黑龙江争光金矿床英云闪长斑岩年代学、地球化学及地质意义
|
摘要
黑龙江省黑河市争光金矿床位于大兴安岭东北缘多宝山矿集区东南端,于Ⅰ号矿带钻孔中发现较大规模的隐伏英云闪长斑岩体,其LA-ICP-MS锆石U-Pb谐和年龄和加权平均年龄分别为462.0±0.9 Ma(MSWD=0.0025)和462.1±1.8 Ma(MSWD=0.34),属中奥陶世晚期,代表岩体结晶年龄。岩石具高镁埃达克质岩特征:SiO_2(62.54%~64.62%)≥56%,高Al,富集LILE(Rb、Ba、Sr、U)和LREE,亏损HFSE(Nb、Ta、Ti)、Y及HREE,无Eu异常;高MgO和Cr,高Mg#(56~61),低FeO~T/MgO比值。Sr、Sr/Y、La/Yb及Na_2O/K_2O较典型埃达克岩偏低。与多宝山花岗闪长岩可对比且具演化关系,二者均为俯冲洋壳熔融成因,随俯冲深度增加,体系温度和压力增大,H_2O含量降低,主要矿物相稳定性逐渐发生改变,在16.9Ma时间差的地质历史时期,先后形成早、中奥陶世多宝山和争光两期埃达克质岩,后者岩浆在上升过程中与地幔楔发生了一定程度的交代作用;二者均形成于陆缘弧大地构造背景。争光矿床奥陶纪成矿作用更可能与该岩体有关,熔体高氧逸度、较低聚合度及低演化和分异程度是Cu、Au成矿的有利因素。
The Zhengguang gold deposit is located in the southeast of the Duobaoshan metallogenic belt in the northeastern Great Hinggan Range, Heihe city, Heilongjiang province. Relatively large-scale tonalite porphyry, which may relate to the mineralization, has been discovered in the No.Ⅰ ore belt. The LA-ICP-MS U-Pb concordant age and 206Pb/238 U weighted average age of zircons from the tonalite porphyry are 462.0±0.9 Ma(MSWD=0.0025) and 462.1±1.8 Ma(MSWD=0.34) respectively, which represent its crystallization age and belong to the late of Middle Ordovician. The tonalite porphyry exhibits geochemical features like high Mg adakitic rock, including the SiO_2(62.54%~64.62%)≥56%, high Al content, enriched in large ion lithophile elements(LILE)(Rb, Ba, Sr, U) and light rare earth elements(LREE), depleted in the high field strength elements(HFSE)(Nb, Ta, Ti), Y and heavy rare earth elements(HREE), without Eu anomaly, high Mg~#(56~61), MgO and Cr contents and low FeO~T/MgO ratios. The Sr contents, Sr/Y, La/Yb and Na_2O/K_2O ratios are lower than those of the typical adakites. There are lots of geochemical similarities between the tonalite porphyry in the Zhengguang gold deposit and the Duobaoshan granodiorite. They may have evolution relationship to some extent. They are originated from partial melting of subducted oceanic slab. And with the increase of subduction depth, the temperature and pressure increased, the H_2O content decreased and the stability of the main minerals, such as plagioclase, amphibole, garnet and rutile, gradually changed. The early Ordovician Duobaoshan granodiorite and the Middle Ordovician Zhengguang tonalite porphyry belong to the two periods of adakitic magmatic activity during a period of 16.9 Ma. They both came from continental margin arc, but the Zhengguang tonalite porphyry interacted with the mantle wedge during accending. The Ordovician mineralization of the Zhengguang deposit may relate to the tonalite porphyry pluton that is characterized by high oxygen fugacity, low polymerization degree, low evolution degree and fractionation degree, which is critical for Cu and Au mineralization.
The Zhengguang gold deposit is located in the southeast of the Duobaoshan metallogenic belt in the northeastern Great Hinggan Range, Heihe city, Heilongjiang province. Relatively large-scale tonalite porphyry, which may relate to the mineralization, has been discovered in the No.Ⅰ ore belt. The LA-ICP-MS U-Pb concordant age and 206Pb/238 U weighted average age of zircons from the tonalite porphyry are 462.0±0.9 Ma(MSWD=0.0025) and 462.1±1.8 Ma(MSWD=0.34) respectively, which represent its crystallization age and belong to the late of Middle Ordovician. The tonalite porphyry exhibits geochemical features like high Mg adakitic rock, including the SiO_2(62.54%~64.62%)≥56%, high Al content, enriched in large ion lithophile elements(LILE)(Rb, Ba, Sr, U) and light rare earth elements(LREE), depleted in the high field strength elements(HFSE)(Nb, Ta, Ti), Y and heavy rare earth elements(HREE), without Eu anomaly, high Mg~#(56~61), MgO and Cr contents and low FeO~T/MgO ratios. The Sr contents, Sr/Y, La/Yb and Na_2O/K_2O ratios are lower than those of the typical adakites. There are lots of geochemical similarities between the tonalite porphyry in the Zhengguang gold deposit and the Duobaoshan granodiorite. They may have evolution relationship to some extent. They are originated from partial melting of subducted oceanic slab. And with the increase of subduction depth, the temperature and pressure increased, the H_2O content decreased and the stability of the main minerals, such as plagioclase, amphibole, garnet and rutile, gradually changed. The early Ordovician Duobaoshan granodiorite and the Middle Ordovician Zhengguang tonalite porphyry belong to the two periods of adakitic magmatic activity during a period of 16.9 Ma. They both came from continental margin arc, but the Zhengguang tonalite porphyry interacted with the mantle wedge during accending. The Ordovician mineralization of the Zhengguang deposit may relate to the tonalite porphyry pluton that is characterized by high oxygen fugacity, low polymerization degree, low evolution degree and fractionation degree, which is critical for Cu and Au mineralization.
引文
陈育晓,夏小洪,宋述光.2012.北祁连山西段志留纪高硅埃达克岩:洋壳减压熔融的证据.科学通报,57(22):2072-2085.
崔根,王金益,张景仙,崔革.2008.黑龙江多宝山花岗闪长岩的锆石SHRIMP U-Pb年龄及其地质意义.世界地质,27(4):387-394.
代宇,刘江领,刘旭光,王建民.2012.黑龙江多宝山地区大岔子正长花岗岩锆石U-Pb年龄及其地质意义.地质与资源,21(2):188-193.
邓晋福,肖庆辉,苏尚国,刘翠,赵国春,吴宗絮,刘勇.2007.火成岩组合与构造环境:讨论.高校地质学报13(3):392-402.
邓轲,李诺,杨永飞,张成,于援帮,张东财.2013.黑龙江省黑河市争光金矿流体包裹体研究及矿床成因.岩石学报,29(1):231-240.
杜琦,赵玉明,卢秉刚,马德友,李佩兰,律景凯,李文深,敖立志,崔革.1988.多宝山斑岩铜矿床.北京:地质出版社:1-386.
符家骏,赵元艺,曾辉,李运.2014.黑龙江省争光金矿地球化学与年代学特征初步研究//2014年中国地球科学联合学术年会--专题45:中亚-兴蒙造山带.北京:2171-2173.
