用户名: 密码: 验证码:
新疆智博铁矿火山岩中富铁岩屑地球化学特征及其地质意义
详细信息    查看全文 | 推荐本文 |
  • 英文篇名:Geochemistry of iron-rich debris from Zhibo submarine volcanic rocks in Xinjiang and its geological implications
  • 作者:骆文娟 ; 张作衡 ; 段士刚 ; 蒋宗胜 ; 王大川 ; 康永建
  • 英文作者:LUO WenJuan;ZHANG ZuoHeng;DUAN ShiGang;JIANG ZongSheng;WANG DaChuan;KANG YongJian;MNR Key Laboratory of Metallogeny and Mineral Assessment, Institute of Mineral Resources, Chinese Academy of Geological Sciences;State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences;
  • 关键词:地球化学 ; 富铁岩屑 ; 碱铁效应 ; 铁矿成因 ; 智博铁矿 ; 海相火山岩型铁矿
  • 英文关键词:geochemistry;;iron-rich debris;;alkali-iron effect;;genesis of iron deposit;;Zhibo iron deposit;;submarine volcanic-hosted iron deposit
  • 中文刊名:矿床地质
  • 英文刊名:Mineral Deposits
  • 机构:中国地质科学院矿产资源研究所自然资源部成矿作用与资源评价重点实验室;中国地质大学地质过程与矿产资源国家重点实验室;
  • 出版日期:2019-02-15
  • 出版单位:矿床地质
  • 年:2019
  • 期:01
  • 基金:国家自然科学基金项目(编号:41503041);; 中央级公益性科研院所基本科研业务专项资金(编号:K1412);; 中国地质调查局地质调查项目(编号:DD20160124)资助
  • 语种:中文;
  • 页:64-82
  • 页数:19
  • CN:11-1965/P
  • ISSN:0258-7106
  • 分类号:P618.31
摘要
研究表明,西天山阿吾拉勒铁铜成矿带中智博铁矿区火山碎屑岩中的富铁岩屑主要由自形针状/板条状钠长石和富铁基质组成,呈辉绿/斑状结构。电子探针分析显示,富铁岩屑中钠长石端员组分变化范围为An=0.38~2.89,Ab=95.2~99.32,Or=0.17~2.79,端员组分平均值为An_(0.94)Ab_(98.01)Or_(1.06),类似于火山岩中钠长石端员组分变化范围(An=0.74~6.75,Ab=92.85~98.91,Or=0.32~1.76,端员组分平均值为An_(2.63)Ab_(96.65)Or_(0.72)),两者均为岩浆成因钠长石,而非热液交代成因钠长石。富铁基质成分变化范围较大且连续(w(SiO_2)为0.08%~50.04%,w(FeO)为24.89%~87.13%,w(Al_2O_3)为0.04%~14.83%,w(TiO_2)为0.01%~2.83%,w(Na_2O)为0~9.76%,w(MgO)为0.03%~4.88%,w(MnO)为0~0.61%),富铁基质中高Ti磁铁矿和低Ti磁铁矿同时发育,总体上成分不均一,且钠长石呈细针状,为浅成-超浅成低压下快速结晶的产物或为火山喷发作用下快速冷凝结晶所致。通过对磁铁矿-磷灰石矿物组合与安山岩中副矿物磷灰石、矿区磁铁矿的对比研究,认为智博铁矿发生磁铁矿-磷灰石岩浆不混溶作用的可能性很小。通过安山岩基质成分与安山岩成分的对比研究,得出安山岩基质比原岩w(SiO_2)、w(Al_2O_3)、w(CaO)有所降低,w(FeO)、w(Na_2O)、w(MgO)有一定升高,但是程度有限,表明岩浆结晶分异不足以使残留岩浆形成富铁矿。钠长石-磁铁矿富铁岩屑的发育是一种碱铁效应的表现,而碱铁效应对于海相火山岩型铁矿的形成具有重要意义。
        Iron-rich debris in the Zhibo submarine volcanoclastic rocks from the Awulale Fe-Cu metallogenic belt, Western Tianshan Mountains, is composed of acicular or lath-shaped euhedral albite and iron-rich matrix and exhibits diabasic or porphyritic texture. Electron microprobe analyses of albites from iron-rich debris show the compositional spectrum of An from 0.38 to 2.89, Ab from 95.2 to 99.32 and Or from 0.17 to 2.79, with the average endmember beingAn_(0.94) Ab_(98.01) Or_(1.06), which are similar to the compositional variation of the albites from volcanic rocks(An=0.74~6.75,Ab=92.85~98.91,Or=0.32~1.76,with the average endmember being An_(2.63) Ab_(96.65) Or_(0.72)). Both of them are magmatic albites rather than hydrothermal metasomatic albites. The chemical composition of iron-rich matrix is variable and continuous e. g., w(SiO_2) range from 0.08% to 50.04%,w(FeO) range from 24.89% to 87.13%, w(Al_2O_3) range from0.04% to 14.83%, w(TiO_2) range from 0.01% to 2.83%, w(Na_2 O) range from 0 to 9.76%, w(MgO) range from 0.03%to 4.88%, and w(MnO) range from 0 to 