东天山卡拉塔格泥盆纪岩浆岩地球化学特征及成因
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摘要
文中对卡拉塔格地区泥盆纪岩浆岩进行了系统的岩相学、岩石地球化学研究,探讨其成因及形成构造背景。卡拉塔格地区泥盆纪火山岩主要为安山岩,并被同期一套成分连续的侵入体,包括辉长岩、闪长岩、石英闪长岩、二长岩等侵入。其中,辉长岩为钙碱性-低钾系列准铝质岩石,具有较高的Al2O3含量(18.76%~19.06%)和Mg#(57.28~69.37),具有正Eu异常;闪长岩、石英闪长岩、二长岩和安山岩为钙碱性-高钾钙碱性系列的准铝质-弱过铝质岩石,也具有较高的Al_2O_3含量(15.02%～17.43%)和Mg#(53.67～72.91),具有较弱的Eu负异常或无Eu异常。这些岩浆岩都具有较低的初始Sr值(0.703 11～0.705 18)以及较高的ε值Nd(t)(5.36～7.72),均富集轻稀土和大离子亲石元素Rb、Ba、K等,亏损重稀土和高场强元素Ta、Nb、Ti等,都具有岛弧岩浆岩的特征。相似的岩石地球化学特征显示它们可能为同源岩浆活动的产物,可能是由俯冲洋壳形成的流体交代地幔楔岩石发生部分熔融而形成。泥盆纪岩浆岩形成于康古尔洋向卡拉麦里洋俯冲的岛弧背景。
We conducted petrologic investigation and performed major and trace elemental and Sr-Nd isotopic analysis on magmatic rocks from the Kalatag district,eastern Tianshan in order to understand the petrogenesis and geodynamic setting of Devonian magmatic rocks.The results show that Devonian magmatic rocks were mainly composed of intermediate-basic rocks including gabbro,diorite,quartz diorite,monzonite and andesite.Gabbro was calc-alkaline to tholeiitic with high Al_2O_3 content(18.96%-19.06%)and Mg#value(57.28-69.37),yielding A/CNK value of 0.73-0.88.Diorite,quartz diorite,monzonite and andesite were calc-alkaline to high-K calc-alkaline with high Al_2O_3 contents(15.02%-17.43%)and Mg#values(53.67-72.91),and A/CNK values of 0.73-1.17.Sr-Nd isotopic analysis yielded positiveεNd(t)values ranging from 5.36 to 7.72 with low initial 87 Sr/86 Sr ratios of 0.70311 to 0.70518.Devonian magmatic rocks were enriched in large ion lithophile elements(Rb,Ba and K)while depleted in high field strength elements(Ta,Nb and Ti).These geochemical characteristics indicate that Devonian magmatic rocks were derived from the same magma chamber with an enriched mantle wedge metasomatized by subduction slab fluid and emplaced in an island arc setting during the northward subduction of the Kanggur Ocean.
We conducted petrologic investigation and performed major and trace elemental and Sr-Nd isotopic analysis on magmatic rocks from the Kalatag district,eastern Tianshan in order to understand the petrogenesis and geodynamic setting of Devonian magmatic rocks.The results show that Devonian magmatic rocks were mainly composed of intermediate-basic rocks including gabbro,diorite,quartz diorite,monzonite and andesite.Gabbro was calc-alkaline to tholeiitic with high Al_2O_3 content(18.96%-19.06%)and Mg#value(57.28-69.37),yielding A/CNK value of 0.73-0.88.Diorite,quartz diorite,monzonite and andesite were calc-alkaline to high-K calc-alkaline with high Al_2O_3 contents(15.02%-17.43%)and Mg#values(53.67-72.91),and A/CNK values of 0.73-1.17.Sr-Nd isotopic analysis yielded positiveεNd(t)values ranging from 5.36 to 7.72 with low initial 87 Sr/86 Sr ratios of 0.70311 to 0.70518.Devonian magmatic rocks were enriched in large ion lithophile elements(Rb,Ba and K)while depleted in high field strength elements(Ta,Nb and Ti).These geochemical characteristics indicate that Devonian magmatic rocks were derived from the same magma chamber with an enriched mantle wedge metasomatized by subduction slab fluid and emplaced in an island arc setting during the northward subduction of the Kanggur Ocean.
引文
[1]SENGOR A M C,NATALIN B A,BURTMAN V S.Evolution of the Altaid tectonic collage and Paleozoic crustal growth in Eurasia[J].Nature,1993,364(6435):299-307.
