黄山东铜镍矿的韧性变形特征和磁黄铁矿形成机制研究
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摘要
黄山东铜镍硫化物矿床产于东天山地区的黄山—镜儿泉韧性剪切带中,大地构造上属中亚造山带东天山觉罗塔格岛弧带。该铜镍矿所在的黄山东镁铁—超镁铁岩体呈纺锤状侵位于晚石炭世火山岩中,其边部发生了与区域剪切带总体走向一致的强烈糜棱岩化作用。矿床中的部分矿体发生强烈韧性变形,其中17号矿体完全产于韧性变形带内,岩石和矿石都发生了强烈的破碎和蚀变而形成矿石糜棱岩。在上述韧性变形带内,还发育一定规模的网脉状和细脉状富铜碳酸盐—硫化物脉。论文在野外地质和构造形迹观察的基础上,对黄山东矿床不同类型的矿石开展了细致的显微岩相和矿相学观察,识别出三种类型矿石:原生矿石、强烈变形矿石和热液叠加矿石。海绵陨铁结构的原生矿石中,脉石矿物几乎不发生蚀变和变形,矿石矿物仅发生脆性破裂;强烈变形矿石中,脉石矿物和矿石矿物均发生强烈变形,主要以纤闪石的波状消光和膝折、金云母的书斜构造、磁黄铁矿的定向拉长为特征;热液叠加矿石中的磁黄铁矿普遍发育颗粒的扁平化、重结晶,局部可见磁黄铁矿的退火平衡结构。黄山东铜镍硫化物矿床的侵位与变形时间与区域黄山-镜儿泉剪切带的韧性剪切作用时间相一致。岩体冷却过程经历的强烈韧性剪切变形作用不但造成矿石矿物的强烈韧性变形而形成矿石糜棱岩,还使伴生脉石矿物发生细粒化和热液蚀变,释放出流体和成矿元素,并叠加于变形的矿石和岩石之上,从而形成了网脉状和细脉状矿体。黄山东铜镍矿的原生硫化物固熔体铁含量较高,因而在硫化物熔体结晶过程只形成六方磁黄铁矿而无伴生单斜磁黄铁矿和黄铁矿。在热液叠加过程中,流体沿边缘和裂隙面交代早期六方磁黄铁矿,形成单斜磁黄铁矿反应边。本次研究还发现六方磁黄铁矿形成的新机制:即在高硫逸度和高氧逸度的条件下,随着体系温度的降低,单斜磁黄铁矿可从热液六方磁黄铁矿中出溶形成呈叶片状单斜—六方磁黄铁矿交生体。
Huangshandong Ni-Cu sulfide deposit,located in the Huangshan-Jing'erquan ductile shear zone,belongs to the Jueluotage island arc belt of the Eastern Tianshan area,Central Asian Orogenic Belt. The Huangshandong mafic-ultramafic pluton,in shape offusiform,intruded in the Late Carboniferous volcanic rocks with intensive foliation near the margin of the pluton which is consistent with the strike of the regional ductile shear zone. Some orebodies in the deposit also show intensive ductile deformation. The No.17 orebody was totally controlled and hosted by the ductile shear zone. The rocks and ores from the No.17 orebody show intensive deformation and alteration and could be called as ore mylonites. Considerable amounts of network and veinlet copper-rich carbonate-sulfide veins can be also observed in this ductile shear zone. In this contribution,detailed microscopy petrography and mineralography observation were carried out on different types of ores from the Huangshandong deposit. Combined with field geological investigation and ore fabric observation,three different types of ores were distinguished,that is,magmatic ores,deformed ores and fluid-overprinted ores. Magmatic ores with sideronitic fabric are barely altered and deformed,and sulfide minerals in it only show some brittle fractures. Deformed ores develop intensive deformation fabric in silicate and sulfide minerals,such as the kink bands,wavy extinction of uralite,domino structure of phlogopite and the elongation of pyrrhotite. Fluid-overprinted ores are characterized by strongly deformation,flattened grains and recrystallization of pyrrhotites,and annealing of pyrrhotites can also be occasionally observed. Intruding of Huangshandong pluton is coeval with ductile deformation and regional ductile shearing. During intruding and cooling of the pluton,intensive regional ductile shearing induced ductile deformation of sulfide ores and then ore mylonites formed. Gangue minerals in the deformed orebodies were crushed to fine-grained minerals and altered. In these processes,fluid and metallogenic elements were released and overprinted into deformed rocks and ores,forming network and veinlet ores. Owing to containing higher iron in original sulfide solid solution,the magmatic Ni-Cu sulfide ores in Huangshandong deposit could only form hexagonal pyrrhotite without associated monoclinic pyrrhotite and pyrite during the crystallization process of sulfide solid solution. During hydrothermal overprinting process,fluid overprinting occurred along margins and fractures of earlier stage magmatic hexagonal pyrrhotite,formed monoclinic pyrrhotite reactional rims. Our studies argued that monoclinic pyrrhotite can also be formed during hydrothermal precipitation processes. In this process,monoclinic pyrrhotites can exsolved from hexagonal grains in high oxygen and sulfur fugacity environments,as the cooling of such hydrothermal fluids.