0.61%. The modes of occurrence of high Ti magnetite, low Ti magnetite and the acicular albite in the iron-rich matrix suggest the debris formed under hypabyssal-ultrahypabyssal conditions or through rapid condensation crystallization during a volcanic eruption. The comparisons of the magnetite-apatite paragenesis with accessory mineral apatite from andesite and magnetite from iron ores in terms of the element features show that the Zhibo iron ore deposit did not originate from the immiscibility of magnetite-apatite magma. Furthermore, the matrix of andesite has lower SiO_2, Al_2O_3, CaO and higher FeO, NaO, MgO than those of the whole rock.However, the Fe-enrichment in the matrix of andesite is not too obvious on the whole, and thus the authors hold that single magma crystallization differentiation would not cause the residual magma to form iron-rich ores. In summary,it is considered that the iron-rich debris was produced by"alkali-iron effect", which was likely the key factor inducing the mineralization of submarine volcanic-hosted iron deposit.
引文
Allen M B,Windley B F and Zhang C.1992.Palaeozoic collisional tectonics and magmatism of the Chinese Tien Shan,Central Asia[J].Tectonophysics,220:89-115.
    Andersen D.1984.Crystallization history of a Permian composite monzonite-alkali syenite pluton in the Sande Couldron,Oslo rift,southern Norway[J].Lithos,17:153-170.
    Buddington A F and Lindsley D H.1964.Iron-titanium oxide minerals and synthetic equivalents[J].Journal of Petrology,5(2):310-357.
    Chai F M,Yang F Q,Liu F,Santosh M,Geng X X,Li Q and Liu G R.2014.The Abagong apatite-rich magnetite deposit in the Chinese Altay Orogenic Belt:A Kiruna-type iron deposit[J].Ore Geology Reviews,57:482-497.
    Charlier B,Namur O and Grove T L.2013.Compositional and kinetic controls on liquid immiscibility in ferrobasalt-rhyolite volcanic and plutonic series[J].Geochimica.et Cosmochimica.Acta,113:79-93.
    Duan S G,Zhang Z H,Jiang Z S,Zhao J,Zhang Y P,Li F M and Tian J Q.2014.Geology,geochemistry,and geochronology of the Dunde iron-zinc ore deposit in western Tianshan,China[J].Ore Geology Reviews,57:441-461.
    Duan S G,Zhang Z H,Wei M Y,Tian J Q,Jiang Z S,Li F M,Zhao Jand Wang H F.2014.Geochemistry and zircon U-Pb geochronology of the diorite associated with the Wuling iron deposit in Western Tianshan Mountains,Xinjiang[J].Geology in China,41(6):1757-1770(in Chinese with English abstract).
    Duan S G,Zhang Z H,Wang D C,Jiang Z S,Luo W J and Li F M.2018.Pyrite Re-Os and muscovite 40Ar/39Ar dating of the Beizhan iron deposit in the Chinese Tianshan Orogen and its geological significance[J].International Geology Review,60(1):57-71.
    Feng J X,Shi F P,Wang B Y,Hu J M,Wang J T and Tian J Q.2010.The volcanogenic iron ore deposits in Awulale metallogenetic belt,Western Tianshan Mountains[M].Beijing:Geological Publishing House.111-112,132(in Chinese).