付艳丽,杨言辰.2010.黑龙江省争光金矿床成因及找矿标志.黄金,31(6):13-18.
高剑峰,陆建军,赖鸣远,林雨萍,濮巍.2003.岩石样品中微量元素的高分辨率等离子质谱分析.南京大学学报(自然科学版),39(6):844-850.
高利娥,曾令森,侯可军,郭春丽,唐索寒,谢克家,胡古月,王莉.2013.藏南马拉山穹窿佩枯错复合淡色花岗岩体的多期深熔作用.科学通报,58(27):2810-2822.
高荣臻.2015.黑龙江争光金矿床地质特征及其成因探讨.武汉:中国地质大学硕士学位论文:1-82.
高荣臻,吕新彪,杨永胜,李春诚.2014.黑龙江争光金矿床隐爆角砾岩特征及其地质意义.地质与勘探,50(5):874-883.
葛文春,吴福元,周长勇,Abdel Rahman A A.2005.大兴安岭北部塔河花岗岩体的时代及对额尔古纳地块构造归属的制约.科学通报,50(12):1239-1247.
葛文春,吴福元,周长勇,张吉衡.2007.兴蒙造山带东段斑岩型Cu,Mo矿床成矿时代及其地球动力学意义.科学通报,52(20):2407-2417.
葛小月,李献华,陈志刚,李伍平.2002.中国东部燕山期高Sr低Y型中酸性火成岩的地球化学特征及成因:对中国东部地壳厚度的制约.科学通报,47(6):474-480.
龚庆杰,周连壮,胡杨,闫磊,张翰奇,贾玉杰.2012.胶东玲珑金矿田煌斑岩蚀变过程元素迁移行为及其意义.现代地质,26(5):1065-1077.
郭顺,叶凯,陈意,刘景波,张灵敏.2013.开放地质体系中物质迁移质量平衡计算方法介绍.岩石学报,29(5):1486-1498.
韩振新,徐衍强,郑庆道.2004.黑龙江省重要金属和非金属矿产的矿床成矿系列及其演化.哈尔滨:黑龙江人民出版社:1-241.
黑龙江齐齐哈尔矿产勘查开发总院.2007.黑龙江省黑河市争光岩金矿详查地质报告:1-149.
李德荣.2011.黑龙江三矿沟铜多金属矿区(床)成矿规律及找矿方向.北京:中国地质大学博士学位论文:1-138.
李锦轶,莫申国,和政军,孙桂华,陈文.2004.大兴安岭北段地壳左行走滑运动的时代及其对中国东北及邻区中生代以来地壳构造演化重建的制约.地学前缘,11(3):157-168.
李仰春,汪岩,吴淦国,金哲岩,张达,杨晓平.2013.大兴安岭北段扎兰屯地区铜山组源区特征:地球化学及碎屑锆石U-Pb年代学制约.中国地质,40(2):391-402.
廖时理,陈守余,邓小虎,李培.2014.个旧西凹铜-锡多金属矿床花岗岩蚀变带稀土元素特征及意义.中南大学学报(自然科学版),45(5):1555-1565.
凌其聪,刘丛强.2002.低级变质岩在热液蚀变过程中的微量元素地球化学行为--以赣东北银山地区双桥山群为例.岩石学报,18(1):100-108.
刘建辉,刘敦一,张玉海,杨之青.2011.使用SHRIMP测定锆石铀-铅年龄的选点技巧.岩矿测试,30(3):265-268.
刘军,武广,钟伟,朱明田.2010.黑龙江省多宝山斑岩型铜(钼)矿床成矿流体特征及演化.岩石学报,26(5):1450-1464.
刘军,周振华,何哲峰,欧阳荷根.2015.黑龙江省铜山铜矿床英云闪长岩锆石U-Pb年龄及地球化学特征.矿床地质,34(2):289-308.
孟凡超,刘嘉麒,崔岩,高金亮,刘祥,童英.2014.中国东北地区中生代构造体制的转变:来自火山岩时空分布与岩石组合的制约.岩石学报,30(12):3569-3586.
内蒙古自治区地质矿产局.1996.内蒙古自治区岩石地层.武汉:中国地质大学出版社:1-344.
倪怀玮.2013.硅酸盐熔体的物理化学性质研究进展及其应用.科学通报,58(10):865-890.
曲晖,李成禄,赵忠海,王卓,张俭峰.2011.大兴安岭东北部多宝山地区花岗岩锆石U-Pb年龄及岩石地球化学特征.中国地质,38(2):292-300.
佘宏全,李进文,向安平,关继东,杨郧城,张德全,谭刚,张斌.2012.大兴安岭中北段原岩锆石U-Pb测年及其与区域构造演化关系.岩石学报,28(2):571-594.
宋文磊,许成,王林均,吴敏,曾亮,王丽泽,冯梦.2013.与碳酸岩-碱性杂岩体相关的内生稀土矿床成矿作用研究进展.北京大学学报(自然科学版),49(4):725-740.
谭成印.2009.黑龙江省主要金属矿产构造-成矿系统基本特征.北京:中国地质大学博士学位论文:1-261.
王水龙,尚林波,毕献武,樊文苓.2014.硅酸盐熔体和流体中金的性质及行为研究进展.地球科学进展,29(6):683-690.
魏俊浩,刘丛强,丁振举.2000.热液型金矿床围岩蚀变过程中元素迁移规律--以张家口地区东坪、后沟、水晶屯金矿为例.矿物学报,20(2):200-206.
吴福元,葛文春,孙德有.2002.埃达克岩的概念,识别标志及其地质意义//肖庆辉,邓晋福,马大铨等.花岗岩研究思维与方法.北京:地质出版社:172-191.
吴元保,郑永飞.2004.锆石成因矿物学研究及其对U-Pb年龄解释的制约.科学通报,49(16):1589-1604.
武广,刘军,钟伟,朱明田,糜梅,万秋.2009.黑龙江省铜山斑岩铜矿床流体包裹体研究.岩石学报,25(11):2995-3006.
武子玉,孙有才,王保全.2006.黑龙江争光金矿地质地球化学研究.地质与勘探,42(1):38-42.
肖庆辉,邓晋福,马大铨,洪大卫,莫宣学,卢欣祥,李志昌,汪雄武,马昌前,吴福元,王涛.2002.花岗岩研究思维与方法.北京:地质出版社:1-294.
谢建成,陈思,孙卫东,杨晓勇.2012.安徽铜陵早白垩世埃达克质岩地球化学:成岩成矿制约.岩石学报,28(10):3181-3196.
熊小林,Adam J,Green T H,牛贺才,吴金花,蔡志勇.2005a.变质玄武岩部分熔体微量元素特征及埃达克熔体产生条件.中国科学(D辑),35(9):41-50.
熊小林,蔡志勇,牛贺才,陈义兵,王强,赵振华,吴金花.2005b.东天山晚古生代埃达克岩成因及铜金成矿意义.岩石学报,21(3):967-976.
