沙坪沟钼矿区橄榄角闪石岩岩石成因——矿物学特征约束
|
摘要
对位于秦岭-大别造山带的沙坪沟钼矿矿区出露的橄榄角闪石岩开展了系统的岩石学、岩相学及电子探针原位分析,厘定了其成岩物理化学条件,并探讨了岩石成因及形成的构造环境。橄榄角闪石岩主要造岩矿物为橄榄石、角闪石、金云母和辉石;副矿物为磷灰石、铬铁尖晶石、镁铁尖晶石、磁铁矿、磁黄铁矿、镍黄铁矿等。电子探针原位分析结果显示,橄榄石属于贵橄榄石系列,角闪石主要是韭闪石,辉石为透辉石,云母为金云母。造岩矿物结晶顺序为橄榄石-辉石-角闪石,结晶温度介于1 111. 64～1 223. 30℃之间,形成压力为350～740 MPa,形成于较高的氧逸度环境(角闪石结晶时的氧逸度范围为NNO+0. 59～NNO+2. 27)。角闪石和金云母的矿物学特征显示它们均是与幔源岩浆作用相关的原生矿物,表明该套基性-超基性岩与幔源岩浆作用有关。综合分析认为,在大别造山带中生代地壳减薄的伸展构造背景下,该橄榄角闪石岩母岩浆源于地幔,是经过地幔7. 92%部分熔融的玄武质岩浆经结晶分异作用形成的幔源岩浆底侵下地壳的产物。
The Shapinggou molybdenum deposit is the second largest porphyry molybdenum deposit in the world.The mafic-ultramafic rock widely exposed in the area of Shapinggou molybdenum ore deposit is an important medium to reveal the deep information of the deposit.In this paper,the olivine-bearing amphibolite outcropped in the mining area were studied based on petrology,petrography and in situ analysis so as to clarify physicochemical conditions of diagenesis and discuss the petrogenesis and tectonic setting.The main rock-forming minerals contain olivine,amphibole,phlogopite and pyroxene,and the accessory minerals are apatite,chromium-iron spinel,mafic spinel,magnetite,pyrrhotite and pentlandite.The results of in-situ analysis of EPMA show that olivine belongs to the chrysolite series,amphibole is parasite,pyroxene is diopside and mica is phlogopite.The order of crystallization is olivine-pyroxene-amphibole,the temperature ranges from 1 111.64 to 1 223.30℃ and the formation pressure ranges from 350 to 740 MPa,with high oxygen fugacity(the oxygen fugacity varies from NNO + 0.59 to NNO+ 2.27).The mineralogical characteristics of phlogopite and amphibole indicate that phlogopite was related to mantle-derived magmatism.The study shows that the parent magma of olivine-bearing amphibolite originated from the mantle and was formed through crystallization differentiation of basalt magma which was partially melted by 7.92% of the mantle.The olivine-bearing amphibolite outcropped in the north of Shapinggou mining area should be the product of partial melting of mantle-derived magma under the extensional tectonic background.
The Shapinggou molybdenum deposit is the second largest porphyry molybdenum deposit in the world.The mafic-ultramafic rock widely exposed in the area of Shapinggou molybdenum ore deposit is an important medium to reveal the deep information of the deposit.In this paper,the olivine-bearing amphibolite outcropped in the mining area were studied based on petrology,petrography and in situ analysis so as to clarify physicochemical conditions of diagenesis and discuss the petrogenesis and tectonic setting.The main rock-forming minerals contain olivine,amphibole,phlogopite and pyroxene,and the accessory minerals are apatite,chromium-iron spinel,mafic spinel,magnetite,pyrrhotite and pentlandite.The results of in-situ analysis of EPMA show that olivine belongs to the chrysolite series,amphibole is parasite,pyroxene is diopside and mica is phlogopite.The order of crystallization is olivine-pyroxene-amphibole,the temperature ranges from 1 111.64 to 1 223.30℃ and the formation pressure ranges from 350 to 740 MPa,with high oxygen fugacity(the oxygen fugacity varies from NNO + 0.59 to NNO+ 2.27).The mineralogical characteristics of phlogopite and amphibole indicate that phlogopite was related to mantle-derived magmatism.The study shows that the parent magma of olivine-bearing amphibolite originated from the mantle and was formed through crystallization differentiation of basalt magma which was partially melted by 7.92% of the mantle.The olivine-bearing amphibolite outcropped in the north of Shapinggou mining area should be the product of partial melting of mantle-derived magma under the extensional tectonic background.
引文
Audétat A.2010.Source and evolution of molybdenum in the porphyry Mo(-Pb)deposit at Cave Peak,Texas[J].Journal of Petrology,51(8):1 739~1 760.
Candela P A.1989.Felsic magmas,volatiles,and metallogenesis[J].Reviews in Economic Geology,4:223~233.
Carten R B,White W H and Stein H J.1993.High-grade granite-related molybdenum systems classification and origin.Mineral Deposit Modeling[J].Geological Association of Canada Special Paper,40:521~554.
Cong B L.1996.Ultrahigh-pressure metamorphic rocks in the Dabie-Sulu region of China[J].Beijing:Science Press,China and Kluwer Acad Pub,Dordrecht,224~228.
Chen Hongjin,Chen Yanjing,Zhang Jing,et al.2013.Zircon U-Pb ages and Hf isotope characteristics of the ore-bearing intrusion from the Shapinggou molybdenum deposit,Jinzhai County,Anhui Province[J].Acta Petrologica Sinica,29(1):132~145(in Chinese with English abstract).
Chen Y J,Li C,Zhang J,et al.2000.Sr and O isotopic characteristics of porphyries in the Qinling molybdenum deposit belt and their implication to genetic mechanism and type[J].Science in China(Series D:Earth Sciences),43:82~94.
Chen Yuezhi and Sang Baoliang.1995.Metamorphic petrology and metamorphism of the foziling group in northern Huaiyang and its age[J].Regional Geology of China,14(3):280~288(in Chinese with English abstract).
Chiara G,Franco R,Yican Liu,et al.2014.P-T evolution of elusive UHP eclogites from the Luotian dome(North Dabie Zone,China):How far can the thermodynamic modeling lead us?[J].Lithos,226(6):183~200.
Dai Shengqian,Xu Jiacong,Shi Qianhua,et al.1992.New recognition of the foziling group in the eastern part of northern Huaiyang[J].Regional Geology of China,11(4):369~375(in Chinese with English abstract).
Deng Jinfu.1983.Melt-mineral Equilibrium Thermodynamics[M].Beijing:Geological Publishing House,74~92(in Chinese).
Deng Jinfu,Dai Shengqian,Wu Zongxu,et al.2000.Petrological structure and thermal structure of the Dabie orogenic belt and its geological implications[J].Acta Geologica Sinica,74(3):207~215(in Chinese with English abstract).
Du Jianguo.2000.On Researching of Mesozoic Magmatism and Geochemsitry of Mineralization in Dabie Orogenic belt[D].Hefei:Hefei University of Technology,14~36(in Chinese with English abstract).
Feng Hongye,Xu Yingxia,Tang Dongmei,et al.2014.Mineralogical characteristics of olivine and spinel from Getashankou Cu-Ni-bearing maficultramaficintrusions in eastern Tianshan,NW China[J].Geology and Exploration,50(2):346~359(in Chinese with Englishabstract).
Foster M D.1960.Interpretation of the Composition of Trioctahedral Micas[M].Washington:Mineral Society of America,11~49.