    Frost B and Lindsley D.1991.Chapter 12.Occurrence of iron-titanium oxides in igneous rocks[A].In:Linsley D H,ed.Oxide minerals:Petrologic and magnetic significance[C].Reviews in Mineralogy(Mineralogical Society of America),25:433-468.
    Gao J,Li M S,Xiao X C,Tang Y Q and He G Q.1998.Paleozoic tectonic evolution of the Tianshan Orogen,northwestern China[J].Tectonophysics,287(1-4):213-231.
    Gao J,Long L L,Klemd R,Qian Q,Liu D Y,Xiong X M,Su W,Liu W,Wang Y T and Yang F Q.2009.Tectonic evolution of the South Tianshan orogen and adjacent regions,NW China:Geochemical and age constraints of granitoid rocks[J].International Journal of Earth Sciences,98:1221-1238.
    Guilbert J M and Park C F.2007.The geology of ore deposits[M].Waveland Press.p399,948.
    Hong W,Zhang Z H,Li H Q,Li F M and Liu X Z.2012.Metallogenic epoch of Chagangnuoer iron deposit in western Tianshan Mountains,Xinjiang:Information for garnet Sm-Nd isochron age[J].Mineral Deposits,31(5):1067-1074(in Chinese with English abstract).
    Hou T,Zhang Z C,Santosh M,Encarnacion J,Zhu J and Luo W J.2014.Geochronology and geochemistry of submarine volcanic rocks in the Yamansu iron deposit,Eastern Tianshan Mountains,NW China:Constraints on the metallogenesis[J].Ore Geology Reviews,56:487-502.
    Hu X J and Chen W G.2010.Geologial characteristics and genesis of Chagangnuoer large-sized magnetite deposit in Southern Tianshan,Xinjiang[J].Resources survey and environment,31(3):185-193(in Chinese with English abstract).
    Huang J Q,Ren J S,Jiang C F,Zhang Z K and Qin D Y.1980.The Geotectonic Evolution of China[M].Beijing:Science Press.1-124(in Chinese)
    Jiang H J,Han J S,Chen H Y,Zheng Y,Zhang W F,Lu W J,Deng Gand Tan Z X.2016.Hydrothermal alteration,fluid inclusions and stable isotope characteristics of the Shaquanzi Fe-Cu deposit,Eastern Tianshan:Implications for deposit type and metallogenesis[J].Ore Geology Reviews,http://dx.doi.org/10.1016/j.oregeorev.2016.09.025.
    Jiang Z S,Zhang Z H,Hou K J,Hong W,Wang Z H,Li F M and Tian J Q.2012.Geochemistry and zircon U-Pb age of volcanic rocks from the Chagangnuoer and Zhibo iron deposits,western Tianshan,and their geological significance[J].Acta Petrologica Sinica,28(7):2074-2088(in Chinese with English abstrct).
    Jiang Z S,Zhang Z H,Wang Z H,Duan S G,Li F M and Tian J Q.2014.Geology,geochemistry,and geochronology of the Zhibo iron deposit in the Western Tianshan,NW China:Constraints on metallogenesis and tectonic setting[J].Ore Geology Reviews,57:406-424.
    Johnson H P.1979.Opaque mineralogy of the igneous rock samples from DSDP hole 395A[J].Initial Reports Deep Sea Drill Project,45:407-420.
    Jonsson E,Troll V R,H?gdahl K,Harris C,Weis F,Nilsson K P and Skelton A.2013.Magmatic origin of giant‘Kiruna-type’apatiteiron-oxide ores in Central Sweden[J].Scientific Reports 3,1644DOI:10.1038/srepo1644.
    Lan C Y,Zhao T P,Luo Z Z,Wang C L,Wen Q F and Liu L X.2015.The genesis of the Zhaoanzhuang Fe oxide deposit in Wuyang region of Henan Province:Insights from magnetite and apatite[J].Acta Petrologica Sinica,31(6):1653-1670(in Chinese with English abstract).