Huangshandong Ni-Cu sulfide deposit,located in the Huangshan-Jing'erquan ductile shear zone,belongs to the Jueluotage island arc belt of the Eastern Tianshan area,Central Asian Orogenic Belt. The Huangshandong mafic-ultramafic pluton,in shape offusiform,intruded in the Late Carboniferous volcanic rocks with intensive foliation near the margin of the pluton which is consistent with the strike of the regional ductile shear zone. Some orebodies in the deposit also show intensive ductile deformation. The No.17 orebody was totally controlled and hosted by the ductile shear zone. The rocks and ores from the No.17 orebody show intensive deformation and alteration and could be called as ore mylonites. Considerable amounts of network and veinlet copper-rich carbonate-sulfide veins can be also observed in this ductile shear zone. In this contribution,detailed microscopy petrography and mineralography observation were carried out on different types of ores from the Huangshandong deposit. Combined with field geological investigation and ore fabric observation,three different types of ores were distinguished,that is,magmatic ores,deformed ores and fluid-overprinted ores. Magmatic ores with sideronitic fabric are barely altered and deformed,and sulfide minerals in it only show some brittle fractures. Deformed ores develop intensive deformation fabric in silicate and sulfide minerals,such as the kink bands,wavy extinction of uralite,domino structure of phlogopite and the elongation of pyrrhotite. Fluid-overprinted ores are characterized by strongly deformation,flattened grains and recrystallization of pyrrhotites,and annealing of pyrrhotites can also be occasionally observed. Intruding of Huangshandong pluton is coeval with ductile deformation and regional ductile shearing. During intruding and cooling of the pluton,intensive regional ductile shearing induced ductile deformation of sulfide ores and then ore mylonites formed. Gangue minerals in the deformed orebodies were crushed to fine-grained minerals and altered. In these processes,fluid and metallogenic elements were released and overprinted into deformed rocks and ores,forming network and veinlet ores. Owing to containing higher iron in original sulfide solid solution,the magmatic Ni-Cu sulfide ores in Huangshandong deposit could only form hexagonal pyrrhotite without associated monoclinic pyrrhotite and pyrite during the crystallization process of sulfide solid solution. During hydrothermal overprinting process,fluid overprinting occurred along margins and fractures of earlier stage magmatic hexagonal pyrrhotite,formed monoclinic pyrrhotite reactional rims. Our studies argued that monoclinic pyrrhotite can also be formed during hydrothermal precipitation processes. In this process,monoclinic pyrrhotites can exsolved from hexagonal grains in high oxygen and sulfur fugacity environments,as the cooling of such hydrothermal fluids.
引文
陈文,孙枢,张彦,等.2005.新疆东天山秋格明塔什-黄山韧性剪切带40Ar/39Ar年代学研究[J].地质学报,79(6):790-804.
顾连兴,胡受奚,于春水,等.2001.论博格达俯冲撕裂型裂谷的形成与演化[J].岩石学报,17(4):585-597.
顾连兴,张遵忠,吴昌志,等.2007.东天山黄山-镜儿泉地区二叠纪地质-成矿-热事件:幔源岩浆内侵及其地表效应[J].岩石学报,23(11):2869-2880.
顾连兴,张遵忠,吴昌志,等.2006.关于东天山花岗岩与陆壳垂向增生的若干认识[J].岩石学报,22(5):1103-1120.
郭召杰,马瑞士.1990.东天山晚古生带康古尔弧间盆地研究[J].南京大学学报(地球科学),2(3):103-113.
韩宝福,何国琦,王式洸,等.1998.新疆北部后碰撞幔源岩浆活动与陆壳纵向生长[J].地质评论,44(4):396-406.
李锦轶,宋彪,王克卓,等.2006a.东天山吐哈盆地南缘二叠纪幔源岩浆杂岩:中亚地区陆壳垂向增生的地质记录[J].地球学报,27(5):424-446.
李锦轶,王克卓,孙桂华,等.2006b.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,22(5):424-446
马瑞士,舒良树,孙家齐.1997.东天山构造演化与成矿[M].北京:地质出版社.
马瑞士,王赐银,叶尚夫.1993.东天山构造格架与地壳演化[M].北京:地质出版社.
毛景文,杨建明,屈文俊,等.2002a.新疆黄山东铜镍硫化物矿床Re-Os同位素测定及其地球动力学意义[J].矿床地质,21(4):323-330.
毛启贵,肖文交,韩春明,等.2006.新疆东天山白石泉铜镍矿床基性-超基性岩体锆石U-Pb同位素年龄、地球化学特征及其对古亚洲洋闭合时限的制约[J].岩石学报,22(1):153-162.
秦克章,方同辉,王书来,等.2002.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,20(4):302-308.
孙涛,钱壮志,汤中立,等.2010.新疆葫芦铜镍矿床锆石U-Pb年代学、铂族元素地球化学特征及其地质意义[J].岩石学报,26(11):3339-3349.
汤中立,李文渊.1995金川铜镍硫化物矿床模式及地质特征对比[M].北京:地质出版社:208-209.
唐俊华,顾连兴,张遵忠,等.2007.东天山咸水泉片麻状花岗岩特征、年龄及成因[J].岩石学报,23(6):1803-1820.
王赐银,朱文斌,马瑞士.1992.东天山苦水变质地带变质作用特征及其成因研究[J].南京大学学报(自然科学版),28(4):595-604.
王瑞廷,毛景文,赫英,等.2005.煎茶岭硫化镍矿床的铂族元素地球化学特征及其意义[J].岩石学报,21:215-226.
王亚磊,张照伟,尤敏鑫,等.2015.东天山白鑫滩铜镍矿锆石U-Pb年代学、地球化学特征及对Ni-Cu找矿的启示[J].中国地质,42(3):452-467.
吴昌志,张遵忠,Khin Zaw,等.2006.东天山觉罗塔格红云滩花岗岩年代学、地球化学及其构造意义[J].岩石学报,22(5):1121-1134.
肖庆华,秦克章,唐冬梅,等.2010.新疆哈密香山西铜镍-钛铁矿床系同源岩浆分异演化产物-矿相学、锆石U-Pb年代学及岩石地球化学证据[J].岩石学报,26(2):503-522.
徐湘康,李新峰.1994.康古尔塔格韧性剪切带变质作用研究[J].新疆地质,12(3):259-264.
周济元,茅燕石,黄志勋,等.1994.东天山古大陆边缘火山地质[M].成都:成都科技大学出版社.
Almeida C M and Olivo G R.2007.The Ni-Cu-PGE sulfide ores of the komatiite-hosted Fortaleza de Minas deposit,Brazil:evidence of hydrothermal remobilization[J].The Canadian Mineralogist,45(4):751-773.
Arnold R G.1962.Equilibrium relations between pyrrhotite and pyrite from 325°C to 743°C[J].Economic Geology,57:72-90.
Arnold R G.1967.Range in composition and structure of 82 natural terrestrial pyrrhotites[J].The Canadian Mineralogist,9:31-50.
Arnold R G.1969.Pyrrhotite phase relation below 304 atm total pressure[J].Economic Geology,64(4):405-419.
Avouac J P,Tapponnier P,Bai M,et al.1993.Active thrusting and folding along the northern Tien Shan and Late Cenozoic rotation of the Tarim relative to Dzungaria and Kazakhstan[J].Journal of Geophysical Research-Solid Earth,98(B4):6755-6804
Barnes S and Hill R.2000.Metamorphism of komatiite-hosted nickel sulfide deposits[J].Reviews in Economic Geology,11:203-215.
