华北克拉通北缘显生宙含石榴石淡色花岗岩:特征、时代及成因初探
|
摘要
淡色花岗岩是一种特殊的花岗岩类型,其暗色矿物含量低,且多含有白云母、电气石或石榴石等富铝矿物。通常认为,淡色花岗岩是大陆碰撞造山带最具标志性的岩石类型,主要来自于地壳内沉积物的部分熔融,虽然一些最新研究强调它只是岩浆高度分异与演化的产物。显生宙时期,华北克拉通北缘花岗质岩浆作用强烈,然而对于区域存在的少量具有淡色花岗岩特征的岩体却关注较少。本文在对冀东麻地含石榴石白云母二长花岗岩详细研究的基础上,对华北北缘显生宙含石榴石淡色花岗岩的特征、时代进行了总结与对比,并对其成因进行了初步探讨。结果表明,这些岩石具有淡色花岗岩的典型矿物组成与地球化学特征,但已有数据还不足以充分论证其是否由变沉积岩部分熔融形成。与此同时,稀土元素四分组效应与Nb/Ta、Zr/Hf、Y/Ho、K/Rb、Rb/Sr等比值以及CaO、Ba、Sr等元素含量的差异性指示,这些花岗岩经历了不同程度的岩浆分异作用,部分岩石受到了岩浆演化晚期熔-流体相互作用的影响。岩浆分异程度的不同,是导致这些淡色花岗岩具有不同稀有金属成矿潜力的重要因素,高度分异演化有利于成矿元素的富集。由于仅部分淡色花岗岩经历了较高程度的分异,因此岩浆分异可能并非淡色花岗岩形成的必要机制。华北北缘含石榴石淡色花岗岩集中出现在中-晚二叠世、中-晚侏罗世。前者的形成,与古亚洲洋闭合时的碰撞造山有关;后者与东北、华南等中国东部相似岩石同时代产出,形成于古太平洋俯冲的大地构造背景下,其地球动力学内涵值得进一步探讨。
Leucogranites,which usually contain very few mafic minerals but with muscovite,tourmaline or garnet,are characteristic igneous rocks in collisional orogens. They were frequently proved to be the products of crustal paragneiss melting,although extensive magmatic differentiation and later evolution was proposed dominantly in their genesis recently. In this paper,we investigate the Phanerozoic garnet-bearing leucogranites,which has been ignored mostly,in the northern margin of North China Craton( NCC). Taken the Madi stock as an example,the recognized leucogranites in the northern NCC are proved to be typical leucogranite with high silica and A/CNK ratios. They have similar mineral assemblage and geochemical composition with the Manaslu Himalayan leucogranite which was alleged to be S-type granite. The garnets also have prevailing almandine-spessartine composition,which also resembles those in other previously reported leucogranite in the world. However,the available whole rock Sr-O-Nd isotopes and P_2O_5 contents make their derivation controversial. Their sccattered CaO/Na_2O, Rb/Sr and Rb/Ba ratios can't be confidently interpreted by systematic compositional difference of the sedimentary provenance. Instead,the variable tetrad REE patterns and deviation of Nb/Ta,Zr/Hf,Y/Ho,K/Rb and Rb/Sr ratios from the common chondrite and granite imply undoubtedly different degree of magma fractional crystallization with later melt-fluids interaction. The most highly evolved leucocratic magma in the region,which is represented by the Madi stock in which columbite and topaz are found here,is economically mineralized. Absence of significant magmatic differentiation in some garnet-bearing leucogranites( such as the Fangniugou,Houzhuo and some Jiangjia samples) suggests that not all leucogranites are high-evolved granite. Thus,the magma evolution process may contribute to just some imprints of the leucogranites but are not necessary in their genesis. Despite,the highly differentiaon processes,together with the enrichment of fluorine in the late evolutional stage,are crucial to the rare metal mineralization. Temporally,the Phanerozoic garnet-bearing leucogranites appeared in both mid-late Permian and mid-late Jurassic. The former may be related to the collisional process between NCC and the adjacent blocks during the closure of Paleo-Asian Ocean,while the latter seem to be formed contemporaneously with the leucogranite found in South China and Northeastern China area when the Paleo-Pacific ocean plate was subducting beneath the NCC. Further exploration on geodynamics is still needed for the Jurassic ones. So the study promotes our understanding on the petrogenesis of leucogranite and their relationship with rare-metal mineralization and regional tectonic evolution.
Leucogranites,which usually contain very few mafic minerals but with muscovite,tourmaline or garnet,are characteristic igneous rocks in collisional orogens. They were frequently proved to be the products of crustal paragneiss melting,although extensive magmatic differentiation and later evolution was proposed dominantly in their genesis recently. In this paper,we investigate the Phanerozoic garnet-bearing leucogranites,which has been ignored mostly,in the northern margin of North China Craton( NCC). Taken the Madi stock as an example,the recognized leucogranites in the northern NCC are proved to be typical leucogranite with high silica and A/CNK ratios. They have similar mineral assemblage and geochemical composition with the Manaslu Himalayan leucogranite which was alleged to be S-type granite. The garnets also have prevailing almandine-spessartine composition,which also resembles those in other previously reported leucogranite in the world. However,the available whole rock Sr-O-Nd isotopes and P_2O_5 contents make their derivation controversial. Their sccattered CaO/Na_2O, Rb/Sr and Rb/Ba ratios can't be confidently interpreted by systematic compositional difference of the sedimentary provenance. Instead,the variable tetrad REE patterns and deviation of Nb/Ta,Zr/Hf,Y/Ho,K/Rb and Rb/Sr ratios from the common chondrite and granite imply undoubtedly different degree of magma fractional crystallization with later melt-fluids interaction. The most highly evolved leucocratic magma in the region,which is represented by the Madi stock in which columbite and topaz are found here,is economically mineralized. Absence of significant magmatic differentiation in some garnet-bearing leucogranites( such as the Fangniugou,Houzhuo and some Jiangjia samples) suggests that not all leucogranites are high-evolved granite. Thus,the magma evolution process may contribute to just some imprints of the leucogranites but are not necessary in their genesis. Despite,the highly differentiaon processes,together with the enrichment of fluorine in the late evolutional stage,are crucial to the rare metal mineralization. Temporally,the Phanerozoic garnet-bearing leucogranites appeared in both mid-late Permian and mid-late Jurassic. The former may be related to the collisional process between NCC and the adjacent blocks during the closure of Paleo-Asian Ocean,while the latter seem to be formed contemporaneously with the leucogranite found in South China and Northeastern China area when the Paleo-Pacific ocean plate was subducting beneath the NCC. Further exploration on geodynamics is still needed for the Jurassic ones. So the study promotes our understanding on the petrogenesis of leucogranite and their relationship with rare-metal mineralization and regional tectonic evolution.