    Li D P,Du Y S,Pang Z S,Tu Q J,Zhang Y P,Ge S S,Shen L J and Wang K H.2013.Zircon U-Pb chronology and geochemistry of carboniferous volcanic rocks in Awulale Area,Western Tianshan Mountains[J].Acta Geoscientica Sinica,34(2):176-192(in Chinese with English abstrct).
    Li H M,Ding J H,Zhang Z C,Li L X,Chen J and Yao T.2015.Ironrich fragments in the Yamansu iron deposit,Xinjiang,NW China:Constraints on metallogenesis[J].Journal of Asian Earth Sciences,113:1068-1081.
    Li J L,Su W,Zhang X and Liu X.2009.Zircon Cameca U-Pb dating and its significance for granulite-facies granitic gneisses from the west Awulale Mountains,West Tianshan[J].Geological Bulletin of China,28:1852-1862(in Chinese with English abstract).
    Long L L,Gao J,Klemd R,Beier C,Qian Q,Zhang X,Wang J B and Jiang T.2011.Geochemical and geochronological studies of granitoid rocks from the Western Tianshan Orogen:Implications for continental growth in the southwestern Central Asian Orogenic Belt[J].Lithos,126:321-340.
    Long L L,Gao J,Qian Q,Xiong X M,Wang J B,Wang Y W and Gao LM.2008.Geochemical characteristics and tectonic settings of carboniferous volcanic rocks from Yili region,western Tianshan[J].Acta Petrologica Sinica,24(4):699-710(in Chinese with English abstract).
    Luo W J,Zhang Z H,Duan S G,Jiang Z S,Wang D C,Chen J and Sun J.2018.Geochemistry of the Zhibo submarine intermediate-mafic volcanic rocks and associated iron ores,Western Tianshan,Northwest China:Implications for ore genesis[J].Geological Journal,53:3147-3172.
    Luo W J and Sun J.2019.Oxygen isotope geochemistry of Fe oxide minerals and its applications to the study of iron ore deposit[J].Acta Petrologica et Mineralogica,38(1):121-130(in Chinese with English abstract).
    Miles A J,Graham C M,Hawkesworth C J,Gillespie M R,Hinton RW and Bromiley G D.2014.Apatite:A new redox proxy for silicic magmas[J]?Geochimica et Cosmochimica Acta,132:101-119.
    Mokhtari M A A,Zadeh G H and Emami M H.2013.Genesis of ironapatite ores in Posht-e-Badam Block(Central Iran)using REEgeochemistry[J].Journal of Earth System Science,122(3):795-807.
    Moore F and Modaberi S.2003.Origin of the Choghart iron oxide deposit,Bafq mining district,Central Iran:New isotopic and geochemical evidences[J].Journal of Sciences Islamic Republic of Iran,14(3):259-269.
    Nesbitt R W,Sun S S and Purvis A C.1979.Komatiites:Geochemistry and genesis[J].Canadian Mineralogist,17:165-186.
    No.11 Geological Party of Xinjiang Bureau of Geology and Mineral Resources.2012.1:50000 Geologic and mineral resources map of Chagangnuoer-Beizhan iron deposit,Hejing County,Xinjiang Province(Unpublished)[M].
    Philpotts A R.1967.Origin of certain iron-titanium oxide and apatite rocks[J].Econ.Geol.,62(3):303-315.
    Qian Q,Gao J,Klemd R,He G Q,Song B,Liu D Y and Xu R H.2009.Early Paleozoic tectonic evolution of the Chinese South Tianshan Orogen:constraints from SHRIMP zircon U-Pb geochronology and geochemistry of basaltic and dioritic rocks from Xiate,NWChina[J].International Journal of Earth Sciences,98:551-569.
    Rapp J F,Klemme S,Butler I B and Harley S L.2010.Extremely high solubility of rutile in chloride and fluoride-bearing metamorphic fluids:An experimental investigation[J].Geology,38:323-326.
    Ray G E and Webster I C L.2007.Geology and chemistry of the low Ti magnetite-bearing Heff Cu-Au skarn and its associated plutonic rocks,Heffley Lake,south-central British Columbia[J].Exploration and Mining Geology,163(3-4):159-186.
    Song X X,Chen Y C,Sheng J F and Ai Y D.1981.On iron deposits formed from volcanogenic-hypabyssal ore magma[J].Acta Geologica Sinica,1:41-54(in Chinese with English abstract).