[2]CHEN Y J,PIRAJNO F,WU G,et al.Epithermal deposits in north Xinjiang,NW China[J].International Journal of Earth Sciences,2012,101(4):889-917.
[3]XIAO W J,ZHANG L C,QIN K Z,et al.Paleozoic accretionary and collisional tectonics of the eastern Tianshan(China):implications for the continental growth of Central Asia[J].American Journal of Science,2004,304(4):370-395.
[4]WINDLEY B F,ALEXEIEV D,XIAO W J,et al.Tectonic models for accretion of the Central Asian Orogenic Belt[J].Journal of the Geological Society,2007,164(12):31-47.
[5]XIAO W J,SANTOSH M.The western Central Asian Orogenic Belt:a window to accretionary orogenesis and continental growth[J].Gondwana Research,2014,25(4):1429-1444.
[6]GUO Q Q,CHUNG S L,XIAO W J,et al.Petrogenesis and tectonic implications of Late Devonian arc volcanic rocks in southern Beishan orogen,NW China:geochemical and Nd-Sr-Hf isotopic constraints[J].Lithos,2017,278-281:84-96.
[7]王京彬,王玉往,何志军.东天山大地构造演化的成矿示踪[J].中国地质,2006,33(3):461-469.
[8]PIRAJNO F,SELTMANN R.A review of mineral systems and associated tectonic settings of northern Xinjiang,NWChina[J].Geoscience Frontiers,2011,2(2):157-185.
[9]ZHANG F F,WANG Y H,LIU J J.Fluid inclusions and H-O-S-Pb isotope systematics of the Baishan giant porphyry Mo deposit in Eastern Tianshan,China[J].Ore Geology Reviews,2016,78:409-423.
[10]王登红,李纯杰,陈郑辉,等.东天山成矿规律与找矿方向的初步研究[J].地质通报,2006,25(8):910-915.
[11]马比阿伟,木合塔尔·扎日,阿以拉者.东天山花岗岩与造山带演化[J].矿产与地质,2014,28(4):546-550.
[12]SHEN P,PAN H D,DONG L H.Yandong porphyry Cu deposit,Xinjiang,China:geology,geochemistry and SIMSU-Pb zircon geochronology of host porphyries and associated alteration and mineralization[J].Journal of Asian Earth Sciences,2014,80(2):197-217.
[13]马星华,陈斌,王超,等.早古生代古亚洲洋俯冲作用:来自新疆哈尔里克侵入岩的锆石U-Pb年代学、岩石地球化学和Sr-Nd同位素证据[J].岩石学报,2015,31(1):89-104.
[14]WANG Y H,ZHANG F F,LIU J J.The genesis of the ores and intrusions at the Yuhai Cu-Mo deposit in eastern Tianshan,NW China:constraints from geology,geochronology,geochemistry and Hf isotope systematics[J].Ore Geology Reviews,2016,77:312-331.
[15]邓小华,王京彬,王玉往,等.东天山卡拉塔格红石铜矿地质特征及矿床成因初步探讨[J].矿产勘查,2014,5(2):159-168.
[16]DENG X H,WANG J B,PIRAJNO F,et al.Re-Os dating of chalcopyrite from selected mineral deposits in the Kalatag district in the eastern Tianshan Orogen,China[J].Ore Geology Reviews,2016,77:72-81.
[17]毛启贵,方同辉,王京彬,等.东天山卡拉塔格早古生代红海块状硫化物矿床精确定年及其地质意义[J].岩石学报,2010,26(10):3017-3026.
[18]DENG X H,WANG J B,SANTOSH M,et al.New40 Ar/39 Ar ages from the Kalatag VMS deposits,eastern Tianshan,NW China:constraints on the timing of Cu mineralization and stratigraphy[J].Ore Geology Reviews,2016.DOI:10.1016/j.oregeorev.2016.08.006.
[19]李文铅,王冉,王核,等.“吐哈天窗”卡拉塔格岩体的地球化学和岩石成因[J].中国地质,2006,33(3):559-565.
[20]唐俊华,顾连兴,郑远川,等.东天山卡拉塔格钠质火山岩岩石学、地球化学及成因[J].岩石学报,2006,22(5):1150-1166.
[21]李玮,陈隽璐,董云鹏,等.早古生代古亚洲洋俯冲记录:来自东天山卡拉塔格高镁安山岩的年代学、地球化学证据[J].岩石学报,2016,32(2):505-521.