引文
ГрабежевAИand Ye DL.1984.Geochemical markers of rare metal mineralized granite.Geological Science and Technology Information,(2):74-81(in Chinese)
Agangi A,Kamenetsky VS,Hofmann A,Przybyowicz W and Vladykin NV.2014.Crystallisation of magmatic topaz and implications for Nb-Ta-W mineralisation in F-rich silicic melts:The Ary-Bulak ongonite massif.Lithos,202-203:317-330
Anders E and Grevesse N.1989.Abundances of the elements:Meteoritic and solar.Geochimica et Cosmochimica Acta,53(1):197-214
Ballouard C,Poujol M,Boulvais P,Branquet Y,Tartèse R and Vigneresse JL.2016.Nb-Ta fractionation in peraluminous granites:A marker of the magmatic-hydrothermal transition.Geology,44(3):231-234
Barbarin B.1990.Granitoids:Main petrogenetic classifications in relation to origin and tectonic setting.Geological Journal,25(3-4):227-238
Barbarin B.1996.Genesis of the two main types of peraluminous granitoids.Geology,24(4):295-298
Barbarin B.1999.A review of the relationships between granitoid types,their origins and their geodynamic environments.Lithos,46(3):605-626
Bau M.1996.Controls on the fractionation of isovalent trace elements in magmatic and aqueous systems:Evidence from Y/Ho,Zr/Hf,and lanthanide tetrad effect.Contributions to Mineralogy and Petrology,123(3):323-333
Bea F.1996.Residence of REE,Y,Th and U in granites and crustal protoliths:Implications for the chemistry of crustal melts.Journal of Petrology,37(3):521-552
Bernard-Griffiths J,Peucat JJ,Sheppard S and Vidal P.1985.Petrogenesis of Hercynian leucogranites from the southern Armorican Massif:Contribution of REE and isotopic(Sr,Nd,Pb and O)geochemical data to the study of source rock characteristics and ages.Earth and Planetary Science Letters,74(2-3):235-250
Cao HH,Xu WL,Pei FP,Wang ZW,Wang F and Wang ZJ.2013.Zircon U-Pb geochronology and petrogenesis of the Late PaleozoicEarly Mesozoic intrusive rocks in the eastern segment of the northern margin of the North China Block.Lithos,170-171:191-207
Cao JY,Yang XY,Du JG,Wu QH,Kong H,Li H,Wan Q,Xi XS,Gong YS and Zhao HR.2018.Formation and geodynamic implication of the Early Yanshanian granites associated with W-Sn mineralization in the Nanling range,South China:An overview.International Geology Review,60(11-14):1744-1771
Chang HL.1985.A study of the melting inclusions in the porphyritic topaz phenocrysts of Xianghualingite,Hunan Province.Proceedings of Bulletin of Yichang Institute Geology and Mineral Resources,CAGS,(9):33-40(in Chinese)
Chappell BW and White AJR.1992.I-and S-type granites in the Lachlan Fold Belt.Earth and Environmental Science Transactions of the Royal Society of Edinburgh,83(1-2):1-26
Chappell BW.1999.Aluminium saturation in I-and S-type granites and the characterization of fractionated haplogranites.Lithos,46(3):535-551
Chappell BW and White AJR.2001.Two contrasting granite types:25years later.Australian Journal of Earth Sciences,48(4):489-499
Christiansen EH and Lee DE.1986.Fluorine and chlorine in granitoids from the Basin and Range Province,Western United States.Economic Geology,81(6):1484-1494
Clarke DB.1981.The mineralogy of peraluminous granites:A review.The Canadian Mineralogist,19(1):3-17
Coira B,Kay SM,Viramonte JG,Kay RW and Galli C.2018.Origin of Late Miocene peraluminous Mn-rich garnet-bearing rhyolitic ashes in the Andean foreland(Northern Argentina).Journal of Volcanology and Geothermal Research,364:20-34
Condie KC.1993.Chemical composition and evolution of the upper continental crust:Contrasting results from surface samples and shales.Chemical Geology,104(1-4):1-37
Dahlquist JA,Galindo C,Pankhurst RJ,Rapela CW,Alasino PH,Saavedra J and Fanning CM.2007.Magmatic evolution of the Pe1ón Rosado granite:Petrogenesis of garnet-bearing granitoids.Lithos,95(3-4):177-207
Dong SH,Bi XW,Hu RZ and Chen YW.2014.Petrogenesis of the Yaogangxian granites and implications for W mineralization,Hunan Province.Acta Petrologica Sinica,30(9):2749-2765(in Chinese with English abstract)
Dostal J and Chatterjee AK.1995.Origin of topaz-bearing and related peraluminous granites of the Late Devonian Davis Lake Pluton,Nova Scotia,Canada:Crystal versus fluid fractionation.Chemical Geology,123(1-4):67-88
Fan WB,Jiang N,Xu XY,Hu J and Zong KQ.2017.Petrogenesis of the middle Jurassic appinite and coeval granitoids in the eastern Hebei area of North China Craton.Lithos,278-281:331-346
Fan WB.2017.Petrogenesis of the mesozoic granitoids in the fengning area of northern Hebei area,North China Craton.Ph.D.Dissertation.Beijing:University of Chinese Academy of Sciences(in Chinese with English summary)
Faure G.1986.Principles of Isotope Geology.2ndEdition.New York:John Wiley&Sons
France-Lanord C and Le Fort P.1988.Crustal melting and granite genesis during the Himalayan collision orogenesis.Earth and Environmental Science Transactions of the Royal Society of Edinburgh,79(2-3):183-195
Gao LE,Zeng LS and Asimow PD.2017.Contrasting geochemical signatures of fluid-absent versus fluid-fluxed melting of muscovite in metasedimentary sources:The Himalayan leucogranites.Geology,45(1):39-42
Gao P,Zheng YF and Zhao ZF.2016.Distinction between S-type and peraluminous I-type granites:Zircon versus whole-rock geochemistry.Lithos,258-259:77-91
Green TH.1977.Garnet in silicic liquids and its possible use as a P-Tindicator.Contributions to Mineralogy and Petrology,65(1):59-67
Gu LX,Zhang ZZ,Wu CZ,Gou XQ,Liao JJ and Yang H.2011.Atopaz-and amazonite-bearing leucogranite pluton in eastern Xinjiang,NW China and its zoning.Journal of Asian Earth Sciences,42(5):885-902
Guo CL,Zeng LS,Gao LE,Su HZ,Ma XH and Yin B.2017.Highly fractionated grantitic minerals and whole-rock geochemistry prospecting markers in Hetian,Fujian Province.Acta Geologica Sinica,91(8):1796-1817(in Chinese with English abstract)
Guo ZF and Wilson M.2012.The Himalayan leucogranites:Constraints on the nature of their crustal source region and geodynamic setting.Gondwana Research,22(2):360-376
Haapala I and Lukkari S.2005.Petrological and geochemical evolution of the Kymi stock,a topaz granite cupola within the Wiborg rapakivi batholith,Finland.Lithos,80(1-4):347-362
Harangi SZ,Downes H,Kósa L,SzabóCS,Thirlwall MF,Mason PRDand Mattey D.2001.Almandine garnet in calc-alkaline volcanic rocks of the northern Pannonian Basin(Eastern-Central Europe):Geochemistry,petrogenesis and geodynamic implications.Journal of Petrology,42(10):1813-1843
Harris NBW,Pearce JA and Tindle AG.1986.Geochemical characteristics of collision-zone magmatism.In:Coward MP and Ries AC(eds.).Collision Tectonics.Geological Society,London,Special Publications,19(1):67-81
Hoskin PWO and Schaltegger U.2003.The composition of zircon and igneous and metamorphic petrogenesis.Reviews in Mineralogy and Geochemistry,53(1):27-62
Hu GY,Zeng LS,Gao LE,Liu QP,Chen H and Guo YS.2018.Diverse magma sources for the Himalayan leucogranites:Evidence from B-Sr-Nd isotopes.Lithos,314-315:88-99
Irber W.1999.The lanthanide tetrad effect and its correlation with K/Rb,Eu/Eu*,Sr/Eu,Y/Ho,and Zr/Hf of evolving peraluminous granite suites.Geochimica et Cosmochimica Acta,63(3-4):489-508
