新疆琼河坝地区铁矿床类型及其成矿特征
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摘要
新疆琼河坝位于准噶尔成矿带东段,是一个潜在的以铁、铜、金为主的矿集区。区内铁矿床(点)众多,以往的找矿和研究工作大多聚焦于矽卡岩型富铁矿,对其他类型的铁矿床缺乏足够的重视。为了拓宽琼河坝地区铁矿床勘查思路,需要对区内铁矿床的类型和成矿特征进行系统归纳。文章在野外调查和室内测试分析的基础上,依据矿床(点)的产出地质环境、矿体及矿石矿物成分特征,结合铁矿石主要矿物的主量、微量及稀土元素特征,将琼河坝地区铁矿床划分为矽卡岩型、火山岩型、岩浆分异型、火山间歇期沉积型和湖相沉积型5种类型。矽卡岩型、火山岩型、岩浆分异型和火山间歇期沉积型铁矿赋存在晚古生代泥盆纪—石炭纪火山岩中,湖相沉积型铁矿床赋存于中侏罗统湖沼相含煤碎屑沉积岩中。火山间歇期沉积型铁矿床是在琼河坝地区首次发现的新类型,矿体赋存部位、矿石颗粒磨圆度及胶结成分特征均显示了该类铁矿成矿作用的特殊性。从找矿角度分析,目前主攻方向为矽卡岩型铁矿,而火山岩型铁矿是下一步找矿研究的重点。
Xinjiang Qiongheba area is a potential Fe_Cu_Au ore concentration area located in the eastern section of Junggar metallogenic belt. There are many iron ore deposits or occurrences in this area, yet previous prospecting and research mostly focused on high_grad skarn type iron ore deposits, as well as lack of sufficient attention to other types iron ore. In order to widen the thought of iron ore exploration in this area, systematic induction on the types and mineralization characteristics of iron ore must be carried out. In this paper, we have conducted field survey and laboratory tests, and analyzed the characteristic of geological environment, ore bodies and ore mineral composition, and combined with the characteristic of the major elements, trace elements, rare earth elements of iron ore. These iron ore deposits can be divided into five types: skarn type, volcanic type, magmatic differentiation type, detritus sedimentary type, lacustrine sedimentary type,The first four iron deposit types occur in the Devonian and Carboniferous volcanic rocks, and the last type occur in clastic sedimentary rocks, which formed in coal_bearing lacustrine environment during the Middle Jurassic period. The detritus sedimentary type is a new type of first discovered in Qiongheba, whose ore body location, psephicity of ore particles and agglutinates show the special mineralization. From ore prospecting perspective, the skarn type with great economic value is the main prospecting direction at present. Besides, volcanic type iron ore is the key type for further exploration.
Xinjiang Qiongheba area is a potential Fe_Cu_Au ore concentration area located in the eastern section of Junggar metallogenic belt. There are many iron ore deposits or occurrences in this area, yet previous prospecting and research mostly focused on high_grad skarn type iron ore deposits, as well as lack of sufficient attention to other types iron ore. In order to widen the thought of iron ore exploration in this area, systematic induction on the types and mineralization characteristics of iron ore must be carried out. In this paper, we have conducted field survey and laboratory tests, and analyzed the characteristic of geological environment, ore bodies and ore mineral composition, and combined with the characteristic of the major elements, trace elements, rare earth elements of iron ore. These iron ore deposits can be divided into five types: skarn type, volcanic type, magmatic differentiation type, detritus sedimentary type, lacustrine sedimentary type,The first four iron deposit types occur in the Devonian and Carboniferous volcanic rocks, and the last type occur in clastic sedimentary rocks, which formed in coal_bearing lacustrine environment during the Middle Jurassic period. The detritus sedimentary type is a new type of first discovered in Qiongheba, whose ore body location, psephicity of ore particles and agglutinates show the special mineralization. From ore prospecting perspective, the skarn type with great economic value is the main prospecting direction at present. Besides, volcanic type iron ore is the key type for further exploration.
