全部 标题 作者
关键词 摘要

OALib Journal期刊
ISSN: 2333-9721
费用:99美元

查看量下载量

相关文章

更多...
矿床地质  2008 

青藏高原碰撞造山带Pb-Zn-Ag-Cu矿床新类型:成矿基本特征与构造控矿模型

Keywords: 地质学,Pb-Zn-Ag-Cu矿床,成矿特征,构造控矿模型,逆冲推覆构造系统,碰撞造山带,青藏高原,青藏高原,碰撞造山带,新类型矿床,成矿模式,基本特征,中生代构造,控矿模型,orogenicbelt,Tibetan,northern,model,tectonic,要素,勘查,综合分析,沟通,物质,围岩,淋滤,运移

Full-Text   Cite this paper   Add to My Lib

Abstract:

地处青藏高原东、北缘的兰坪、玉树及沱沱河地区,广泛发育包括金顶超大型矿床在内的大量新生代Pb、Zn、Cu多金属矿床.这些矿床均产于该高原东缘晚碰撞构造转换环境,主体赋存于第三纪前陆盆地内部,以沉积岩容矿,与岩浆活动无关,受逆冲推覆构造系统控制,显著区别于世界已知的各类以沉积岩容矿的贱金属矿床.研究表明,伴随印度.亚洲大陆碰撞造山而产生一系列逆冲断裂系,将前陆盆地侧缘的中生代地层切割成叠置的构造岩片,并推覆叠置于盆地沉积地层之上,形成单冲式或对冲式逆冲推覆构造系统,并控制了Pb-Zn-Ag-C矿床的形成与发育.根据逆冲推覆构造控矿式样和矿化特征,可以识别出4种矿床式:①产于逆冲推覆构造系统前锋带"构造穹隆岩性圈闭"内的金顶式Zn-Pb矿床;②受控于前锋带冲起构造的河西.三山式Pb-Zn-Ag-Cu矿床;③产于主逆冲断裂带派生的次级断层或平移断层内的富隆厂式Ag-Cu或Cu矿床;④产于主逆冲断裂上盘灰岩层间破碎带内的东莫扎抓式Pb-Zn矿床.这些矿床的矿体多受不同级次的断裂控制,多孔砂岩、白云岩化灰岩及构造破碎带是有利矿化部位.多数矿体显示开放空间充填成矿特点,少数显示层控性,属后生成矿.金属矿物组合主要为低Fe闪锌矿方铅矿黄铁矿组合及低温Cu硫化物(黝铜矿系列为主)Ag硫化物(辉银矿、黝银矿、汞银矿)方铅矿±闪锌矿组合,脉石矿物组合主要为方解石±重晶石±萤石±白云石±天青石,局部见沥青.成矿流体以盐水体系为主,盐度w(NaCleq)变化于1%~28.0%之间,成矿温度较低,通常在80~190℃,显示盆地卤水±大气降水的特点.逆冲推覆构造系统对矿床的控制主要体现在:其深部拆离滑脱带可能是流体流长距离侧向迁移的优选通道,主逆冲断裂是成矿流体垂向运移和向上排泄的主要途径,浅部各类样式的逆冲构造是流体汇聚的主要场所.成矿物质以盆地沉积岩贡献为主,部分可能来自幔源岩石.矿床金属组合可能与成矿流体迁移-汇聚过程中流经岩石的性质有关:矿区发育灰岩建造时,出现Zn-Pb(Zn多于Pb)矿化;若发育碎屑岩建造,尤其是红层,则出现Cu-Ag(-Pb)矿化.因此,笔者将这种逆冲推覆构造控制的新类型矿床称之为造山型Pb-Zn-Ag-Cu矿床,其成矿模式可表述为:伴随着印度-亚洲大陆持续碰撞,青藏高原东、北缘中生代构造岩片向盆地中央推覆并置,形成单冲式或对冲式逆冲推覆构造系统,流体从造山带沿拆离滑脱带长距离向前陆盆地方向运移,运移过程中淋滤围岩的金属物质,通过主逆冲断裂垂向沟通,进入浅部各式逆冲构造部位从而形成不同样式的矿床.经综合分析,提出了青藏高原东、北缘受逆冲推覆构造控制的贱金属矿床的勘查要素.

