implications for Cu-Mo Mineralization.Acta Petrologica Sinica,28(10):3373-3388(in Chinese with English abstract).
Zhao,X.F.,Li,J.W.,Ma,C.Q.,2006.40 Ar/39 Ar Geochronology of the Tongshankou Cu(Mo)Deposit in the Southeastern Hubei Fe-Cu Province:Implications for Regional Metallogeny.Acta Geologica Sinica,80(6):849-862(in Chinese with English abstract).
Zhou,T.F.,Fan,Y.,Wang,S.W.,et al.,2017.Metallogenic Regularity and Metallogenic Model of the Middle-Lower Yangtze River Valley Metallogenic Belt.Acta Petrologica Sinica,33(11):3353-3372(in Chinese with English abstract).
Zhu,Q.Q.,Xie,G.Q.,Han,Y.X.,2017.SHRIMP Zircon U-Pb Dating of Quartz Diorite Porphyry from the Shizilishan Sr(Pb-Zn)Deposit in Hubei Province and Its Geological Significance.Acta Petrologica Sinica,33(11):3484-3494(in Chinese with English abstract).
Zhu,Z.Q.,1987.Discussion of Skarn Scheelite Deposit from Middle-Lower Yangtze River.Jiangsu Geology,(3):8-11(in Chinese).
毕承思,1987.中国矽卡岩型白钨矿矿床成矿基本地质特征.中国地质科学院院报,17(3):49-64.
常印佛,董树文,黄德志,1996.论中-下扬子“一盖多底”格局与演化.火山地质与矿产,17(1-2):1-15.
常印佛,刘湘培,吴言昌,1991.长江中下游铜铁成矿带.地质出版社,北京.
丁丽雪,黄圭成,夏金龙,2014.鄂东南地区龙角山-付家山斑岩体成因及其对成矿作用的指示.地质学报,88(8):1513-1527.
丁丽雪,黄圭成,夏金龙,2018.鄂东南地区鄂城岩体的时代、成因及其对成矿作用的指示.地球科学,43(7):2350-2369.
梁学堂,全浩理,马玄龙,等,2012.湖北大冶铜山口地区地球物理深部找矿模式.物探与化探,36(4):697-704.
刘英俊,马东升,1987.钨的地球化学.科学出版社,北京.
吕新彪,姚书振,林新多,1992.湖北大冶铜山口矽卡岩-斑岩复合型铜(钼)矿床地质特征和成矿机制.地球科学,(2):171-180.
吕新彪,姚书振,林新多,1993.大冶铜山口铜钼矿床蚀变-矿化分带找矿意义.矿山地质,(2):97-106.
马振东,单光祥,1997.长江中下游地区多位一体大型、超大型铜矿形成机制的地质、地球化学研究.矿床地质,16(3):225-234.
聂利青,周涛发,范裕,等,2016.长江中下游成矿带庐枞矿集区首例钨矿床成岩成矿时代及其意义.岩石学报,32(2):303-318.
舒全安,陈培良,程建荣,1992.鄂东铁铜矿产地质.冶金工业出版社,北京.
孙家福,1984.大冶-阳新地区夕卡岩型白钨矿床的成矿特点.地质与勘探,(8):11-13,31.
孙洋,马昌前,刘彬,2017.长江中下游地区燕山晚期基性岩浆活动的记录.地球科学,42(6):891-908.
王登红,陈郑辉,黄国成,等,2012.华南“南钨北扩”、“东钨西扩”及其找矿方向探讨.大地构造与成矿学,36(3):322-329.
谢桂青,李瑞玲,蒋国豪,等,2008.鄂东南地区晚中生代侵入岩的地球化学和成因及对岩石圈减薄时限的制约.岩石学报,24(8):1703-1714.
颜代蓉,邓晓东,胡浩,等,2012.鄂东南地区阮家湾和犀牛山花岗闪长岩的时代、成因及成矿和找矿意义.岩石学报,28(10):3373-3388.
赵新福,李建威,马昌前,2006.鄂东南铁铜矿集区铜山口铜(钼)矿床40 Ar/39 Ar年代学及对区域成矿作用的指示.地质学报,80(6):849-862.
周涛发,范裕,王世伟,等,2017.长江中下游成矿带成矿规律和成矿模式.岩石学报,33(11):3353-3372.
朱乔乔,谢桂青,韩颖霄,2017.湖北狮子立山锶(铅锌)矿区石英闪长玢岩锆石SHRIMP U-Pb定年及其意义.岩石学报,33(11):3484-3494.
朱增青,1987.长江中、下游矽卡岩型白钨矿床成矿特征浅析.江苏地质,(3):8-11.
© 2004-2018 中国地质图书馆版权所有 京ICP备05064691号 京公网安备11010802017129号 地址：北京市海淀区学院路29号 邮编：100083 电话：办公室：(+86 10)66554848；文献借阅、咨询服务、科技查新：66554700 |