Jahn BM,Wu FY,Capdevila R,Martineau F,Zhao ZH and Wang YX.2001.Highly evolved juvenile granites with tetrad REE patterns:The Woduhe and Baerzhe granites from the Great Xing’an Mountains in NE China.Lithos,59(4):171-198
Jian P,Liu DY,Kr9ner A,Windley BF,Shi YR,Zhang W,Zhang FQ,Miao LC,Zhang LQ and Tomurhuu D.2010.Evolution of a Permian intraoceanic arc-trench system in the Solonker suture zone,Central Asian Orogenic Belt,China and Mongolia.Lithos,118(1-2):169-190
Jiang SH,Bagas L,Liu YF and Zhang LL.2018.Geochronology and petrogenesis of the granites in Malanyu Anticline in eastern North China Block.Lithos,312-313:21-37
Johannes W and Holtz F.1996.Petrogenesis and Experimental Petrology of Granitic Rocks.Berlin:Springer-Verlag
Jung S,Hoernes S and Mezger K.2000.Geochronology and petrogenesis of Pan-African,syn-tectonic,S-type and post-tectonic A-type granite(Namibia):Products of melting of crustal sources,fractional crystallization and wall rock entrainment.Lithos,50(4):259-287
Kebede T,Koeberl C and Koller F.2001.Magmatic evolution of the Suqii-Wagga garnet-bearing two-mica granite,Wallagga area,western Ethiopia.Journal of African Earth Sciences,32(2):193-221
Le Fort P.1973.Les leucogranitesàtourmaline de l’Himalaya sur l'exemple du granite du Manaslu(Népal central).Bulletin de la Societe Geologique De France,15:555-561
Le Fort P.1981.Manaslu leucogranite:A collision signature of the Himalaya:A model for its genesis and emplacement.Journal of Geophysical Research:Solid Earth,86(B11):10545-10568
Le Fort P,Cuney M,Deniel C,France-Lanord C,Sheppard SMF,Upreti BN and Vidal P.1987.Crustal generation of the Himalayan leucogranites.Tectonophysics,134(1-3):39-57
Li CF,Li XH,Li QL,Guo JH,Li XH and Yang YH.2012.Rapid and precise determination of Sr and Nd isotopic ratios in geological samples from the same filament loading by thermal ionization mass spectrometry employing a single-step separation scheme.Analytica Chimica Acta,727:54-60
Li J,Huang XL,He PL,Li WX,Yu Y and Chen LL.2015.In situ analyses of micas in the Yashan granite,South China:Constraints on magmatic and hydrothermal evolutions of W and Ta-Nb bearing granites.Ore Geology Reviews,65:793-810
Li SZ,Suo YH,Li XY,Zhou J,Santosh M,Wang PC,Wang GZ,Guo LL,Yu SY,Lan HY,Dai LM,Zhou ZZ,Cao XZ,Zhu JJ,Liu B,Jiang SH,Wang G and Zhang GW.2019.Mesozoic tectonomagmatic response in the East Asian ocean-continent connection zone to subduction of the Paleo-Pacific Plate.Earth-Science Reviews,192:91-137
Li XH,Li WX and Li ZX.2007.On the genetic classification and tectonic implications of the Early Yanshanian granitoids in the Nanling Range,South China.Chinese Science Bulletin,52(14):1873-1885
Li YJ,Wu X,Qi YF,Miao QF,Xiong C and Gong CW.2017.A superlarge Rb-Nb rare metal deposit has been discovered in Huashi Village of Xinglong County,Hebei Province.Acta Geologica Sinica,91(6):2344-2345
Li YJ,Wang YF,Xu GX,Li ZB,Qi YF,Sun JL,Zhao BG,Zhang Band Yue Y.2018.Geochronology,geochemical characteristics in the Fenshuiling complex in the east Hebei Province and its Significance.Acta Geologica Sinica,92(9):1904-1917(in Chinese with English abstract)
Liu CS,Wang RC,Shu LS,Chen XM and Huang XL.2002.Formation and evolution of the S-type granitoids in continental setting.In:Wang DZ and Zhou XM(eds.).Petrogenesis and Evolution of the Late Mesozoic Granitic Volcanic-Intrusive Complex Rocks in South China.Beijing:Science Press,93-135(in Chinese)
Liu HT,Zhai M G,Liu JM and Sun SH.2002.The Mesozoic granitoids in the northern marginal region of North China Craton:Evolution from post-collisional to anorogenic settings.Acta Petrologica Sinica,18(4):433-448(in Chinese with English abstract)
Liu J,Zhang J,Liu ZH,Yin CQ,Zhao C and Peng YB.2018.Petrogenesis of Jurassic granitoids at the northeastern margin of the North China Craton:New geochemical and geochronological constraints on subduction of the Paleo-Pacific Plate.Journal of Asian Earth Sciences,158(1):287-300
Liu JZ,Liu XS,Zhang FQ,Li SX,Li GL and Ouyang ZY.2000.Characteristics and genesis of granitic complex in Fuxin-Jinzhou area,Liaoning Province.Geology-Geochemistry,28(4):65-74(in Chinese with English abstract)
Liu YS,Zong KQ,Kelemen PB and Gao S.2008.Geochemistry and magmatic history of eclogites and ultramafic rocks from the Chinese continental scientific drill hole:Subduction and ultrahigh-pressure metamorphism of lower crustal cumulates.Chemical Geology,247(1-2):133-153
Liu YS.2014.The manual of ICPMSDataCal for LA-ICP-MS/LA-MC-ICP-MS data processing(in Chinese)
Liu ZC.2013.Geochoronology and petrogenesis of the Ramba leucogranite,Tethyan Himalaya,Tibet.Ph.D.Dissertation.Beijing:University of Chinese Academy of Sciences(in Chinese with English summary)
Liu ZC,Wu FY,Ji WQ,Wang JG and Liu CZ.2014.Petrogenesis of the Ramba leucogranite in the Tethyan Himalaya and constraints on the channel flow model.Lithos,208-209:118-136
Liu ZC,Wu FY,Ding L,Liu XC,Wang JG and Ji WQ.2016.Highly fractionated Late Eocene(~35Ma)leucogranite in the Xiaru Dome,Tethyan Himalaya,South Tibet.Lithos,240-243:337-354
Lucci F,Rossetti F,Becchio R,Theye T,Gerdes A,Opitz J,Baez W,Bardelli L,De Astis G,Viramonte J and Giordano G.2018.Magmatic Mn-rich garnets in volcanic settings:Age and longevity of the magmatic plumbing system of the Miocene Ramadas volcanism(NW Argentina).Lithos,322:238-249
Ludwig KR.2012.User’s manual for isoplot 3.75:A geochronological toolkit for Microsoft Excel.Special Publication No.5.Berkeley,California:Berkeley Geochronology Center
LüK,Wang Y and Xiao J.2011.Geochemistry characteristics of Xihuashan granite and structural environment discussion.Journal of East China Institute of Technology(Natural Science Edition),34(2):117-128(in Chinese with English abstract)
Ma L,Wang Q,Kerr AC,Yang JH,Xia XP,Ou Q,Yang ZY and Sun P.2017.Paleocene(c.62Ma)leucogranites in southern Lhasa,Tibet:Products of syn-collisional crustal anatexis during slab rollback?Journal of Petrology,58(11):2089-2114
Manning DAC.1981.The effect of fluorine on liquidus phase relationships in the system Qz-Ab-Or with excess water at 1kb.Contributions to Mineralogy and Petrology,76(2):206-215
Masuda A,Kawakami O,Dohmoto Y and Takenaka T.1987.Lanthanide tetrad effects in nature:Two mutually opposite types,W and M.Geochemical Journal,21(3):119-124
Masuda A and Akagi T.1989.Lanthanide tetrad effect observed in leucogranites from China.Geochemical Journal,23:245-253
McD onough WF and Sun SS.1995.The composition of the Earth.Chemical Geology,120(3-4):223-253
Meng QP,He YK,Zhang W,Wu TR,Zheng RG,Xu C and Zhang ZY.2013.Time constraints on the closure of the Paleo-Asian Ocean on the northern margin of North China Craton:Evidence from Xihouhaozisyn-collisional granites in Siziwang Qi area.Geological Bulletin of China,32(11):1749-1759(in Chinese with English abstract)
Miller CF and Stoddard EF.1981.The role of manganese in the paragenesis of magmatic garnet:An example from the old womanpiute range,California.The Journal of Geology,89(2):233-246
Miller CF.1985.Are strongly peraluminous magmas derived from pelitic sedimentary sources?Journal of Geology,93(6):673-689
Mo XX,Hou ZQ,Niu YL,Dong GC,Qu XM,Zhao ZD and Yang ZM.2007.Mantle contributions to crustal thickening during continental collision:Evidence from Cenozoic igneous rocks in southern Tibet.Lithos,96(1-2):225-242