References

[1]  Basuki N I and Spooner.2002.A review of fluid inclusion temperatures and salinities in Mississippi Valley-type Pb-Zn deposits:Identifying thresholds for metal transport[J].Exploration and Mains Geology,11:1~17
[2]  Bjorlykke A and Sangster D F.1981.An overview of sandstone lead deposits and their relation to red-bed copper and carbonated hosted lead-zinc deposits[J].Econ.Geol.,76:179~213.
[3]  Bradley D C and Leach D L.2003.Tectonic controls of Mississippi Valley-type lead-zinc mineralization in orogenic forelands[J].Mineralium Deposita,38:652~667.
[4]  Chen J and Wang H N.2004.Geochemistry[M].Beijing:Science Press.116~129(in Chinese).
[5]  Chen K X,He L Q,Yang Z Q,Wei J Q and Yang A P.2000.Oxygen and carbon isotope geochemistry in Sanshan-Baiyangpmg copper-silver polymetallogenic enrichment district,Lanping,Yunnan[J].Geology and Mineral Resources of South Chim,4:1~8(in Chinese).
[6]  Chen K X,Yao S Z,He L Q,Wei J Q,Yang A P and Huang H L.2004.Ore-forming fluid in Baiyangping silver-polymetallic mineralization concentration field in Larlping,Yunnan Province[J].Geological Science and Technology Information,23:45~50(in Chinese with English abstract).
[7]  Chi G and Savard M M.1998.Basin fluid flow models related to Zn-Pb mineralization in the southern margin of the Maritime basin,Eastern Canada[J].Econ.Geol.,93:896~910.
[8]  Chung S L,Lo C H,Lee T Y,Zhang Y Q,Xie Y W,Li X H,Wang K Land Wang P L.1998.Diechronous uplift of the Tibetan Plateau starting from 40 Ma ago[J].Nature,349:769~773.
[9]  Clendenin C W and Duane M J.1990.Focused fluid flow and Ozark Mississippi Valley-type deposit[J].Geology,18:116~119.
[10]  Dong F L,Mo X X,Hou g Q,Wang Y,Bi X M and Zhou S.2005.40Ar-39Ar ages of Himalayan alkaline rocks in Lanping basin,Yunnan Province,and their geological implications[J].Acts Petrologica et Mineralogica,24:103~109(in Chinese with English abstract).
[11]  Fan S J,Wang A J,Liu H B,Xiu Q Y,Cao D H,Li R P,Gao H and Chen Q S.2006.A discussion on the He and Ar isotopic evidences for genesis of the Baiyangping cooper-eobalt deposit in the Lanping basin[J].Geological Review,9:628~635(in Chinese with English abstract).
[12]  Fu X G and Pang Y C.2004.Geobgical characteristic of Jinding leadzinc deposi twith discussion on its genesis[J].World Geology,9:239~244(in Chinese with English abstract).
[13]  Gao L,Wang A J,Liu J L,Xiu Q Y,Cao D H and Zhao Y F.2005.New progress in study of superlarge Jinding Pb-Zn deposit:Discovery of intrusive breccia and its implacation[J].Mineral Deposits,4:457~467(in Chinese with English abstract).
[14]  Gao Z Q,Zhao Q H and Tong Y H.2006.Jinman sedimentation-hydrothermal reformationCu deposit,Lanping[J].Journal of Yunnan Geology,25:341~347(in Chinese with English abstract).
[15]  Garven G.1985.The role of regional fluid flow in the genesis of the Pine Point deposit,western Canadian sedimentary basin[J].Econ.Geol.,80:307~324.
[16]  Garven G.1986.A hydrogeological model for the genesis of the giant oil sands deposits of the western Canada sedimentary basin(abstract)[J].American Geophysical Union Transactons,67:273.
[17]  Garven G.1989.A hydrogeological model for the formation of the giant oil sands deposits of the western Canada sedimentary basin[J].American Journal of Science,289:105~166.