[22]MAO Q G,YU M J,XIAO W J,et al.Skarn-mineralized porphyry adakites in the Harlik arc at Kalatage,E.Tianshan(NW China):slab melting in the Devonian-Early Carboniferous in the southern Central Asian Orogenic Belt[J].Journal of Asian Earth Sciences,2018,153:365-378.
[23]秦克章,方同辉,王书来,等.东天山板块构造分区、演化与成矿地质背景研究[J].新疆地质,2002,20(4):302-308.
[24]QIN K Z,SU B X,SAKYI P A,et al.SIMS zircon U-Pb geochronology and Sr-Nd isotopes of Ni-Cu-bearing maficultramafic intrusions in eastern Tianshan and Beishan in correlation with flood basalts in Tarim Basin(NW China):constraints on a ca.280Ma mantle plume[J].American Journal of Science,2011,311:237-260.
[25]雷如雄,吴昌志,屈迅,等.中天山天湖东铁钼矿含矿片麻状花岗岩年代学、地球化学和锆石Hf同位素:对于中天山早古生代构造演化的启示[J].吉林大学学报(地球科学版),2014(5):1540-1552.
[26]LI D F,CHEN H Y,ZHANG L,et al.Ore geology and fluid evolution of the giant Caixiashan carbonate-hosted ZnPb deposit in the eastern Tianshan,NW China[J].Ore Geology Reviews,2016,72:355-372.
[27]DENG X H,WANG J B,SANTOSH M,et al.Early Paleozoic volcanic rocks with VMS mineralization from eastern Tianshan Orogen:implication for tectonic evolution[J].Geological Journal,2017.DOI:10.1002/gj.3046.
[28]GAO S,LIU X M,YUAN H L,et al.Determination of forty-two major and trace elements in USGS and NIST SRMglasses by laser ablation-inductively coupled plasma-mass spectrometry[J].Geostandards and Geoanalytical Research,2002,26:181-196.
[29]LI C F,CHEN F,LI X H.Precise isotopic measurements of sub-nanogram Nd of standard reference material by thermal ionization mass spectrometry using the NdO+technique[J].International Journal of Mass Spectrometry,2007,266(1):34-41.
[30]RICKWOOD P C.Boundary lines within petrologic diagrams which use oxides of major and minor elements[J].Lithos,1989,22(4):247-263.
[31]MANIAR P,PICCOLI P.Tectonic discrimination of granitoids[J].Geological Society of American Bulletin,1989,101(5):635-643.
[32]WRIGHT J B.A simple alkalinity ratio and its application to questions of non-orogenic granite genesis[J].Geological Magazine,1969,106(4):370-384.
[33]EWART A.The mineralogy and petrology of Tertiary-recent orogenic volcanic rocks with special reference to the andesitic basaltic compositional range[M]∥Orogenic andesites and related rocks.Chichester,UK:Wiley,1982:25-95.
[34]SUN S S,MCDONOUGH W F.Chemical and isotopic systematics of oceanic basalts:implications for mantle composition and processed[J].Geological Society of London Special Publications,1989,42(1):313-345.
[35]ZINDLER A,HART S R.Chemical geodynamics[J].Annual Review of Earth and Planetary Sciences,1986,14(1):493-571.
[36]GIBSON S A,KIRKPATRICK R J,EMMEMANN R,et al.The trace element composite of lavas and dykes from a3-km vertical section through the lava pile of eastern Iceland[J].Journal of Geophysical Research:Solid Earth,1982,87:6532-6546.
[37]PEARCE J A,THIRLWALL M F,INGRAM G,et al.Isotopic evidence for the origin of boninites and related rocks drilled in the Izu-Bomin(Ogasa Wara)Forearc,Leg 125[J].Proceedings of the Ocean Drilling Program Scientific Results,1992,125:237-261.
[38]GILL J B.Orogenic andesites and plate tectonics[M].Berlin:Springer-Verlag,1981:1-390.
[39]DAVIS J H,STEVENSON D J.Physical model of source region of subduction volcanics[J].Journal of Geophysical Research,1992,97:2037-2070.
[40]STOLZ A J,JOCHUM K P,SPETTEL B,et al.Fluid and melt related enrichment in the subarc mantle:evidence from Nb/Ta variations in island-arc basalts[J].Geology,1996,24(7):587-590.
[41]PEARCE J A,CANN J R.Tectonic setting of basic volcanic rocks determined using trace element analyses[J].Earth and Planetary Science Letters,1973,19(2):290-300.