Pati1o Douce AE.1996.Effects of pressure and H2O content on the compositions of primary crustal melts.Earth and Environmental Science Transactions of the Royal Society of Edinburgh,87(1-2):11-21
Pati1o Douce AE and McC arthy TC.1998.Melting of crustal rocks during continental collision and subduction.In:Hacker BR and Liou JG(eds.).When Continents Collide:Geodynamics and Geochemistry of Ultrahigh-Pressure Rocks.Netherlands:Springer,27-55
Pati1o Douce AE.1999.What do experiments tell us about the relative contributions of crust and mantle to the origin of granitic magmas?In:Castro A,Fernandez C and Vigneresse JL(eds.).Understanding Granites:Integrating New and Classical Techniques.Geological Society,London,Special Publications,168:55-75
Peretyazhko IS and Savina EA.2010.Tetrad effects in the rare earth element patterns of granitoid rocks as an indicator of fluoride-silicate liquid immiscibility in magmatic systems.Petrology,18(5):514-543
Pitcher WS.1983.Granite type and tectonic environment.In:HsüKJ(ed.).Mountain Building Processes.London:Academic Press,19-40
Pitcher WS.1997.The Nature and Origin of Granite.2ndEdition.London:Chapman&Hall,1-387
Rudnick RL and Gao S.2005.Composition of the continental crust.In:Holland HD and Turekian KK(eds.).Treatise on Geochemistry.Amsterdam:Elsevier
Samadi R,Mirnejad H,Kawabata H,Harris C,Valizadeh MV and Gazel E.2014.Magmatic garnet in the Triassic(215Ma)Dehnow pluton of NE Iran and its petrogenetic significance.International Geology Review,56(5):596-621
Scaillet B,Pichavant M and Roux J.1995.Experimental crystallization of leucogranite magmas.Journal of Petrology,36(3):663-705
Sharp Z.2007.Principles of Stable Isotope Geochemistry.Upper Saddle River,NJ:Pearson Education
Song SG,Wang MM,Xu X,Wang C,Niu YL,Allen MB and Su L.2015.Ophiolites in the Xing’an-Inner Mongolia accretionary belt of the CAOB:Implications for two cycles of seafloor spreading and accretionary orogenic events.Tectonics,34(10):2221-2248
temprok M.1991.Ongonite from Ongon Khairkhan,Mongolia.Mineralogy and Petrology,43(4):255-273
Sun DY,Suzuki K,Wu FY and Lu XP.2005.CHIME dating and its application for Mesozoic granites of Huanggoushan,Jilin Province.Geochimica,34(4):1-10(in Chinese with English abstract)
Sun JG and Lian CY.1997.Preliminary discussion on the establishment of Proterozoic stratigraphic framework of fanhe area,Tieling.Liaoning Geology,(1):24-29(in Chinese with English abstract)
Sun T,Zhou XM,Chen PR,Li HM,Zhou HY,Wang ZC and Shen WZ.2005.Strongly peraluminous granites of Mesozoic in eastern Nanling Range,southern China:Petrogenesis and implications for tectonics.Science in China(Series D),48(2):165-174
Sylvester PJ.1998.Post-collisional strongly peraluminous granites.Lithos,45(1-4):29-44
Taylor SR and McL ennan SM.1985.The Continental Crust:Its Composition and Evolution.Oxford:Blackwell Scientific Publications
Wang F,Xu YG,Xu WL,Yang L,Wu W and Sun CY.2017.Early Jurassic calc-alkaline magmatism in Northeast China:Magmatic response to subduction of the Paleo-Pacific Plate beneath the Eurasian continent.Journal of Asian Earth Sciences,143:249-268
Wang JL,Li BZ,Zhou DX,Yao SC and Li ZY.1994.Geological Characteristics of Intermediate-Felsic Plutonic Rocks in Hebei Province and Their Relationship with Mineralization.Beijing:Geological Publishing House,60-64(in Chinese)
Wang LX,Ma CQ,Zhang C,Zhang JY and Marks MAW.2014.Genesis of leucogranite by prolonged fractional crystallization:A case study of the Mufushan complex,South China.Lithos,206-207:147-163
Wang RC,Wu FY,Xie L,Liu XC,Wang JM,Yang L,Lai W and Liu C.2017.A preliminary study of rare-metal mineralization in the Himalayan leucogranite belts,South Tibet.Science China(Earth Sciences),60(9):1655-1663
Wang XL,Zhang C,Liu SW and Shu GM.2007.Electron microprobe dating of monazite in granite from Kangbao area,Hebei Province.Acta Petrologica Sinica,23(4):817-822(in Chinese with English abstract)
Wang XL,Zhou JC,Wan YS,Kitajima K,Wang D,Bonamici C,Qiu JS and Sun T.2013.Magmatic evolution and crustal recycling for Neoproterozoic strongly peraluminous granitoids from southern China:Hf and O isotopes in zircon.Earth and Planetary Science Letters,366:71-82
Wang XP,Li R,Yang ZM,Feng YS and Wang KH.2005.Geologic features and tectonic setting of the garnetiferous muscovite granite in the Fangniugou,Qingyuan County,Liaoning Province.Jilin Geology,24(3):1-4(in Chinese with English abstract)
Weidner JR and Martin RF.1987.Phase equilibria of a fluorine-rich leucogranite from the St.Austell pluton,Cornwall.Geochimica et Cosmochimica Acta,51(6):1591-1597
Weinberg RF.2016.Himalayan leucogranites and migmatites:Nature,timing and duration of anatexis.Journal of Metamorphic Geology,34(8):821-843
White AJR,Clemens JD,Holloway JR,Silver LT,Chappell BW and Wall VJ.1986.S-type granites and their probable absence in southwestern North America.Geology,14(2):115-118
Winter JD.2001.An Introduction to Igneous and Metamorphic Petrology.New Jersey:Prentice-Hall,1-697
Wu FY,Sun DY,Jahn BM and Wilde S.2004.A Jurassic garnetbearing granitic pluton from NE China showing tetrad REE patterns.Journal of Asian Earth Sciences,23(5):731-744
Wu FY,Liu ZC,Liu XC and Ji WQ.2015.Himalayan leucogranite:Petrogenesis and implications to orogenesis and plateau uplift.Acta Petrologica Sinica,31(1):1-36(in Chinese with English abstract)
Wu FY,Liu XC,Ji WQ,Wang JM and Yang L.2017.Highly fractionated granites:Recognition and research.Science China(Earth Sciences),60(7):1201-1219
Xia WH and Chen ZY.1984.The discovery of melt inclusions in topaz and quartz and its significance to genesis of Ta-Nb granites in southern China.Earth Science(Journal of Wuhan College of Geology),(2):79-83(in Chinese with English abstract)
Xia WH.Zhang JT,Feng ZW and Chen ZY.1989.Geology of Nanling Granite-Type Rare Metal Deposit.Wuhan:China University of Geosciences Press,90-115(in Chinese)
Xiao WJ,Windley BF,Hao J and Zhai MG.2003.Accretion leading to collision and the Permian Solonker suture,Inner Mongolia,China:Termination of the central Asian orogenic belt.Tectonics,22(6):1069
Xiao WJ,Windley BF,Sun S,Li JL,Huang BC,Han CM,Yuan C,Sun M and Chen HL.2015.A tale of amalgamation of three PermoTriassic collage systems in Central Asia:Oroclines,sutures,and terminal accretion.Annual Review of Earth and Planetary Sciences,43:477-507
Xie L,Wang ZJ,Wang RC,Zhu JC,Che XD,Gao JF and Zhao X.2018.Mineralogical constraints on the genesis of W-Nb-Ta mineralization in the Laiziling granite(Xianghualing district,South China).Ore Geology Reviews,95:695-712
Yang DG,Sun DY,Gou J and Hou XG.2017.U-Pb ages of zircons from Mesozoic intrusive rocks in the Yanbian area,Jilin Province,NEChina:Transition of the Paleo-Asian oceanic regime to the circumPacific tectonic regime.Journal of Asian Earth Sciences,143:171-190
Yang JH,Sun JF,Zhang M,Wu FY and Wilde SA.2012.Petrogenesisof silica-saturated and silica-undersaturated syenites in the northern North China craton related to post-collisional and intraplate extension.Chemical Geology,328:149-167