Barnes S J and Lightfoot P C.2005.Formation of magmatic nickel sulfide ore deposits and processes affection their copper and platinum group element contents,Economic Geology One Hundredth Anniversary Volume[J].Society of Economic Geologists,179-213.
Barrett F M,Binns R A,Groves D I,et al.1977.Structural history and metamorphic modification of Archean volcanic-type nickel deposits,Yilgarn Block,Western Australia[J].Economic Geology,72(7):1195-1223.
Bennett C E G,Graham J and Thornber M R.1972.New observations on natural pyrrhotites,Part I.mineralographic techniques[J].American Mineralogist,57:445-462.
Branquet Y,Gumiaux C,Sizaret S,et al.2012.Synkinematic mafic/ultramafic sheeted intrusions:emplacement mechanism and strain restoration of the Permian Huangshan Ni-Cu ore belt(Eastern Tianshan,NW China)[J].Journal of Asian Earth Sciences,56:240-257.
Bystr9m A.1945.Monoclinic magnetic pyrites.Ark.Kemi[J].Mineral Geology,19B:1-8.
Carpenter R H and Desborough B A.1964.Range in solid solution and structure of naturally occurring troilite and pyrrhotite[J].American Mineralogist,49:1350-65.
Dare S A,Barnes S J,Prichard H M,et al.2011.Chalcophile and platinum-group element(PGE)concentrations in the sulfide minerals from the Mc Creedy East deposit,Sudbury,Canada,and the origin of PGE in pyrite[J].Mineralium Deposita,46(4):381-407.
Deng Y F,Song X Y,Chen L M,et al.2014.Geochemistry of the Huangshandong Ni-Cu deposit in northwestern China:implications for the formation of magmatic sulfide mineralization in orogenic belts[J].Ore Geology Reviews,56:181-198.
Desborough G A and Carpenter R H.1965.Phase relations of pyrrhotite[J].Economic geology,60(7):1431-1450.
Dillon-Leitch H C H,Watkinson D H and Coats C J A.1986.Distribution of platinum-group elements in the Donaldson West deposit,Cape Smith Belt,Quebec[J].Economic Geology,81:1147-1158.
Duckworth R C and Rickard D.1993.Sulfide mylonites from the Renstrom VMS deposit,Northern Sweden[J].Mineralogical Magazine,57:83-92
Duuring P,Bleeker W and Beresford S W.2007.Structural modification of the komatiite-associated Harmony nickel sulfide deposit,Leinster,Western Australia[J].Economic Geology,102(2):277-297.
Duuring P,Bleeker W,Beresford S W,et al.2010.Towards a volcanicstructural balance:relative importance of volcanism,folding,and remobilisation of nickel sulphides at the Perseverance Ni-Cu-(PGE)deposit,Western Australia[J].Mineralium Deposita,45(3):281-311.
Farrow C E G and Watkinson D H.1996.Geochemical evolution of the epidote zone,Fraser mine,Sudbury,Ontario:Ni-Cu-PGEremobilization by saline fluids[J].Mining Geology,5:17-31.
Gao J F,Zhou M F,Lightfoot P C,et al.2013.Sulfide saturation and magma emplacement in the formation of the Permian Huangshandong Ni-Cu sulfide deposit,Xinjiang,northwestern China[J].Economic Geology,108(8):1833-1848.
Gervilla F and Kojonen K.2002.The platinum-group minerals in the upper section of the Keivitsansarvi Ni-Cu-PGE deposit,Northern Finland[J].The Canadian Mineralogist,40:377-394.
González-álvarez I,Porwal A,Bereford S W,et al.2010.Hydrothermal Ni prospectivity analysis of Tasmania,Australia[J].Ore Geology Reviews,38:168-183.
Grotenhuis S M,Trouw R A J and Passchier C W.2003.Evolution of mica fish in mylonitic rocks[J].Tectonophysics,372:1-21.
Gu L X and Vokes F M.1996.Intergrowths of hexagonal and monoclinic pyrrhotites in some sulphide ores from Norway[J].Mineralogical Magazine,60:303-316.
Gu L X,Zheng Y C,Tang X Q,et al.2007.Copper,gold and silver enrichment in ore mylonites within massive sulphide orebodies at Hongtoushan VHMS deposit,NE China[J].Ore Geology Reviews,30(1):1-29.
Gu L X,Zhu J L,Guo J C,et al.1995.Geology and genesis of the maficultramafic complexes in the Huangshan-Jingerquan belt,East Xinjiang[J].Chinese Journal of Geochemistry(English edition),14(2):97-116.
Han B F,Ji J Q,Song B,et al.2004.SHRIMP zircon U-Pb ages of Kalatongke No.1 and Huangshandong Cu-Ni-bearing maficultramafic complexes,North Xinjiang,and geological implications[J].Chinese Science Bulletin,49(22):2424-2429.
Han C M,Xiao W J,Zhao G C,et al.2010.In-situ U-Pb,Hf and Re-Os isotopic analyses of the Xiangshan Ni-Cu-Co deposit in Eastern Tianshan(Xinjiang),Central Asia Orogenic Belt:constraints on the timing and genesis of the mineralization[J].Lithos,120(3):547-562.
Han C M,Xiao W J,Zhao G C,et al.2013.SIMS U-Pb zircon dating and Re-Os isotopic analysis of the Hulu Cu-Ni deposit,eastern Tianshan,Central Asian Orogenic Belt,and its geological significance[J].Journal of Geoscience,58:251-270.
Hoatson D M,Jaireth S and Jaques A L.2006.Nickel sulfide deposits in Australia:Characteristics,resources,and potential[J].Ore Geology Reviews,29:177-241.
Kissin S A and Scott S D.1982.Phase relations involving pyrrhotite below 350 degrees[J].Economic Geology,77(7):1739-1754.
Lei R X,Wu C Z,Gu L X,et al.2011.Zircon U-Pb chronology and Hf isotope of the Xingxingxia granodiorite from the Central Tianshan zone(NW China):Implications for the tectonic evolution of the southern Altaids[J].Gondwana Research,20:582-593.