引文
Chen Y and Zhang Z C.2012.Stady on source,transport and the enrichment mechanism of iron in iron skarn deposits[J].Rock and Mineral Analysis,31(5):889-897(in Chinese with English abstract).
Department of Land and Resources of the Xinjiang Uygur Autonomous.1993.Rejional geological survey report,the Peoples Republic ofChina[R].The internal data(in Chinese).
Department of Land and Resources of the Xinjiang uygur autonomous.2010.Rejional geological survey report,the People Republic of China[R].The internal data(in Chinese).
Dong L H,Xu X W,Qu X and Li G M.2009.Tectonic setting and formation mechanism of the cirum-Junggar porphyritic copper depositbelts[J].Acta Petrologica Sinica,25(4):713-737(in Chinese withEnglish abstract).
Dong L H,Qu X,Zhu Z X and Zhang L C.2010.Tctonic evolution andmetallogenesis of Xinjiang,China[J].Xinjiang Geology,28(40):351-357(in Chinese with English abstract).
Dong L H,Feng J,Zhang D Z,Li F M,Qu X,Liu D Q and Tang Y L.2011.Discussion of metallogenic models,mineralization characteristic and main type of rich iron ore of Xinjiang[J].Xinjiang Geology,29(4):416-422(in Chinese with English abstract).
Dong L H,Feng J,Liu D Q,Qu X,Tang Y L,Zhang D Z,Li F M,Yang Z F and Tu Q J.2012.Regional metallogenic regularity and evolution model of iron deposit in Xinjiang[J].Mineral Deposits,31(Supp):97-98(in Chinese).
Du S J,Qu X,Deng G,Zhang Y,Cheng S L,Lu H F,Wu Q and Xu XW.2010.Chronology and tectonic setting of the intrusive bodies andassociated porphyry copper deposite in Hersai area,eastern Junggar[J].Acta Petrologica Sinica,26(10):2981-2996(in Chinese withEnglish abstract).
Du Y S,Cao Y,Zhang Z Y,Pang Z S and Li D P.2011.Mesozoic in-situ and external skarn magmatic hydrothermal mineralization in theAnhui segment of the lower Yangzi metallogenic belt[J].ActaGeologica Sinica,85(5):699-711(in Chinese with English abstract).
Feng J X,Shi F P,Wang B Y,Hu J M,Wang J T and Tian J Q.2011.Volcanic type iron deposites of Awule metallogenic belt,westernTiansh,Xinjiang[M].Beijing:Geological Publishing House.1-132(in Chinese).
Li C,Xu Z H,De S A,Ripley E M and Maier W D.2004.Compositionalvariations of olivine from the Jinchuan Ni-Cu sulfide doposit,westernChina:Implications for ore genesisi[J].Mineralium Deposita,39:159-172.
Li W C.1992.Geology and genesic of the Panzhihua vanado-magnesitedeposits[J].Geology and Prospecting,10:18-21(in Chinese withEnglish abstract).
Lin X D and Xu G J.1989.A Preliminary investigation on some characteristics and forming mechanism of the magma-genetic skarn[J].Geoscience,3(3):351-358(in Chinese with English abstract).
Lin X D.1998.Geological characteristics of magmatic-hyduothemal transitional ore deposits[J].Geoscience,12(4):485-492(in Chinesewith English abstract).
Liu L M,Shu Z M,Zhao C B,Wan C L,Cai A L and Zhao Y L.2008.The controlling mechanism of ore formation duo to flow-focusing dilation spaces in skarn ore deposits and its significance for deep-ore exploration:Examples from the Tongling-Anqing district[J].ActaPetrologica Sinica,24(8):1848-1856(in Chinese with English abstract).
Meng G X,Lv Q T,Yan J Y,Wang Y,Yang Y Q and Zhao J H.2009.Iron metallogenic characteristics and prospecting potential of Beishanarer,Inner Mongolia[J].Mineral Deposits,28(6):815-829(inChinese with English abstract).
No.6 Geological party,Xinjiang Bureau of geology and mineral explorationand development.2011.Detailed investigation report of No.40 Feore block in Baoshan iron deposit,Yiwu,Xinjiang[R].The internaldata(in Chinese).