    Song X Y,Qi H W,Hu R Z,Chen L M,Yu S Y and Zhang J F.2013.Formation of thick stratiform Fe-Ti oxide layers in layered intrusion and frequent replenishment of fractionated mafic magma:Evidence from the Panzhihua intrusion,SW China[J].Geochemistry,Geophysics,Geosystems,14:712-732.
    Toplis M J,Dingwell D B and Libourel G.1994a.The effect of phosphorus on the iron redox ratio,viscosity,and density of an evolved ferrobasalt[J].Contributions to Mineralogy and Petrology,117(3):293-304.
    Toplis M J,Libourel G and Carroll M R.1994b.The role of phosphorus in crystallisation processes of basalt:An experimental study[J].Geochimica et Cosmochimica Acta,58(2):797-810.
    Veksler I V.2009.Extreme iron enrichment and liquid immiscibility in mafic intrusions:Experimental evidence revisited[J].Lithos,111(1-2):72-82.
    Velasco F,Tornos F and Hanchar J M.2016.Immiscible iron-and silica-rich melts and magnetite geochemistry at the El Laco volcano(northern Chile):Evidence for a magmatic origin for the magnetite deposits[J].Ore Geology Reviews,79:346-366.
    Villemant B and Boudon G.1999.H2O and halogen(F,Cl,Br)behaviour during shallow magma degassing processes[J].Earth and Planetary Science Letters,168(3):271-286.
    Wang B Y,Lang Z J,Li X D,Qu X,Li T F,Hang C and Cui X.1994.Comprehensive survey of geological sections in the west Tianshan of Xinjiang,China[M].Beijing:Science Publish House.202p(in Chinese with English abstract).
    Wang B,Faure M,Shu L S,Cluzel D,Charvet J,De Jong K and Chen Y 2008.Paleozoic tectonic evolution of the Yili Block,western Chinese Tianshan[J].Bulletin de la SociétéGéologique de France,179(5):483-490.
    Wang B,Shu L S,Cluzel D,Faure M and Charvet J.2007.Geochemical constraints on Carboniferous volcanic rocks of the Yili Block(Xinjiang,NW China):Implication for the tectonic evolution of Western Tianshan[J].Journal of Asian Earth Sciences,29(1):148-159.
    Wang C L,Wang Y T,Dong L H,Qin K Z,Evans N J,Zhang B and Ren Y.2018.Iron mineralization at the Songhu deposit,Chinese Western Tianshan:A type locality with regional metallogenic implications[J].International Journal of Earth Sciences,107(1):291-319.
    Wang G Q,Peng J T,Zhang D L,Yang J H and Shen N P.2009.Mineralogy and geochemistry of albties from the Liulincha gold ore belt,Western Hunan Province,China[J].Acta Mineralogica Sinica,(4):463-470(in Chinese with English abstract).
    Wang Q,Zhao Z H,Xu J F,Derek A W,Xiong X L,Zi F and Bai Z H.2006.Carboniferous adakite-high-Mg andesite-Nb-enriched basaltic rock suites in the Northern Tianshan area:Implications for Phanerozoic crustal growth in the Central Asia Orogenic Belt and CuAu mineralization[J].Acta Petrologica Sinica,22(1):11-30(in Chinese with English abstract).
    Wang Z H,Zhang Z H,Jiang Z S,Hong W and Tian J Q.2012.Magnetite composition of Zhibo iron deposit in Western Tianshan Mountains and its genetic significance[J].Mineral Deposits,31(5):983-998(in Chinese with English abstract).
    Wang Z H.2013.Geological characteristics and ore genesis of the Zhibo iron deposit in the western Tianshan Mountains,Xinjiang,NW Chine[D].Supervisor:Zhang Z H Beijing:China University of Geosciences(in Chinese with English abstract).
    Wang Z X,Wu J Y,Liu C D,LüX C and Zhang J G.1990.Polycyclic tectonic evolution and metallogeny of the Tianshan Mountains[M].Beijing:Science Press.217p(in Chinese with English abstract).