Ye DL,Tai DQ and Ren YX.1987.Geological and petrological characteristics of M111 rare metal-bearing granite intrusion in Xinglong,Hebei.Earth Science(Journal of Wuhan College of Geology),12(3):265-275,333(in Chinese with English abstract)
Ye DL,Ren YX and Tai DQ.1991.The study on the characteristics of geochemistry and mineralization of the M111 rare metal contained granitic intrusion in Xinglong,Hebei.Geoscience,5(1):13-23(in Chinese with English abstract)
Yuan W,Yang ZY,Zhao XX,Santosh M and Zhou XJ.2018.Early Jurassic granitoids from deep drill holes in the East China Sea Basin:Implications for the initiation of Palaeo-Pacific tectono-magmatic cycle.International Geology Review,60(7):813-824
Zhang C and Han BF.2004.The characteristics and tectonic significance of Meso-Proterozoic late stage granitoids in Wucuan-Kangbao.Acta Petrologica Sinica,20(3):433-438(in Chinese with English abstract)
Zhang QW,Liu ZH,Chai SL,Xu ZY and Xu XC.2011.Zircon U-Pb dating of the Garnet-bearing granite from Wulan area of Urad Zhongqi in Inner Monglia and its geological significance.Journal of Jilin University(Earth Science Edition),41(3):745-752(in Chinese with English abstract)
Zhang SH,Zhao Y,Kr9ner A,Liu XM,Xie LW and Chen FK.2009.Early permian plutons from the northern north china block:Constraints on continental arc evolution and convergent margin magmatism related to the Central Asian orogenic belt.International Journal of Earth Sciences,98(6):1441-1467
Zhang SH,Zhao Y,Liu JM,Hu JM,Song B,Liu J and Wu H.2010.Geochronology,geochemistry and tectonic setting of the Late Paleozoic-Early Mesozoic magmatism in the northern margin of the North China Block:A preliminary review.Acta Petrologica et Mineralogica,29(6):824-842(in Chinese with English abstract)
Zhang SH,Zhao Y,Davis G A,Ye H and Wu F.2014.Temporal and spatial variations of Mesozoic magmatism and deformation in the North China craton:Implications for lithospheric thinning and decratonization.Earth-Science Reviews,131:49-87
Zhang SH,Zhao Y,Liu JM and Hu ZC.2016.Different sources involved in generation of continental arc volcanism:The CarboniferousPermian volcanic rocks in the northern margin of the North China block.Lithos,240-243:382-401
Zhang XH,Mao Q,Zhang H and Wilde SA.2008.A Jurassic peraluminous leucogranite from Yiwulüshan,western Liaoning,North China craton:Age,origin and tectonic significance.Geological Magazine,145(3):305-320
Zhao QY.2010.Origin and tectonic setting of Late Paleozoic-Early Mesozoic granites in Daqingshan district,Inner Mongolia.Ph.D.Dissertation.Changchun:Jilin University(in Chinese with English summary)
Zhao ZH.1988.A preliminary report on the tetrad REE effect in granites.Geology and Geochemistry,(1):71-72(in Chinese)
Zhao ZH,Masuda A and Shabani MB.1992.Tetrad effects of rare-earth elements in rare-metal granites.Geochimica,(3):221-233(in Chinese with English abstract)
Zhao ZH.2016.Principles of Trace Element Geochemistry.2nded.Beijing:Science Press,115-118(in Chinese)
Zheng K.2016.Genesis of garnet-bearing granite and tectonic implications within Kangbao County,North Hebei Province.Master Degree Thesis.Chengdu:Chengdu University of Technology(in Chinese with English summary)
Zhou JC and Wang XL.2005.Experimental and Theoretical Petrology.Beijing:Geological Publishing House,1-256(in Chinese)
Zhou ZB,Pei FP,Wang ZW,Cao HH,Xu WL,Wang ZJ and Zhang Y.2017.Using detrital zircons from Late Permian to Triassic sedimentary rocks in the south-eastern Central Asian Orogenic Belt(NE China)to constrain the timing of the final closure of the Paleo-Asian Ocean.Journal of Asian Earth Sciences,144:82-109
ГрабежевAИ,叶德隆.1984.稀有金属矿化花岗岩专属性的地球化学标志.地质科技情报,(2):74-81
常海亮.1985.香花岭岩黄玉斑晶中熔融包裹体的研究.中国地质科学院宜昌地质矿产研究所文集,(9):33-40
董少花,毕献武,胡瑞忠,陈佑纬.2014.湖南瑶岗仙复式花岗岩岩石成因及与钨成矿关系.岩石学报,30(9):2749-2765
范文博.2017.华北克拉通北缘丰宁地区中生代花岗岩类岩石成因研究.博士学位论文.北京:中国科学院大学
郭春丽,曾令森,高利娥,苏红中,马星华,尹冰.2017.福建河田高分异花岗岩的矿物和全岩地球化学找矿标志研究.地质学报,91(8):1796-1817
李献华,李武显,李正祥.2007.再论南岭燕山早期花岗岩的成因类型与构造意义.科学通报,52(9):981-991
李玉静,王玉芳,徐国新,李智斌,齐云飞,孙金龙,赵丙刚,张勃,越悦.2018.冀东分水岭岩体锆石U-Pb年代学、地球化学特征及地质意义.地质学报,92(9):1904-1917
刘昌实,王汝成,舒良树,陈小明,黄小龙.2002.陆内S型花岗岩的形成与演化.见:王德滋,周新民编.中国东南部晚中生代花岗质火山-侵入杂岩成因与地壳演化.北京:科学出版社,93-135
刘红涛,翟明国,刘建明,孙世华.2002.华北克拉通北缘中生代花岗岩:从碰撞后到非造山.岩石学报,18(4):433-448
刘建忠,刘喜山,张福勤,李树勋,李桂林,欧阳自远.2000.辽宁阜新-锦州地区花岗杂岩特征及成因.地质地球化学,28(4):65-74
刘勇胜.2014.LA-ICP-MS/LA-MC-ICP-MS数据处理软件ICPMSDataCal(V9.5)使用手册
刘志超.2013.喜马拉雅然巴淡色花岗岩时代与成因.博士学位论文.北京:中国科学院大学
吕科,王勇,肖剑.2011.西华山复式花岗岩株地球化学特征及构造环境探讨.东华理工大学学报(自然科学版),34(2):117-128
孟庆鹏,贺元凯,张文,吴泰然,郑荣国,徐操,张昭昱.2013.华北板块北缘古大洋闭合时间的限定---来自四子王旗西后壕子同碰撞花岗岩的证据.地质通报,32(11):1749-1759
孙德有,铃木和博,吴福元,路孝平.2005.吉林省南部荒沟山地区中生代花岗岩CHIME定年.地球化学,34(4):1-10
孙景贵,连长云.1997.辽西地区花岗岩的形成时代.辽宁地质,(1):24-29
孙涛,周新民,陈培荣,李惠民,周红英,王志成,沈渭洲.2003.南岭东段中生代强过铝花岗岩成因及其大地构造意义.中国科学(地球科学),33(12):1209-1218
王季亮,李丙泽,周德星,姚士臣,李枝荫.1994.河北省中酸性岩体地质特征及其与成矿关系.北京:地质出版社,60-64
王汝成,吴福元,谢磊,刘小驰,王佳敏,杨雷,赖文,刘晨.2017.藏南喜马拉雅淡色花岗岩稀有金属成矿作用初步研究.中国科学(地球科学),47(8):871-880
王鑫琳,张臣,刘树文,舒桂明.2007.河北康保地区花岗岩独居石电子探针定年.岩石学报,23(4):817-822
王秀萍,李睿,杨志猛,冯义生,王凯红.2005.辽宁省清源县放牛沟含榴白云母花岗岩地质特征及构造环境探讨.吉林地质,24(3):1-4
吴福元,刘志超,刘小驰,纪伟强.2015.喜马拉雅淡色花岗岩.岩石学报,31(1):1-36
吴福元,刘小驰,纪伟强,王佳敏,杨雷.2017.高分异花岗岩的识别与研究.中国科学(地球科学),47(7):745-765
夏卫华,陈紫英.1984.黄玉、石英中熔浆包裹体的发现及其在华南钽铌花岗岩成因上的意义.地球科学(武汉地质学院学报),(2):79-83
夏卫华,章锦统,冯志文,陈紫英.1989.南岭花岗岩型稀有金属矿床地质.武汉:中国地质大学出版社,90-115
叶德隆,邰道乾,任迎新.1987.河北兴隆M111稀有金属花岗岩体地质和岩石学特征.地球科学(武汉地质学院学报),12(3):265-275,333
叶德隆,任迎新,邰道乾.1991.河北兴隆M111稀有金属花岗岩体地球化学和矿化特征研究.现代地质,5(1):13-23
张臣,韩宝福.2004.华北北部武川-康保地区中元古代晚期花岗岩类基本特征及其构造意义.岩石学报,20(3):433-438
张青伟,刘正宏,柴社立,徐仲元,徐学纯.2011.内蒙古乌拉特中旗乌兰地区含石榴石花岗岩锆石U-Pb年龄及地质意义.吉林大学学报(地球科学版),41(3):745-752
张拴宏,赵越,刘建民,胡健民,宋彪,刘健,吴海.2010.华北地块北缘晚古生代-早中生代岩浆活动期次、特征及构造背景.岩石矿物学杂志,29(6):824-842
赵庆英.2010.内蒙古大青山地区晚古生代-早中生代花岗岩成因及其形成构造环境.博士学位论文.长春:吉林大学
赵振华.1988.花岗岩中发现稀土元素四重分布效应的初步报道.地质地球化学,(1):71-72
赵振华,增田彰正,夏巴尼MB.1992.稀有金属花岗岩的稀土元素四分组效应.地球化学,(3):221-233
赵振华.2016.微量元素地球化学原理.第2版.北京:科学出版社,115-118
郑坤.2016.冀北康保石榴花岗岩成因及大地构造意义.硕士学位论文.成都:成都理工大学
周金城,王孝磊.2005.实验及理论岩石学.北京:地质出版社,1-256
Agangi A,Kamenetsky VS,Hofmann A,Przybyowicz W and Vladykin NV.2014.Crystallisation of magmatic topaz and implications for Nb-Ta-W mineralisation in F-rich silicic melts:The Ary-Bulak ongonite massif.Lithos,202-203:317-330
Anders E and Grevesse N.1989.Abundances of the elements:Meteoritic and solar.Geochimica et Cosmochimica Acta,53(1):197-214
Ballouard C,Poujol M,Boulvais P,Branquet Y,Tartèse R and Vigneresse JL.2016.Nb-Ta fractionation in peraluminous granites:A marker of the magmatic-hydrothermal transition.Geology,44(3):231-234
Barbarin B.1990.Granitoids:Main petrogenetic classifications in relation to origin and tectonic setting.Geological Journal,25(3-4):227-238
Barbarin B.1996.Genesis of the two main types of peraluminous granitoids.Geology,24(4):295-298
Barbarin B.1999.A review of the relationships between granitoid types,their origins and their geodynamic environments.Lithos,46(3):605-626
Bau M.1996.Controls on the fractionation of isovalent trace elements in magmatic and aqueous systems:Evidence from Y/Ho,Zr/Hf,and lanthanide tetrad effect.Contributions to Mineralogy and Petrology,123(3):323-333
Bea F.1996.Residence of REE,Y,Th and U in granites and crustal protoliths:Implications for the chemistry of crustal melts.Journal of Petrology,37(3):521-552