[18]  Gsrven G.1995.Continental-scale groundwater flow and geological pro cesses[J].Annual Review of Earth and Planetary Sciences,23:89~117.
[19]  Garvern G and Raffensperger J P.1997.Hydrogeology and geochemistry of ore genesisin sedimentary bssins[A].In:Barnes H L,ed.Geochemistry of hydrothermal ore deposit[C].New York:Wiley.125~189.
[20]  Gong W J,Tan K X,Li X M and Gong G L.2000.Geochemical characteristics of fluid and mechanism for ore formation in the Baiyangping copper-silver deposit,Yunnan[J].Geotectonica et Metsllogenia,24:175~181(in Chinese with English abstract).
[21]  更多...
[22]  He L Q,Chen K X,Yu F M,Wei J Q,Yang A P and Li H.2004.Nappe tectonics and their ore-controlling of Lanping basin in Yunnan Province[J].Geology and Prospecting,40:7~12(in Chinese with English abstract).
[23]  He M Q,Liu J J,Li C Y,Li Z M and Liu Y P.2004.Mechanism of ore-forming fluids of the Lanping fb-Zn-Cu polymetallic mineralized concentration area:An example study on the Baiyansping ore district[J].Beijing:Geol.Pub.House.117 p(in Chinese).
[24]  Hon g Q,Ma H W,Khin Z,Zhang Y Q,Wang M J,Wang Z,Pan G T and Tang R L.2003.The Himalayan Yulong porphyry copper belt:product of large-scah strike-slip faulting in eastern Tibet[J].Econ.Geol.,98:125~145.
[25]  Hou Z Q,Pan G T,Wang A J,Mo X X,Tian S H,Sun X M,Ding L,Wang E Q,Gao Y F,Xie Y L,Zeng P S,Qin K Z,Xu J F,Qu X M,Yang Z M,Yang Z S,Fei H C,Meng X J and Li Z Q.2006a.Metallogenesis in Tibetan collisional orogenic belt:Ⅱ.Mineralization in late-collisional transformation setting[J].Mineral Deposits,25(5):521~543(in Chinese with English abstract).
[26]  Hou Z Q,Yang Z S,Xu W Y,Mo X X,Ding L,Gao Y F,Dong F L,Li G M,Qu X M,Li G M,Zhao Z D,Jiang S H,Meng X J,Li Z Q,Qin K Z and Yang Z M.2006b.Metallogenesis in Tibetan collisional orogenic belt:Ⅰ.Mineralization in main collisional orogenic setting[J].Mineral Deposits,25(4):337~358(in Chinese with English abstract).
[27]  Huston D L,Stevens B,Southgate P N,Muhling P and Wyborn L.2006.Austaralian Zn-Pb-Ag ore-forming systems:A review and analysis[J].Econ.Geol.,101:1117~1157.
[28]  Ji H B and Li C Y.1998.Geochemical characteristics and source of oreforming fluid for Jinman copper deposit in western Yunnan Province,China[J].Acta Mineralogica Sinica,18:28~37(in Chinese with English abstract).
[29]  Large D E.1988.The evaluation of sedimentary basins for massive sulfide mineralization[A].In:Friedrich G H and Herzig P M,eds.Base metal sulfide deposits[C].The Netherlands:Springer-verlag.2~11.
[30]  Leach D L and Rowan E L.1986.Genetic link between Ouachita fold belt tectonism and the Mississippi Valley-type deposits of the Ozarks[J].Geology,14:931~935.
[31]  Leach D L and Sangster D F.1993.Mississippi Vailey-type lead-zinc de-posits[A].Geological Association of Ganada Special Paper,40:289~314.
[32]  Leach D L,Sangster D F,Kelley K D,Large R R,Garven G,Allen C R,Gutzmer J and Waltera S.2005.Sediment-hosted lead-fine deposits:A global perspective[J].Econ.Geol.,100th Anniversary Volume:561~607.
[33]  Li F,Hueng D Y end Fu W M.1995.Metallngenic law of red-bsd copper deposim of the Lanping-Siman basin,Yunnan,China[J].Geotectonica et Metallogenia,19:322~335(in Chinese with English abstract).