    Windley B F,Allen M B,Zhang C,Zhao Z Y and Wang G R.1990.Paleozoic accretion and Cenozoic redeformation of the Chinese Tien Shan Range,central Asia[J].Geology,18(2):128-131.
    Xiao W J,Han C M,Yuan C,Sun M,Lin S F,Chen H L,Li Z L,Li J Land Sun S.2008.Middle Cambrian to Permian subduction-related accretionary orogenesis of Northern Xinjiang,NW China:Implications for the tectonic evolution of central Asia[J].Journal of Asian Earth Sciences,32(2):102-117.
    Xiao W J,Windley B F,Allen M B and Han C M.2013.Paleozoic multiple accretionary and collisional tectonics of the Chinese Tianshan orogenic collage[J].Gondwana Research,23(4):1316-1341.
    Xu L G,Mao J W,Yang F Q,Daniel H and Zheng J M.2010.Geology,geochemistry and age constraints on the Mengku skarn iron deposit in Xinjiang Altai,NW China[J].Journal of Asian Earth Sciences,39:423-440.
    Xu Q D.1989.Genesis and geological significance of feldspars in Limu granites,Guangxi[J].Minerals and Rocks,9(1):15-26(in Chinese with English abstract).
    Yan S,Niu H C,Zhao J X,Bao Z W and Sun W D.2016.Ore-fluid geochemistry and metallogeny of the Dunde iron-zinc deposit in western Tianshan,Xinjiang,China:Evidence from fluid inclusions,REE and C-O-Sr isotopes of calcite[J].Ore Geology Reviews,http://dx.doi.org/10.1016/j.oregeorev.2016.06.024.
    Yang F Q,Mao J W,Xu L G,Zhang Y,Liu F,Huang C L,Zhou G,Liu G R and Dai J Z.2007.REE geochemistry of the Mengku iron deposit,Xingjiang,and its indication for iron mineralization[J].Acta Petrologica Sinica,23(10):2443-2456(in Chinese with English abstract).
    Yang F Q,Mao J W,Chai F M,Liu F,Zhou G,Geng X X,Liu G R and Xu L G.2008.Ore-forming fluids and metallogenesis of Mengku iron deposit in Altay,Xinjiang[J].Mineral Deposits,(6):659-680(in Chinese with English abstract).
    Yang F Q,Mao J W,Liu F,Chai F M,Geng X X,Zhang Z X,Guo X Jand Liu G R.2013.A review of the geological characteristics and mineralization history of iron deposits in the Altay orogenic belt of the Xinjiang,Northwest China[J].Ore Geology Reviews,54:1-16.
    Yuan T.2003.Contrast of geological characteristics between Motuoshala iron(manganese)deposit and Shikebutai iron deposit in West Tianshan Mountain of Xinjiang Autonomous Region[J].Contributions to Geology and Mineral Resources Research,18:88-92(in Chinese with English abstract).
    Zhang J Z,Feng B H,Jin H J,Liu B,Luo Y P,Jin Z M,Zhu M Z and Chen S Z.1987.The genetic relationship between marine volcanic rocks and iron deposit at Abagong-Mengku area,Altay district,Xinjiang and ore-forming geological features[J].Bulletin of Xi'an Institute Geology Mineral Resources,CAGS,20:89-180(in Chinese with English abstract).
    Zhang L M,Liu J B,Cheng N F,Ye K,Guo S,Chen Y and Mao Q.2013.Study on the relationship between the fluid salinity and chlorine content of apatites in eclogite and veins from HP and UHP metamorphic belt of the Dabie-Sulu[J].Acta Petrologica Sinica,29(5):1525-1539(in Chinese with English abstract).
    Zhang X,Tian J Q,Gao J,Klemd R,Dong L H,Fan J J,Jiang T,Hu CJ and Qian Q.2012b.Geochronology and geochemistry of granitoid rocks from the Zhibo syngenetic volcanogenic iron ore deposit in the Western Tianshan Mountains(NW-China):Constraints on the age of mineralization and tectonic setting[J].Gondwana Research,22(2):585-596.
    Zhang Z C,Hou T,Li H M,Li J W,Zhang Z H and Song X Y.2014.Enrichment mechanism of iron in magmatic-hydrothermal system[J].Acta Petrologica Sinica,30(5):1189-1204(in Chinese with English abstract).