Gao Y,Mao J W and Ye H S.2015.A review of the geological characteristics and geodynamic setting of the late Ealy cretaceous molybdenum deposits in the East Qinling-Dabie Molybdenum belt,East China[J].Joural of Asia Eath Science,108:81~96.
Hacker B R,Ratschbacher L,Webb L,et al.2000.Exhumation of ultrahigh-pressure continental crust in east central China:Late TriassicEarly Jurassic tectonic unroofing[J].Journal of Geophysical Research,OS(B6):13 339~13 364.
Hammarstrom J M and Zen E A.1986.Aluminum in hornblende:An empirical igneousgeobarometer[J].American Mineralogist,71:1 297~1 313.
He Yongsheng.2011.Geochemistry of Post-collisional Granitic Magmatism from the Dabie Orogen:Constraints on Removal Processes and Architecture of the Mountain Root[D].Hefei:University of Science and Technology of China(in Chinese with English abstract).
Hollister L S,Grissom G C,Peters E K,et al.1987.Confirmation of the empirical correlation of al in hornblende with pressure of solidification of calc-alkaline plutons[J].American Mineralogist,72:231~239.
Hong Dawei,Wang Tao,Tong Ying,et al.2003.Mesozoic granitoids from North China Block and Qingling-Dabie-Sulu orogenic belt and their deep dynamic process[J].Earth Science Frontiers,10(3):231~256(in Chinese with English abstract).
Huang Fan,Wang Denghong,Lu Sanming,et al.2011.Molybdenite ReOs isotopic age of Shapinggou Mo deposit in Anhui Province and Mesozoic Mo ore-forming stages in East Qinling-Dabie Mountain region[J].Mineral Deposits,30(6):1 040~1 057(in Chinese with English abstract).
Irvine T N.1977.Origin of chromitite layers in the Muskox intrusion and other strtiform intrusions:A new interpretation[J].Geology,5:273~277.
Jiang Changyi and An Sanyuan.1984.On chemical characteristics ofcalcic amphiboles from igneous rocsk and their petrogenesissignificance[J].Journal of Mineralogy and Petrology,4(3):1~9(in Chinese with English abstract).
Jiang Laili,Liu Yican,Wu Weiping,et al.1999.The deformation history and exhumation process of the UHPM rocks in the Dabieshan[J].Scientia Geologica Sinica,34(4):432~441(in Chinese with English abstract).
Kay S M,Snedden W T,Foster B P,et al.1983.Upper mantle and crustal fragments in the Ithaca kimberlites[J].Journal of Geology,91(3):277~290.
Keith J D,Christiansen E H and Carten R B.1993.The genesis of giant porphyry molybdenum deposits[J].Giant Ore Deposits,Society of Economic Geologists Special Publication,2:285~316.
Leake B E.1997.Nomenclature of amphiboles:Report of the Subcommittee on Amphibole of the International Mineralogical Association,Commission on new minerals and mineral names[J].Amer.Mineral.,82:1 019~1 037.
Leterrier J,Maury R C,Thonon P,et al.1982.Clinopyroxene composition as a method of identification of the magmatic affinities of paleovolcanic series[J].Earth&Planetary Science Letters,59(1):139~154.
Li Junping,Li Yongfeng,Luo Zhengchuan,et al.2011.Geological features of molybdenum deposits and ore prospecting in northern slope of the Dabie Mountain,China[J].Geotectonica et Metallogenia,4(3):457~468(in Chinese with English abstract).
Li Nuo,Chen Yanjing,Zhang Hui,et al.2007.Molybdenum deposits in East Qinling[J].Earth Science Frontiers,14(5):186~198(in Chinese with English abstract).
Li Shuguang.2004.Exhumation mechanism of the ultrahigh-pressure metamorphic rocks in the Dabie Mountains and continental collision process between the North and South China blocks[J].Earth Science Frontiers,11(3):63~70(in Chinese with English abstract).
Li Shuguang,He Yongsheng,Wang Shuitong,et al.2013.Process and mechanism of mountain-root removal of the Dabie Orogen:Constraints from geochronology and geochemistry of post-collisional igneous rocks[J].China Sci.Bull.,58(23):2 316~2 322(in Chinese with English abstract).
Li Yi,Li Nuo,Yang Yongfei et al.2013.Geological features and geodynamic settings of the Mo deposits in the northern segment of the Dabie Mountains[J].Acta Petrologica Sinica,29(1):95~106(in Chinese with English abstract).
Liu Fei,Yang Jingsui,Chen Songyong,et al.2013.Geochemistry and Sr-Nd-Pb isotopic composition of mafic rocks in the western part of Yarlung Zangbo suture zone:Evidence for intra-oceanic supra-subduction within the Neo-Tethys[J].Geology in China,40(3):742~755(in Chinese with English abstract).
Lu Fengxiang,Shang Longkang,Wu Jinhua,et al.2001.Petrology[M].Beijing:Geological Publishing House,1~338(in Chinese).
Luan Y,Song X Y,Chen L M,et al.2014.Key factors controlling the accumulation of the Fe-Ti oxides in the Hongge layered intrusion in the Emeishan Large Igneous Province,SW China[J].Ore Geol.Rev.,57:518~538.
Ma Hongwen.1985.A formular about modified geothermograph of clinopyroxene[J].Geological Science and Technology Information,4(2):82~84(in Chinese).
Mao J W,Pirajno F and Xiang J F.2011.Mesozoic molybdenum deposits in the East Qinling-Dabie Orogenic belt:Characteristics and tectonic settines[J].Ore Geoloev Reviews,43:264~293.
Meng Xiangjin,Xu Wenyi,LüQingtian,et al.2012.Zircon U-Pb dating of ore-bearing rocks and molybdenite Re-Os age in Shapinggou porphyry molybdenum deposit,Anhui Province[J].Acta Geologica Sinica,86(3):487~494(in Chinese with English abstract).
Ni Zhiyao.1991.Chemical composition and petrologic significance of olivines in Huangshandong mafic-ultramafic complex in Hami,Xinjiang,China[J].Mineralogy and Petrology,11(3):40~47(in Chinese with English abstract).
Ni Pei,Wang Guoguang,Wen Yu,et al.2005.Evidence of fluid inclusions for two stages of fluid boiling in the formation of the giant Shapinggou porphyry Mo deposit,Dabie Orogen,Central China[J].Ore Geology Reviews,65(3):1 078~1 094.
Niu Yaoling,Charles H L,Rosamond J,et al.1997.The origin of abyssal peridoties a new perspective[J].Earth and Planetary Science Letters,152(4):251~265.
Peng Zhi,Du Jianguo,Chen Fang,et al.2015.Geochemical characteristics and LA-ICP-Ms zircon U-Pb geochronology of the Tongxingsi alkaline intrusion in the Eastern North Huaiyang and their geological significance[J].Acta Geologica Sinica,89(4):701~714(in Chinese with English abstract).
Powell R H T and Worley B.1998.Calculating phase diagrams involving solid solutions via non-linear equations,with examples using THER-MOCALC[J].Metamorphic Geol.,16(4):577~588.
Qiu Jiaxiang and Liao Qun’an.1987.The main characteristics and genetic information of clinopyroxene megaecrysts in Cenozoic basalt of Eastern China[J].Acta Petrologica et Mineralogica,6(1):53~63(in Chinese with English abstract).
Qiu Jiaxiang and Lin Jingqian.1991.Lithochemistry[M].Beijing:Geological Publishing House,140~156(in Chinese).