[42]GREEN M G,SYLVESTER P J,BUICK R.Growthand recycling of early Archaean continental crust:geochemical evidence from the Coonterunah and Warrawoona Groups,Pilbara Craton,Australia[J].Tectonophysics,2000,322(1):69-88.
[43]LASSITER J C,DEPAOLO D J.Plume/lithosphere interaction in the generation of continental and oceanic flood basalts:chemical and isotopic constraints[J].Geophysical Monograph Series,1997,100:335-355.
[44]MECDONALD R,ROGERS N W,FITTON J G,et al.Plume-Lithosphere interactions in the generation of the basalts of the Kenya Rift,East Africa[J].Journal of Petrology,2001,42(5):877-900.
[45]BAKER J A,MENZIES M A,THIRLWALL M F,et al.Petrogenesis of Quaternary intraplate volcanism Sana’a Yenmen:implication and polybaric melt hybridization[J].Journal of Petrology,1997,38:1359-1390.
[46]CAMPHELL I H,GRIFFITHS R W.The evolution of mantle’s chemical structure[J].Lithos,1993,30:389-399.
[47]夏明哲,姜常义,钱壮志,等.新疆东天山葫芦岩体岩石学与地球化学研究[J].岩石学报,2008,24(12):2749-2760.
[48]RAPP R P,WATSON E B.Dehydration melting of meta basalt at 8-32kbar:implications for continental growth and crust-mantle recycling[J].Journal of Petrology,1995,36(4):891-931.
[49]SCHMIDT M W,VIELZEUF D,AUZANNEAU E.Melting and dissolution of subducting crust at high pressures:the key role of white mica[J].Earth and Planetary Science Letters,2004,228(1/2):65-84.
[50]章永梅,张力强,高虎,等.新疆西天山呼斯特杂岩体岩石学、锆石U-Pb年龄及Hf同位素特征[J].岩石学报,2016,32(6):1749-1769.
[51]TATSUMI Y,TAKAHASHI T.Operation of subduction factory and production of andesite[J].Journal of Mineralogical and Petrological Sciences,2006,101(3):145-153.
[52]邢浩,赵晓波,张招崇,等.西天山巴音布鲁克地区早古生代成矿地质环境:岩浆岩及其时代和元素同位素约束[J].岩石学报,2016,32(6):1770-1794.
[53]ZHU Y F,ZHANG L F,GU L B,et al.The zircon SHRIMP chronology and trace element geochemistry of the Carboniferous volcanic rocks in western Tianshan Mountains[J].Chinese Science Bulletin,2005,50(19):2201-2212.
[54]WOODHEAD J D,EGGINS S M,JOHNSON R W.Magma genesis in the New Britain island arc:further insights into melting and mass transfer processes[J].Journal of Petrology,1998,39(9):1641-1668.
[55]PLANK T,LANGMUIR C H.Tracing trace elements from sediment input to volcanic output at subduction zones[J].Nature,1993,362(6422):739-743.
[56]OTHMAN D B,WHITE W M,PATCHETT J.The geochemistry of marine sediments,island arc magma genesis and crust-mantle recycling[J].Earth and Planetary Science Letters,1989,94(1/2):1-21.
[57]YOU C F,CASTILLO P R,GIESKES J M,et al.Trace element behavior in hydrothermal experiments:implications for fluid processes at shallow depths in subduction zones[J].Earth and Planetary Science Letters,1996,140:41-52.
[58]WILSON M.Igneous petrogenesis[M].London:Unwin Hyman,1989:1-466.
[59]ELLIOTT T,PLANK T,ZINDLER A,et al.Elements transport from slab to volcanic front the Mariana arc[J].Journal of Geophysical Research,1997,102:14991-15019.
[60]SAUNDERS A D,STOREY M,KENT R W,et al.Consequences of plume-lithosphere interactions[J].Geological Society of London Special Publication,1992,68(1):41-60.
[61]WOODHEAD J D,HERGT J M,DAVIDSON J P,et al.Hafnium isotope evidence for“conservative”element mobility during subduction zone processes[J].Earth and Planetary Science Letters,2001,192(3):331-346.
[62]夏明哲,姜常义,钱壮志,等.新疆东天山黄山东岩体岩石地球化学特征与岩石成因[J].岩石学报,2010,26(8):2413-2430.
[63]MARTIN M.A method of discriminating between different types of min-ocean ridge basalts and continental tholeiites with the Nb-Zr-Y diagram[J].Chemical Geology,1986,56(3/4):207-218.