[34]  Li X Z,Liu W J,Wang Y Z and Zhu Q W.1999.Tectonic evolution of the tethys end mineralization in the Sanjiang region,S W China[M].Beijing:Geol.Pub.House.258p(in Chinese with English abstract).
[35]  Li Y G,Hou Z J,Wang A J,Tang J X,Liu J L,Xue C J and Xiu Q Y.2006.Geochemistry of Cenozoic detrital rocks and its constraints on provenance in Lanping basin[J].Acta Geologica Sinica,22:751~760(in Chinese with English abstract).
[36]  Li Y L,Wang C S,Yi H S,Lju Z Fend Li Y.2006.Cenozoic thrust system and uplifting of the Tanggula Mountain,Northem Tibet[J].Acta Geologica Sinica.80:1118~1131(in Chinese with English abstract).
[37]  Li Z M,Liu J J,Qin J Z,Liao Z T and Zheng C J.2004.C,O and H isotopic compositions of polymetallie deposits in Lanping basin,western Yunnan Province and their geological significance[J].Journal of Jilin Urfiversity(Earth Science Edition),34:360~366(in Chinese with English abstract).
[38]  Li Z M,Liu J J,Qin J Z,Liao Z T,He M Q and Liu Y P.2005.Oreforming matieral source of the Baiyengping copper-cobalt-silver polymetallic deposit in Lanping basin,western Yunnan[J].Geology and Prospecting.1:1~6(in Chinese with English abstract).
[39]  Liang H Y,Campbell I H,Allen C A,Sun W D,Xie Y W and Zhang Y Q.2008.The age of the potsssic alkaline igneous rocks along the Ailao Shen-Red River shear zone:Implications for the Onset age of left-lateral shearing:A reply[J].J.Geol.,116:205~207.
[40]  Liao Z T and Chen Y K.2005.Nature and evolution of Lanping-Simao basin prototype[J].Journal of Tongii University(Nature Science),33:1528~1531(in Chinese with English abstract).
[41]  Liu J J,Li C Y and Pen J Y.2000.Isotopic geochemistry in the copper deposits from sandstone and shale in Lanping,simao basin,western Yunnan[J].Mineral Deposits,19(3):223~234(in Chinese with English abstract).
[42]  Liu J J,Li C Y and Zhang Q Pan J Y,Liu Y P,Liu X F and Liu S R.2001.Wood cell texture from Jinman copper deposit in west Yunnan and its genesis significance[J].Science in China(Series D),32:89~95(in Chinese).
[43]  Liu J J,He M Q,Li Z M,Liu Y P,Li C Y,Zheng Q,Yang W G and Yang A P.2004.Oxygen end carbon isotopic geochemistry of Baiyangping silver-copper polymetallic ore concentration area in Lanping basin of Yunnan province and its significance[J].Mineral Deposits,23(1):1~10(in Chinese with English abstract).
[44]  Liu J L,Song Z J,Cao S Y,Zhai Y F,Wang A J,Gao L,Xiu Q Y and Cao D H.2006.The dynamic setting and processes of tectonic and magmatic evolution of the oblique collision zone between Indien and Eurasian phtes:Exemplified by the tectonic evolution of the Three River region,esstena Tibet[J].Acta Petrologiea Sinica,4:755~786(in Chinese with English abstract).
[45]  Liu Z F,Wang C S,Jin W,Yi HS,Zheng H B,Zhao X X and Li Y L.2005.Oligo-Miocene depositional environment of the Tuotuohe Basin,Central Tibetan Plateau[J].Acta Sedimentologica Sinica,3:210~217(in Chinese with English abstract).
[46]  Liu Z Q,Li X Z,Ye Q T,Luo J N and Shen G F.1993.Division of tectono-magmatic zones and the distribution of deposits in the Sanjiang Area[M].Beijing:Geol.Pub.House.246p(in Chinese with English abstract).