熊小林,韩江伟,吴金花.2007.变质玄武岩体系相平衡及矿物?熔体微量元素分配:限定TTG/埃达克岩形成条件和大陆壳生长模型.地学前缘,14(2):149-158.
熊小林,刘星成,朱志敏,李元,肖万生,宋茂双,张生,吴金花.2011.华北埃达克质岩与克拉通破坏:实验岩石学和地球化学依据.中国科学(D辑),41(5):654-667.
杨文麟,骆满生,王成刚,徐增连.2014.兴蒙造山系新元古代?古生代沉积盆地演化.地球科学,39(8):1155-1168.
张宏飞,高山.2012.地球化学.北京:地质出版社:1-410.
张旗,李承东,王焰,王元龙,金惟俊,贾秀勤,韩松.2005.中国东部中生代高Sr低Yb和低Sr高Yb型花岗岩:对比及其地质意义.岩石学报,21(6):1527-1537.
张旗,潘国强,李承东,金惟俊,贾秀勤.2007.花岗岩构造环境问题:关于花岗岩研究的思考之三.岩石学报,23(11):2683-2698.
张旗,王焰,刘红涛,王元龙,李之彤.2003.中国埃达克岩的时空分布及其形成背景.地学前缘,10(4):385-400.
张旗,王焰,熊小林,李承东.2008.埃达克岩和花岗岩:挑战与机遇.北京:中国大地出版社:1-340.
张旗,殷先明,殷勇,金惟俊,王元龙,赵彦庆.2009.西秦岭与埃达克岩和喜马拉雅型花岗岩有关的金铜成矿及找矿问题.岩石学报,25(12):3103-3122.
张兴洲,杨宝俊,吴福元,刘国兴.2006.中国兴蒙-吉黑地区岩石圈结构基本特征.中国地质,33(4):816-823.
赵广江,候玉树,程富强.2007.黑龙江黑河市争光岩金矿床地质特征及成因浅析.有色金属,59(3):91-94.
赵广江,侯玉树,王宝权.2006.黑龙江省争光金矿地质特征及成因初探.有色矿冶,22(3):3-6.
赵焕利,朱春艳,刘海洋,刘宝山.2012.黑龙江多宝山铜矿床中花岗闪长岩锆石SHRIMP U-Pb测年及其构造意义.地质与资源,21(5):421-424.
赵元艺,王江朋,赵广江,崔玉斌.2011.黑龙江多宝山矿集区成矿规律与找矿方向.吉林大学学报(地球科学版),41(6):1676-1688.
赵振华.2007.关于岩石微量元素构造环境判别图解使用的有关问题.大地构造与成矿学,31(1):92-103.
赵振华.2010.副矿物微量元素地球化学特征在成岩成矿作用研究中的应用.地学前缘,17(1):267-286.
赵振华,熊小林,王强,白正华,梅厚均.2004.新疆西天山莫斯早特石英钠长斑岩铜矿床--一个与埃达克质岩石有关的铜矿实例.岩石学报,20(2):249-258.
赵忠海,郑卫政,曲晖,郭艳,李成禄,王卓,张俭峰.2012.黑龙江多宝山地区铜金成矿作用及成矿规律.矿床地质,31(3):601-614.
郑全波.2012.黑龙江省黑河市争光金矿床地质特征及成因.长春:吉林大学硕士学位论文:1-45.
朱碧,蒋少涌,丁昕,姜耀辉,倪培,顾连兴.2008.江西永平铜矿区花岗岩热液蚀变与岩石成因:矿物化学、元素地球化学和Sr-Nd-Hf同位素制约.岩石学报,24(8):1900-1916.
Abdurrahman D,Erkan T and Salim G.2006.A mantle-and a lower crust-derived bimodal suite in the Yusufeli(Artvin)area,NE Turkey trace element and REEevidence for subduction-related rift origin of early Jurassic Demirkent intrusive complex.International Journal of Earth Sciences,95(3):370-394.
Aguillón-Robles A,Calmus T,Benoit M,Bellon H,Maury R C,Cotten J,Bourgois J and Michaud F.2001.Late Miocene adakites and Nb-enriched basalts from Vizcaino Peninsula,Mexico:Indicators of East Pacific rise subduction below southern Baja California?Geology,29(6):531.
Asadi S,Moore F and Zarasvandi A.2014.Discriminating productive and barren porphyry copper deposits in the southeastern part of the central Iranian volcanoplutonic belt,Kerman region,Iran:A review.EarthScience Reviews,138:25-46.
Ballard J R,Palin M J and Campbell I H.2002.Relative oxidation states of magmas inferred from Ce(IV)/Ce(III)in zircon:Application to porphyry copper deposits of northern Chile.Contributions to Mineralogy and Petrology,144(3):347-364.
Blevin P L.2003.Metallogeny of granitic rocks//Gemoc Macquarie University.The Ishihara Symposium:Granites and Associated Metallogenesis.Australia,Canberra:Geoscience Australia:1-4.
Blevin P L.2004.Redox and compositional parameters for interpreting the granitoid metallogeny of eastern Australia:Implications for gold-rich ore systems.Resource Geology,54(3):241-252.
Carmichael I S E.1991.The redox states of basic and silicic magmas:A reflection of their source regions?Contributions to Mineralogy and Petrology,106(2):129-141.
Castillo P R.2012.Adakite petrogenesis.Lithos,134(3):304-316.
Charles R S and Rolf K.1996.Role of the subducted slab,mantle wedge and continental crust in the generation of adakites from the Andean Austral Volcanic Zone.Contributions to Mineralogy and Petrology,123(3):263-281.
Defant M J and Drummond M S.1990.Derivation of some modern arc magmas by melting of young subducted lithosphere.Nature,374(6294):662-665.
Drummond M S and Defant M J.1990.A model for trondhjemite-tonalite-dacite genesis and crustal growth via slab melting:Archean to modern comparisons.Journal of Geophysical Research:Solid Earth(1978-2012),95(B13):21503-21521.
Escuder Viruete J,Contreras F,Stein G,Urien P,Joubert M,Pérez-Estaún A,Friedman R and Ullrich T.2007.Magmatic relationships and ages between adakites,magnesian andesites and Nb-enriched basalt-andesites from Hispaniola:Record of a major change in the Caribbean island arc magma sources.Lithos,99(3-4):151-177.
Falloon T J,Danyushevsky L V,Crawford A J,Meffre S,Woodhead J D and Bloomer S H.2008.Boninites and adakites from the northern termination of the Tonga Trench:Implications for adakite petrogenesis.Journal of Petrology,49(4):697-715.
Fu J J,Zhao Y Y,Zeng H and Li Y.2014.Chronological and isotopic characteristics of Zhengguang gold deposit in Heilongjiang province,China.Acta Geologica Sinica,88(s2):718-719.
Gao S,Liu X M,Yuan H L,Hattendorf B,Günther D,Chen L and Hu S H.2002.Determination of forty two major and trace elements in USGS and NIST SRM glasses by laser ablation-inductively coupled plasma-mass spectrometry.Geostandards and Geoanalytical Research,26(2):181-196.