[64]PEARCE J A.Trace element characteristics of lavas from destructive plate boundaries[J].Andesites,1982:528-548.
[65]BAILEY J C.Geochemical criteria for a refined tectonic discrimination of orogenic andesites[J].Chemical Geology,1981,32(1):139-154.
[66]CONDIE K C.Geochemistry and tectonic setting of early Proterozoic suprocrustal rocks in the Southwestern United States[J].The Journal of Geology,1986,94(6):845-864.
[67]HARRIS H B W,PEARCE J A,TINDLE A G.Geochemical characteristics of collision-zone magmatism[J].Geological Society of London Special Publication,1986,19(5):67-81.
[68]PEARCE J A,HARRIS H B W,TINDLE A G.Trace element discrimination diagrams for the tectonic interpretation of granitic rocks[J].Journal of Petrology,1984,25(4):956-983.
[69]马瑞士,舒良树,孙家齐,等.东天山构造演化与成矿[M].北京:地质出版社,1997:1-202.
[70]李锦轶,王克卓,孙桂华,等.东天山吐哈盆地南缘古生代活动陆缘残片:中亚地区古亚洲洋板块俯冲的地质记录[J].岩石学报,2006,22(5):1087-1102.
[71]宋彪,李锦轶,李文铅,等.吐哈盆地南缘克孜尔卡拉萨依和大南湖花岗质岩基锆石SHRIMP定年及其地质意义[J].新疆地质,2002,20(4):342-345.
[72]李亚萍,孙桂华,李锦轶,等.东天山吐哈盆地东缘泥盆纪花岗岩的确定及其地质意义[J].地质通报,2006,25(8):932-936.
[73]唐俊华,顾连兴,张遵忠,等.东天山咸水泉片麻状花岗岩特征、年龄及成因[J].岩石学报,2007,23(8):1803-1820.
[74]周涛发,袁锋,张达玉,等.新疆东天山觉罗塔格地区花岗岩类年代学、构造背景及其成矿作用研究[J].岩石学报,2010,26(2):478-502.
[75]肖兵,陈华勇,王云峰,等.东天山土屋-延东铜矿矿区晚志留世岩体的发现及构造意义[J].地学前缘,2015,22(6):251-266.
[2]CHEN Y J,PIRAJNO F,WU G,et al.Epithermal deposits in north Xinjiang,NW China[J].International Journal of Earth Sciences,2012,101(4):889-917.
[3]XIAO W J,ZHANG L C,QIN K Z,et al.Paleozoic accretionary and collisional tectonics of the eastern Tianshan(China):implications for the continental growth of Central Asia[J].American Journal of Science,2004,304(4):370-395.
[4]WINDLEY B F,ALEXEIEV D,XIAO W J,et al.Tectonic models for accretion of the Central Asian Orogenic Belt[J].Journal of the Geological Society,2007,164(12):31-47.
[5]XIAO W J,SANTOSH M.The western Central Asian Orogenic Belt:a window to accretionary orogenesis and continental growth[J].Gondwana Research,2014,25(4):1429-1444.
[6]GUO Q Q,CHUNG S L,XIAO W J,et al.Petrogenesis and tectonic implications of Late Devonian arc volcanic rocks in southern Beishan orogen,NW China:geochemical and Nd-Sr-Hf isotopic constraints[J].Lithos,2017,278-281:84-96.
[7]王京彬,王玉往,何志军.东天山大地构造演化的成矿示踪[J].中国地质,2006,33(3):461-469.
[8]PIRAJNO F,SELTMANN R.A review of mineral systems and associated tectonic settings of northern Xinjiang,NWChina[J].Geoscience Frontiers,2011,2(2):157-185.
[9]ZHANG F F,WANG Y H,LIU J J.Fluid inclusions and H-O-S-Pb isotope systematics of the Baishan giant porphyry Mo deposit in Eastern Tianshan,China[J].Ore Geology Reviews,2016,78:409-423.
[10]王登红,李纯杰,陈郑辉,等.东天山成矿规律与找矿方向的初步研究[J].地质通报,2006,25(8):910-915.
[11]马比阿伟,木合塔尔·扎日,阿以拉者.东天山花岗岩与造山带演化[J].矿产与地质,2014,28(4):546-550.
[12]SHEN P,PAN H D,DONG L H.Yandong porphyry Cu deposit,Xinjiang,China:geology,geochemistry and SIMSU-Pb zircon geochronology of host porphyries and associated alteration and mineralization[J].Journal of Asian Earth Sciences,2014,80(2):197-217.