Nystrom J O and Hoenriquez F.1994.Magmatic features of iron ores ofthe Kiruna type in Chile and Sweden:Ore textures and magnetite geochemistry[J].Econ.Geol.,89:820-839.
Rsler H J and Lange H.1972.Geochmical Tanles[M].Edition Leipzig.
Wang C L,Wang Y T,Dong L H,Zhang B and Ren Y.2012.Geochamical characteristics of rare earth and trace elements compositions ofSonghu iron deposit in western Tianshan of Xinjiang and their significance[J].Mineral Deposits,31(5):1038-1050(in Chinese withEnglish abstract).
Wang X D,Liu D Q,Tang Y L and Zhou R H.2006.Metallogenic characteristics and perspective of the porphyry copper in Qiongheba,Yiwu County[J].Xinjiang Geology,24(4):398-404(in Chinese withEnglish abstract).
Wang Z H,Zhang Z H,Jiang Z S,Hong W and Tian J Q.2012.Magnetic composition of Zhibo iron deposit in Western TianshanMountains and its genetic significance[J].Mineral Deposits,31(5):983-998(in Chinese with English abstract).
Wu Y C.1992.Magmatic skarn:A new type skarn[J].Geology of Anhui,2(1):12-26(in Chinese with English abstract).
Xu J G and Lin X D.1990.An investigation into the genesis of thechanglongshan skarn-magma type of iron deposit,Anhui Province,Earth Magma type of iron deposit,Anhui province[J].EarthScience,15(6):649-656(in Chinese with English abstract).
Yang F Q,Yan S H,Liu G R,Zhou G,Zhang Z X,Liu F,Geng X Xand Guo C L.2010.Geological characteristics and metallogenesis ofporphyry copper doposits in Juggar,Xinjiang[J].Mineral Deposits,29(6):956-971(in Chinese with English abstract).
Yang F Q,Liu F,Chai F M,Zhang Z X,Geng X X,Lv S J,Jiang L Pand Ouyang L J.2011.Iron deposits in Altay,Xinjiang:Geologicalcharacteristics,time-space distribution and metallogenesis[J].Mineral Deposits,30(4):575-598(in Chinese with English abstract).
Yu M,Feng C Y,Bao G Y,Liu H C,Zhao Y M,Li D X,Xiao Y andLiu J N.2013.Characteristics and zonation of skarn minerals inGalinge iron deposit,Qinghai Province[J].Mineral Deposits,32(1):55-76(in Chinese with English abstract).
Zang M,Dong L H,Chai F M,Yang F Q,Liu F,Li Q and Ouyang L J.2013.Research on REE Geochmistry of the Baliersi Iron Deposit inAltay,Xiniang[J].Acta Geoscientica Sinica,34(2):203-212(inChinese with English abstract).
Zhang J X,Nie W D,Zhao X L,Zhang M J,Zhu J and Xu X W.2007.Geological chracteristics and metallogenic model of the Baoshan irondeposit and some prospectinc indicators in the Yiwu County,Xinjiang[J].Xinjiang Geology,25(4):369-372(in Chinese withEnglish abstract).
Zhang Y,Liang G L,Qu X,Du S J,Wu Q,Zhang Z F,Dong L H andXu X W.2010a.Evidence of U-Pb age and Hf isotope of zircons forEarly Paleozoic magmatism in the Qiongheba arc,East Junggar[J].Acta Petrologica Sinica,26(8):2389-2398.(in Chinese with English abstract).
Zhang Y,Liang G L,Wu Q Y,Wu Q,Zhang Z F,Wu H P,Qu X andXu X W.2010b.Characteristics and fomation mechanism of theveins in Mengxi pophyry Cu-Mo deposit,eastern Junggar of Xinjiang,China[J].Acta Petrologica Sinica,26(10):2997-3006(in Chinese with English abstract).
Zhang Z H,Hong W,Jiang Z S,Duan S G,Wang Z H,Li F M,Shi FP,Zhao J and Zheng R Q.2012.Geological features,mineralization type and metalligenic setting of Late Paleozoic iron deposits inwestern Tiansan Mountains of Xijiang[J].Mineral Deposits,31(5):941-964(in Chinese with English abstract).