Ratschbacher L,Harcker B R,Webb L E,et al.2000.Exhumation of the ultrahigh-pressure continental crust in east central China:Cretaceous and Cenozoic unroofing and the Tan-Lu fault[J].Journal of Geophysical Research,105(B6):13 303~13 338.
Ren Zhi,Zhou Taofa,Pete Hollings,et al.2018.Magmatism in the Shapinggou district of the Dabie Orogen,China:Implications for the formation of porphyry Mo deposits in a collisional orogenic belt[J].Lithos,308~309:346~363.
Ren Zhi,Zhou Taofa,Zhang Dayu,et al.2015.Characteristics of alteration and mineralization of Shapinggou porphyry molybdenum deposit,Dabie orogenic belt[J].Acta Petrologica Sinica,31(9):2 708~2 723(in Chinese with English abstract).
Richards J.2003.Tectono-magmatic precursors for porphyry Cu-(MoAu)deposit formation[J].Econ.Geol.,98(8):1 515~1 533.
Ridolfi F,Renzulli A and Puerini M.2010.Stability and chemical equilibrium of amphibole in calc-alkaline magmas:An overview,new thermobarometric formulations and application to subduction-re-lated volcanoes[J].Contributions to Mineralogy and Petrology,160(1):45~66.
Roeder P L and Emslie R F.1970.Olivine-liquid equilibrium[J].Contribu-tions to Mineralogy and Petrology,29:275~289.
Sato H.1977.Nickel content of basaltic magmas:Identification of primary magma and a measure of the degree of olivine fractionation[J].Lithos,10(4):113~120.
Schmidt M W.1992.Amphibole composition in tonalite as a function of pressure:An experimental calibration of the Al-in-hornblende barometer[J].Contributions to Mineralogy&Petrology,110:304~310.
Sinclair W.2007.Mineral deposits of Canada:A synthesis of major deposit-types,district metallogeny,the evolution of geological provinces,and exploration methods[J].Geological Association of Canada,Mineral Deposits Division,Special Publication,5(1):223~243.
Stein H J and Hannah J L.1985.Movement and origin of ore fluids in Climax-type systems[J].Geology,13(7):469~474.
Tan Hongyan,Shu Guanglong,LüJunchao,et al.2012.LA-ICP-MS zircon U-Pb and molybdenite Re-Os dating for the Luming large-scale molybdenum deposit in Xiao Hinggan mountains and its geological implication[J].Journal of Jilin University(Earth Science Edition),42(6):1 758~1 764(in Chinese with English abstract).
Thompson A B,Aerts M and Hack A C.2007.Liquid immiscibility in silicate melts and related systems[J].Reviews in Mineralogy and Geochemistry,65:99~127.
Wallace S R,Mac Kenzie W B,Blair R G,et al.1978.Geology of the Urad and Henderson molybdenite deposits,Clear Creek County,Colorado,with a section on a comparison of these deposits with those at Climax,Colorado[J].Economic Geology,73(3):325~368.
Wang Bohua,Wu Zongling,Zhang Huaidong,et al.2007.Geological and geochemical features of Mesozoic igneous rocks in the Yinsha area,Jinzhai Anhui Province,and the implications[J].Geology of Anhui,17(4):245~248(in Chinese with English abstract).
Wang Ping.2013.The Characteristics and Genesis of Magmatic Rocks in Shapinggou Molybdenum Ore Disdrict,Jinzhai,Anhui[D].Hefei:Hefei University of Technology(in Chinese with English abstract).
Wang Qingchen and Lin Wei.2002.Geodynamics of the Dabieshan collisional orogenic belt[J].Earth Science Frontiers,9(4):257~265(in Chinese with English abstract).
Wang Yun,Chen Yanjing,Ma Hongwei,et al.2009.Study On ore geology and fluid inclusion of the Tangjiaping Mo deposit,Shangcheng County,Henan Province[J].Acta Petrologica Sinica,25(2):469~480(in Chinese with English abstract).
Westra G and Keith S B.1981.Classification and genesis of stockwork molybdenum deposits[J].Economic Geology,76(4):844~873.
Wones D R and Eugster H P.1965.Stability of biotite:Experiment,theory,and application[J].Am.Miner.,50(9):1 228~1 272.
Xie Caifu,Xiong Chengyun,Hu Ning,et al.2001.A study on regional metallogenic regularity of the East Qinling-Dable orogenic belt[J].Geology and M ineral Resources of South China,17(3):15~21(in Chinese with English abstract).
Xie Yuling,Li Lamei,Guo Xiang,et al.2015.Chronology,petrochemistry of fine grained granite and their implication to Mo-Cu mineralization in Xichong Mo deposit,Anhui Province,China[J].Acta Petrologica Sinica,31(7):1 929~1 942(in Chinese with English abstract).
Xu Gang,Tang Zhongli,Jiao Jiangang,et al.2012.The comparative study on small intrusion type molybdenum deposits of Shapinggou and Jinduicheng[J].Northwestern Geology,45(4):359~369(in Chinese with English abstract).
Xu Xiangzhen,Yang Jingsui,Guo Guolin,et al.2011.Lithological research on the Purang mantle peridotite in western Yarlung Zangbo suture zone in Tibet[J].Acta Petrologica Sinica,27(11):3 179~3 196(in Chinese with English abstract).
Xu Xiaochun,Lou Jinwei,Lu Sanming,et al.2009.Re-Os ages of molybdenum-lead-zinc polymetallic deposits and40Ar-39Ar ages of related magmatic rocks in Yinshan area,Jinzhai,Anhui Province[J].Mineral Deposits,28(5):621~632(in Chinese with English abstract).
Xu Yigang.1993.Geothermometers applicable to the mantle xenoliths[J].Acta Petrologica Sinica,9(2):167~180(in Chinese with English abstract).
Xue Junzhi,Bai Xuerang and Chen Wu.1986.Genetic Mineralogy[M].Wuhan:China University of Geosciences Press,114~121(in Chinese).
Yang Shan,Wang Bohua,Wang Feng,et al.2013.The occurrence of niobium in Shapinggou molybdenum deposits,Jinzhai County,Anhui Province[J].Rock And Mineral Analysis,32(2):269~277(in Chinese with English abstract).
Yang Yanchen,Han Shijiong,Sun Deyou,et al.2012.Geological and geochemical features and geochronology of porphyry molybdenum deposits in the Lesser Xing’an Range-Zhangguangcai Range metallogenic belt[J].Acta Petrologica Sinica,28(2):379~390(in Chinese with English abstract).
Yang Zeqiang.2007.Re-Os isotopic ages of Tangjiaping molybdenum deposit in Shangcheng County,Henan and their geological significance[J].Mineral Deposits,26(3):289~295(in Chinese with English abstract).
Yu Wen,Ni Pei,Wang Guoguang,et al.2013.Evolution of ore-forming fluids of the Shapinggou porphyry molybdenum[J].Journal of Nanjing University(Natural Sciences),48(3):241~255(in Chinese with English abstract).
Zhang Zhaochong and Wang Fusheng.2003.A method for identifying primary magma-Examples from pickite and alkali basalts[J].Journal of Jilin University(Earth Science Edition),33(2):130~134(in Chinese with English abstract).
Zhao Zifu and Zheng Yongfei.2009.Remelting of subducted continental lithosphere:Petrogenesis of Mesozoic magmatic rocks in the DabieSulu orogenic belt[J].Sci.China Ser.D-Earth Sci.,39(7):888~909(in Chinese with English abstract).