[13]马星华,陈斌,王超,等.早古生代古亚洲洋俯冲作用:来自新疆哈尔里克侵入岩的锆石U-Pb年代学、岩石地球化学和Sr-Nd同位素证据[J].岩石学报,2015,31(1):89-104.
[14]WANG Y H,ZHANG F F,LIU J J.The genesis of the ores and intrusions at the Yuhai Cu-Mo deposit in eastern Tianshan,NW China:constraints from geology,geochronology,geochemistry and Hf isotope systematics[J].Ore Geology Reviews,2016,77:312-331.
[15]邓小华,王京彬,王玉往,等.东天山卡拉塔格红石铜矿地质特征及矿床成因初步探讨[J].矿产勘查,2014,5(2):159-168.
[16]DENG X H,WANG J B,PIRAJNO F,et al.Re-Os dating of chalcopyrite from selected mineral deposits in the Kalatag district in the eastern Tianshan Orogen,China[J].Ore Geology Reviews,2016,77:72-81.
[17]毛启贵,方同辉,王京彬,等.东天山卡拉塔格早古生代红海块状硫化物矿床精确定年及其地质意义[J].岩石学报,2010,26(10):3017-3026.
[18]DENG X H,WANG J B,SANTOSH M,et al.New40 Ar/39 Ar ages from the Kalatag VMS deposits,eastern Tianshan,NW China:constraints on the timing of Cu mineralization and stratigraphy[J].Ore Geology Reviews,2016.DOI:10.1016/j.oregeorev.2016.08.006.
[19]李文铅,王冉,王核,等.“吐哈天窗”卡拉塔格岩体的地球化学和岩石成因[J].中国地质,2006,33(3):559-565.
[20]唐俊华,顾连兴,郑远川,等.东天山卡拉塔格钠质火山岩岩石学、地球化学及成因[J].岩石学报,2006,22(5):1150-1166.
[21]李玮,陈隽璐,董云鹏,等.早古生代古亚洲洋俯冲记录:来自东天山卡拉塔格高镁安山岩的年代学、地球化学证据[J].岩石学报,2016,32(2):505-521.
[22]MAO Q G,YU M J,XIAO W J,et al.Skarn-mineralized porphyry adakites in the Harlik arc at Kalatage,E.Tianshan(NW China):slab melting in the Devonian-Early Carboniferous in the southern Central Asian Orogenic Belt[J].Journal of Asian Earth Sciences,2018,153:365-378.
[23]秦克章,方同辉,王书来,等.东天山板块构造分区、演化与成矿地质背景研究[J].新疆地质,2002,20(4):302-308.
[24]QIN K Z,SU B X,SAKYI P A,et al.SIMS zircon U-Pb geochronology and Sr-Nd isotopes of Ni-Cu-bearing maficultramafic intrusions in eastern Tianshan and Beishan in correlation with flood basalts in Tarim Basin(NW China):constraints on a ca.280Ma mantle plume[J].American Journal of Science,2011,311:237-260.
[25]雷如雄,吴昌志,屈迅,等.中天山天湖东铁钼矿含矿片麻状花岗岩年代学、地球化学和锆石Hf同位素:对于中天山早古生代构造演化的启示[J].吉林大学学报(地球科学版),2014(5):1540-1552.
[26]LI D F,CHEN H Y,ZHANG L,et al.Ore geology and fluid evolution of the giant Caixiashan carbonate-hosted ZnPb deposit in the eastern Tianshan,NW China[J].Ore Geology Reviews,2016,72:355-372.
[27]DENG X H,WANG J B,SANTOSH M,et al.Early Paleozoic volcanic rocks with VMS mineralization from eastern Tianshan Orogen:implication for tectonic evolution[J].Geological Journal,2017.DOI:10.1002/gj.3046.
[28]GAO S,LIU X M,YUAN H L,et al.Determination of forty-two major and trace elements in USGS and NIST SRMglasses by laser ablation-inductively coupled plasma-mass spectrometry[J].Geostandards and Geoanalytical Research,2002,26:181-196.
[29]LI C F,CHEN F,LI X H.Precise isotopic measurements of sub-nanogram Nd of standard reference material by thermal ionization mass spectrometry using the NdO+technique[J].International Journal of Mass Spectrometry,2007,266(1):34-41.
[30]RICKWOOD P C.Boundary lines within petrologic diagrams which use oxides of major and minor elements[J].Lithos,1989,22(4):247-263.