Zhao B and Barton M D.1987.Compositional characteristics of garnetsand pyroxenes in contact-metasomatic skarn deposits and their pelationship to metallization[J].Acta Mineralogica Sinica,7(1):1-8(in Chinese with English abstract).
Zhao Y M,Lin W W,Bi C S,Li D X and Jiang C J.1990.Skarn depositsof China[M].Beijing:Geological Publishing House.1-345(inChinese with English abstract).
陈艳,张招崇.2012.矽卡岩铁矿的铁质来源与迁移富集机理探讨[J].岩矿测试,31(5):889-897.
董连慧,徐兴旺,屈迅,李光明.2009.初论环准噶尔斑岩铜矿带的地质构造背景与形成机制[J].岩石学报,25(4):713-737.
董连慧,屈迅,朱志新,张良臣.2010.新疆大地构造演化与成矿[J].新疆地质,28(40):351-357.
董连慧,冯京,庄道泽,李凤鸣,屈迅,刘德权,唐延龄.2011.新疆富铁矿成矿特征及主要类型成矿模式探讨[J].新疆地质,29(4):416-422.
董连慧,冯京,刘德权,屈迅,唐延龄,庄道泽,李凤鸣,杨在峰,涂其军.2012.新疆铁矿床成矿规律及区域成矿演化模式[J].矿床地质,31(增刊):97-98.
杜世俊,屈迅,邓刚,张永,程松林,卢鸿飞,吴琪,徐兴旺.2010.东准噶尔和尔赛斑岩铜矿成岩成矿时代与形成构造背景[J].岩石学报,26(10):2981-2996.
杜杨松,曹毅,张智宇,庞振山,李大鹏.2011.安徽沿江地区中生代原地和异地矽卡岩岩浆-热液成矿作用[J].地质学报,85(5):699-711.
冯金星,石福品,汪帮耀,胡建明,王江涛,田敬全.2011.西天山阿吾拉勒成矿带火山岩型铁矿[M].北京:地质出版社.1-132.
李文臣.1992.攀枝花钒钛磁铁矿矿床地质及其成因[J].地质与勘探,10:18-21.
林新多,许国建.1989.岩浆成因矽卡岩的某些特征及形成机制探讨[J].现代地质,3(3):351-358.
林新多.1998.岩浆-热液过渡型矿床的若干特征[J].现代地质,12(4):485-492.
刘亮明,疏志明,赵崇斌,万昌林,蔡爱良,赵义来.2008.矽卡岩矿床的汇流扩容空间控矿机制及其对深部找矿的意义:以铜陵-安庆地区为例[J].岩石学报,24(8):1848-1856.
孟贵祥,吕庆田,严加永,王勇,杨岳清,赵金花.2009.北山内蒙古地区铁矿成矿特征及其找矿前景[J].矿床地质,28(6):815-829.
王春龙,王义天,董连慧,张兵,任毅.2012.新疆西天山松湖铁矿床稀土和微量元素地球化学特征及其意义[J].矿床地质,31(5):1038-1050.
王晓地,刘德权,唐延龄,周汝洪.2006.伊吾县琼河坝地区斑岩铜矿成矿地质特征及远景评价[J].新疆地质,24(4):398-404.
王志华,张作衡,蒋宗胜,洪为,田敬.2012.西天山智博铁矿床磁铁矿成分特征及其矿床成因[J].矿床地质,31(5):983-998.
吴言昌.1992.论岩浆矽卡岩:一种新类型矽卡岩[J].安徽地质,2(1):12-26.
新疆地矿局第六地质大队.2011.新疆伊吾县宝山铁矿Fe-40号矿段详查地质报告[R].内部资料.
新疆维吾尔自治区国土资源厅.1993.中华人民共和国区域地质调查报告(1:50 000)[R].内部资料.
新疆维吾尔自治区国土资源厅.2010.中华人民共和国区域地质调查报告(1:50 000)[R].内部资料.