Li J Y,Xiao W J,Wang K Z,et al.2003.Neoproterozoic-Paleozoic tectonostratigraphy,magmatic activities and tectonic evolugion of Eastern Xinjiang,NW China[C]//.Mao J,Goldfarb R J,Seltmann R,Wang D,Xiao W,Hart C(eds),Tectonic Evolution and Metallogeny of the Chinese Altay and Tianshan.Proceedings Volume of the International Symposium of the IGCP-473 Project in Urumuqi and Guidebook of the Field Excursion in Xinjiang,China.August 9-21,IAGOD Guidbook Series 10:CERCAMS/NHM London,31-74.
Maiden K J,Chimimba L R and Smalley T J.1986.Cuspate ore-wall rock interfaces,piercement structures and the localization of some sulfide ores in deformed sulfide deposits[J].Economic Geology,81(6):1464-1472.
Mancini F and Papunen H.2000.Metamorphism of Ni-Cu sulfides in mafic-ultramafic intrusions:The Svecofennian Saaksjarvi complex,southern Finland[J].Metamorphosed and metamorphogenic ore deposits(Reviews in Economic Geology),11:217-231.
Mao Y J,Qin K Z,Li C,et al.2015.A modified genetic model for the Huangshandong magmatic sulfide deposit in the Central Asian Orogenic Belt,Xinjiang,western China[J].Mineralium Deposita,50:65-82.
Mao J W,Yang J M,Qu W J,et al.2003.Re-Os age of cu-Ni ores from the Huangshandong Cu-Ni sulfide deposit in the east Tianshan Mountains and its Implication for geodynamic processes[J].Acta Geologica Sinica(English Edition),77(2):220-226.
Menard T,Lesher C M,Stowell H H,et al.1996.Geology,genesis,and metamorphic history of the Namew Lake Ni-Cu deposit,Manitoba[J].Economic Geology,91(8):1394-1413.
Miyashiro A.1994.Metamorphic Petrology[J].London:University College London Press.
Molnár F,Watkinson D H and Everest J O.1999.Fluid-inclusion characteristics of hydrothermal Cu-Ni-PGE veins in granitic and metavolcanic rocks at the contact of the Little Stobie deposit,Sudbury,Canada[J].Chemical Geology,154(1):279-301.
Naldrett A J,Wilson A,Kinnaird J,et al.2009.PGE tenor and metal ratios within and below the Merensky Reef,Bushveld Complex:implications for its genesis[J].Journal of Petrology,50(4):625-659.
Naldrett A J.2004.Magmatic Sulfide Deposits:Geology,Geochemistry and Exploration[M].Springer Science&Business Media.
Qi L and Zhou M F.2008.Platinum-group elemental and Sr-Nd-Os isotopic geochemistry of Permian Emeishan flood basalts in Guizhou Province,SW China[J].Chemical Geology,248:83-103.
Qin K Z,Su B X,Sayyi P A,et al.2011.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[J].American Journal of Science,311(3):237-260.
Shu L S,Charvet J,Guo L Z,et al.1999.A large-scale Palaeozoic dextral ductile strike-slip zone:The Aqqikkudug-Weiya zone along the northern margin of the Central Tianshan belt,Xinjiang,NW China[J].Acta Geologica Sinica(English Edition),73(2):148-162.
Simpson C.1985.Deformation of granitic rock across the brittle-ductile transition[J].Journal of Structural Geology,7(5):503-511.
Song X Y,Keays R R,Zhou M F,et al.2009.Siderophile and chalcophile elemental constraints on the origin of the Jinchuan NiCu-(PGE)sulfide deposit,NW China[J].Geochimica et Cosmochimica Acta,73:404-424.
Su B X,Qin K Z,Sakyi P A,et al.2010.U-Pb ages and Hf-O isotopes of zircons from Late Paleozoic mafic-ultramafic units in the southern Central Asian Orogenic Belt:Tectonic implications and evidence for an Early-Permian mantle plume[J].Gondwana Research,20:516-531.
Su B,Qin K,Sakyi P A,et al.2012.Geochronologic-petrochemical studies of the Hongshishan mafic-ultramafic intrusion,Beishan area,Xinjiang(NW China):petrogenesis and tectonic implications[J].International Geology Review,54(3):270-289.
Sun X M,Wang S W,Sun W D,et al.2008.PGE geochemistry and ReOs dating of massive sulfide ores from the Baimazhai Cu-Ni deposit,Yunnan province,China[J].Lithos,105:12-24.
Sugaki A,Shima A,Kitakaze A,et al.1977.Hydrothermal synthesis of pyrrhotites and their phase relation at low temperature.Studies on the pyrrhotite group minerals(4).Tohoku Univ.Sci.Rept.,ser.3(13):65-82
Schiffries C M.1982.The petrogenesis of a platiniferous dunite pipe in the Bushveld Complex:infiltration metasomatism by a chloride solution[J].Economic Geology,77:1439-1453.
Seng9r A M C,Natal'In B A and Burtman V S.1993.Evolution of the Altaid tectonic collage and Palaeozoic crustal growth in Eurasia[J].Nature,364:299-307.
Ripley E M,Sarkar A and Li C S.2005.Mineralogic and stable isotope studies of hydrothermal alteration at the Jinchuan Ni-Cu deposit,China[J].Economic Geology,100(7):1349-1361.
Tang D M,Qin K Z,Li C S,et al.2011.Zircon dating,Hf-Sr-Nd-Os isotopes and PGE geochemistry of the Tianyu sulfide-bearing maficultramafic intrusion in the Central Asian Orogenic Belt,NW China[J].Lithos,126:84-98.
Tang D M,Qin K Z,Sun H,et al.2012.The role of crustal contamination in the formation of Ni-Cu sulfide deposits in Eastern Tianshan,Xinjiang,Northwest China:Evidence from trace element geochemistry,Re-Os,Sr-Nd,zircon Hf-O,and sulfur isotopes[J].Journal of Asian Earth Sciences,49:145-160.
Tao Y,Li C S,Hu R Z,et al.2010.Re-Os isotopic constranits on the genesis of the Limahe Ni-Cu deposit in hte Emeishan large ignous province,SW China[J].Lithos,119:137-146.
Tapponnier P and Molnár P.1979.Active faulting and Cenozoic tectonics of the Tienshan,Mongolia and Baykal regions[J].Journal of Geophysical Research,84:3425-3459.