Zhang Hong,Sun Weidong,Yang Xiaoyong,et al,2011.Geochronology and Metallogenesis of the Shapinggou Giant Porphyry Molbdenum Deposit in the Dabie Orogenic Belt[J].Acta Geologica Sinica,85(12):2 040~2 059(in Chinese with English abstract).
Zhang Huaidong,Wang Bohua,Hao Yuejin,et al.2012.Geological characteristics and comprehensive ore-prospecting information of Shapinggou porphyry-type molybdenum deposit in Anhui Province[J].Mineral Deposits,31(1):41~51(in Chinese with English abstract).
Zheng Yongfei,Xu Zheng,Zhao Zifu,et al.2018.Mesozoic mafic magmatism in North China:Implications for thinning and destruction of cratonic lithosphere[J].Science China:Earth Sciences,48(4):379~414(in Chinese with English abstract).
Zhou Zuoxia.1986.The origin of intrusive mass in Fengshandong,Hubei Province[J].Acta Petrotogica Sinica,2(1):59~70(in Chinese with English abstract).
Zhou Zuoxia.1988.Chemical characteristics of mafic mica in intrusive rocks and its geological meaning[J].Acta Petrotogica Sinica,4(3):63~73(in Chinese with English abstract).
Zhou Zuoxia.1991.Application of Mg-Fe mica chemical composition,rare elements,REE,Cu,Cl,F to distinguishing petrogenetic types[A].Wu Liren and Li Bingglun.Two Great Mesozoic Types of Porphyry Ore Deposits in the East of China[C].Beijing:Science Press,76~82(in Chinese).
陈红瑾,陈衍景,张静,等.2013.安徽省金寨县沙坪沟钼矿含矿岩体锆石U-Pb年龄和Hf同位素特征及其地质意义[J].岩石学报,29(1):132~145.
陈跃志,桑宝梁.1995.佛子岭群变质岩石学变质作用及时代的初步研究[J].中国区域地质,14(3):280~288.
邓晋福.1983.熔浆-矿物平衡热力学[M].北京:地质出版社,74~92.
邓晋福,戴圣潜,吴宗絮,等.2000.大别造山带岩石学结构和热结构及其地质意义[J].地质学报,74(3):207~215.
戴圣潜,徐家聪,石乾华,等.1992.北淮阳东段佛子岭群新认识[J].中国区域地质,11(4):369~375.
杜建国.2000.大别造山带中生代岩浆作用与成矿地球化学研究[D].合肥:合肥工业大学,14~36.
冯宏业,许英霞,唐冬梅,等.2014.东天山圪塔山口铜镍矿区镁铁-超镁铁质岩体橄榄石与尖晶石矿物学特征[J].地质与勘探,50(2):346~359.
何永胜.2011.大别造山带碰撞后花岗质岩浆作用地球化学:对去山根过程及山根结构的制约[D].合肥:中国科学技术大学.
洪大卫,王涛,童英,等.2003.华北地台和秦岭-大别-苏鲁造山带的中生代花岗岩与深部地球动力学过程[J].地学前缘,10(3):231~256.
黄凡,王登红,陆三明,等.2011.安徽省金寨县沙坪沟钼矿辉钼矿Re-Os年龄-兼论东秦岭-大别山中生代钼成矿作用期次划分[J].矿床地质,30(6):1 040~1 057.
姜常义,安三元.1984.论火成岩中钙质角闪石的化学组成特征及其岩石学意义[J].矿物岩石,4(3):1~9.
江来利,刘贻灿,吴维平,等.1999.大别山超高压变质岩的变形历史及折返过程[J].地质科学,34(4):432~441.
李俊平,李永峰,罗正传,等.2011.大别山北麓钼矿找矿重大进展及其矿床地质特征研究[J].大地构造与成矿学,4(3):457~468.
李诺,陈衍景,张辉,等.2007.东秦岭斑岩钼矿带的地质特征和成矿构造背景[J].地学前缘,14(5):186~198.
李曙光.2004.大别山超高压变质岩折返机制与华北-华南陆块碰撞过程[J].地学前缘,11(3):63~70.
李曙光,何永胜,王水炯.2013.大别造山带的去山根过程与机制:碰撞后岩浆岩的年代学和地球化学制约[J].科学通报,58(23):2 316~2 322.
李毅,李诺,杨永飞,等.2013.大别山北麓钼矿床地质特征和地球动力学背景[J].岩石学报,29(1):95~106.
刘飞,杨经绥,陈松永,等.2013.雅鲁藏布江缝合带西段基性岩地球化学和Sr-Nd-Pb同位素特征:新特提斯洋内俯冲的证据[J].中国地质,40(3):742~755.
路凤香,桑隆康,邬金华,等.2001.岩石学[M].北京:地质出版社,1~338.
马鸿文.1985.介绍改进的单斜辉石地质温度计公式[J].地质科技情报,4(2):82~84.
孟祥金,徐文艺,吕庆田,等.2012.安徽沙坪沟斑岩钼矿锆石U-Pb和辉钼矿Re-Os年龄[J].地质学报,86(3):487~494.
倪志耀.1991.新疆哈密黄山东镁铁-超镁铁杂岩体中橄榄石的化学成分及其岩石学意义[J].矿物岩石,11(3):40~47.
彭智,杜建国,陈芳,等.2015.北淮阳东段同兴寺碱性岩体地球化学特征、LA-ICP-MS锆石U-Pb年龄及其地质意义[J].地质学报,89(4):701~714.
邱家骧,廖群安.1987.中国东部新生代玄武岩中单斜辉石巨晶的主要特征及成因信息[J].岩石矿物学杂志,6(1):56~63.
邱家骧,林景仟.1991.岩石化学[M].北京:地质出版社,140~156.
任志,周涛发,张达玉,等.2015.大别山地区沙坪沟斑岩型钼矿床蚀变及矿化特征研究[J].岩石学报,31(9):2 708~2 723.
谭红艳,舒广龙,吕骏超,等.2012.小兴安岭鹿鸣大型钼矿LA-ICP-MS锆石U-Pb和辉钼矿Re-Os年龄及其地质意义[J].吉林大学学报(地球科学版),42(6):1 758~1 764.
王波华,邬宗玲,张怀东,等.2007.安徽省金寨银沙地区中生代岩浆岩地质地球化学特征及其找矿意义[J].安徽地质,17(4):245~248.
王萍.2013.安徽金寨沙坪沟钼矿区岩浆岩特征及成因[D].合肥:合肥工业大学.
王清晨,林伟.2002.大别山碰撞造山带的地球动力学[J].地学前缘,9(4):257~265.
王运,陈衍景,马宏卫,等.2009.河南省商城县汤家坪钼床地质和流体包裹体研究[J].岩石学报,25(2):469~480.
谢才富,熊成云,胡宁,等.2001.东秦岭-大别造山带区域成矿规律研究[J].华南地质和矿产,17(3):15~21.
谢玉玲,李腊梅,郭翔,等.2015.安徽西冲钼矿床细粒花岗岩的岩石定年、岩石化学及与成矿的关系研究[J].岩石学报,31(7):1 929~1 942.
徐刚,汤中立,焦建刚,等.2012.金堆城与沙坪沟小岩体型斑岩钼矿床对比研究[J].西北地质,45(4):359~369.
徐向珍,杨经绥,郭国林,等.2011.雅鲁藏布江缝合带西段普兰蛇绿岩中地幔橄榄岩的岩石学研究[J].岩石学报,27(11):3 179~3 196.
徐义刚.1993.适用于幔源包体的地质温度计[J].岩石学报,9(2):167~180.