许建国,林新多.1990.安徽长龙山矽卡岩浆型铁矿床成因探讨[J].地球科学,15(6):649-656.
杨富全,闫升好,刘国仁,周刚,张志欣,刘锋,耿新霞,郭春丽.2010.新疆准噶尔斑岩铜矿地质特征及成矿作用[J].矿床地质,29(6):956-971.
杨富全,刘锋,柴凤梅,张志欣,耿新霞,吕书君,姜丽萍,欧阳刘进.2011.新疆阿尔泰铁矿地质特征、时空分布及成矿作用[J].矿床地质30(4):575-598.
于淼,丰成友,保广英,刘洪川,赵一鸣,李大新,肖晔,刘建楠.2013.青海尕林格铁矿床夕卡岩矿物学及蚀变分带[J].矿床地质,32(1):55-76.
藏梅,董连慧,柴凤梅,杨富全,刘锋,李强,欧阳刘进.2013.新疆阿尔泰南缘巴利尔斯铁矿床稀土元素地球化学研究[J].地球科学,34(2):203-212.
张锦祥,聂卫东,赵献丽,张明君,朱靖,徐兴旺.2007.新疆伊吾县宝山铁矿地质特征、成矿模式与找矿方向[J].新疆地质,25(4):368-372.
张永,梁广林,屈迅,杜世俊,吴琪,张征峰,董连慧,徐兴旺.2010a.东准噶尔琼河坝岛弧早古生代岩浆活动的锆石U-Pb年龄和Hf同位素证据[J].岩石学报,26(8):2389-2398.
张永,梁广林,吴倩怡,吴琪,张征峰,吴慧平,屈迅,徐兴旺.2010b.东准噶尔蒙西斑岩铜钼矿床脉体特征及其形成机制[J].岩石学报,26(10):2997-3006.
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.
赵斌,Barton M D.1987.接触交代矽卡岩矿床中石榴石和辉石成分特点及其与矿化的关系[J].矿物学报,7(1):1-8.
赵一鸣,林文蔚,毕承思,李大新,蒋崇俊.1990.中国矽卡岩矿床[M].北京:地质出版社.1-345.
Department of Land and Resources of the Xinjiang Uygur Autonomous.1993.Rejional geological survey report,the Peoples Republic ofChina[R].The internal data(in Chinese).
Department of Land and Resources of the Xinjiang uygur autonomous.2010.Rejional geological survey report,the People Republic of China[R].The internal data(in Chinese).
Dong L H,Xu X W,Qu X and Li G M.2009.Tectonic setting and formation mechanism of the cirum-Junggar porphyritic copper depositbelts[J].Acta Petrologica Sinica,25(4):713-737(in Chinese withEnglish abstract).
Dong L H,Qu X,Zhu Z X and Zhang L C.2010.Tctonic evolution andmetallogenesis of Xinjiang,China[J].Xinjiang Geology,28(40):351-357(in Chinese with English abstract).
Dong L H,Feng J,Zhang D Z,Li F M,Qu X,Liu D Q and Tang Y L.2011.Discussion of metallogenic models,mineralization characteristic and main type of rich iron ore of Xinjiang[J].Xinjiang Geology,29(4):416-422(in Chinese with English abstract).
Dong L H,Feng J,Liu D Q,Qu X,Tang Y L,Zhang D Z,Li F M,Yang Z F and Tu Q J.2012.Regional metallogenic regularity and evolution model of iron deposit in Xinjiang[J].Mineral Deposits,31(Supp):97-98(in Chinese).
Du S J,Qu X,Deng G,Zhang Y,Cheng S L,Lu H F,Wu Q and Xu XW.2010.Chronology and tectonic setting of the intrusive bodies andassociated porphyry copper deposite in Hersai area,eastern Junggar[J].Acta Petrologica Sinica,26(10):2981-2996(in Chinese withEnglish abstract).
Du Y S,Cao Y,Zhang Z Y,Pang Z S and Li D P.2011.Mesozoic in-situ and external skarn magmatic hydrothermal mineralization in theAnhui segment of the lower Yangzi metallogenic belt[J].ActaGeologica Sinica,85(5):699-711(in Chinese with English abstract).