Tomkins A G,Frost B R and Pattison D R M.2006.Arsenopyrite melting during metamorphism of sulfide ore deposits[J].The Canadian Mineralogist,44:1325-1342.
Vaughan D J and Ridout M S.1970.M9ssbauer study of pyrrhotite[J].Solid State Communications,8(24):2165-2167.
Wang B,Cluzel D,Jahn B M,et al.2014.Late Paleozoic pre and syn-kinematic plutons of the Kangguer-Huangshan shear zone:inference on the tectonic evolution of the eastern Chinese north Tianshan[J].American Journal of Science,314(1):43-79.
Wang B,Faure M,Shu L S,et al.2008.Paleozoic tectonic evolution of the Yili Block,western Chinese Tianshan[J].Bulletin de la SociétéGéologique de France,179(5):483-490.
Wang C Y and Zhou M F.2006.Genesis of the Permian Baimazhai magmatic Ni-Cu-(PGE)sulfide deposit,Yunnan,SW China[J].Mineralium Deposita,41:771-783.
Wood S A,Mountain BW and Fenlon B J.1992.Thermodynamic constraints on the solubility of platinum and palladium in hydrothermal solutions:Reassessment of hydroxide,bisulfide,and ammonia complexing[J].Economic Geolgoy,84:2020-2028.
Wu F Y,Wilde S A,Zhang G L,et al.2004.Geochronology and petrogenesis of the post-orogenic Cu-Ni sulfide-bearing mafic-ultramafic complexes in Jilin Province,NE China[J].Journal of Asian Earth Sciences,23:781-797.
Xiao W J,Windley B F,Badarch G,et al.2004.Palaeozoic accretionary and convergent tectonics of the southern Altaids:implications for the lateral growth of Central Asia[J].Journal of the Geological Society,London,161:339-342.
Xu X M,Ma T L,Sun L Q,et al.2003.Characteristics and dynamic origin of the large-scale Jiaoluotage ductile compressional zone in the eastern Tianshan Mountains,China[J].Journal of Structural Geology,25:1901-1915.
Yang X Z,Ishihara S and Zhao D H.2006.Genesis of the Jinchuan PGEdeposit,China:evidence from fluid inclusions,mineralogy and geochemistry of preious elements[J].Mineralogy and Petrology,86:109-128.
Yund R A and Hall H T.1969.Hexagonal and monoclinic pyrrhotites[J].Economic Geology,64:420-3.
Zhang L C,Shen Y C and Ji J S.2003.Characteristics and genesis of Kanggur gold deposit in the eastern Tianshan mountains,NW China:Evidence from geology,isotope distribution and chronology[J].Ore Geology Reviews,23:71-90.
Zhang M J,Li C S,Fu P E,et al.2011.The Permian Huangshanxi Cu-Ni deposit in western China:intrusive-extrusive association,ore genesis,and exploration implications[J].Mineralium Deposita,46:153-170.
Zhang Z C,Zhi X C,Chen L,et al.2008.Re-Os isotopic compositions of picrites form the Emeishan flood basalt province,China[J].Earth and Planetary Science Letters,276:30-39.
Zhong H,Yao Y,Prevec S A,et al.2004.Trace-element and Sr-Nd isotopic geochemistry of the PGE-bearing Xiejie layed intrusion in SW China[J].Chemical Geology,203:237-252.
Zhou M F,Lesher C M,Yang Z,et al.2004.Geochemistry and petrogenesis of 270 Ma Ni-Cu-(PGE)sulfide-bearing mafic intrusions in the Huangshan district,Eastern Xinjiang,Northwest China:implications for the tectonic evolution of the Central Asian orogenic belt[J].Chemical Geology,209(3):233-257.
Zhu W G,Zhong H,Hu R Z,et al.2010.Platinum-group minerals and tellurides from the PGE-bearing Xinjie layered intrusion in the Eemishan Large Igneous Province,SW China[J].Mineralogy and Petrology,98(1-4):167-180.
(1)据新疆地质矿产勘查开发局第6大队1988年的勘察报告。
顾连兴,胡受奚,于春水,等.2001.论博格达俯冲撕裂型裂谷的形成与演化[J].岩石学报,17(4):585-597.
顾连兴,张遵忠,吴昌志,等.2007.东天山黄山-镜儿泉地区二叠纪地质-成矿-热事件:幔源岩浆内侵及其地表效应[J].岩石学报,23(11):2869-2880.
顾连兴,张遵忠,吴昌志,等.2006.关于东天山花岗岩与陆壳垂向增生的若干认识[J].岩石学报,22(5):1103-1120.
郭召杰,马瑞士.1990.东天山晚古生带康古尔弧间盆地研究[J].南京大学学报(地球科学),2(3):103-113.
韩宝福,何国琦,王式洸,等.1998.新疆北部后碰撞幔源岩浆活动与陆壳纵向生长[J].地质评论,44(4):396-406.
李锦轶,宋彪,王克卓,等.2006a.东天山吐哈盆地南缘二叠纪幔源岩浆杂岩:中亚地区陆壳垂向增生的地质记录[J].地球学报,27(5):424-446.
李锦轶,王克卓,孙桂华,等.2006b.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,22(5):424-446
马瑞士,舒良树,孙家齐.1997.东天山构造演化与成矿[M].北京:地质出版社.
马瑞士,王赐银,叶尚夫.1993.东天山构造格架与地壳演化[M].北京:地质出版社.
毛景文,杨建明,屈文俊,等.2002a.新疆黄山东铜镍硫化物矿床Re-Os同位素测定及其地球动力学意义[J].矿床地质,21(4):323-330.
毛启贵,肖文交,韩春明,等.2006.新疆东天山白石泉铜镍矿床基性-超基性岩体锆石U-Pb同位素年龄、地球化学特征及其对古亚洲洋闭合时限的制约[J].岩石学报,22(1):153-162.
秦克章,方同辉,王书来,等.2002.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,20(4):302-308.
孙涛,钱壮志,汤中立,等.2010.新疆葫芦铜镍矿床锆石U-Pb年代学、铂族元素地球化学特征及其地质意义[J].岩石学报,26(11):3339-3349.
汤中立,李文渊.1995金川铜镍硫化物矿床模式及地质特征对比[M].北京:地质出版社:208-209.
唐俊华,顾连兴,张遵忠,等.2007.东天山咸水泉片麻状花岗岩特征、年龄及成因[J].岩石学报,23(6):1803-1820.