    Zhang Z C,Mahoney J J,Mao J W and Wang F S.2006.Geochemistry of picritic and associated basalt flows of the western Emeishan flood basalt province,China[J].Journal of Petrology,47(10):1997-2019.
    Zhang Z H,Hong W,Jiang Z S,Duan S G,Wang Z H,Li F M,Shi F P,Zhao J and Zhen R Q.2012.Geological features,mineralization types and metallogenic setting of Late Paleozoic iron deposits in western Tianshan Mountains of Xinjiang[J].Mineral Deposits,31:941-964(in Chinese with English abstract).
    Zhang Z H,Hong W,Jiang Z S,Duan S G,Xu L G,Li F M,Guo X Cand Zhao Z G.2012a.Geological characteristics and zircon U-Pb dating of volcanic rocks from the Beizhan iron deposit in western Tianshan Mountains,Xinjiang,NW China[J].Acta Geologica Sinica(English edition),86(3):737-747.
    Zhang Z H,Hong W,Jiang Z S,Duan S G,Li F M and Shi F P.2014.Geological characteristics and metallogenesis of iron deposits in western Tianshan,China[J].Ore Geology Reviews,57:425-440.
    Zhao L D,Chen H Y,Zhang L,Li D F,Zhang W F,Wang C M,Yang J T and Yan X L.2016.Magnetite geochemistry of the Heijianshan Fe-Cu(-Au)deposit in Eastern Tianshan:Metallogenic implications for submarine volcanic-hosted Fe-Cu deposits in NWChina[J].Ore Geology Reviews,http://dx.doi.org/10.1016/j.oregeorev.2016.07.022.
    Zhou M F,Arndt N T,Malpas J,Wang C Y and Kennedy A K.2008.Two magma series and associated ore deposit types in the Permian Emeishan large igneous province,SW China[J].Lithos,103:352-368.
    Zhu Y F,Guo X,Song B,Zhang L F and Gu L B.2009.Petrology,SrNd-Hf isotopic geochemistry and zircon chronology of the Late Palaeozoic volcanic rocks in the southwestern Tianshan Mountains,Xinjiang,NW China[J].Journal of the Geological Society,166:1085-1099.
    Zhu Z X,Li J Y,Dong L H,Wang K Z,Zhang X F and Xu S Q.2011.Geological characteristics and tectonic significance of Paleozoic intrusive rocks in western Tianshan of Xinjiang Province[J].Earth Science Frontiers,18(2):170-179(in Chinese with English abstract).
    段士刚,张作衡,魏梦元,田敬佺,蒋宗胜,李凤鸣,赵军,王厚方.2014.新疆西天山雾岭铁矿闪长岩地球化学及锆石U-Pb年代学[J].中国地质,41(6):1757-1770.
    冯金星,石福品,汪帮耀,胡建明,王江涛,田敬佺.2010.西天山阿吾拉勒成矿带火山岩型铁矿[M].北京:地质出版社.111-112,132.
    洪为,张作衡,李华芹,李凤鸣,刘兴忠.2012.新疆西天山查岗诺尔铁矿床成矿时代--来自石榴子石Sm-Nd等时线年龄的信息[J].矿床地质,31(5):1067-1074.
    胡秀军,陈文革.2010.新疆南天山查岗诺尔大型磁铁矿矿床地质特征及矿床成因[J].资源调查与环境,31(3):185-193.
    黄汲清,任纪舜,姜春发,张正坤,秦德余.1980.中国大地构造及其演化[M].北京:科学出版社.1-124.
    蒋宗胜,张作衡,侯可军,洪为,王志华,李凤鸣,田敬佺.2012.西天山查岗诺尔和智博铁矿区火山岩地球化学特征、锆石U-Pb年龄及地质意义[J].岩石学报,28(7):2074-2088.
    兰彩云,赵太平,罗正传,王长乐,文启付,刘立新.2015.河南舞阳赵案庄铁矿床成因:来自磁铁矿和磷灰石的矿物学证据[J].岩石学报,31(6):1653-1670.
    李大鹏,杜杨松,庞振山,涂其军,张永平,葛松胜,沈立军,王开虎.2013.西天山阿吾拉勒石炭纪火山岩年代学和地球化学研究[J].地球学报,34(2):176-192.