[31]MANIAR P,PICCOLI P.Tectonic discrimination of granitoids[J].Geological Society of American Bulletin,1989,101(5):635-643.
[32]WRIGHT J B.A simple alkalinity ratio and its application to questions of non-orogenic granite genesis[J].Geological Magazine,1969,106(4):370-384.
[33]EWART A.The mineralogy and petrology of Tertiary-recent orogenic volcanic rocks with special reference to the andesitic basaltic compositional range[M]∥Orogenic andesites and related rocks.Chichester,UK:Wiley,1982:25-95.
[34]SUN S S,MCDONOUGH W F.Chemical and isotopic systematics of oceanic basalts:implications for mantle composition and processed[J].Geological Society of London Special Publications,1989,42(1):313-345.
[35]ZINDLER A,HART S R.Chemical geodynamics[J].Annual Review of Earth and Planetary Sciences,1986,14(1):493-571.
[36]GIBSON S A,KIRKPATRICK R J,EMMEMANN R,et al.The trace element composite of lavas and dykes from a3-km vertical section through the lava pile of eastern Iceland[J].Journal of Geophysical Research:Solid Earth,1982,87:6532-6546.
[37]PEARCE J A,THIRLWALL M F,INGRAM G,et al.Isotopic evidence for the origin of boninites and related rocks drilled in the Izu-Bomin(Ogasa Wara)Forearc,Leg 125[J].Proceedings of the Ocean Drilling Program Scientific Results,1992,125:237-261.
[38]GILL J B.Orogenic andesites and plate tectonics[M].Berlin:Springer-Verlag,1981:1-390.
[39]DAVIS J H,STEVENSON D J.Physical model of source region of subduction volcanics[J].Journal of Geophysical Research,1992,97:2037-2070.
[40]STOLZ A J,JOCHUM K P,SPETTEL B,et al.Fluid and melt related enrichment in the subarc mantle:evidence from Nb/Ta variations in island-arc basalts[J].Geology,1996,24(7):587-590.
[41]PEARCE J A,CANN J R.Tectonic setting of basic volcanic rocks determined using trace element analyses[J].Earth and Planetary Science Letters,1973,19(2):290-300.
[42]GREEN M G,SYLVESTER P J,BUICK R.Growthand recycling of early Archaean continental crust:geochemical evidence from the Coonterunah and Warrawoona Groups,Pilbara Craton,Australia[J].Tectonophysics,2000,322(1):69-88.
[43]LASSITER J C,DEPAOLO D J.Plume/lithosphere interaction in the generation of continental and oceanic flood basalts:chemical and isotopic constraints[J].Geophysical Monograph Series,1997,100:335-355.
[44]MECDONALD R,ROGERS N W,FITTON J G,et al.Plume-Lithosphere interactions in the generation of the basalts of the Kenya Rift,East Africa[J].Journal of Petrology,2001,42(5):877-900.
[45]BAKER J A,MENZIES M A,THIRLWALL M F,et al.Petrogenesis of Quaternary intraplate volcanism Sana’a Yenmen:implication and polybaric melt hybridization[J].Journal of Petrology,1997,38:1359-1390.
[46]CAMPHELL I H,GRIFFITHS R W.The evolution of mantle’s chemical structure[J].Lithos,1993,30:389-399.
[47]夏明哲,姜常义,钱壮志,等.新疆东天山葫芦岩体岩石学与地球化学研究[J].岩石学报,2008,24(12):2749-2760.
[48]RAPP R P,WATSON E B.Dehydration melting of meta basalt at 8-32kbar:implications for continental growth and crust-mantle recycling[J].Journal of Petrology,1995,36(4):891-931.
[49]SCHMIDT M W,VIELZEUF D,AUZANNEAU E.Melting and dissolution of subducting crust at high pressures:the key role of white mica[J].Earth and Planetary Science Letters,2004,228(1/2):65-84.
[50]章永梅,张力强,高虎,等.新疆西天山呼斯特杂岩体岩石学、锆石U-Pb年龄及Hf同位素特征[J].岩石学报,2016,32(6):1749-1769.
[51]TATSUMI Y,TAKAHASHI T.Operation of subduction factory and production of andesite[J].Journal of Mineralogical and Petrological Sciences,2006,101(3):145-153.
[52]邢浩,赵晓波,张招崇,等.西天山巴音布鲁克地区早古生代成矿地质环境:岩浆岩及其时代和元素同位素约束[J].岩石学报,2016,32(6):1770-1794.