Gong Q,Deng J,Yang L,Zhang J,Zhang G and Wang Q.2011.Behavior of major and trace elements during weathering of sericite-quartz schist.Journal of Asian Earth Sciences,42(1):1-13.
Green T H and Pearson N J.1986.Ti-rich accessory phase saturation in hydrous mafic-felsic compositions at high P,T.Chemical Geology,54(3-4):185-201.
Guo S,Ye K,Chen Y and Liu J B.2009.A normalization solution to mass transfer illustration of multiple progressively altered samples using the ISOCONdiagram.Economic Geology,104(6):881-886.
Guo S,Ye K,Chen Y,Liu J,Mao Q and Ma Y.2012.Fluid-rock interaction and element mobilization in UHPmetabasalt:Constraints from an omphacite-epidote vein and host eclogites in the Dabie orogen.Lithos,136(4):145-167.
Hao Y J,Ren Y S,Duan M X,Tong K Y,Chen C,Yang Qand Li C.2015.Metallogenic events and tectonic setting of the Duobaoshan ore field in Heilongjiang province,NE China.Journal of Asian Earth Sciences,97(B1):442-458.
He Y S,Li S G,Hoefs J,Huang F,Liu S A and Hou Z H.2011.Post-collisional granitoids from the Dabie orogen:New evidence for partial melting of a thickened continental crust.Geochimica et Cosmochimica Acta,75(13):3815-3838.
Hermann J and Spandler C J.2007.Sediment melts at sub-arc depths:An experimental study.Journal of Petrology,49(4):717-740.
Hoskin P W O.2005.Trace-element composition of hydrothermal zircon and the alteration of Hadean zircon from the Jack Hills,Australia.Geochimica et Cosmochimica Acta,69(3):637-648.
Hu Z C,Gao S,Liu Y S,Hu S H,Chen H H and Yuan H L.2008.Signal enhancement in laser ablation ICP-MS by addition of nitrogen in the central channel gas.Journal of Analytical Atomic Spectrometry,23(8):1093-1101.
Jahn B and Zhang Z.1984.Archean granulite gneisses from eastern Hebei Province,China:Rare earth geochemistry and tectonic implications.Contributions to Mineralogy and Petrology,85(3):224-243.
Jiang S,Wang R,Xu X and Zhao K.2005.Mobility of high field strength elements(HFSE)in magmatic-,metamorphic-,and submarine-hydrothermal systems.Physics and Chemistry of the Earth,Parts A/B/C,30(17-18):1020-1029.
Karsli O,Dokuz A and Uysal I.2010.Generation of the Early Cenozoic adakitic volcanism by partial melting of mafic lower crust,Eastern Turkey:Implications for crustal thickening to delamination.Lithos,114(1/2):109-120.
Karsli O,Ketenci M and Uysal I.2011.Adakite-like granitoid porphyries in the Eastern Pontides,NETurkey:Potential parental melts and geodynamic implications.Lithos,127(1/2):354-372.
Kay S M and Mpodozis C.2001.Central Andean ore deposits linked to evolving shallow subduction systems and thickening crust.Gsa Today,11(3):4-9.
Kilian R and Stern C R.2002.Constraints on the interaction between slab melts and the mantle wedge from adakitic glass in peridotite xenoliths.European Journal of Mineralogy,14(1):25-36.
Le Maitre R W,Bateman P,Dudek A,Keller J,Lameyre J,Le Bas M J,Sabine P A,Schmid R,Sorensen H,Streckeisen A,Woolley A R and Zanettin B.1989.AClassification of Igneous Rocks and Glossary of Terms.Oxford:Blackwell Sciences Publications:25-34.
Li X P,Zhang L,Wei C,Ai Y and Chen J.2007.Petrology of rodingite derived from eclogite in western Tianshan,China.Journal of Metamorphic Geology,25(3):363-382.
Ling M,Li Y,Ding X,Teng F,Yang X,Fan W,Xu Y and Sun W.2013.Destruction of the North China Craton induced by ridge subductions.The Journal of Geology,121(2):197-213.
Liu Y S,Hu Z C,Gao S,Gunther D,Xu J,Gao C G and Chen H.2008.In situ analysis of major and trace elements of anhydrous minerals by LA-ICP-MSwithout applying an internal standard.Chemical Geology,257(1-2):34-43.
Liu Y S,Hu Z C,Zong K Q,Gao C G,Gao S,Xu J and Chen H H.2010.Reappraisement and refinement of zircon U-Pb isotope and trace element analyses by LA-ICP-MS.Chinese Science Bulletin,55(15):1535-1546.
Ludwig K R.2008.Isoplot 3.7:A geochronological toolkit for Microsoft Excel.Special Publication 4.Berkeley,California:Berkeley Geochronology Center:1-77.
Maniar P D and Piccoli P M.1989.Tectonic discrimination of granitoids.Geological Society of America Bulletin,101(5):635-643.
Martin H.1999.Adakitic magmas:Modern analogues of Archaean granitoids.Lithos,46(3):411-429.
Mclnnes B I,Mc Bride J S,Evans N J,Lambert D D and Andrew A S.1999.Osmium isotope constraints on ore metal recycling in subduction zones.Science,5439(286):512-516.
Middlemost E A K.1994.Naming materials in the magma/igneous rock system.Earth-Science Reviews,37(3):215-224.
Miller C F,Mc Dowell S M and Mapes R W.2003.Hot and cold granites?Implications of zircon saturation temperatures and preservation of inheritance.Geology,31(6):529-532.
Mungall J E.2002.Roasting the mantle:slab melting and the genesis of major Au and Au-rich Cu deposits.Geology,30(10):915-918.
O’Hara K.1988.Fluid flow and volume loss during mylonitization:An origin for phyllonite in an overthrust setting,North Carolina USA.Tectonophysics,156(1):21-36.
Oyarzun R,Márquez A,Lillo J,López I and Rivera S.2001.Giant versus small porphyry copper deposits of Cenozoic age in northern Chile:Adakitic versus normal calc-alkaline magmatism.Mineralium Deposita,36(8):794-798.
Peacock S M,Rushmer T and Thompson A B.1994.Partial melting of subducting oceanic crust.Earth and Planetary Science Letters,121(1):227-244.
Pearce J.1996.Sources and settings of granitic rocks.Episodes,19(4):120-125.
Pearce J A and Peate D W.1995.Tectonic implications of the composition of volcanic arc magmas.Annual Review of Earth and Planetary Sciences,23(1):251-285.
Qin J F,Lai S C,Diwu C R,Ju Y J and Li Y F.2010.Magma mixing origin for the post-collisional adakitic monzogranite of the Triassic Yangba pluton,Northwestern margin of the South China block:Geochemistry,Sr-Nd isotopic,zircon U-Pb dating and Hf isotopic evidences.Contributions to Mineralogy and Petrology,159(3):389-409.
Rapp P R.1997.Heterogeneous source regions for Archaean granitoids:Experimental and geochemical evidence.Oxford Monographs on Geology and Geophysics,35:267-279.
Rapp R P,Shimizu N,Norman M D and Applegate G S.1999.Reaction between slab-derived melts and peridotite in the mantle wedge:Experimental constraints at 3.8 GPa.Chemical Geology,160(4):335-356.