    李继磊,苏文,张喜,刘新.2009.西天山阿吾拉勒西段麻粒岩相片麻岩锆石Cameca U-Pb年龄及其地质意义[J].地质通报,28:1852-1862.
    龙灵利,高俊,钱青,熊贤明,王京彬,王玉往,高立明.2008.西天山伊犁地区石炭纪火山岩地球化学特征及构造环境[J].岩石学报,24(4):699-710.
    骆文娟,孙剑.2019.铁氧化物氧同位素示踪原理及其在铁矿成因研究中的应用[J].岩石矿物学杂志.38(1):121-130.
    宋学信,陈毓川,盛继福,艾永德.1981.论火山-浅成矿浆铁矿床[J].地质学报,1:41-55.
    王宝瑜,郎智君,李向东,屈迅,李天福,黄诚,崔曦.1994.中国天山西段地质剖面综合研究[M].北京:科学出版社.202页.
    王国强,彭建堂,张东亮,阳杰华,沈能平.2009.湘西柳林汊金矿带中钠长石的矿物学和地球化学特征[J].矿物学报,(4):463-470.
    王强,赵振华,许继峰,Derek A.Wyman,熊小林,资峰,白正华.2006.天山北部石炭纪埃达克岩-高镁安山岩-富Nb岛弧玄武质岩:对中亚造山带显生宙地壳增生与铜金成矿的意义[J].岩石学报,22(1):11-30.
    王志华,张作衡,蒋宗胜,洪为,田敬佺.2012.西天山智博铁矿床磁铁矿成分特征及其矿床成因意义[J].矿床地质,31(5):983-998.
    王志华.2013.新疆西天山智博铁矿床地质特征及成因研究[D].导师:张作衡,北京:中国地质大学.
    王作勋,邬继易,刘成德,吕喜朝,张经国.1990.天山多旋回构造演化及成矿[M].北京:科学出版社.217页.
    徐启东.1989.广西栗木稀有金属花岗岩中长石的成因与意义[J].矿物岩石,9(1):15-26.
    新疆地矿局第十一地质大队.2012.新疆和静县查岗诺尔-备战铁矿一带1:50000地质矿产图[M].未出版.
    杨富全,毛景文,徐林刚,张岩,刘锋,黄成林,周刚,刘国仁,代军治.2007.新疆蒙库铁矿床稀土元素地球化学及对铁成矿作用的指示[J].岩石学报,23(10):2443-2456.
    杨富全,毛景文,柴凤梅,刘锋,周刚,耿新霞,刘国仁,徐林刚.2008.新疆阿尔泰蒙库铁矿床的成矿流体及成矿作用[J].矿床地质,27(6):659-680.
    袁涛.2003.新疆西天山莫托沙拉铁(锰)矿床与式可布台铁矿床地质特征对比[J].地质找矿论丛,18:88-92.
    张建中,冯秉寰,金浩甲,刘斌,罗玉鹏,金志明,朱美珠,陈书章.1987.新疆阿勒泰阿巴宫-蒙库海相火山岩与铁矿的成生关系及成矿地质特征[J].中国地质科学院西安地质矿产研究所所刊,20:89-180.
    张灵敏,刘景波,程南飞,叶凯,郭顺,陈意,毛骞.2013.大别-苏鲁高压,超高压变质带榴辉岩和脉体中磷灰石氯含量和流体盐度关系的研究[J].岩石学报,29(5):1525-1539.
    张招崇,侯通,李厚民,李建威,张作衡,宋谢炎.2014.岩浆-热液系统中铁的富集机制探讨[J].岩石学报,30(5):1189-1204.
    张作衡,洪为,蒋宗胜,段士刚,王志华,李凤鸣,石福品,赵军,郑仁乔.2012.新疆西天山晚古生代铁矿床的地质特征、矿化类型及形成环境[J].矿床地质,31(5):941-964.
    朱志新,李锦轶,董连慧,王克卓,张晓帆,徐仕琪.2011.新疆西天山古生代侵入岩的地质特征及构造意义[J].地学前缘,18(2):170-179.

© 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