[47]  Luo J L,Yang Y H and Zhao Z W.1994.Evolution of the Tethys in western yunnan and mineralization for main metal deposits[M].Beijing:Geol.Pub.House.1~235(in Chinese with English abstract).
[48]  Misra K C.2000.Understanding mineral deposits[M].London:Kluwer Academic Publishers.845p.
[49]  Mo X X,Lu F X,Shen S Y,Zhu Q W and Hou Z Q.1993.Volcanism and metallogeny in the Sanjhng Tethys[M].Beijing:Geol.Pub.House.250p(in Chinese with English abstract).
[50]  Nakai S,Halliday A N,Kesler S F,Jones H D,Kyle J R and Lane T E.1990.Rb-Sr dating of sphalerites from Tennessee and the genesis of Mississippi Valley type ore deposits[J].Nature,346:354~357.
[51]  Oliver J.1986.Fluids expelled teetonically from the orogenic belts:Their role in hydrocarbon migration and other geological phenomena[J].Geology,14:99~102.
[52]  Qin G J and Zhu S Q.1991.Genetic model and prospecting prediction of Jinding Pb-Zn ore deposit[J].Journal of Yunan Geology,10:145~190(in Chinese).
[53]  Sangster D F.1990.Mississippi Valley-type and Sedax lead-zinc deposits-a comparative examination[J].Institution of Mining and Metallurgy Transactions,Section B,Applied Earth Sciences,99:21~42.
[54]  Shao Z G,Meng X G,Feng X Y and Zhu D G.2003.Tectonic characterimics of the Baiyangping-Huaehangshen ore belt,Yunnan Province and its ore-controlling effect[J].Journal of Geomechanics,9:246~253(in Chinese with English abstract).
[55]  Spurlin M S,Yin A,Horton B K,Zhou J Y and Wang J H.2005.Structural evolution of the Yushu-Nangqian region and its relationship to syncollisional igneous activity,east-central Tibet[J].GSA Bulletin,117:1293~1317.
[56]  Sverjensky D A.1984.Oil field brines as ore-forming solutions[J].Econ.Geol.,79:23~37.56Sverjensky D A.1986.Genesis of Mississippi Valley-type lead-zinc deposits[J].Annual Review of Earth and Planetary Sciences,14:177~179.
[57]  Sverjensky D A.1987.Calculation of the thermodynamic properties of aqueous species and the solubilities of minerals in supercritical electrolyte solutions[J].Review of Mineralogy,177~209.
[58]  Sverjensky D A.1989.Chemical evolution of basinal brines that formed sediment-hosted Cu-Pb-Zn deposits[J].Geol.Ass.Canada Spec.Paper.36:127~134.
[59]  廖宗廷,陈跃昆.2005.兰坪-思茅盆地原形的性质及演化[J].同济大学学报(自然科学版),33:1527~1531.
[60]  刘家军,李朝阳,潘家永,刘显凡,张乾,刘玉平.2000.兰坪,思茅盆地砂页岩中铜矿床同位素地球化学[J].矿床地质,19(3):223~234.
[61]  刘家军,李朝阳,张乾,潘家永,刘玉平,刘显凡,刘世荣.2001.滇西金满铜矿床中木质结构及其成因意义[J].中国科学(D辑),31:89~95.
[62]  Tang J X,Zhong K H,Liu Z C,Li Z J,Dong S Y and Zhang L.2006.Intracontinent orogen and matallogensis in Himalayan epoch:Changdu large compsosite,Eastern Tibet[J].Acta Sedimentologica Sinica,9:1364~1376(in Chinese with English abstract).
[63]  Tapponnier P,Lacassin R,Leloup P H,et al.1990.The Ailao Shan/Red River metamorphic belt:Tertiary left-lateral shear between Indochina and South China[J].Nature,343:431~437.
[64]  Tian H L.1997.The geological features of Baiyangping Cu-Ag polymetallic deposit,LanpingEJ].Jonrnal of Yunan Geology,16:105-108(in Chinese).
[65]  Vaasjoki M and Gulson B L.1986.Carbonate-husted base metal deposits:Lead isotope data bearing on their genesis and exploration[J].Econ.Geol.,81:156~172
[66]  Wang A J,Gao L,Liu J L,Cao D H,Xiu Q Y and Fan S J.2007.Genesis of the host brecda in the Lanping Jinding superlarge Pb-Zn deposit[J].Acta Geologica Sinica,7:891~899(in chinese with english abstact).