Feng J X,Shi F P,Wang B Y,Hu J M,Wang J T and Tian J Q.2011.Volcanic type iron deposites of Awule metallogenic belt,westernTiansh,Xinjiang[M].Beijing:Geological Publishing House.1-132(in Chinese).
Li C,Xu Z H,De S A,Ripley E M and Maier W D.2004.Compositionalvariations of olivine from the Jinchuan Ni-Cu sulfide doposit,westernChina:Implications for ore genesisi[J].Mineralium Deposita,39:159-172.
Li W C.1992.Geology and genesic of the Panzhihua vanado-magnesitedeposits[J].Geology and Prospecting,10:18-21(in Chinese withEnglish abstract).
Lin X D and Xu G J.1989.A Preliminary investigation on some characteristics and forming mechanism of the magma-genetic skarn[J].Geoscience,3(3):351-358(in Chinese with English abstract).
Lin X D.1998.Geological characteristics of magmatic-hyduothemal transitional ore deposits[J].Geoscience,12(4):485-492(in Chinesewith English abstract).
Liu L M,Shu Z M,Zhao C B,Wan C L,Cai A L and Zhao Y L.2008.The controlling mechanism of ore formation duo to flow-focusing dilation spaces in skarn ore deposits and its significance for deep-ore exploration:Examples from the Tongling-Anqing district[J].ActaPetrologica Sinica,24(8):1848-1856(in Chinese with English abstract).
Meng G X,Lv Q T,Yan J Y,Wang Y,Yang Y Q and Zhao J H.2009.Iron metallogenic characteristics and prospecting potential of Beishanarer,Inner Mongolia[J].Mineral Deposits,28(6):815-829(inChinese with English abstract).
No.6 Geological party,Xinjiang Bureau of geology and mineral explorationand development.2011.Detailed investigation report of No.40 Feore block in Baoshan iron deposit,Yiwu,Xinjiang[R].The internaldata(in Chinese).
Nystrom J O and Hoenriquez F.1994.Magmatic features of iron ores ofthe Kiruna type in Chile and Sweden:Ore textures and magnetite geochemistry[J].Econ.Geol.,89:820-839.
Rsler H J and Lange H.1972.Geochmical Tanles[M].Edition Leipzig.
Wang C L,Wang Y T,Dong L H,Zhang B and Ren Y.2012.Geochamical characteristics of rare earth and trace elements compositions ofSonghu iron deposit in western Tianshan of Xinjiang and their significance[J].Mineral Deposits,31(5):1038-1050(in Chinese withEnglish abstract).
Wang X D,Liu D Q,Tang Y L and Zhou R H.2006.Metallogenic characteristics and perspective of the porphyry copper in Qiongheba,Yiwu County[J].Xinjiang Geology,24(4):398-404(in Chinese withEnglish abstract).
Wang Z H,Zhang Z H,Jiang Z S,Hong W and Tian J Q.2012.Magnetic composition of Zhibo iron deposit in Western TianshanMountains and its genetic significance[J].Mineral Deposits,31(5):983-998(in Chinese with English abstract).
Wu Y C.1992.Magmatic skarn:A new type skarn[J].Geology of Anhui,2(1):12-26(in Chinese with English abstract).
Xu J G and Lin X D.1990.An investigation into the genesis of thechanglongshan skarn-magma type of iron deposit,Anhui Province,Earth Magma type of iron deposit,Anhui province[J].EarthScience,15(6):649-656(in Chinese with English abstract).
Yang F Q,Yan S H,Liu G R,Zhou G,Zhang Z X,Liu F,Geng X Xand Guo C L.2010.Geological characteristics and metallogenesis ofporphyry copper doposits in Juggar,Xinjiang[J].Mineral Deposits,29(6):956-971(in Chinese with English abstract).
Yang F Q,Liu F,Chai F M,Zhang Z X,Geng X X,Lv S J,Jiang L Pand Ouyang L J.2011.Iron deposits in Altay,Xinjiang:Geologicalcharacteristics,time-space distribution and metallogenesis[J].Mineral Deposits,30(4):575-598(in Chinese with English abstract).