Rapp R P,Xiao L and Shimizu N.2002.Experimental constraints on the origin of potassium-rich adakites in eastern China.Acta Petrologica Sinica,18(3):293-302.
Rickwood P C.1989.Boundary lines within petrologic diagrams which use oxides of major and minor elements.Lithos,22(4):247-263.
Shen J,He M and Ding Z.2014.Geological characteristics and discussion on metallogenic epoch of Zhengguang gold deposit,Heihe city,Heilongjiang province.Acta Geologica Sinica,88(s2):599-600.
Smithies R H.2000.The Archaean tonalite-trondhjemitegranodiorite(TTG)series is not an analogue of Cenozoic adakite.Earth and Planetary Science Letters,182(1):115-125.
Sun S S and Mc Donough W F.1989.Chemical and isotopic systematics of oceanic basalts:Implications for mantle composition and processes.Geological Society,London,Special Publications,42(1):313-345.
Tang J,Xu W L,Wang F,Wang W,Xu M J and Zhang Y H.2013.Geochronology and geochemistry of Neoproterozoic magmatism in the Erguna massif,NE China:Petrogenesis and implications for the breakup of the Rodinia supercontinent.Precambrian Research,224:597-611.
Watson E B and Harrison T M.1983.Zircon saturation revisited:Temperature and composition effects in a variety of crustal magma types.Earth and Planetary Science Letters,64(2):295-304.
Winchester J A and Floyd P A.1977.Geochemical discrimination of different magma series and their differentiation products using immobile elements.Chemical Geology,20(4):325-343.doi:10.1016/0009-2541(77)90057-2
Wu G,Chen Y C,Sun F Y,Liu J,Wang G R and Xu B.2015.Geochronology,geochemistry,and Sr-Nd-Hf Isotopes of the Early Paleozoic igneous rocks in the Duobaoshan area,NE China,and their geological significance.Journal of Asian Earth Sciences,97:229-250.
Xiong X L.2006.Trace element evidence for growth of early continental crust by melting of rutile-bearing hydrous eclogite.Geology,34(11):945-948.
Xiong X L,Adam J and Green T H.2005.Rutile stability and rutile/melt HFSE partitioning during partial melting of hydrous basalt:Implications for TTGgenesis.Chemical Geology,218(3-4):339-359.
Xiong X L,Xia B,Xu J F,Niu H C and Xiao W S.2006.Na depletion in modern adakites via melt/rock reaction within the sub-arc mantle.Chemical Geology,229(4):273-292.
Zajacz Z,Candela P A,Piccoli P M,Sanchez-Valle C and W?lle M.2013.Solubility and partitioning behavior of Au,Cu,Ag and reduced S in magmas.Geochimica et Cosmochimica Acta,112(3):288-304.
Zhang W,Pease V and Wu T.2012.Discovery of an adakite-like pluton near Dongqiyishan(Beishan,NWChina)-Its age and tectonic significance.Lithos,142(6):148-160.
崔根,王金益,张景仙,崔革.2008.黑龙江多宝山花岗闪长岩的锆石SHRIMP U-Pb年龄及其地质意义.世界地质,27(4):387-394.
代宇,刘江领,刘旭光,王建民.2012.黑龙江多宝山地区大岔子正长花岗岩锆石U-Pb年龄及其地质意义.地质与资源,21(2):188-193.
邓晋福,肖庆辉,苏尚国,刘翠,赵国春,吴宗絮,刘勇.2007.火成岩组合与构造环境:讨论.高校地质学报13(3):392-402.
邓轲,李诺,杨永飞,张成,于援帮,张东财.2013.黑龙江省黑河市争光金矿流体包裹体研究及矿床成因.岩石学报,29(1):231-240.
杜琦,赵玉明,卢秉刚,马德友,李佩兰,律景凯,李文深,敖立志,崔革.1988.多宝山斑岩铜矿床.北京:地质出版社:1-386.
符家骏,赵元艺,曾辉,李运.2014.黑龙江省争光金矿地球化学与年代学特征初步研究//2014年中国地球科学联合学术年会--专题45:中亚-兴蒙造山带.北京:2171-2173.
付艳丽,杨言辰.2010.黑龙江省争光金矿床成因及找矿标志.黄金,31(6):13-18.
高剑峰,陆建军,赖鸣远,林雨萍,濮巍.2003.岩石样品中微量元素的高分辨率等离子质谱分析.南京大学学报(自然科学版),39(6):844-850.
高利娥,曾令森,侯可军,郭春丽,唐索寒,谢克家,胡古月,王莉.2013.藏南马拉山穹窿佩枯错复合淡色花岗岩体的多期深熔作用.科学通报,58(27):2810-2822.
高荣臻.2015.黑龙江争光金矿床地质特征及其成因探讨.武汉:中国地质大学硕士学位论文:1-82.
高荣臻,吕新彪,杨永胜,李春诚.2014.黑龙江争光金矿床隐爆角砾岩特征及其地质意义.地质与勘探,50(5):874-883.
葛文春,吴福元,周长勇,Abdel Rahman A A.2005.大兴安岭北部塔河花岗岩体的时代及对额尔古纳地块构造归属的制约.科学通报,50(12):1239-1247.
葛文春,吴福元,周长勇,张吉衡.2007.兴蒙造山带东段斑岩型Cu,Mo矿床成矿时代及其地球动力学意义.科学通报,52(20):2407-2417.
葛小月,李献华,陈志刚,李伍平.2002.中国东部燕山期高Sr低Y型中酸性火成岩的地球化学特征及成因:对中国东部地壳厚度的制约.科学通报,47(6):474-480.
龚庆杰,周连壮,胡杨,闫磊,张翰奇,贾玉杰.2012.胶东玲珑金矿田煌斑岩蚀变过程元素迁移行为及其意义.现代地质,26(5):1065-1077.
郭顺,叶凯,陈意,刘景波,张灵敏.2013.开放地质体系中物质迁移质量平衡计算方法介绍.岩石学报,29(5):1486-1498.
韩振新,徐衍强,郑庆道.2004.黑龙江省重要金属和非金属矿产的矿床成矿系列及其演化.哈尔滨:黑龙江人民出版社:1-241.
黑龙江齐齐哈尔矿产勘查开发总院.2007.黑龙江省黑河市争光岩金矿详查地质报告:1-149.
李德荣.2011.黑龙江三矿沟铜多金属矿区(床)成矿规律及找矿方向.北京:中国地质大学博士学位论文:1-138.
李锦轶,莫申国,和政军,孙桂华,陈文.2004.大兴安岭北段地壳左行走滑运动的时代及其对中国东北及邻区中生代以来地壳构造演化重建的制约.地学前缘,11(3):157-168.
李仰春,汪岩,吴淦国,金哲岩,张达,杨晓平.2013.大兴安岭北段扎兰屯地区铜山组源区特征:地球化学及碎屑锆石U-Pb年代学制约.中国地质,40(2):391-402.