[67]  Wang C S,Tang J X,Gu X X and Lu Y.2001.Preliminary analysis on Himalayan tectonic-metallogenetie domain and its mineralization effect[J].Joural of Mineralogy and Petrogeology,21:146~152(in chinese with english abstact).
[68]  Wang C S,Liu Z F,Yi H S,Liu S and Zhao X X.2002.Tertiary crustal shortening and peneplanation in the Hoh Xil region:Implications for the tectonic history of the northern Tibetan phtesu[J].Journal of Asian Earth Sciences,2002:20(3):211~223.
[69]  Wang E Q and Burehfiel B C.1997.Interpretation of Cencgoic tectonics in the fight-lateral accommodation zone between the Ailao Shah shear zone and the eastern Himalayan syntaxis[J].International Geological Review,39:191~219.
[70]  Wang F and He M Y.2003.Lead and sulfur isotopic tracing of the ore forming material from the Baiyangping copper-silver polymetallic deposit in Lanping,Yunnan[J].Sedimentary Geology and Tethyan Geology,23:82~85(in Chinese with English abstract).
[71]  Wang J H,Yin A,Harrison T M,Grove M,Zhang Y Q and Xie G H.2001.A tectonic model for Cenozoic igneous activities in the eastern Indo-Asian collision zone[J].Earth and Planetary Science Letters,188:123~133.
[72]  Wei J Q.2001.S-Pb Isotopic geochemistry of copper multi-metal deposits in Hexi,Yunnan Province[J].Geology and Mineral Resouraes of South China,3:36~39(in Chinese with English abstract).
[73]  Wu N P,Jiang S Y,Liao Q L,Pan J Y and Dai B Z.2003.Lead and sulfur isotope geochemistry and the ore sources of the vein-type copper deposit in Lanping-Simao basin,Yunan Province[J].Acta Petrologica Sinica,19:799~807(in Chinese with English abstract).
[74]  Xiao R G.1989.Reservation of thermal brine with ore-forming materials and abrupt mineralization[D].Unpublished Postdoctoral Report,Guiyang:Institute of Geochemistry.Chinese Academy of Sciences.77 P(in Chinese).
[75]  Xiu Q Y,Wang A J,Cao L,Liu J L,Yu C L,Cao D H,Zhai Y F and Fan S J.2006.Discussion on the geologic time of host rocks of jinding super large deposit and its geological implications[J].Geological Survey and Research,29:293~302(in Chinese with English abstract).
[76]  Xu Q D and Li J W.2003.Migration of ore-forming fluids and its relation to zoning of mineralization in northern Lanping Cu-polymetallic area,Yunnan Province:Evidence from fluid inclusions and stable isotopesIJ].Mineral Deposits,22(4):366~376(in Chinese with English abstract).
[77]  Xu Q D and Zhou L.2004.Ore-forming fluid migration in relation to mineralization zoning in Cu-polymetallic mineralization district of northern Lanping,Yunnan:Evidence from Lead isotope and mineral chemistry of ores[J].Mineral Deposits,23:452~463(in Chinese with English abstract).
[78]  Xu X C,Xie Q Q,Lu S M,Chen T H,Huan Z and Yue S C.2005.Fluid inclusion characteristics of copper deposit on the western border of Lanpin basin,Yonnan Province[J].Acta Mineralogiea Siniea,3:170~176(in Chinese with English abstract).
[79]  Xue C J,Chen Y C,Yang J M and Wang D H.2002.Jinding Pb-Zn deposit:geology and geochemistry[J].Mineral Deposits,21:270~277(in Chinese with English abstract).