徐晓春,楼金伟,陆三明,等.2009.安徽金寨银山钼-铅-锌多金属矿床Re-Os和有关岩浆岩40Ar-39Ar年龄测定[J].矿床地质,28(5):621~632.
薛君治,白学让,陈武.1986.成因矿物学[M].武汉:中国地质大学出版社,114~121.
阳珊,王波华,王枫,等.2013.安徽金寨县沙坪沟钼矿区铌赋存状态研究[J].岩矿测试,32(2):269~277.
杨泽强.2007.河南商城县汤家坪钼矿辉钼矿铼-锇同位素年龄及地质意义[J].矿床地质,26(3):289~295.
杨言辰,韩世炯,孙德有,等.2012.小兴安岭-张广才岭成矿带斑岩型钼矿床岩石地球化学特征及其年代学研究[J].岩石学报,28(2):379~390.
于文,倪培,王国光,等.2013.安徽金寨县沙坪沟斑岩钼矿床成矿流体演化特征[J].南京大学学报(自然科学),48(3):241~255.
赵子福,郑永飞.2009.俯冲大陆岩石圈重熔:大别-苏鲁造山带中生代岩浆岩成因[J].中国科学D辑-地球科学,39(7):888~909.
张红,孙卫东,杨晓勇,等.2011.大别造山带沙坪沟特大型斑岩钼矿床年代学及成矿机理研究[J].地质学报,85(12):2 040~2 059.
张怀东,王波华,郝越进,等.2012.安徽沙坪沟斑岩型钼矿床地质特征及综合找矿信息[J].矿床地质,31(1):41~51.
张招崇,王福生.2003.一种判断原始岩浆的方法-以苦橄岩和碱性玄武岩为例[J].吉林大学学报,33(2):130~134.
郑永飞,徐峥,赵子福,等.2018.华北中生代镁铁质岩浆作用与克拉通减薄和破坏[J].中国科学:地球科学,48(4):379~414.
周作侠.1986.湖北丰山洞岩体成因探讨[J].岩石学报,2(1):59~70.
周作侠.1988.侵入岩的镁铁云母化学成分特征及其地质意义[J].岩石学报,4(3):63~73.
(1)安徽省地质矿产勘查局313地质队. 2011.安徽省金寨县沙坪沟钼矿普查地质报告(内部资料)[R]. 1~18.
Candela P A.1989.Felsic magmas,volatiles,and metallogenesis[J].Reviews in Economic Geology,4:223~233.
Carten R B,White W H and Stein H J.1993.High-grade granite-related molybdenum systems classification and origin.Mineral Deposit Modeling[J].Geological Association of Canada Special Paper,40:521~554.
Cong B L.1996.Ultrahigh-pressure metamorphic rocks in the Dabie-Sulu region of China[J].Beijing:Science Press,China and Kluwer Acad Pub,Dordrecht,224~228.
Chen Hongjin,Chen Yanjing,Zhang Jing,et al.2013.Zircon U-Pb ages and Hf isotope characteristics of the ore-bearing intrusion from the Shapinggou molybdenum deposit,Jinzhai County,Anhui Province[J].Acta Petrologica Sinica,29(1):132~145(in Chinese with English abstract).
Chen Y J,Li C,Zhang J,et al.2000.Sr and O isotopic characteristics of porphyries in the Qinling molybdenum deposit belt and their implication to genetic mechanism and type[J].Science in China(Series D:Earth Sciences),43:82~94.
Chen Yuezhi and Sang Baoliang.1995.Metamorphic petrology and metamorphism of the foziling group in northern Huaiyang and its age[J].Regional Geology of China,14(3):280~288(in Chinese with English abstract).
Chiara G,Franco R,Yican Liu,et al.2014.P-T evolution of elusive UHP eclogites from the Luotian dome(North Dabie Zone,China):How far can the thermodynamic modeling lead us?[J].Lithos,226(6):183~200.
Dai Shengqian,Xu Jiacong,Shi Qianhua,et al.1992.New recognition of the foziling group in the eastern part of northern Huaiyang[J].Regional Geology of China,11(4):369~375(in Chinese with English abstract).
Deng Jinfu.1983.Melt-mineral Equilibrium Thermodynamics[M].Beijing:Geological Publishing House,74~92(in Chinese).
Deng Jinfu,Dai Shengqian,Wu Zongxu,et al.2000.Petrological structure and thermal structure of the Dabie orogenic belt and its geological implications[J].Acta Geologica Sinica,74(3):207~215(in Chinese with English abstract).
Du Jianguo.2000.On Researching of Mesozoic Magmatism and Geochemsitry of Mineralization in Dabie Orogenic belt[D].Hefei:Hefei University of Technology,14~36(in Chinese with English abstract).
Feng Hongye,Xu Yingxia,Tang Dongmei,et al.2014.Mineralogical characteristics of olivine and spinel from Getashankou Cu-Ni-bearing maficultramaficintrusions in eastern Tianshan,NW China[J].Geology and Exploration,50(2):346~359(in Chinese with Englishabstract).
Foster M D.1960.Interpretation of the Composition of Trioctahedral Micas[M].Washington:Mineral Society of America,11~49.
Gao Y,Mao J W and Ye H S.2015.A review of the geological characteristics and geodynamic setting of the late Ealy cretaceous molybdenum deposits in the East Qinling-Dabie Molybdenum belt,East China[J].Joural of Asia Eath Science,108:81~96.
Hacker B R,Ratschbacher L,Webb L,et al.2000.Exhumation of ultrahigh-pressure continental crust in east central China:Late TriassicEarly Jurassic tectonic unroofing[J].Journal of Geophysical Research,OS(B6):13 339~13 364.
Hammarstrom J M and Zen E A.1986.Aluminum in hornblende:An empirical igneousgeobarometer[J].American Mineralogist,71:1 297~1 313.
He Yongsheng.2011.Geochemistry of Post-collisional Granitic Magmatism from the Dabie Orogen:Constraints on Removal Processes and Architecture of the Mountain Root[D].Hefei:University of Science and Technology of China(in Chinese with English abstract).
Hollister L S,Grissom G C,Peters E K,et al.1987.Confirmation of the empirical correlation of al in hornblende with pressure of solidification of calc-alkaline plutons[J].American Mineralogist,72:231~239.
Hong Dawei,Wang Tao,Tong Ying,et al.2003.Mesozoic granitoids from North China Block and Qingling-Dabie-Sulu orogenic belt and their deep dynamic process[J].Earth Science Frontiers,10(3):231~256(in Chinese with English abstract).
Huang Fan,Wang Denghong,Lu Sanming,et al.2011.Molybdenite ReOs isotopic age of Shapinggou Mo deposit in Anhui Province and Mesozoic Mo ore-forming stages in East Qinling-Dabie Mountain region[J].Mineral Deposits,30(6):1 040~1 057(in Chinese with English abstract).
Irvine T N.1977.Origin of chromitite layers in the Muskox intrusion and other strtiform intrusions:A new interpretation[J].Geology,5:273~277.
Jiang Changyi and An Sanyuan.1984.On chemical characteristics ofcalcic amphiboles from igneous rocsk and their petrogenesissignificance[J].Journal of Mineralogy and Petrology,4(3):1~9(in Chinese with English abstract).
Jiang Laili,Liu Yican,Wu Weiping,et al.1999.The deformation history and exhumation process of the UHPM rocks in the Dabieshan[J].Scientia Geologica Sinica,34(4):432~441(in Chinese with English abstract).