廖时理,陈守余,邓小虎,李培.2014.个旧西凹铜-锡多金属矿床花岗岩蚀变带稀土元素特征及意义.中南大学学报(自然科学版),45(5):1555-1565.
凌其聪,刘丛强.2002.低级变质岩在热液蚀变过程中的微量元素地球化学行为--以赣东北银山地区双桥山群为例.岩石学报,18(1):100-108.
刘建辉,刘敦一,张玉海,杨之青.2011.使用SHRIMP测定锆石铀-铅年龄的选点技巧.岩矿测试,30(3):265-268.
刘军,武广,钟伟,朱明田.2010.黑龙江省多宝山斑岩型铜(钼)矿床成矿流体特征及演化.岩石学报,26(5):1450-1464.
刘军,周振华,何哲峰,欧阳荷根.2015.黑龙江省铜山铜矿床英云闪长岩锆石U-Pb年龄及地球化学特征.矿床地质,34(2):289-308.
孟凡超,刘嘉麒,崔岩,高金亮,刘祥,童英.2014.中国东北地区中生代构造体制的转变:来自火山岩时空分布与岩石组合的制约.岩石学报,30(12):3569-3586.
内蒙古自治区地质矿产局.1996.内蒙古自治区岩石地层.武汉:中国地质大学出版社:1-344.
倪怀玮.2013.硅酸盐熔体的物理化学性质研究进展及其应用.科学通报,58(10):865-890.
曲晖,李成禄,赵忠海,王卓,张俭峰.2011.大兴安岭东北部多宝山地区花岗岩锆石U-Pb年龄及岩石地球化学特征.中国地质,38(2):292-300.
佘宏全,李进文,向安平,关继东,杨郧城,张德全,谭刚,张斌.2012.大兴安岭中北段原岩锆石U-Pb测年及其与区域构造演化关系.岩石学报,28(2):571-594.
宋文磊,许成,王林均,吴敏,曾亮,王丽泽,冯梦.2013.与碳酸岩-碱性杂岩体相关的内生稀土矿床成矿作用研究进展.北京大学学报(自然科学版),49(4):725-740.
谭成印.2009.黑龙江省主要金属矿产构造-成矿系统基本特征.北京:中国地质大学博士学位论文:1-261.
王水龙,尚林波,毕献武,樊文苓.2014.硅酸盐熔体和流体中金的性质及行为研究进展.地球科学进展,29(6):683-690.
魏俊浩,刘丛强,丁振举.2000.热液型金矿床围岩蚀变过程中元素迁移规律--以张家口地区东坪、后沟、水晶屯金矿为例.矿物学报,20(2):200-206.
吴福元,葛文春,孙德有.2002.埃达克岩的概念,识别标志及其地质意义//肖庆辉,邓晋福,马大铨等.花岗岩研究思维与方法.北京:地质出版社:172-191.
吴元保,郑永飞.2004.锆石成因矿物学研究及其对U-Pb年龄解释的制约.科学通报,49(16):1589-1604.
武广,刘军,钟伟,朱明田,糜梅,万秋.2009.黑龙江省铜山斑岩铜矿床流体包裹体研究.岩石学报,25(11):2995-3006.
武子玉,孙有才,王保全.2006.黑龙江争光金矿地质地球化学研究.地质与勘探,42(1):38-42.
肖庆辉,邓晋福,马大铨,洪大卫,莫宣学,卢欣祥,李志昌,汪雄武,马昌前,吴福元,王涛.2002.花岗岩研究思维与方法.北京:地质出版社:1-294.
谢建成,陈思,孙卫东,杨晓勇.2012.安徽铜陵早白垩世埃达克质岩地球化学:成岩成矿制约.岩石学报,28(10):3181-3196.
熊小林,Adam J,Green T H,牛贺才,吴金花,蔡志勇.2005a.变质玄武岩部分熔体微量元素特征及埃达克熔体产生条件.中国科学(D辑),35(9):41-50.
熊小林,蔡志勇,牛贺才,陈义兵,王强,赵振华,吴金花.2005b.东天山晚古生代埃达克岩成因及铜金成矿意义.岩石学报,21(3):967-976.
熊小林,韩江伟,吴金花.2007.变质玄武岩体系相平衡及矿物?熔体微量元素分配:限定TTG/埃达克岩形成条件和大陆壳生长模型.地学前缘,14(2):149-158.
熊小林,刘星成,朱志敏,李元,肖万生,宋茂双,张生,吴金花.2011.华北埃达克质岩与克拉通破坏:实验岩石学和地球化学依据.中国科学(D辑),41(5):654-667.
杨文麟,骆满生,王成刚,徐增连.2014.兴蒙造山系新元古代?古生代沉积盆地演化.地球科学,39(8):1155-1168.
张宏飞,高山.2012.地球化学.北京:地质出版社:1-410.
张旗,李承东,王焰,王元龙,金惟俊,贾秀勤,韩松.2005.中国东部中生代高Sr低Yb和低Sr高Yb型花岗岩:对比及其地质意义.岩石学报,21(6):1527-1537.
张旗,潘国强,李承东,金惟俊,贾秀勤.2007.花岗岩构造环境问题:关于花岗岩研究的思考之三.岩石学报,23(11):2683-2698.
张旗,王焰,刘红涛,王元龙,李之彤.2003.中国埃达克岩的时空分布及其形成背景.地学前缘,10(4):385-400.
张旗,王焰,熊小林,李承东.2008.埃达克岩和花岗岩:挑战与机遇.北京:中国大地出版社:1-340.
张旗,殷先明,殷勇,金惟俊,王元龙,赵彦庆.2009.西秦岭与埃达克岩和喜马拉雅型花岗岩有关的金铜成矿及找矿问题.岩石学报,25(12):3103-3122.
张兴洲,杨宝俊,吴福元,刘国兴.2006.中国兴蒙-吉黑地区岩石圈结构基本特征.中国地质,33(4):816-823.
赵广江,候玉树,程富强.2007.黑龙江黑河市争光岩金矿床地质特征及成因浅析.有色金属,59(3):91-94.
赵广江,侯玉树,王宝权.2006.黑龙江省争光金矿地质特征及成因初探.有色矿冶,22(3):3-6.
赵焕利,朱春艳,刘海洋,刘宝山.2012.黑龙江多宝山铜矿床中花岗闪长岩锆石SHRIMP U-Pb测年及其构造意义.地质与资源,21(5):421-424.
赵元艺,王江朋,赵广江,崔玉斌.2011.黑龙江多宝山矿集区成矿规律与找矿方向.吉林大学学报(地球科学版),41(6):1676-1688.
赵振华.2007.关于岩石微量元素构造环境判别图解使用的有关问题.大地构造与成矿学,31(1):92-103.
赵振华.2010.副矿物微量元素地球化学特征在成岩成矿作用研究中的应用.地学前缘,17(1):267-286.
赵振华,熊小林,王强,白正华,梅厚均.2004.新疆西天山莫斯早特石英钠长斑岩铜矿床--一个与埃达克质岩石有关的铜矿实例.岩石学报,20(2):249-258.
赵忠海,郑卫政,曲晖,郭艳,李成禄,王卓,张俭峰.2012.黑龙江多宝山地区铜金成矿作用及成矿规律.矿床地质,31(3):601-614.