[80]  Xue C J.Liu S W and Chen Y C.2003.Geology and isotopic composition of helium,neon,xenon and metaUogenie age of the Jinding and Baiyangping ore deposits,northwest Yunnan,China[J].Science in China(series D),46:789~800(in Chinese).
[81]  Xue C J,Zeng R,Liu S W,Chi G X,Qing H R,Chen Y C,Yang J M and Wang D H.2007.Geologic,fluid inclusion and isotopic characteristics of the Jinding Zn-Pb deposit,western Yunnan,South China:A review[J].Ore Geology Reviews,31:337~359.
[82]  Yan W.1993.Study on geochemistry of a new type copper deposit[D](Dissertation for Master Degree).Guiyang:Institute of Geochemistry,Chinese Academy of Sciences.87p(in Chinese).
[83]  Yan W and Li C Y.1997.Geochemical characteristics and their hydrothermal sedimentary genesis of a new type of copper deposit[J].Geochimica,26:54~63(in Chinese with English abstract).
[84]  Yang W G,Yu X H,Li W C,Dong F L and Mo X X.2003.The characteristics of metallogenie fluids and metallogenie mechanism in Baiyangping silver and polymetallic mineralization concentration area in Yunnan Province[J].Geoscienee,17:27~33(in Chinese with English abstract).
[85]  Yi H S,Zhao X X,Lin J H,Shi Z Q,Li B H and Zhao B.2004.Magnetostratigraphic studies of Tertiary continental redbeds in Wulanwula Lake area of Northem Tibetan Plateau and thdr geologic significance[J].Acta Geosidentia Sinica,23:633~638.
[86]  Yin A and Harrison T M.2000.Geologic evolution of the HimalayanTibetan orogen[J].Annual Review of Earth and Planetary Sciences,28:211~280.
[87]  Zeng R,Xue C J,Liu S W,Gao Y B and Zhu H P.2007.REE of fluid inclusion and pre-forming fluids in the gaim Jinding Pb-Zn deposit,Yunnan[J].Geology and Prospecting.3:55~61(in Chinese with English abstract).
[88]  Zhang E X.2005.On the genesis of ore deposit in western metallogenetic zone of Baiyangping Cu-Ag polymetallic deposit concentration area,Lanping[J].Yunnan Geology,3:281~289(in Chinese with English abstract).
[89]  ghao H B.2006.Study on the characteristics and metallogenic condition of copper-polymetallic deposits in Middle-northern Lanping basin,western Yurman(Dissertation for PhD)[D].Tutor:Mo X X.Beijing:China University of Geosciences.1~123(in Chinese with English abstract).
[90]  Zhong K H,Tang J X,Liu Z C,Kou L L,Dong S Y,Li Z J and Zhou HW.2006.Mesozoic-Cenozoic intracontinental rifting of ChangduSimao tectonic zone in east margin of Qinghai-Tibet,SW China[J].Aeta Genlogica Sinica,9:1296~1311(in Chinese with English abstract).
[91]  Zhou J Y,Wang J H,Yin A,Spurlin M S and Horton B K.2002.Deposotional patterns and tectomcs setting of early tertiary basin in the NE margin of the Tibetan Plateau:A case study of the Nangqian and Xialaxiu basins[J].Acta Sedimentologica Sinica,1:85~91(in Chinese with English abstract).
[92]  陈开旭,何龙清,杨振强,魏君奇,杨爱平.2000.云南兰坪三山-白秧坪铜银多金属成矿富集区的碳氧同位素地球化学[J].华南地质与矿产,4:1~8.
[93]  陈开旭,姚书振,何龙清,杨爱平,杨伟光,黄惠兰.2004.云南兰坪白秧坪银多金属矿集区成矿流体研究[J].地质科技情报,23:45~50.
[94]  董方浏,莫宣学,侯增谦,王勇,毕先梅,周肃.2005.云南兰坪盆地喜马拉雅期碱性岩40Ar/39Ar年龄及地质意义[J].岩石矿物学杂志,24:103~109.
[95]  范世家,王安建,刘汉斌,修群业,曹殿华,李瑞萍,高辉,陈其慎.2006.论兰坪盆地白秧坪铜(钴)矿床成因的氦氩同位素证据[J].地质评论,9:628~635.
[96]  付修根,庞艳春.2004.金顶铅锌矿床地质特征及成因探讨[J].世界地质,9:239~244.
[97]  郜周全,赵庆红,童映红.2006.兰坪金满沉积.热液改造型铜矿[J].云南地质,3:341~347.
[98]  高兰,王安建,刘俊来,修群业,曹殿华,翟云峰.2005.滇西北兰坪金顶床矿超大型矿床研究新进展:浸位角砾岩的发现及其地质意义[J].矿床地质,24(4):457-461.