Bernard-Griffiths J,Peucat JJ,Sheppard S and Vidal P.1985.Petrogenesis of Hercynian leucogranites from the southern Armorican Massif:Contribution of REE and isotopic(Sr,Nd,Pb and O)geochemical data to the study of source rock characteristics and ages.Earth and Planetary Science Letters,74(2-3):235-250
Cao HH,Xu WL,Pei FP,Wang ZW,Wang F and Wang ZJ.2013.Zircon U-Pb geochronology and petrogenesis of the Late PaleozoicEarly Mesozoic intrusive rocks in the eastern segment of the northern margin of the North China Block.Lithos,170-171:191-207
Cao JY,Yang XY,Du JG,Wu QH,Kong H,Li H,Wan Q,Xi XS,Gong YS and Zhao HR.2018.Formation and geodynamic implication of the Early Yanshanian granites associated with W-Sn mineralization in the Nanling range,South China:An overview.International Geology Review,60(11-14):1744-1771
Chang HL.1985.A study of the melting inclusions in the porphyritic topaz phenocrysts of Xianghualingite,Hunan Province.Proceedings of Bulletin of Yichang Institute Geology and Mineral Resources,CAGS,(9):33-40(in Chinese)
Chappell BW and White AJR.1992.I-and S-type granites in the Lachlan Fold Belt.Earth and Environmental Science Transactions of the Royal Society of Edinburgh,83(1-2):1-26
Chappell BW.1999.Aluminium saturation in I-and S-type granites and the characterization of fractionated haplogranites.Lithos,46(3):535-551
Chappell BW and White AJR.2001.Two contrasting granite types:25years later.Australian Journal of Earth Sciences,48(4):489-499
Christiansen EH and Lee DE.1986.Fluorine and chlorine in granitoids from the Basin and Range Province,Western United States.Economic Geology,81(6):1484-1494
Clarke DB.1981.The mineralogy of peraluminous granites:A review.The Canadian Mineralogist,19(1):3-17
Coira B,Kay SM,Viramonte JG,Kay RW and Galli C.2018.Origin of Late Miocene peraluminous Mn-rich garnet-bearing rhyolitic ashes in the Andean foreland(Northern Argentina).Journal of Volcanology and Geothermal Research,364:20-34
Condie KC.1993.Chemical composition and evolution of the upper continental crust:Contrasting results from surface samples and shales.Chemical Geology,104(1-4):1-37
Dahlquist JA,Galindo C,Pankhurst RJ,Rapela CW,Alasino PH,Saavedra J and Fanning CM.2007.Magmatic evolution of the Pe1ón Rosado granite:Petrogenesis of garnet-bearing granitoids.Lithos,95(3-4):177-207
Dong SH,Bi XW,Hu RZ and Chen YW.2014.Petrogenesis of the Yaogangxian granites and implications for W mineralization,Hunan Province.Acta Petrologica Sinica,30(9):2749-2765(in Chinese with English abstract)
Dostal J and Chatterjee AK.1995.Origin of topaz-bearing and related peraluminous granites of the Late Devonian Davis Lake Pluton,Nova Scotia,Canada:Crystal versus fluid fractionation.Chemical Geology,123(1-4):67-88
Fan WB,Jiang N,Xu XY,Hu J and Zong KQ.2017.Petrogenesis of the middle Jurassic appinite and coeval granitoids in the eastern Hebei area of North China Craton.Lithos,278-281:331-346
Fan WB.2017.Petrogenesis of the mesozoic granitoids in the fengning area of northern Hebei area,North China Craton.Ph.D.Dissertation.Beijing:University of Chinese Academy of Sciences(in Chinese with English summary)
Faure G.1986.Principles of Isotope Geology.2ndEdition.New York:John Wiley&Sons
France-Lanord C and Le Fort P.1988.Crustal melting and granite genesis during the Himalayan collision orogenesis.Earth and Environmental Science Transactions of the Royal Society of Edinburgh,79(2-3):183-195
Gao LE,Zeng LS and Asimow PD.2017.Contrasting geochemical signatures of fluid-absent versus fluid-fluxed melting of muscovite in metasedimentary sources:The Himalayan leucogranites.Geology,45(1):39-42
Gao P,Zheng YF and Zhao ZF.2016.Distinction between S-type and peraluminous I-type granites:Zircon versus whole-rock geochemistry.Lithos,258-259:77-91
Green TH.1977.Garnet in silicic liquids and its possible use as a P-Tindicator.Contributions to Mineralogy and Petrology,65(1):59-67
Gu LX,Zhang ZZ,Wu CZ,Gou XQ,Liao JJ and Yang H.2011.Atopaz-and amazonite-bearing leucogranite pluton in eastern Xinjiang,NW China and its zoning.Journal of Asian Earth Sciences,42(5):885-902
Guo CL,Zeng LS,Gao LE,Su HZ,Ma XH and Yin B.2017.Highly fractionated grantitic minerals and whole-rock geochemistry prospecting markers in Hetian,Fujian Province.Acta Geologica Sinica,91(8):1796-1817(in Chinese with English abstract)
Guo ZF and Wilson M.2012.The Himalayan leucogranites:Constraints on the nature of their crustal source region and geodynamic setting.Gondwana Research,22(2):360-376
Haapala I and Lukkari S.2005.Petrological and geochemical evolution of the Kymi stock,a topaz granite cupola within the Wiborg rapakivi batholith,Finland.Lithos,80(1-4):347-362
Harangi SZ,Downes H,Kósa L,SzabóCS,Thirlwall MF,Mason PRDand Mattey D.2001.Almandine garnet in calc-alkaline volcanic rocks of the northern Pannonian Basin(Eastern-Central Europe):Geochemistry,petrogenesis and geodynamic implications.Journal of Petrology,42(10):1813-1843
Harris NBW,Pearce JA and Tindle AG.1986.Geochemical characteristics of collision-zone magmatism.In:Coward MP and Ries AC(eds.).Collision Tectonics.Geological Society,London,Special Publications,19(1):67-81
Hoskin PWO and Schaltegger U.2003.The composition of zircon and igneous and metamorphic petrogenesis.Reviews in Mineralogy and Geochemistry,53(1):27-62
Hu GY,Zeng LS,Gao LE,Liu QP,Chen H and Guo YS.2018.Diverse magma sources for the Himalayan leucogranites:Evidence from B-Sr-Nd isotopes.Lithos,314-315:88-99
Irber W.1999.The lanthanide tetrad effect and its correlation with K/Rb,Eu/Eu*,Sr/Eu,Y/Ho,and Zr/Hf of evolving peraluminous granite suites.Geochimica et Cosmochimica Acta,63(3-4):489-508
Jahn BM,Wu FY,Capdevila R,Martineau F,Zhao ZH and Wang YX.2001.Highly evolved juvenile granites with tetrad REE patterns:The Woduhe and Baerzhe granites from the Great Xing’an Mountains in NE China.Lithos,59(4):171-198
Jian P,Liu DY,Kr9ner A,Windley BF,Shi YR,Zhang W,Zhang FQ,Miao LC,Zhang LQ and Tomurhuu D.2010.Evolution of a Permian intraoceanic arc-trench system in the Solonker suture zone,Central Asian Orogenic Belt,China and Mongolia.Lithos,118(1-2):169-190
Jiang SH,Bagas L,Liu YF and Zhang LL.2018.Geochronology and petrogenesis of the granites in Malanyu Anticline in eastern North China Block.Lithos,312-313:21-37
Johannes W and Holtz F.1996.Petrogenesis and Experimental Petrology of Granitic Rocks.Berlin:Springer-Verlag
Jung S,Hoernes S and Mezger K.2000.Geochronology and petrogenesis of Pan-African,syn-tectonic,S-type and post-tectonic A-type granite(Namibia):Products of melting of crustal sources,fractional crystallization and wall rock entrainment.Lithos,50(4):259-287
Kebede T,Koeberl C and Koller F.2001.Magmatic evolution of the Suqii-Wagga garnet-bearing two-mica granite,Wallagga area,western Ethiopia.Journal of African Earth Sciences,32(2):193-221
Le Fort P.1973.Les leucogranitesàtourmaline de l’Himalaya sur l'exemple du granite du Manaslu(Népal central).Bulletin de la Societe Geologique De France,15:555-561
Le Fort P.1981.Manaslu leucogranite:A collision signature of the Himalaya:A model for its genesis and emplacement.Journal of Geophysical Research:Solid Earth,86(B11):10545-10568