郑全波.2012.黑龙江省黑河市争光金矿床地质特征及成因.长春:吉林大学硕士学位论文:1-45.
朱碧,蒋少涌,丁昕,姜耀辉,倪培,顾连兴.2008.江西永平铜矿区花岗岩热液蚀变与岩石成因:矿物化学、元素地球化学和Sr-Nd-Hf同位素制约.岩石学报,24(8):1900-1916.
Abdurrahman D,Erkan T and Salim G.2006.A mantle-and a lower crust-derived bimodal suite in the Yusufeli(Artvin)area,NE Turkey trace element and REEevidence for subduction-related rift origin of early Jurassic Demirkent intrusive complex.International Journal of Earth Sciences,95(3):370-394.
Aguillón-Robles A,Calmus T,Benoit M,Bellon H,Maury R C,Cotten J,Bourgois J and Michaud F.2001.Late Miocene adakites and Nb-enriched basalts from Vizcaino Peninsula,Mexico:Indicators of East Pacific rise subduction below southern Baja California?Geology,29(6):531.
Asadi S,Moore F and Zarasvandi A.2014.Discriminating productive and barren porphyry copper deposits in the southeastern part of the central Iranian volcanoplutonic belt,Kerman region,Iran:A review.EarthScience Reviews,138:25-46.
Ballard J R,Palin M J and Campbell I H.2002.Relative oxidation states of magmas inferred from Ce(IV)/Ce(III)in zircon:Application to porphyry copper deposits of northern Chile.Contributions to Mineralogy and Petrology,144(3):347-364.
Blevin P L.2003.Metallogeny of granitic rocks//Gemoc Macquarie University.The Ishihara Symposium:Granites and Associated Metallogenesis.Australia,Canberra:Geoscience Australia:1-4.
Blevin P L.2004.Redox and compositional parameters for interpreting the granitoid metallogeny of eastern Australia:Implications for gold-rich ore systems.Resource Geology,54(3):241-252.
Carmichael I S E.1991.The redox states of basic and silicic magmas:A reflection of their source regions?Contributions to Mineralogy and Petrology,106(2):129-141.
Castillo P R.2012.Adakite petrogenesis.Lithos,134(3):304-316.
Charles R S and Rolf K.1996.Role of the subducted slab,mantle wedge and continental crust in the generation of adakites from the Andean Austral Volcanic Zone.Contributions to Mineralogy and Petrology,123(3):263-281.
Defant M J and Drummond M S.1990.Derivation of some modern arc magmas by melting of young subducted lithosphere.Nature,374(6294):662-665.
Drummond M S and Defant M J.1990.A model for trondhjemite-tonalite-dacite genesis and crustal growth via slab melting:Archean to modern comparisons.Journal of Geophysical Research:Solid Earth(1978-2012),95(B13):21503-21521.
Escuder Viruete J,Contreras F,Stein G,Urien P,Joubert M,Pérez-Estaún A,Friedman R and Ullrich T.2007.Magmatic relationships and ages between adakites,magnesian andesites and Nb-enriched basalt-andesites from Hispaniola:Record of a major change in the Caribbean island arc magma sources.Lithos,99(3-4):151-177.
Falloon T J,Danyushevsky L V,Crawford A J,Meffre S,Woodhead J D and Bloomer S H.2008.Boninites and adakites from the northern termination of the Tonga Trench:Implications for adakite petrogenesis.Journal of Petrology,49(4):697-715.
Fu J J,Zhao Y Y,Zeng H and Li Y.2014.Chronological and isotopic characteristics of Zhengguang gold deposit in Heilongjiang province,China.Acta Geologica Sinica,88(s2):718-719.
Gao S,Liu X M,Yuan H L,Hattendorf B,Günther D,Chen L and Hu S H.2002.Determination of forty two major and trace elements in USGS and NIST SRM glasses by laser ablation-inductively coupled plasma-mass spectrometry.Geostandards and Geoanalytical Research,26(2):181-196.
Gong Q,Deng J,Yang L,Zhang J,Zhang G and Wang Q.2011.Behavior of major and trace elements during weathering of sericite-quartz schist.Journal of Asian Earth Sciences,42(1):1-13.
Green T H and Pearson N J.1986.Ti-rich accessory phase saturation in hydrous mafic-felsic compositions at high P,T.Chemical Geology,54(3-4):185-201.
Guo S,Ye K,Chen Y and Liu J B.2009.A normalization solution to mass transfer illustration of multiple progressively altered samples using the ISOCONdiagram.Economic Geology,104(6):881-886.
Guo S,Ye K,Chen Y,Liu J,Mao Q and Ma Y.2012.Fluid-rock interaction and element mobilization in UHPmetabasalt:Constraints from an omphacite-epidote vein and host eclogites in the Dabie orogen.Lithos,136(4):145-167.
Hao Y J,Ren Y S,Duan M X,Tong K Y,Chen C,Yang Qand Li C.2015.Metallogenic events and tectonic setting of the Duobaoshan ore field in Heilongjiang province,NE China.Journal of Asian Earth Sciences,97(B1):442-458.
He Y S,Li S G,Hoefs J,Huang F,Liu S A and Hou Z H.2011.Post-collisional granitoids from the Dabie orogen:New evidence for partial melting of a thickened continental crust.Geochimica et Cosmochimica Acta,75(13):3815-3838.
Hermann J and Spandler C J.2007.Sediment melts at sub-arc depths:An experimental study.Journal of Petrology,49(4):717-740.
Hoskin P W O.2005.Trace-element composition of hydrothermal zircon and the alteration of Hadean zircon from the Jack Hills,Australia.Geochimica et Cosmochimica Acta,69(3):637-648.
Hu Z C,Gao S,Liu Y S,Hu S H,Chen H H and Yuan H L.2008.Signal enhancement in laser ablation ICP-MS by addition of nitrogen in the central channel gas.Journal of Analytical Atomic Spectrometry,23(8):1093-1101.
Jahn B and Zhang Z.1984.Archean granulite gneisses from eastern Hebei Province,China:Rare earth geochemistry and tectonic implications.Contributions to Mineralogy and Petrology,85(3):224-243.
Jiang S,Wang R,Xu X and Zhao K.2005.Mobility of high field strength elements(HFSE)in magmatic-,metamorphic-,and submarine-hydrothermal systems.Physics and Chemistry of the Earth,Parts A/B/C,30(17-18):1020-1029.
Karsli O,Dokuz A and Uysal I.2010.Generation of the Early Cenozoic adakitic volcanism by partial melting of mafic lower crust,Eastern Turkey:Implications for crustal thickening to delamination.Lithos,114(1/2):109-120.
Karsli O,Ketenci M and Uysal I.2011.Adakite-like granitoid porphyries in the Eastern Pontides,NETurkey:Potential parental melts and geodynamic implications.Lithos,127(1/2):354-372.
Kay S M and Mpodozis C.2001.Central Andean ore deposits linked to evolving shallow subduction systems and thickening crust.Gsa Today,11(3):4-9.