王赐银,朱文斌,马瑞士.1992.东天山苦水变质地带变质作用特征及其成因研究[J].南京大学学报(自然科学版),28(4):595-604.
王瑞廷,毛景文,赫英,等.2005.煎茶岭硫化镍矿床的铂族元素地球化学特征及其意义[J].岩石学报,21:215-226.
王亚磊,张照伟,尤敏鑫,等.2015.东天山白鑫滩铜镍矿锆石U-Pb年代学、地球化学特征及对Ni-Cu找矿的启示[J].中国地质,42(3):452-467.
吴昌志,张遵忠,Khin Zaw,等.2006.东天山觉罗塔格红云滩花岗岩年代学、地球化学及其构造意义[J].岩石学报,22(5):1121-1134.
肖庆华,秦克章,唐冬梅,等.2010.新疆哈密香山西铜镍-钛铁矿床系同源岩浆分异演化产物-矿相学、锆石U-Pb年代学及岩石地球化学证据[J].岩石学报,26(2):503-522.
徐湘康,李新峰.1994.康古尔塔格韧性剪切带变质作用研究[J].新疆地质,12(3):259-264.
周济元,茅燕石,黄志勋,等.1994.东天山古大陆边缘火山地质[M].成都:成都科技大学出版社.
Almeida C M and Olivo G R.2007.The Ni-Cu-PGE sulfide ores of the komatiite-hosted Fortaleza de Minas deposit,Brazil:evidence of hydrothermal remobilization[J].The Canadian Mineralogist,45(4):751-773.
Arnold R G.1962.Equilibrium relations between pyrrhotite and pyrite from 325°C to 743°C[J].Economic Geology,57:72-90.
Arnold R G.1967.Range in composition and structure of 82 natural terrestrial pyrrhotites[J].The Canadian Mineralogist,9:31-50.
Arnold R G.1969.Pyrrhotite phase relation below 304 atm total pressure[J].Economic Geology,64(4):405-419.
Avouac J P,Tapponnier P,Bai M,et al.1993.Active thrusting and folding along the northern Tien Shan and Late Cenozoic rotation of the Tarim relative to Dzungaria and Kazakhstan[J].Journal of Geophysical Research-Solid Earth,98(B4):6755-6804
Barnes S and Hill R.2000.Metamorphism of komatiite-hosted nickel sulfide deposits[J].Reviews in Economic Geology,11:203-215.
Barnes S J and Lightfoot P C.2005.Formation of magmatic nickel sulfide ore deposits and processes affection their copper and platinum group element contents,Economic Geology One Hundredth Anniversary Volume[J].Society of Economic Geologists,179-213.
Barrett F M,Binns R A,Groves D I,et al.1977.Structural history and metamorphic modification of Archean volcanic-type nickel deposits,Yilgarn Block,Western Australia[J].Economic Geology,72(7):1195-1223.
Bennett C E G,Graham J and Thornber M R.1972.New observations on natural pyrrhotites,Part I.mineralographic techniques[J].American Mineralogist,57:445-462.
Branquet Y,Gumiaux C,Sizaret S,et al.2012.Synkinematic mafic/ultramafic sheeted intrusions:emplacement mechanism and strain restoration of the Permian Huangshan Ni-Cu ore belt(Eastern Tianshan,NW China)[J].Journal of Asian Earth Sciences,56:240-257.
Bystr9m A.1945.Monoclinic magnetic pyrites.Ark.Kemi[J].Mineral Geology,19B:1-8.
Carpenter R H and Desborough B A.1964.Range in solid solution and structure of naturally occurring troilite and pyrrhotite[J].American Mineralogist,49:1350-65.
Dare S A,Barnes S J,Prichard H M,et al.2011.Chalcophile and platinum-group element(PGE)concentrations in the sulfide minerals from the Mc Creedy East deposit,Sudbury,Canada,and the origin of PGE in pyrite[J].Mineralium Deposita,46(4):381-407.
Deng Y F,Song X Y,Chen L M,et al.2014.Geochemistry of the Huangshandong Ni-Cu deposit in northwestern China:implications for the formation of magmatic sulfide mineralization in orogenic belts[J].Ore Geology Reviews,56:181-198.
Desborough G A and Carpenter R H.1965.Phase relations of pyrrhotite[J].Economic geology,60(7):1431-1450.
Dillon-Leitch H C H,Watkinson D H and Coats C J A.1986.Distribution of platinum-group elements in the Donaldson West deposit,Cape Smith Belt,Quebec[J].Economic Geology,81:1147-1158.
Duckworth R C and Rickard D.1993.Sulfide mylonites from the Renstrom VMS deposit,Northern Sweden[J].Mineralogical Magazine,57:83-92
Duuring P,Bleeker W and Beresford S W.2007.Structural modification of the komatiite-associated Harmony nickel sulfide deposit,Leinster,Western Australia[J].Economic Geology,102(2):277-297.
Duuring P,Bleeker W,Beresford S W,et al.2010.Towards a volcanicstructural balance:relative importance of volcanism,folding,and remobilisation of nickel sulphides at the Perseverance Ni-Cu-(PGE)deposit,Western Australia[J].Mineralium Deposita,45(3):281-311.
Farrow C E G and Watkinson D H.1996.Geochemical evolution of the epidote zone,Fraser mine,Sudbury,Ontario:Ni-Cu-PGEremobilization by saline fluids[J].Mining Geology,5:17-31.
Gao J F,Zhou M F,Lightfoot P C,et al.2013.Sulfide saturation and magma emplacement in the formation of the Permian Huangshandong Ni-Cu sulfide deposit,Xinjiang,northwestern China[J].Economic Geology,108(8):1833-1848.
Gervilla F and Kojonen K.2002.The platinum-group minerals in the upper section of the Keivitsansarvi Ni-Cu-PGE deposit,Northern Finland[J].The Canadian Mineralogist,40:377-394.
González-álvarez I,Porwal A,Bereford S W,et al.2010.Hydrothermal Ni prospectivity analysis of Tasmania,Australia[J].Ore Geology Reviews,38:168-183.
Grotenhuis S M,Trouw R A J and Passchier C W.2003.Evolution of mica fish in mylonitic rocks[J].Tectonophysics,372:1-21.