[53]ZHU Y F,ZHANG L F,GU L B,et al.The zircon SHRIMP chronology and trace element geochemistry of the Carboniferous volcanic rocks in western Tianshan Mountains[J].Chinese Science Bulletin,2005,50(19):2201-2212.
[54]WOODHEAD J D,EGGINS S M,JOHNSON R W.Magma genesis in the New Britain island arc:further insights into melting and mass transfer processes[J].Journal of Petrology,1998,39(9):1641-1668.
[55]PLANK T,LANGMUIR C H.Tracing trace elements from sediment input to volcanic output at subduction zones[J].Nature,1993,362(6422):739-743.
[56]OTHMAN D B,WHITE W M,PATCHETT J.The geochemistry of marine sediments,island arc magma genesis and crust-mantle recycling[J].Earth and Planetary Science Letters,1989,94(1/2):1-21.
[57]YOU C F,CASTILLO P R,GIESKES J M,et al.Trace element behavior in hydrothermal experiments:implications for fluid processes at shallow depths in subduction zones[J].Earth and Planetary Science Letters,1996,140:41-52.
[58]WILSON M.Igneous petrogenesis[M].London:Unwin Hyman,1989:1-466.
[59]ELLIOTT T,PLANK T,ZINDLER A,et al.Elements transport from slab to volcanic front the Mariana arc[J].Journal of Geophysical Research,1997,102:14991-15019.
[60]SAUNDERS A D,STOREY M,KENT R W,et al.Consequences of plume-lithosphere interactions[J].Geological Society of London Special Publication,1992,68(1):41-60.
[61]WOODHEAD J D,HERGT J M,DAVIDSON J P,et al.Hafnium isotope evidence for“conservative”element mobility during subduction zone processes[J].Earth and Planetary Science Letters,2001,192(3):331-346.
[62]夏明哲,姜常义,钱壮志,等.新疆东天山黄山东岩体岩石地球化学特征与岩石成因[J].岩石学报,2010,26(8):2413-2430.
[63]MARTIN M.A method of discriminating between different types of min-ocean ridge basalts and continental tholeiites with the Nb-Zr-Y diagram[J].Chemical Geology,1986,56(3/4):207-218.
[64]PEARCE J A.Trace element characteristics of lavas from destructive plate boundaries[J].Andesites,1982:528-548.
[65]BAILEY J C.Geochemical criteria for a refined tectonic discrimination of orogenic andesites[J].Chemical Geology,1981,32(1):139-154.
[66]CONDIE K C.Geochemistry and tectonic setting of early Proterozoic suprocrustal rocks in the Southwestern United States[J].The Journal of Geology,1986,94(6):845-864.
[67]HARRIS H B W,PEARCE J A,TINDLE A G.Geochemical characteristics of collision-zone magmatism[J].Geological Society of London Special Publication,1986,19(5):67-81.
[68]PEARCE J A,HARRIS H B W,TINDLE A G.Trace element discrimination diagrams for the tectonic interpretation of granitic rocks[J].Journal of Petrology,1984,25(4):956-983.
[69]马瑞士,舒良树,孙家齐,等.东天山构造演化与成矿[M].北京:地质出版社,1997:1-202.
[70]李锦轶,王克卓,孙桂华,等.东天山吐哈盆地南缘古生代活动陆缘残片:中亚地区古亚洲洋板块俯冲的地质记录[J].岩石学报,2006,22(5):1087-1102.
[71]宋彪,李锦轶,李文铅,等.吐哈盆地南缘克孜尔卡拉萨依和大南湖花岗质岩基锆石SHRIMP定年及其地质意义[J].新疆地质,2002,20(4):342-345.
[72]李亚萍,孙桂华,李锦轶,等.东天山吐哈盆地东缘泥盆纪花岗岩的确定及其地质意义[J].地质通报,2006,25(8):932-936.
[73]唐俊华,顾连兴,张遵忠,等.东天山咸水泉片麻状花岗岩特征、年龄及成因[J].岩石学报,2007,23(8):1803-1820.
[74]周涛发,袁锋,张达玉,等.新疆东天山觉罗塔格地区花岗岩类年代学、构造背景及其成矿作用研究[J].岩石学报,2010,26(2):478-502.
[75]肖兵,陈华勇,王云峰,等.东天山土屋-延东铜矿矿区晚志留世岩体的发现及构造意义[J].地学前缘,2015,22(6):251-266.
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