Kilian R and Stern C R.2002.Constraints on the interaction between slab melts and the mantle wedge from adakitic glass in peridotite xenoliths.European Journal of Mineralogy,14(1):25-36.
Le Maitre R W,Bateman P,Dudek A,Keller J,Lameyre J,Le Bas M J,Sabine P A,Schmid R,Sorensen H,Streckeisen A,Woolley A R and Zanettin B.1989.AClassification of Igneous Rocks and Glossary of Terms.Oxford:Blackwell Sciences Publications:25-34.
Li X P,Zhang L,Wei C,Ai Y and Chen J.2007.Petrology of rodingite derived from eclogite in western Tianshan,China.Journal of Metamorphic Geology,25(3):363-382.
Ling M,Li Y,Ding X,Teng F,Yang X,Fan W,Xu Y and Sun W.2013.Destruction of the North China Craton induced by ridge subductions.The Journal of Geology,121(2):197-213.
Liu Y S,Hu Z C,Gao S,Gunther D,Xu J,Gao C G and Chen H.2008.In situ analysis of major and trace elements of anhydrous minerals by LA-ICP-MSwithout applying an internal standard.Chemical Geology,257(1-2):34-43.
Liu Y S,Hu Z C,Zong K Q,Gao C G,Gao S,Xu J and Chen H H.2010.Reappraisement and refinement of zircon U-Pb isotope and trace element analyses by LA-ICP-MS.Chinese Science Bulletin,55(15):1535-1546.
Ludwig K R.2008.Isoplot 3.7:A geochronological toolkit for Microsoft Excel.Special Publication 4.Berkeley,California:Berkeley Geochronology Center:1-77.
Maniar P D and Piccoli P M.1989.Tectonic discrimination of granitoids.Geological Society of America Bulletin,101(5):635-643.
Martin H.1999.Adakitic magmas:Modern analogues of Archaean granitoids.Lithos,46(3):411-429.
Mclnnes B I,Mc Bride J S,Evans N J,Lambert D D and Andrew A S.1999.Osmium isotope constraints on ore metal recycling in subduction zones.Science,5439(286):512-516.
Middlemost E A K.1994.Naming materials in the magma/igneous rock system.Earth-Science Reviews,37(3):215-224.
Miller C F,Mc Dowell S M and Mapes R W.2003.Hot and cold granites?Implications of zircon saturation temperatures and preservation of inheritance.Geology,31(6):529-532.
Mungall J E.2002.Roasting the mantle:slab melting and the genesis of major Au and Au-rich Cu deposits.Geology,30(10):915-918.
O’Hara K.1988.Fluid flow and volume loss during mylonitization:An origin for phyllonite in an overthrust setting,North Carolina USA.Tectonophysics,156(1):21-36.
Oyarzun R,Márquez A,Lillo J,López I and Rivera S.2001.Giant versus small porphyry copper deposits of Cenozoic age in northern Chile:Adakitic versus normal calc-alkaline magmatism.Mineralium Deposita,36(8):794-798.
Peacock S M,Rushmer T and Thompson A B.1994.Partial melting of subducting oceanic crust.Earth and Planetary Science Letters,121(1):227-244.
Pearce J.1996.Sources and settings of granitic rocks.Episodes,19(4):120-125.
Pearce J A and Peate D W.1995.Tectonic implications of the composition of volcanic arc magmas.Annual Review of Earth and Planetary Sciences,23(1):251-285.
Qin J F,Lai S C,Diwu C R,Ju Y J and Li Y F.2010.Magma mixing origin for the post-collisional adakitic monzogranite of the Triassic Yangba pluton,Northwestern margin of the South China block:Geochemistry,Sr-Nd isotopic,zircon U-Pb dating and Hf isotopic evidences.Contributions to Mineralogy and Petrology,159(3):389-409.
Rapp P R.1997.Heterogeneous source regions for Archaean granitoids:Experimental and geochemical evidence.Oxford Monographs on Geology and Geophysics,35:267-279.
Rapp R P,Shimizu N,Norman M D and Applegate G S.1999.Reaction between slab-derived melts and peridotite in the mantle wedge:Experimental constraints at 3.8 GPa.Chemical Geology,160(4):335-356.
Rapp R P,Xiao L and Shimizu N.2002.Experimental constraints on the origin of potassium-rich adakites in eastern China.Acta Petrologica Sinica,18(3):293-302.
Rickwood P C.1989.Boundary lines within petrologic diagrams which use oxides of major and minor elements.Lithos,22(4):247-263.
Shen J,He M and Ding Z.2014.Geological characteristics and discussion on metallogenic epoch of Zhengguang gold deposit,Heihe city,Heilongjiang province.Acta Geologica Sinica,88(s2):599-600.
Smithies R H.2000.The Archaean tonalite-trondhjemitegranodiorite(TTG)series is not an analogue of Cenozoic adakite.Earth and Planetary Science Letters,182(1):115-125.
Sun S S and Mc Donough W F.1989.Chemical and isotopic systematics of oceanic basalts:Implications for mantle composition and processes.Geological Society,London,Special Publications,42(1):313-345.
Tang J,Xu W L,Wang F,Wang W,Xu M J and Zhang Y H.2013.Geochronology and geochemistry of Neoproterozoic magmatism in the Erguna massif,NE China:Petrogenesis and implications for the breakup of the Rodinia supercontinent.Precambrian Research,224:597-611.
Watson E B and Harrison T M.1983.Zircon saturation revisited:Temperature and composition effects in a variety of crustal magma types.Earth and Planetary Science Letters,64(2):295-304.
Winchester J A and Floyd P A.1977.Geochemical discrimination of different magma series and their differentiation products using immobile elements.Chemical Geology,20(4):325-343.doi:10.1016/0009-2541(77)90057-2
Wu G,Chen Y C,Sun F Y,Liu J,Wang G R and Xu B.2015.Geochronology,geochemistry,and Sr-Nd-Hf Isotopes of the Early Paleozoic igneous rocks in the Duobaoshan area,NE China,and their geological significance.Journal of Asian Earth Sciences,97:229-250.
Xiong X L.2006.Trace element evidence for growth of early continental crust by melting of rutile-bearing hydrous eclogite.Geology,34(11):945-948.
Xiong X L,Adam J and Green T H.2005.Rutile stability and rutile/melt HFSE partitioning during partial melting of hydrous basalt:Implications for TTGgenesis.Chemical Geology,218(3-4):339-359.
Xiong X L,Xia B,Xu J F,Niu H C and Xiao W S.2006.Na depletion in modern adakites via melt/rock reaction within the sub-arc mantle.Chemical Geology,229(4):273-292.
Zajacz Z,Candela P A,Piccoli P M,Sanchez-Valle C and W?lle M.2013.Solubility and partitioning behavior of Au,Cu,Ag and reduced S in magmas.Geochimica et Cosmochimica Acta,112(3):288-304.
Zhang W,Pease V and Wu T.2012.Discovery of an adakite-like pluton near Dongqiyishan(Beishan,NWChina)-Its age and tectonic significance.Lithos,142(6):148-160.
© 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 |