Le Fort P,Cuney M,Deniel C,France-Lanord C,Sheppard SMF,Upreti BN and Vidal P.1987.Crustal generation of the Himalayan leucogranites.Tectonophysics,134(1-3):39-57
Li CF,Li XH,Li QL,Guo JH,Li XH and Yang YH.2012.Rapid and precise determination of Sr and Nd isotopic ratios in geological samples from the same filament loading by thermal ionization mass spectrometry employing a single-step separation scheme.Analytica Chimica Acta,727:54-60
Li J,Huang XL,He PL,Li WX,Yu Y and Chen LL.2015.In situ analyses of micas in the Yashan granite,South China:Constraints on magmatic and hydrothermal evolutions of W and Ta-Nb bearing granites.Ore Geology Reviews,65:793-810
Li SZ,Suo YH,Li XY,Zhou J,Santosh M,Wang PC,Wang GZ,Guo LL,Yu SY,Lan HY,Dai LM,Zhou ZZ,Cao XZ,Zhu JJ,Liu B,Jiang SH,Wang G and Zhang GW.2019.Mesozoic tectonomagmatic response in the East Asian ocean-continent connection zone to subduction of the Paleo-Pacific Plate.Earth-Science Reviews,192:91-137
Li XH,Li WX and Li ZX.2007.On the genetic classification and tectonic implications of the Early Yanshanian granitoids in the Nanling Range,South China.Chinese Science Bulletin,52(14):1873-1885
Li YJ,Wu X,Qi YF,Miao QF,Xiong C and Gong CW.2017.A superlarge Rb-Nb rare metal deposit has been discovered in Huashi Village of Xinglong County,Hebei Province.Acta Geologica Sinica,91(6):2344-2345
Li YJ,Wang YF,Xu GX,Li ZB,Qi YF,Sun JL,Zhao BG,Zhang Band Yue Y.2018.Geochronology,geochemical characteristics in the Fenshuiling complex in the east Hebei Province and its Significance.Acta Geologica Sinica,92(9):1904-1917(in Chinese with English abstract)
Liu CS,Wang RC,Shu LS,Chen XM and Huang XL.2002.Formation and evolution of the S-type granitoids in continental setting.In:Wang DZ and Zhou XM(eds.).Petrogenesis and Evolution of the Late Mesozoic Granitic Volcanic-Intrusive Complex Rocks in South China.Beijing:Science Press,93-135(in Chinese)
Liu HT,Zhai M G,Liu JM and Sun SH.2002.The Mesozoic granitoids in the northern marginal region of North China Craton:Evolution from post-collisional to anorogenic settings.Acta Petrologica Sinica,18(4):433-448(in Chinese with English abstract)
Liu J,Zhang J,Liu ZH,Yin CQ,Zhao C and Peng YB.2018.Petrogenesis of Jurassic granitoids at the northeastern margin of the North China Craton:New geochemical and geochronological constraints on subduction of the Paleo-Pacific Plate.Journal of Asian Earth Sciences,158(1):287-300
Liu JZ,Liu XS,Zhang FQ,Li SX,Li GL and Ouyang ZY.2000.Characteristics and genesis of granitic complex in Fuxin-Jinzhou area,Liaoning Province.Geology-Geochemistry,28(4):65-74(in Chinese with English abstract)
Liu YS,Zong KQ,Kelemen PB and Gao S.2008.Geochemistry and magmatic history of eclogites and ultramafic rocks from the Chinese continental scientific drill hole:Subduction and ultrahigh-pressure metamorphism of lower crustal cumulates.Chemical Geology,247(1-2):133-153
Liu YS.2014.The manual of ICPMSDataCal for LA-ICP-MS/LA-MC-ICP-MS data processing(in Chinese)
Liu ZC.2013.Geochoronology and petrogenesis of the Ramba leucogranite,Tethyan Himalaya,Tibet.Ph.D.Dissertation.Beijing:University of Chinese Academy of Sciences(in Chinese with English summary)
Liu ZC,Wu FY,Ji WQ,Wang JG and Liu CZ.2014.Petrogenesis of the Ramba leucogranite in the Tethyan Himalaya and constraints on the channel flow model.Lithos,208-209:118-136
Liu ZC,Wu FY,Ding L,Liu XC,Wang JG and Ji WQ.2016.Highly fractionated Late Eocene(~35Ma)leucogranite in the Xiaru Dome,Tethyan Himalaya,South Tibet.Lithos,240-243:337-354
Lucci F,Rossetti F,Becchio R,Theye T,Gerdes A,Opitz J,Baez W,Bardelli L,De Astis G,Viramonte J and Giordano G.2018.Magmatic Mn-rich garnets in volcanic settings:Age and longevity of the magmatic plumbing system of the Miocene Ramadas volcanism(NW Argentina).Lithos,322:238-249
Ludwig KR.2012.User’s manual for isoplot 3.75:A geochronological toolkit for Microsoft Excel.Special Publication No.5.Berkeley,California:Berkeley Geochronology Center
LüK,Wang Y and Xiao J.2011.Geochemistry characteristics of Xihuashan granite and structural environment discussion.Journal of East China Institute of Technology(Natural Science Edition),34(2):117-128(in Chinese with English abstract)
Ma L,Wang Q,Kerr AC,Yang JH,Xia XP,Ou Q,Yang ZY and Sun P.2017.Paleocene(c.62Ma)leucogranites in southern Lhasa,Tibet:Products of syn-collisional crustal anatexis during slab rollback?Journal of Petrology,58(11):2089-2114
Manning DAC.1981.The effect of fluorine on liquidus phase relationships in the system Qz-Ab-Or with excess water at 1kb.Contributions to Mineralogy and Petrology,76(2):206-215
Masuda A,Kawakami O,Dohmoto Y and Takenaka T.1987.Lanthanide tetrad effects in nature:Two mutually opposite types,W and M.Geochemical Journal,21(3):119-124
Masuda A and Akagi T.1989.Lanthanide tetrad effect observed in leucogranites from China.Geochemical Journal,23:245-253
McD onough WF and Sun SS.1995.The composition of the Earth.Chemical Geology,120(3-4):223-253
Meng QP,He YK,Zhang W,Wu TR,Zheng RG,Xu C and Zhang ZY.2013.Time constraints on the closure of the Paleo-Asian Ocean on the northern margin of North China Craton:Evidence from Xihouhaozisyn-collisional granites in Siziwang Qi area.Geological Bulletin of China,32(11):1749-1759(in Chinese with English abstract)
Miller CF and Stoddard EF.1981.The role of manganese in the paragenesis of magmatic garnet:An example from the old womanpiute range,California.The Journal of Geology,89(2):233-246
Miller CF.1985.Are strongly peraluminous magmas derived from pelitic sedimentary sources?Journal of Geology,93(6):673-689
Mo XX,Hou ZQ,Niu YL,Dong GC,Qu XM,Zhao ZD and Yang ZM.2007.Mantle contributions to crustal thickening during continental collision:Evidence from Cenozoic igneous rocks in southern Tibet.Lithos,96(1-2):225-242
Pati1o Douce AE.1996.Effects of pressure and H2O content on the compositions of primary crustal melts.Earth and Environmental Science Transactions of the Royal Society of Edinburgh,87(1-2):11-21
Pati1o Douce AE and McC arthy TC.1998.Melting of crustal rocks during continental collision and subduction.In:Hacker BR and Liou JG(eds.).When Continents Collide:Geodynamics and Geochemistry of Ultrahigh-Pressure Rocks.Netherlands:Springer,27-55
Pati1o Douce AE.1999.What do experiments tell us about the relative contributions of crust and mantle to the origin of granitic magmas?In:Castro A,Fernandez C and Vigneresse JL(eds.).Understanding Granites:Integrating New and Classical Techniques.Geological Society,London,Special Publications,168:55-75
Peretyazhko IS and Savina EA.2010.Tetrad effects in the rare earth element patterns of granitoid rocks as an indicator of fluoride-silicate liquid immiscibility in magmatic systems.Petrology,18(5):514-543
Pitcher WS.1983.Granite type and tectonic environment.In:HsüKJ(ed.).Mountain Building Processes.London:Academic Press,19-40
Pitcher WS.1997.The Nature and Origin of Granite.2ndEdition.London:Chapman&Hall,1-387
Rudnick RL and Gao S.2005.Composition of the continental crust.In:Holland HD and Turekian KK(eds.).Treatise on Geochemistry.Amsterdam:Elsevier