Yu M,Feng C Y,Bao G Y,Liu H C,Zhao Y M,Li D X,Xiao Y andLiu J N.2013.Characteristics and zonation of skarn minerals inGalinge iron deposit,Qinghai Province[J].Mineral Deposits,32(1):55-76(in Chinese with English abstract).
Zang M,Dong L H,Chai F M,Yang F Q,Liu F,Li Q and Ouyang L J.2013.Research on REE Geochmistry of the Baliersi Iron Deposit inAltay,Xiniang[J].Acta Geoscientica Sinica,34(2):203-212(inChinese with English abstract).
Zhang J X,Nie W D,Zhao X L,Zhang M J,Zhu J and Xu X W.2007.Geological chracteristics and metallogenic model of the Baoshan irondeposit and some prospectinc indicators in the Yiwu County,Xinjiang[J].Xinjiang Geology,25(4):369-372(in Chinese withEnglish abstract).
Zhang Y,Liang G L,Qu X,Du S J,Wu Q,Zhang Z F,Dong L H andXu X W.2010a.Evidence of U-Pb age and Hf isotope of zircons forEarly Paleozoic magmatism in the Qiongheba arc,East Junggar[J].Acta Petrologica Sinica,26(8):2389-2398.(in Chinese with English abstract).
Zhang Y,Liang G L,Wu Q Y,Wu Q,Zhang Z F,Wu H P,Qu X andXu X W.2010b.Characteristics and fomation mechanism of theveins in Mengxi pophyry Cu-Mo deposit,eastern Junggar of Xinjiang,China[J].Acta Petrologica Sinica,26(10):2997-3006(in Chinese with English abstract).
Zhang Z H,Hong W,Jiang Z S,Duan S G,Wang Z H,Li F M,Shi FP,Zhao J and Zheng R Q.2012.Geological features,mineralization type and metalligenic setting of Late Paleozoic iron deposits inwestern Tiansan Mountains of Xijiang[J].Mineral Deposits,31(5):941-964(in Chinese with English abstract).
Zhao B and Barton M D.1987.Compositional characteristics of garnetsand pyroxenes in contact-metasomatic skarn deposits and their pelationship to metallization[J].Acta Mineralogica Sinica,7(1):1-8(in Chinese with English abstract).
Zhao Y M,Lin W W,Bi C S,Li D X and Jiang C J.1990.Skarn depositsof China[M].Beijing:Geological Publishing House.1-345(inChinese with English abstract).
陈艳,张招崇.2012.矽卡岩铁矿的铁质来源与迁移富集机理探讨[J].岩矿测试,31(5):889-897.
董连慧,徐兴旺,屈迅,李光明.2009.初论环准噶尔斑岩铜矿带的地质构造背景与形成机制[J].岩石学报,25(4):713-737.
董连慧,屈迅,朱志新,张良臣.2010.新疆大地构造演化与成矿[J].新疆地质,28(40):351-357.
董连慧,冯京,庄道泽,李凤鸣,屈迅,刘德权,唐延龄.2011.新疆富铁矿成矿特征及主要类型成矿模式探讨[J].新疆地质,29(4):416-422.
董连慧,冯京,刘德权,屈迅,唐延龄,庄道泽,李凤鸣,杨在峰,涂其军.2012.新疆铁矿床成矿规律及区域成矿演化模式[J].矿床地质,31(增刊):97-98.
杜世俊,屈迅,邓刚,张永,程松林,卢鸿飞,吴琪,徐兴旺.2010.东准噶尔和尔赛斑岩铜矿成岩成矿时代与形成构造背景[J].岩石学报,26(10):2981-2996.
杜杨松,曹毅,张智宇,庞振山,李大鹏.2011.安徽沿江地区中生代原地和异地矽卡岩岩浆-热液成矿作用[J].地质学报,85(5):699-711.
冯金星,石福品,汪帮耀,胡建明,王江涛,田敬全.2011.西天山阿吾拉勒成矿带火山岩型铁矿[M].北京:地质出版社.1-132.