Kay S M,Snedden W T,Foster B P,et al.1983.Upper mantle and crustal fragments in the Ithaca kimberlites[J].Journal of Geology,91(3):277~290.
Keith J D,Christiansen E H and Carten R B.1993.The genesis of giant porphyry molybdenum deposits[J].Giant Ore Deposits,Society of Economic Geologists Special Publication,2:285~316.
Leake B E.1997.Nomenclature of amphiboles:Report of the Subcommittee on Amphibole of the International Mineralogical Association,Commission on new minerals and mineral names[J].Amer.Mineral.,82:1 019~1 037.
Leterrier J,Maury R C,Thonon P,et al.1982.Clinopyroxene composition as a method of identification of the magmatic affinities of paleovolcanic series[J].Earth&Planetary Science Letters,59(1):139~154.
Li Junping,Li Yongfeng,Luo Zhengchuan,et al.2011.Geological features of molybdenum deposits and ore prospecting in northern slope of the Dabie Mountain,China[J].Geotectonica et Metallogenia,4(3):457~468(in Chinese with English abstract).
Li Nuo,Chen Yanjing,Zhang Hui,et al.2007.Molybdenum deposits in East Qinling[J].Earth Science Frontiers,14(5):186~198(in Chinese with English abstract).
Li Shuguang.2004.Exhumation mechanism of the ultrahigh-pressure metamorphic rocks in the Dabie Mountains and continental collision process between the North and South China blocks[J].Earth Science Frontiers,11(3):63~70(in Chinese with English abstract).
Li Shuguang,He Yongsheng,Wang Shuitong,et al.2013.Process and mechanism of mountain-root removal of the Dabie Orogen:Constraints from geochronology and geochemistry of post-collisional igneous rocks[J].China Sci.Bull.,58(23):2 316~2 322(in Chinese with English abstract).
Li Yi,Li Nuo,Yang Yongfei et al.2013.Geological features and geodynamic settings of the Mo deposits in the northern segment of the Dabie Mountains[J].Acta Petrologica Sinica,29(1):95~106(in Chinese with English abstract).
Liu Fei,Yang Jingsui,Chen Songyong,et al.2013.Geochemistry and Sr-Nd-Pb isotopic composition of mafic rocks in the western part of Yarlung Zangbo suture zone:Evidence for intra-oceanic supra-subduction within the Neo-Tethys[J].Geology in China,40(3):742~755(in Chinese with English abstract).
Lu Fengxiang,Shang Longkang,Wu Jinhua,et al.2001.Petrology[M].Beijing:Geological Publishing House,1~338(in Chinese).
Luan Y,Song X Y,Chen L M,et al.2014.Key factors controlling the accumulation of the Fe-Ti oxides in the Hongge layered intrusion in the Emeishan Large Igneous Province,SW China[J].Ore Geol.Rev.,57:518~538.
Ma Hongwen.1985.A formular about modified geothermograph of clinopyroxene[J].Geological Science and Technology Information,4(2):82~84(in Chinese).
Mao J W,Pirajno F and Xiang J F.2011.Mesozoic molybdenum deposits in the East Qinling-Dabie Orogenic belt:Characteristics and tectonic settines[J].Ore Geoloev Reviews,43:264~293.
Meng Xiangjin,Xu Wenyi,LüQingtian,et al.2012.Zircon U-Pb dating of ore-bearing rocks and molybdenite Re-Os age in Shapinggou porphyry molybdenum deposit,Anhui Province[J].Acta Geologica Sinica,86(3):487~494(in Chinese with English abstract).
Ni Zhiyao.1991.Chemical composition and petrologic significance of olivines in Huangshandong mafic-ultramafic complex in Hami,Xinjiang,China[J].Mineralogy and Petrology,11(3):40~47(in Chinese with English abstract).
Ni Pei,Wang Guoguang,Wen Yu,et al.2005.Evidence of fluid inclusions for two stages of fluid boiling in the formation of the giant Shapinggou porphyry Mo deposit,Dabie Orogen,Central China[J].Ore Geology Reviews,65(3):1 078~1 094.
Niu Yaoling,Charles H L,Rosamond J,et al.1997.The origin of abyssal peridoties a new perspective[J].Earth and Planetary Science Letters,152(4):251~265.
Peng Zhi,Du Jianguo,Chen Fang,et al.2015.Geochemical characteristics and LA-ICP-Ms zircon U-Pb geochronology of the Tongxingsi alkaline intrusion in the Eastern North Huaiyang and their geological significance[J].Acta Geologica Sinica,89(4):701~714(in Chinese with English abstract).
Powell R H T and Worley B.1998.Calculating phase diagrams involving solid solutions via non-linear equations,with examples using THER-MOCALC[J].Metamorphic Geol.,16(4):577~588.
Qiu Jiaxiang and Liao Qun’an.1987.The main characteristics and genetic information of clinopyroxene megaecrysts in Cenozoic basalt of Eastern China[J].Acta Petrologica et Mineralogica,6(1):53~63(in Chinese with English abstract).
Qiu Jiaxiang and Lin Jingqian.1991.Lithochemistry[M].Beijing:Geological Publishing House,140~156(in Chinese).
Ratschbacher L,Harcker B R,Webb L E,et al.2000.Exhumation of the ultrahigh-pressure continental crust in east central China:Cretaceous and Cenozoic unroofing and the Tan-Lu fault[J].Journal of Geophysical Research,105(B6):13 303~13 338.
Ren Zhi,Zhou Taofa,Pete Hollings,et al.2018.Magmatism in the Shapinggou district of the Dabie Orogen,China:Implications for the formation of porphyry Mo deposits in a collisional orogenic belt[J].Lithos,308~309:346~363.
Ren Zhi,Zhou Taofa,Zhang Dayu,et al.2015.Characteristics of alteration and mineralization of Shapinggou porphyry molybdenum deposit,Dabie orogenic belt[J].Acta Petrologica Sinica,31(9):2 708~2 723(in Chinese with English abstract).
Richards J.2003.Tectono-magmatic precursors for porphyry Cu-(MoAu)deposit formation[J].Econ.Geol.,98(8):1 515~1 533.
Ridolfi F,Renzulli A and Puerini M.2010.Stability and chemical equilibrium of amphibole in calc-alkaline magmas:An overview,new thermobarometric formulations and application to subduction-re-lated volcanoes[J].Contributions to Mineralogy and Petrology,160(1):45~66.
Roeder P L and Emslie R F.1970.Olivine-liquid equilibrium[J].Contribu-tions to Mineralogy and Petrology,29:275~289.
Sato H.1977.Nickel content of basaltic magmas:Identification of primary magma and a measure of the degree of olivine fractionation[J].Lithos,10(4):113~120.
Schmidt M W.1992.Amphibole composition in tonalite as a function of pressure:An experimental calibration of the Al-in-hornblende barometer[J].Contributions to Mineralogy&Petrology,110:304~310.
Sinclair W.2007.Mineral deposits of Canada:A synthesis of major deposit-types,district metallogeny,the evolution of geological provinces,and exploration methods[J].Geological Association of Canada,Mineral Deposits Division,Special Publication,5(1):223~243.
Stein H J and Hannah J L.1985.Movement and origin of ore fluids in Climax-type systems[J].Geology,13(7):469~474.
Tan Hongyan,Shu Guanglong,LüJunchao,et al.2012.LA-ICP-MS zircon U-Pb and molybdenite Re-Os dating for the Luming large-scale molybdenum deposit in Xiao Hinggan mountains and its geological implication[J].Journal of Jilin University(Earth Science Edition),42(6):1 758~1 764(in Chinese with English abstract).