Gu L X and Vokes F M.1996.Intergrowths of hexagonal and monoclinic pyrrhotites in some sulphide ores from Norway[J].Mineralogical Magazine,60:303-316.
Gu L X,Zheng Y C,Tang X Q,et al.2007.Copper,gold and silver enrichment in ore mylonites within massive sulphide orebodies at Hongtoushan VHMS deposit,NE China[J].Ore Geology Reviews,30(1):1-29.
Gu L X,Zhu J L,Guo J C,et al.1995.Geology and genesis of the maficultramafic complexes in the Huangshan-Jingerquan belt,East Xinjiang[J].Chinese Journal of Geochemistry(English edition),14(2):97-116.
Han B F,Ji J Q,Song B,et al.2004.SHRIMP zircon U-Pb ages of Kalatongke No.1 and Huangshandong Cu-Ni-bearing maficultramafic complexes,North Xinjiang,and geological implications[J].Chinese Science Bulletin,49(22):2424-2429.
Han C M,Xiao W J,Zhao G C,et al.2010.In-situ U-Pb,Hf and Re-Os isotopic analyses of the Xiangshan Ni-Cu-Co deposit in Eastern Tianshan(Xinjiang),Central Asia Orogenic Belt:constraints on the timing and genesis of the mineralization[J].Lithos,120(3):547-562.
Han C M,Xiao W J,Zhao G C,et al.2013.SIMS U-Pb zircon dating and Re-Os isotopic analysis of the Hulu Cu-Ni deposit,eastern Tianshan,Central Asian Orogenic Belt,and its geological significance[J].Journal of Geoscience,58:251-270.
Hoatson D M,Jaireth S and Jaques A L.2006.Nickel sulfide deposits in Australia:Characteristics,resources,and potential[J].Ore Geology Reviews,29:177-241.
Kissin S A and Scott S D.1982.Phase relations involving pyrrhotite below 350 degrees[J].Economic Geology,77(7):1739-1754.
Lei R X,Wu C Z,Gu L X,et al.2011.Zircon U-Pb chronology and Hf isotope of the Xingxingxia granodiorite from the Central Tianshan zone(NW China):Implications for the tectonic evolution of the southern Altaids[J].Gondwana Research,20:582-593.
Li J Y,Xiao W J,Wang K Z,et al.2003.Neoproterozoic-Paleozoic tectonostratigraphy,magmatic activities and tectonic evolugion of Eastern Xinjiang,NW China[C]//.Mao J,Goldfarb R J,Seltmann R,Wang D,Xiao W,Hart C(eds),Tectonic Evolution and Metallogeny of the Chinese Altay and Tianshan.Proceedings Volume of the International Symposium of the IGCP-473 Project in Urumuqi and Guidebook of the Field Excursion in Xinjiang,China.August 9-21,IAGOD Guidbook Series 10:CERCAMS/NHM London,31-74.
Maiden K J,Chimimba L R and Smalley T J.1986.Cuspate ore-wall rock interfaces,piercement structures and the localization of some sulfide ores in deformed sulfide deposits[J].Economic Geology,81(6):1464-1472.
Mancini F and Papunen H.2000.Metamorphism of Ni-Cu sulfides in mafic-ultramafic intrusions:The Svecofennian Saaksjarvi complex,southern Finland[J].Metamorphosed and metamorphogenic ore deposits(Reviews in Economic Geology),11:217-231.
Mao Y J,Qin K Z,Li C,et al.2015.A modified genetic model for the Huangshandong magmatic sulfide deposit in the Central Asian Orogenic Belt,Xinjiang,western China[J].Mineralium Deposita,50:65-82.
Mao J W,Yang J M,Qu W J,et al.2003.Re-Os age of cu-Ni ores from the Huangshandong Cu-Ni sulfide deposit in the east Tianshan Mountains and its Implication for geodynamic processes[J].Acta Geologica Sinica(English Edition),77(2):220-226.
Menard T,Lesher C M,Stowell H H,et al.1996.Geology,genesis,and metamorphic history of the Namew Lake Ni-Cu deposit,Manitoba[J].Economic Geology,91(8):1394-1413.
Miyashiro A.1994.Metamorphic Petrology[J].London:University College London Press.
Molnár F,Watkinson D H and Everest J O.1999.Fluid-inclusion characteristics of hydrothermal Cu-Ni-PGE veins in granitic and metavolcanic rocks at the contact of the Little Stobie deposit,Sudbury,Canada[J].Chemical Geology,154(1):279-301.
Naldrett A J,Wilson A,Kinnaird J,et al.2009.PGE tenor and metal ratios within and below the Merensky Reef,Bushveld Complex:implications for its genesis[J].Journal of Petrology,50(4):625-659.
Naldrett A J.2004.Magmatic Sulfide Deposits:Geology,Geochemistry and Exploration[M].Springer Science&Business Media.
Qi L and Zhou M F.2008.Platinum-group elemental and Sr-Nd-Os isotopic geochemistry of Permian Emeishan flood basalts in Guizhou Province,SW China[J].Chemical Geology,248:83-103.
Qin K Z,Su B X,Sayyi P A,et al.2011.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[J].American Journal of Science,311(3):237-260.
Shu L S,Charvet J,Guo L Z,et al.1999.A large-scale Palaeozoic dextral ductile strike-slip zone:The Aqqikkudug-Weiya zone along the northern margin of the Central Tianshan belt,Xinjiang,NW China[J].Acta Geologica Sinica(English Edition),73(2):148-162.
Simpson C.1985.Deformation of granitic rock across the brittle-ductile transition[J].Journal of Structural Geology,7(5):503-511.
Song X Y,Keays R R,Zhou M F,et al.2009.Siderophile and chalcophile elemental constraints on the origin of the Jinchuan NiCu-(PGE)sulfide deposit,NW China[J].Geochimica et Cosmochimica Acta,73:404-424.
Su B X,Qin K Z,Sakyi P A,et al.2010.U-Pb ages and Hf-O isotopes of zircons from Late Paleozoic mafic-ultramafic units in the southern Central Asian Orogenic Belt:Tectonic implications and evidence for an Early-Permian mantle plume[J].Gondwana Research,20:516-531.