李文臣.1992.攀枝花钒钛磁铁矿矿床地质及其成因[J].地质与勘探,10:18-21.
林新多,许国建.1989.岩浆成因矽卡岩的某些特征及形成机制探讨[J].现代地质,3(3):351-358.
林新多.1998.岩浆-热液过渡型矿床的若干特征[J].现代地质,12(4):485-492.
刘亮明,疏志明,赵崇斌,万昌林,蔡爱良,赵义来.2008.矽卡岩矿床的汇流扩容空间控矿机制及其对深部找矿的意义:以铜陵-安庆地区为例[J].岩石学报,24(8):1848-1856.
孟贵祥,吕庆田,严加永,王勇,杨岳清,赵金花.2009.北山内蒙古地区铁矿成矿特征及其找矿前景[J].矿床地质,28(6):815-829.
王春龙,王义天,董连慧,张兵,任毅.2012.新疆西天山松湖铁矿床稀土和微量元素地球化学特征及其意义[J].矿床地质,31(5):1038-1050.
王晓地,刘德权,唐延龄,周汝洪.2006.伊吾县琼河坝地区斑岩铜矿成矿地质特征及远景评价[J].新疆地质,24(4):398-404.
王志华,张作衡,蒋宗胜,洪为,田敬.2012.西天山智博铁矿床磁铁矿成分特征及其矿床成因[J].矿床地质,31(5):983-998.
吴言昌.1992.论岩浆矽卡岩:一种新类型矽卡岩[J].安徽地质,2(1):12-26.
新疆地矿局第六地质大队.2011.新疆伊吾县宝山铁矿Fe-40号矿段详查地质报告[R].内部资料.
新疆维吾尔自治区国土资源厅.1993.中华人民共和国区域地质调查报告(1:50 000)[R].内部资料.
新疆维吾尔自治区国土资源厅.2010.中华人民共和国区域地质调查报告(1:50 000)[R].内部资料.
许建国,林新多.1990.安徽长龙山矽卡岩浆型铁矿床成因探讨[J].地球科学,15(6):649-656.
杨富全,闫升好,刘国仁,周刚,张志欣,刘锋,耿新霞,郭春丽.2010.新疆准噶尔斑岩铜矿地质特征及成矿作用[J].矿床地质,29(6):956-971.
杨富全,刘锋,柴凤梅,张志欣,耿新霞,吕书君,姜丽萍,欧阳刘进.2011.新疆阿尔泰铁矿地质特征、时空分布及成矿作用[J].矿床地质30(4):575-598.
于淼,丰成友,保广英,刘洪川,赵一鸣,李大新,肖晔,刘建楠.2013.青海尕林格铁矿床夕卡岩矿物学及蚀变分带[J].矿床地质,32(1):55-76.
藏梅,董连慧,柴凤梅,杨富全,刘锋,李强,欧阳刘进.2013.新疆阿尔泰南缘巴利尔斯铁矿床稀土元素地球化学研究[J].地球科学,34(2):203-212.
张锦祥,聂卫东,赵献丽,张明君,朱靖,徐兴旺.2007.新疆伊吾县宝山铁矿地质特征、成矿模式与找矿方向[J].新疆地质,25(4):368-372.
张永,梁广林,屈迅,杜世俊,吴琪,张征峰,董连慧,徐兴旺.2010a.东准噶尔琼河坝岛弧早古生代岩浆活动的锆石U-Pb年龄和Hf同位素证据[J].岩石学报,26(8):2389-2398.
张永,梁广林,吴倩怡,吴琪,张征峰,吴慧平,屈迅,徐兴旺.2010b.东准噶尔蒙西斑岩铜钼矿床脉体特征及其形成机制[J].岩石学报,26(10):2997-3006.
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.
赵斌,Barton M D.1987.接触交代矽卡岩矿床中石榴石和辉石成分特点及其与矿化的关系[J].矿物学报,7(1):1-8.
赵一鸣,林文蔚,毕承思,李大新,蒋崇俊.1990.中国矽卡岩矿床[M].北京:地质出版社.1-345.