[99]  龚文君,谭凯旋,李小明,龚革联.2000.兰坪白秧坪铜银多金属矿床流体地球化学特征及成矿机制探讨[J].大地构造与成矿学,24(2):175-180.
[100]  何龙清,陈开旭,余凤鸣,魏君奇.2004.云南兰坪盆地推覆构造及其控矿作用[J].地质与勘探,40(4):7~12.
[101]  何明勤,刘家军,李朝阳,李志明,刘玉平.2004.兰坪盆地铅锌铜大型矿集区的流体成矿作用机制--以白秧坪铜钴多金属地区为例[M].北京:地质出版社.
[102]  侯增谦,潘桂棠,王安建,莫宣学,田世洪,孙晓明,丁林,王二七,高永丰,谢玉玲,曾酱胜,秦克章,许继峰,曲晓明,杨志明,杨竹森,费红彩,孟详金,李振清.2006a.青藏高原碰撞造山带:Ⅱ.晚碰撞转换成矿作用[J].矿床地质,25(5):521~533.
[103]  侯增谦,杨竹森,徐文艺,莫宣学,丁林,高永丰,董方浏,李光明,曲晓明,赵志丹,江思宏,孟祥金,李振清,秦克章,杨志明.2006b.青藏高原碰撞造山带:Ⅰ.主碰撞造山成矿作用[J].矿床地质,25(4):337~358.
[104]  季宏兵,李朝阳.1998.滇西金满铜矿床成矿流体地球化学特征及来源[J].矿物学报,3:28~37.
[105]  李峰,黄敦义,甫为民.1995.兰坪.思茅盆地红层铜矿成矿规律[J].大地构造与成矿学,12:322~335.
[106]  李兴振,刘文举,王义昭,朱勤文.1999.西南"三江"特提斯构造演化与成矿[M].北京:地质出版社.1~258.
[107]  李亚林,王成善,伊海生,刘志飞,李勇.2006.西藏北部新生代大型逆冲推覆构造与唐古拉山的隆起[J].地质学报,80:1118~1130.
[108]  李佑国,侯中健,王安建,唐菊兴,刘俊来,薛春纪,修群业.2006.兰坪盆地新生代碎屑岩地球化学特征及其对物源约束[J].岩石学报,22(3):751-760.
[109]  李志明,刘家军,秦建中,廖宗廷,张长江.2004.滇西兰坪盆地多金属矿床碳、氧、氢同位素组成及其地质意义[J].吉林大学学报(地球科学版),34:360~366.
[110]  李志明,刘家军,秦建中,廖宗廷,何明勤,刘玉平.2005.兰坪盆地白秧坪铜钴银多金属矿床成矿物资来源研究[J].地质与勘探,1:1~6.
[111]  刘家军,何明勤,李志明,刘玉平,李朝阳,张乾,杨伟光,杨爱平.2004.云南白秧坪银铜多金属矿集区碳氧同位素组成及其意义[J].矿床地质,23(1):1~10.
[112]  刘俊来,宋志杰,曹淑云,翟云峰,王安建,高兰,修群业,曹殿华.2006.印度-欧亚侧向碰撞带构造-岩浆演化的动力学背景与过程-以藏东三江地区构造演化为例[J].岩石学报,22:775~786.
[113]  刘增乾,李兴振,叶庆同,罗建宁,沈敢富,杨岳清.1993.三江地区构造岩浆带的划分与矿产分布规律[M].北京:地质出版社.1~243.
[114]  刘志飞,王成善,金巍,伊海生,郑洪波,赵西西,李亚林.2005.青藏高原沱沱河盆地渐新世-中新世沉积环境分析[J].沉积学报,23:210~217.
[115]  罗君烈,杨友华,赵准,陈吉琛,杨荆舟.1994.滇西特提斯的演化及主要金属矿床成矿作用[M].北京:地质出版社.1~235.
[116]  莫宣学,路凤香,沈上越,朱勤文,侯增谦.1993.三江特提斯火山作用与成矿[M].北京:地质出版社.1~267.
[117]  邵兆刚,孟宪刚,冯向阳,朱大岗.2003.云南白秧坪-华昌山矿带构造特征及其控矿作用[J].地质力学学报,9:246~253.
[118]  唐菊兴,钟康惠,刘肇昌,李志军,董树义,张丽.2006.藏东缘昌都大型复合盆地喜马拉雅期陆内造山与成矿作用[J].沉积学报,9:1364.~1376.
[119]  田洪亮.1997.兰坪白秧坪铜银多金属矿床地质特征[J].云南地质,16(1):105~108.
[120]  王安建,高兰,刘俊来,曹殿华,修群业.范世家.2007.论兰坪金顶超大型铅锌矿容矿角砾岩的成因[J].地质学报,7:891~899.
[121]  王成善,唐菊兴,顾雪祥,陆彦.2001.喜马拉雅构造-成矿域及其成矿效应初步分析[J].矿物岩石,21(3):146~152.
[122]  王峰,金景福.2003.云南南角河银多金属矿床同位素地球化学研究[J].沉积与特提斯地质,2:95~98.
[123]  魏君奇.2001.云南河西铜多金属矿S-Pb同位素地球化学[J].华南地质与矿产,3:36~39.
[124]  吴南坪,蒋少涌,廖启林,潘家永,戴宝章.2003.云南兰坪~思茅盆地脉状铜矿床铅、硫同位素地球化学与成矿物质来源研究[J].岩石学报,19(4):799~795.
[125]  肖荣阁.1989.含矿热卤水储备与突发成矿作用[D].贵阳:中国科学院地球化学研究所.
[126]  修群业,王安建,高兰,刘俊来,于春林,曹殿华,范世家,翟云峰.2006.金顶超大型矿床容矿围岩时代探讨及地质意义[J].地质调查与研究,12:298~302.
[127]  徐启东,李建威.2003.云南兰坪北部多金属矿化区区域流体流动与矿化分带--流体包裹体与稳定同位素依据[J].矿床地质,22(4):365-376.
[128]  徐启东,周炼.2004.云南兰坪北部铜多金属矿化区成矿流体流动与矿化分带-矿石铅同位素和特征元素组成依据[J].矿床地质,23(4):452~461
[129]  徐晓春,谢巧勤,陆三明,陈天虎,黄震,岳书仓.2005.滇西兰坪盆地西缘铜矿床矿物流体包裹体研究[J].矿物学报,6:170~176.
[130]  薛春纪,陈毓川,杨建明,王登红,杨伟光,杨清标.2002滇西兰坪盆地构造体制和成矿背景分析[J].矿床地质,21(1):36~43.
[131]  薛春纪,陈毓川,王登红,杨建民,杨伟光,曾荣.2003.滇西北金顶和白秧坪矿床:地质和He,Ne,Xe同位素组成及成矿时代[J].中国科学,33:316~322.
[132]  颜文,李朝阳.1997.一种新类型铜矿床的地球化学特征及其热水沉积成因[J].地球化学,26(10):54~63.
[133]  杨伟光,喻学惠,李文昌,董方浏,莫宣学.2003.云南白秧坪银多金属矿集区成矿流体特征及成矿机制[J].现代地质,17:27~33.
[134]  伊海生,赵西西,林金辉,时志强,李保华,赵兵.2004.藏北乌兰乌拉湖地区第三纪陆相红层古地磁研究的初步结果及地质意义[J].地球学报,23:633~638.
[135]  曾荣,薛春纪,刘淑文,高永宝,朱和平.2007.云南金顶铅锌矿成矿流体与流体的稀土元素研究[J].地质与勘探,3:55~61.
[136]  张尔新.2005.兰坪白秧坪铜银多金属矿集区西矿带矿床成因[J].云南地质,3:282~289.
[137]  赵海滨.2006.滇西兰坪盆地中北部铜多金属矿床成矿特征及地质条件[D].北京:中国地质大学博士论文.1~123.
[138]  钟康惠,唐菊兴,刘肇昌,寇林林,董树义,李志军,周慧文.2006.青藏东缘昌都-思茅构造带中新生代陆内裂谷作用[J].地质学报,9:1296~1311.
[139]  周江羽,王江海,尹安,Spurlin M S,Horton B K.2002.青藏东北缘早第三纪盆地充填的沉积型式及构造背景-以囊谦和下拉秀盆地为例[J].沉积学报,1:85~91.

Full-Text

Contact Us

service@oalib.com

QQ:3279437679

WhatsApp +8615387084133