Su B,Qin K,Sakyi P A,et al.2012.Geochronologic-petrochemical studies of the Hongshishan mafic-ultramafic intrusion,Beishan area,Xinjiang(NW China):petrogenesis and tectonic implications[J].International Geology Review,54(3):270-289.
Sun X M,Wang S W,Sun W D,et al.2008.PGE geochemistry and ReOs dating of massive sulfide ores from the Baimazhai Cu-Ni deposit,Yunnan province,China[J].Lithos,105:12-24.
Sugaki A,Shima A,Kitakaze A,et al.1977.Hydrothermal synthesis of pyrrhotites and their phase relation at low temperature.Studies on the pyrrhotite group minerals(4).Tohoku Univ.Sci.Rept.,ser.3(13):65-82
Schiffries C M.1982.The petrogenesis of a platiniferous dunite pipe in the Bushveld Complex:infiltration metasomatism by a chloride solution[J].Economic Geology,77:1439-1453.
Seng9r A M C,Natal'In B A and Burtman V S.1993.Evolution of the Altaid tectonic collage and Palaeozoic crustal growth in Eurasia[J].Nature,364:299-307.
Ripley E M,Sarkar A and Li C S.2005.Mineralogic and stable isotope studies of hydrothermal alteration at the Jinchuan Ni-Cu deposit,China[J].Economic Geology,100(7):1349-1361.
Tang D M,Qin K Z,Li C S,et al.2011.Zircon dating,Hf-Sr-Nd-Os isotopes and PGE geochemistry of the Tianyu sulfide-bearing maficultramafic intrusion in the Central Asian Orogenic Belt,NW China[J].Lithos,126:84-98.
Tang D M,Qin K Z,Sun H,et al.2012.The role of crustal contamination in the formation of Ni-Cu sulfide deposits in Eastern Tianshan,Xinjiang,Northwest China:Evidence from trace element geochemistry,Re-Os,Sr-Nd,zircon Hf-O,and sulfur isotopes[J].Journal of Asian Earth Sciences,49:145-160.
Tao Y,Li C S,Hu R Z,et al.2010.Re-Os isotopic constranits on the genesis of the Limahe Ni-Cu deposit in hte Emeishan large ignous province,SW China[J].Lithos,119:137-146.
Tapponnier P and Molnár P.1979.Active faulting and Cenozoic tectonics of the Tienshan,Mongolia and Baykal regions[J].Journal of Geophysical Research,84:3425-3459.
Tomkins A G,Frost B R and Pattison D R M.2006.Arsenopyrite melting during metamorphism of sulfide ore deposits[J].The Canadian Mineralogist,44:1325-1342.
Vaughan D J and Ridout M S.1970.M9ssbauer study of pyrrhotite[J].Solid State Communications,8(24):2165-2167.
Wang B,Cluzel D,Jahn B M,et al.2014.Late Paleozoic pre and syn-kinematic plutons of the Kangguer-Huangshan shear zone:inference on the tectonic evolution of the eastern Chinese north Tianshan[J].American Journal of Science,314(1):43-79.
Wang B,Faure M,Shu L S,et al.2008.Paleozoic tectonic evolution of the Yili Block,western Chinese Tianshan[J].Bulletin de la SociétéGéologique de France,179(5):483-490.
Wang C Y and Zhou M F.2006.Genesis of the Permian Baimazhai magmatic Ni-Cu-(PGE)sulfide deposit,Yunnan,SW China[J].Mineralium Deposita,41:771-783.
Wood S A,Mountain BW and Fenlon B J.1992.Thermodynamic constraints on the solubility of platinum and palladium in hydrothermal solutions:Reassessment of hydroxide,bisulfide,and ammonia complexing[J].Economic Geolgoy,84:2020-2028.
Wu F Y,Wilde S A,Zhang G L,et al.2004.Geochronology and petrogenesis of the post-orogenic Cu-Ni sulfide-bearing mafic-ultramafic complexes in Jilin Province,NE China[J].Journal of Asian Earth Sciences,23:781-797.
Xiao W J,Windley B F,Badarch G,et al.2004.Palaeozoic accretionary and convergent tectonics of the southern Altaids:implications for the lateral growth of Central Asia[J].Journal of the Geological Society,London,161:339-342.
Xu X M,Ma T L,Sun L Q,et al.2003.Characteristics and dynamic origin of the large-scale Jiaoluotage ductile compressional zone in the eastern Tianshan Mountains,China[J].Journal of Structural Geology,25:1901-1915.
Yang X Z,Ishihara S and Zhao D H.2006.Genesis of the Jinchuan PGEdeposit,China:evidence from fluid inclusions,mineralogy and geochemistry of preious elements[J].Mineralogy and Petrology,86:109-128.
Yund R A and Hall H T.1969.Hexagonal and monoclinic pyrrhotites[J].Economic Geology,64:420-3.
Zhang L C,Shen Y C and Ji J S.2003.Characteristics and genesis of Kanggur gold deposit in the eastern Tianshan mountains,NW China:Evidence from geology,isotope distribution and chronology[J].Ore Geology Reviews,23:71-90.
Zhang M J,Li C S,Fu P E,et al.2011.The Permian Huangshanxi Cu-Ni deposit in western China:intrusive-extrusive association,ore genesis,and exploration implications[J].Mineralium Deposita,46:153-170.
Zhang Z C,Zhi X C,Chen L,et al.2008.Re-Os isotopic compositions of picrites form the Emeishan flood basalt province,China[J].Earth and Planetary Science Letters,276:30-39.
Zhong H,Yao Y,Prevec S A,et al.2004.Trace-element and Sr-Nd isotopic geochemistry of the PGE-bearing Xiejie layed intrusion in SW China[J].Chemical Geology,203:237-252.
Zhou M F,Lesher C M,Yang Z,et al.2004.Geochemistry and petrogenesis of 270 Ma Ni-Cu-(PGE)sulfide-bearing mafic intrusions in the Huangshan district,Eastern Xinjiang,Northwest China:implications for the tectonic evolution of the Central Asian orogenic belt[J].Chemical Geology,209(3):233-257.
Zhu W G,Zhong H,Hu R Z,et al.2010.Platinum-group minerals and tellurides from the PGE-bearing Xinjie layered intrusion in the Eemishan Large Igneous Province,SW China[J].Mineralogy and Petrology,98(1-4):167-180.
(1)据新疆地质矿产勘查开发局第6大队1988年的勘察报告。