Thompson A B,Aerts M and Hack A C.2007.Liquid immiscibility in silicate melts and related systems[J].Reviews in Mineralogy and Geochemistry,65:99~127.
Wallace S R,Mac Kenzie W B,Blair R G,et al.1978.Geology of the Urad and Henderson molybdenite deposits,Clear Creek County,Colorado,with a section on a comparison of these deposits with those at Climax,Colorado[J].Economic Geology,73(3):325~368.
Wang Bohua,Wu Zongling,Zhang Huaidong,et al.2007.Geological and geochemical features of Mesozoic igneous rocks in the Yinsha area,Jinzhai Anhui Province,and the implications[J].Geology of Anhui,17(4):245~248(in Chinese with English abstract).
Wang Ping.2013.The Characteristics and Genesis of Magmatic Rocks in Shapinggou Molybdenum Ore Disdrict,Jinzhai,Anhui[D].Hefei:Hefei University of Technology(in Chinese with English abstract).
Wang Qingchen and Lin Wei.2002.Geodynamics of the Dabieshan collisional orogenic belt[J].Earth Science Frontiers,9(4):257~265(in Chinese with English abstract).
Wang Yun,Chen Yanjing,Ma Hongwei,et al.2009.Study On ore geology and fluid inclusion of the Tangjiaping Mo deposit,Shangcheng County,Henan Province[J].Acta Petrologica Sinica,25(2):469~480(in Chinese with English abstract).
Westra G and Keith S B.1981.Classification and genesis of stockwork molybdenum deposits[J].Economic Geology,76(4):844~873.
Wones D R and Eugster H P.1965.Stability of biotite:Experiment,theory,and application[J].Am.Miner.,50(9):1 228~1 272.
Xie Caifu,Xiong Chengyun,Hu Ning,et al.2001.A study on regional metallogenic regularity of the East Qinling-Dable orogenic belt[J].Geology and M ineral Resources of South China,17(3):15~21(in Chinese with English abstract).
Xie Yuling,Li Lamei,Guo Xiang,et al.2015.Chronology,petrochemistry of fine grained granite and their implication to Mo-Cu mineralization in Xichong Mo deposit,Anhui Province,China[J].Acta Petrologica Sinica,31(7):1 929~1 942(in Chinese with English abstract).
Xu Gang,Tang Zhongli,Jiao Jiangang,et al.2012.The comparative study on small intrusion type molybdenum deposits of Shapinggou and Jinduicheng[J].Northwestern Geology,45(4):359~369(in Chinese with English abstract).
Xu Xiangzhen,Yang Jingsui,Guo Guolin,et al.2011.Lithological research on the Purang mantle peridotite in western Yarlung Zangbo suture zone in Tibet[J].Acta Petrologica Sinica,27(11):3 179~3 196(in Chinese with English abstract).
Xu Xiaochun,Lou Jinwei,Lu Sanming,et al.2009.Re-Os ages of molybdenum-lead-zinc polymetallic deposits and40Ar-39Ar ages of related magmatic rocks in Yinshan area,Jinzhai,Anhui Province[J].Mineral Deposits,28(5):621~632(in Chinese with English abstract).
Xu Yigang.1993.Geothermometers applicable to the mantle xenoliths[J].Acta Petrologica Sinica,9(2):167~180(in Chinese with English abstract).
Xue Junzhi,Bai Xuerang and Chen Wu.1986.Genetic Mineralogy[M].Wuhan:China University of Geosciences Press,114~121(in Chinese).
Yang Shan,Wang Bohua,Wang Feng,et al.2013.The occurrence of niobium in Shapinggou molybdenum deposits,Jinzhai County,Anhui Province[J].Rock And Mineral Analysis,32(2):269~277(in Chinese with English abstract).
Yang Yanchen,Han Shijiong,Sun Deyou,et al.2012.Geological and geochemical features and geochronology of porphyry molybdenum deposits in the Lesser Xing’an Range-Zhangguangcai Range metallogenic belt[J].Acta Petrologica Sinica,28(2):379~390(in Chinese with English abstract).
Yang Zeqiang.2007.Re-Os isotopic ages of Tangjiaping molybdenum deposit in Shangcheng County,Henan and their geological significance[J].Mineral Deposits,26(3):289~295(in Chinese with English abstract).
Yu Wen,Ni Pei,Wang Guoguang,et al.2013.Evolution of ore-forming fluids of the Shapinggou porphyry molybdenum[J].Journal of Nanjing University(Natural Sciences),48(3):241~255(in Chinese with English abstract).
Zhang Zhaochong and Wang Fusheng.2003.A method for identifying primary magma-Examples from pickite and alkali basalts[J].Journal of Jilin University(Earth Science Edition),33(2):130~134(in Chinese with English abstract).
Zhao Zifu and Zheng Yongfei.2009.Remelting of subducted continental lithosphere:Petrogenesis of Mesozoic magmatic rocks in the DabieSulu orogenic belt[J].Sci.China Ser.D-Earth Sci.,39(7):888~909(in Chinese with English abstract).
Zhang Hong,Sun Weidong,Yang Xiaoyong,et al,2011.Geochronology and Metallogenesis of the Shapinggou Giant Porphyry Molbdenum Deposit in the Dabie Orogenic Belt[J].Acta Geologica Sinica,85(12):2 040~2 059(in Chinese with English abstract).
Zhang Huaidong,Wang Bohua,Hao Yuejin,et al.2012.Geological characteristics and comprehensive ore-prospecting information of Shapinggou porphyry-type molybdenum deposit in Anhui Province[J].Mineral Deposits,31(1):41~51(in Chinese with English abstract).
Zheng Yongfei,Xu Zheng,Zhao Zifu,et al.2018.Mesozoic mafic magmatism in North China:Implications for thinning and destruction of cratonic lithosphere[J].Science China:Earth Sciences,48(4):379~414(in Chinese with English abstract).
Zhou Zuoxia.1986.The origin of intrusive mass in Fengshandong,Hubei Province[J].Acta Petrotogica Sinica,2(1):59~70(in Chinese with English abstract).
Zhou Zuoxia.1988.Chemical characteristics of mafic mica in intrusive rocks and its geological meaning[J].Acta Petrotogica Sinica,4(3):63~73(in Chinese with English abstract).
Zhou Zuoxia.1991.Application of Mg-Fe mica chemical composition,rare elements,REE,Cu,Cl,F to distinguishing petrogenetic types[A].Wu Liren and Li Bingglun.Two Great Mesozoic Types of Porphyry Ore Deposits in the East of China[C].Beijing:Science Press,76~82(in Chinese).
陈红瑾,陈衍景,张静,等.2013.安徽省金寨县沙坪沟钼矿含矿岩体锆石U-Pb年龄和Hf同位素特征及其地质意义[J].岩石学报,29(1):132~145.
陈跃志,桑宝梁.1995.佛子岭群变质岩石学变质作用及时代的初步研究[J].中国区域地质,14(3):280~288.
邓晋福.1983.熔浆-矿物平衡热力学[M].北京:地质出版社,74~92.
邓晋福,戴圣潜,吴宗絮,等.2000.大别造山带岩石学结构和热结构及其地质意义[J].地质学报,74(3):207~215.
戴圣潜,徐家聪,石乾华,等.1992.北淮阳东段佛子岭群新认识[J].中国区域地质,11(4):369~375.
杜建国.2000.大别造山带中生代岩浆作用与成矿地球化学研究[D].合肥:合肥工业大学,14~36.
冯宏业,许英霞,唐冬梅,等.2014.东天山圪塔山口铜镍矿区镁铁-超镁铁质岩体橄榄石与尖晶石矿物学特征[J].地质与勘探,50(2):346~359.
何永胜.2011.大别造山带碰撞后花岗质岩浆作用地球化学:对去山根过程及山根结构的制约[D].合肥:中国科学技术大学.
洪大卫,王涛,童英,等.2003.华北地台和秦岭-大别-苏鲁造山带的中生代花岗岩与深部地球动力学过程[J].地学前缘,10(3):231~256.
黄凡,王登红,陆三明,等.2011.安徽省金寨县沙坪沟钼矿辉钼矿Re-Os年龄-兼论东秦岭-大别山中生代钼成矿作用期次划分[J].矿床地质,30(6):1 040~1 057.
姜常义,安三元.1984.论火成岩中钙质角闪石的化学组成特征及其岩石学意义[J].矿物岩石,4(3):1~9.
江来利,刘贻灿,吴维平,等.1999.大别山超高压变质岩的变形历史及折返过程[J].地质科学,34(4):432~441.
李俊平,李永峰,罗正传,等.2011.大别山北麓钼矿找矿重大进展及其矿床地质特征研究[J].大地构造与成矿学,4(3):457~468.
李诺,陈衍景,张辉,等.2007.东秦岭斑岩钼矿带的地质特征和成矿构造背景[J].地学前缘,14(5):186~198.
李曙光.2004.大别山超高压变质岩折返机制与华北-华南陆块碰撞过程[J].地学前缘,11(3):63~70.
李曙光,何永胜,王水炯.2013.大别造山带的去山根过程与机制:碰撞后岩浆岩的年代学和地球化学制约[J].科学通报,58(23):2 316~2 322.
李毅,李诺,杨永飞,等.2013.大别山北麓钼矿床地质特征和地球动力学背景[J].岩石学报,29(1):95~106.
刘飞,杨经绥,陈松永,等.2013.雅鲁藏布江缝合带西段基性岩地球化学和Sr-Nd-Pb同位素特征:新特提斯洋内俯冲的证据[J].中国地质,40(3):742~755.
路凤香,桑隆康,邬金华,等.2001.岩石学[M].北京:地质出版社,1~338.
马鸿文.1985.介绍改进的单斜辉石地质温度计公式[J].地质科技情报,4(2):82~84.
孟祥金,徐文艺,吕庆田,等.2012.安徽沙坪沟斑岩钼矿锆石U-Pb和辉钼矿Re-Os年龄[J].地质学报,86(3):487~494.
倪志耀.1991.新疆哈密黄山东镁铁-超镁铁杂岩体中橄榄石的化学成分及其岩石学意义[J].矿物岩石,11(3):40~47.
彭智,杜建国,陈芳,等.2015.北淮阳东段同兴寺碱性岩体地球化学特征、LA-ICP-MS锆石U-Pb年龄及其地质意义[J].地质学报,89(4):701~714.
邱家骧,廖群安.1987.中国东部新生代玄武岩中单斜辉石巨晶的主要特征及成因信息[J].岩石矿物学杂志,6(1):56~63.
邱家骧,林景仟.1991.岩石化学[M].北京:地质出版社,140~156.
任志,周涛发,张达玉,等.2015.大别山地区沙坪沟斑岩型钼矿床蚀变及矿化特征研究[J].岩石学报,31(9):2 708~2 723.
谭红艳,舒广龙,吕骏超,等.2012.小兴安岭鹿鸣大型钼矿LA-ICP-MS锆石U-Pb和辉钼矿Re-Os年龄及其地质意义[J].吉林大学学报(地球科学版),42(6):1 758~1 764.
王波华,邬宗玲,张怀东,等.2007.安徽省金寨银沙地区中生代岩浆岩地质地球化学特征及其找矿意义[J].安徽地质,17(4):245~248.
王萍.2013.安徽金寨沙坪沟钼矿区岩浆岩特征及成因[D].合肥:合肥工业大学.
王清晨,林伟.2002.大别山碰撞造山带的地球动力学[J].地学前缘,9(4):257~265.
王运,陈衍景,马宏卫,等.2009.河南省商城县汤家坪钼床地质和流体包裹体研究[J].岩石学报,25(2):469~480.
谢才富,熊成云,胡宁,等.2001.东秦岭-大别造山带区域成矿规律研究[J].华南地质和矿产,17(3):15~21.
谢玉玲,李腊梅,郭翔,等.2015.安徽西冲钼矿床细粒花岗岩的岩石定年、岩石化学及与成矿的关系研究[J].岩石学报,31(7):1 929~1 942.
徐刚,汤中立,焦建刚,等.2012.金堆城与沙坪沟小岩体型斑岩钼矿床对比研究[J].西北地质,45(4):359~369.
徐向珍,杨经绥,郭国林,等.2011.雅鲁藏布江缝合带西段普兰蛇绿岩中地幔橄榄岩的岩石学研究[J].岩石学报,27(11):3 179~3 196.
徐义刚.1993.适用于幔源包体的地质温度计[J].岩石学报,9(2):167~180.
徐晓春,楼金伟,陆三明,等.2009.安徽金寨银山钼-铅-锌多金属矿床Re-Os和有关岩浆岩40Ar-39Ar年龄测定[J].矿床地质,28(5):621~632.
薛君治,白学让,陈武.1986.成因矿物学[M].武汉:中国地质大学出版社,114~121.
阳珊,王波华,王枫,等.2013.安徽金寨县沙坪沟钼矿区铌赋存状态研究[J].岩矿测试,32(2):269~277.
杨泽强.2007.河南商城县汤家坪钼矿辉钼矿铼-锇同位素年龄及地质意义[J].矿床地质,26(3):289~295.
杨言辰,韩世炯,孙德有,等.2012.小兴安岭-张广才岭成矿带斑岩型钼矿床岩石地球化学特征及其年代学研究[J].岩石学报,28(2):379~390.
于文,倪培,王国光,等.2013.安徽金寨县沙坪沟斑岩钼矿床成矿流体演化特征[J].南京大学学报(自然科学),48(3):241~255.
赵子福,郑永飞.2009.俯冲大陆岩石圈重熔:大别-苏鲁造山带中生代岩浆岩成因[J].中国科学D辑-地球科学,39(7):888~909.
张红,孙卫东,杨晓勇,等.2011.大别造山带沙坪沟特大型斑岩钼矿床年代学及成矿机理研究[J].地质学报,85(12):2 040~2 059.
张怀东,王波华,郝越进,等.2012.安徽沙坪沟斑岩型钼矿床地质特征及综合找矿信息[J].矿床地质,31(1):41~51.
张招崇,王福生.2003.一种判断原始岩浆的方法-以苦橄岩和碱性玄武岩为例[J].吉林大学学报,33(2):130~134.
郑永飞,徐峥,赵子福,等.2018.华北中生代镁铁质岩浆作用与克拉通减薄和破坏[J].中国科学:地球科学,48(4):379~414.
周作侠.1986.湖北丰山洞岩体成因探讨[J].岩石学报,2(1):59~70.
周作侠.1988.侵入岩的镁铁云母化学成分特征及其地质意义[J].岩石学报,4(3):63~73.
(1)安徽省地质矿产勘查局313地质队. 2011.安徽省金寨县沙坪沟钼矿普查地质报告(内部资料)[R]. 1~18.
© 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 |