Samadi R,Mirnejad H,Kawabata H,Harris C,Valizadeh MV and Gazel E.2014.Magmatic garnet in the Triassic(215Ma)Dehnow pluton of NE Iran and its petrogenetic significance.International Geology Review,56(5):596-621
Scaillet B,Pichavant M and Roux J.1995.Experimental crystallization of leucogranite magmas.Journal of Petrology,36(3):663-705
Sharp Z.2007.Principles of Stable Isotope Geochemistry.Upper Saddle River,NJ:Pearson Education
Song SG,Wang MM,Xu X,Wang C,Niu YL,Allen MB and Su L.2015.Ophiolites in the Xing’an-Inner Mongolia accretionary belt of the CAOB:Implications for two cycles of seafloor spreading and accretionary orogenic events.Tectonics,34(10):2221-2248
temprok M.1991.Ongonite from Ongon Khairkhan,Mongolia.Mineralogy and Petrology,43(4):255-273
Sun DY,Suzuki K,Wu FY and Lu XP.2005.CHIME dating and its application for Mesozoic granites of Huanggoushan,Jilin Province.Geochimica,34(4):1-10(in Chinese with English abstract)
Sun JG and Lian CY.1997.Preliminary discussion on the establishment of Proterozoic stratigraphic framework of fanhe area,Tieling.Liaoning Geology,(1):24-29(in Chinese with English abstract)
Sun T,Zhou XM,Chen PR,Li HM,Zhou HY,Wang ZC and Shen WZ.2005.Strongly peraluminous granites of Mesozoic in eastern Nanling Range,southern China:Petrogenesis and implications for tectonics.Science in China(Series D),48(2):165-174
Sylvester PJ.1998.Post-collisional strongly peraluminous granites.Lithos,45(1-4):29-44
Taylor SR and McL ennan SM.1985.The Continental Crust:Its Composition and Evolution.Oxford:Blackwell Scientific Publications
Wang F,Xu YG,Xu WL,Yang L,Wu W and Sun CY.2017.Early Jurassic calc-alkaline magmatism in Northeast China:Magmatic response to subduction of the Paleo-Pacific Plate beneath the Eurasian continent.Journal of Asian Earth Sciences,143:249-268
Wang JL,Li BZ,Zhou DX,Yao SC and Li ZY.1994.Geological Characteristics of Intermediate-Felsic Plutonic Rocks in Hebei Province and Their Relationship with Mineralization.Beijing:Geological Publishing House,60-64(in Chinese)
Wang LX,Ma CQ,Zhang C,Zhang JY and Marks MAW.2014.Genesis of leucogranite by prolonged fractional crystallization:A case study of the Mufushan complex,South China.Lithos,206-207:147-163
Wang RC,Wu FY,Xie L,Liu XC,Wang JM,Yang L,Lai W and Liu C.2017.A preliminary study of rare-metal mineralization in the Himalayan leucogranite belts,South Tibet.Science China(Earth Sciences),60(9):1655-1663
Wang XL,Zhang C,Liu SW and Shu GM.2007.Electron microprobe dating of monazite in granite from Kangbao area,Hebei Province.Acta Petrologica Sinica,23(4):817-822(in Chinese with English abstract)
Wang XL,Zhou JC,Wan YS,Kitajima K,Wang D,Bonamici C,Qiu JS and Sun T.2013.Magmatic evolution and crustal recycling for Neoproterozoic strongly peraluminous granitoids from southern China:Hf and O isotopes in zircon.Earth and Planetary Science Letters,366:71-82
Wang XP,Li R,Yang ZM,Feng YS and Wang KH.2005.Geologic features and tectonic setting of the garnetiferous muscovite granite in the Fangniugou,Qingyuan County,Liaoning Province.Jilin Geology,24(3):1-4(in Chinese with English abstract)
Weidner JR and Martin RF.1987.Phase equilibria of a fluorine-rich leucogranite from the St.Austell pluton,Cornwall.Geochimica et Cosmochimica Acta,51(6):1591-1597
Weinberg RF.2016.Himalayan leucogranites and migmatites:Nature,timing and duration of anatexis.Journal of Metamorphic Geology,34(8):821-843
White AJR,Clemens JD,Holloway JR,Silver LT,Chappell BW and Wall VJ.1986.S-type granites and their probable absence in southwestern North America.Geology,14(2):115-118
Winter JD.2001.An Introduction to Igneous and Metamorphic Petrology.New Jersey:Prentice-Hall,1-697
Wu FY,Sun DY,Jahn BM and Wilde S.2004.A Jurassic garnetbearing granitic pluton from NE China showing tetrad REE patterns.Journal of Asian Earth Sciences,23(5):731-744
Wu FY,Liu ZC,Liu XC and Ji WQ.2015.Himalayan leucogranite:Petrogenesis and implications to orogenesis and plateau uplift.Acta Petrologica Sinica,31(1):1-36(in Chinese with English abstract)
Wu FY,Liu XC,Ji WQ,Wang JM and Yang L.2017.Highly fractionated granites:Recognition and research.Science China(Earth Sciences),60(7):1201-1219
Xia WH and Chen ZY.1984.The discovery of melt inclusions in topaz and quartz and its significance to genesis of Ta-Nb granites in southern China.Earth Science(Journal of Wuhan College of Geology),(2):79-83(in Chinese with English abstract)
Xia WH.Zhang JT,Feng ZW and Chen ZY.1989.Geology of Nanling Granite-Type Rare Metal Deposit.Wuhan:China University of Geosciences Press,90-115(in Chinese)
Xiao WJ,Windley BF,Hao J and Zhai MG.2003.Accretion leading to collision and the Permian Solonker suture,Inner Mongolia,China:Termination of the central Asian orogenic belt.Tectonics,22(6):1069
Xiao WJ,Windley BF,Sun S,Li JL,Huang BC,Han CM,Yuan C,Sun M and Chen HL.2015.A tale of amalgamation of three PermoTriassic collage systems in Central Asia:Oroclines,sutures,and terminal accretion.Annual Review of Earth and Planetary Sciences,43:477-507
Xie L,Wang ZJ,Wang RC,Zhu JC,Che XD,Gao JF and Zhao X.2018.Mineralogical constraints on the genesis of W-Nb-Ta mineralization in the Laiziling granite(Xianghualing district,South China).Ore Geology Reviews,95:695-712
Yang DG,Sun DY,Gou J and Hou XG.2017.U-Pb ages of zircons from Mesozoic intrusive rocks in the Yanbian area,Jilin Province,NEChina:Transition of the Paleo-Asian oceanic regime to the circumPacific tectonic regime.Journal of Asian Earth Sciences,143:171-190
Yang JH,Sun JF,Zhang M,Wu FY and Wilde SA.2012.Petrogenesisof silica-saturated and silica-undersaturated syenites in the northern North China craton related to post-collisional and intraplate extension.Chemical Geology,328:149-167
Ye DL,Tai DQ and Ren YX.1987.Geological and petrological characteristics of M111 rare metal-bearing granite intrusion in Xinglong,Hebei.Earth Science(Journal of Wuhan College of Geology),12(3):265-275,333(in Chinese with English abstract)
Ye DL,Ren YX and Tai DQ.1991.The study on the characteristics of geochemistry and mineralization of the M111 rare metal contained granitic intrusion in Xinglong,Hebei.Geoscience,5(1):13-23(in Chinese with English abstract)
Yuan W,Yang ZY,Zhao XX,Santosh M and Zhou XJ.2018.Early Jurassic granitoids from deep drill holes in the East China Sea Basin:Implications for the initiation of Palaeo-Pacific tectono-magmatic cycle.International Geology Review,60(7):813-824
Zhang C and Han BF.2004.The characteristics and tectonic significance of Meso-Proterozoic late stage granitoids in Wucuan-Kangbao.Acta Petrologica Sinica,20(3):433-438(in Chinese with English abstract)
Zhang QW,Liu ZH,Chai SL,Xu ZY and Xu XC.2011.Zircon U-Pb dating of the Garnet-bearing granite from Wulan area of Urad Zhongqi in Inner Monglia and its geological significance.Journal of Jilin University(Earth Science Edition),41(3):745-752(in Chinese with English abstract)
Zhang SH,Zhao Y,Kr9ner A,Liu XM,Xie LW and Chen FK.2009.Early permian plutons from the northern north china block:Constraints on continental arc evolution and convergent margin magmatism related to the Central Asian orogenic belt.International Journal of Earth Sciences,98(6):1441-1467
Zhang SH,Zhao Y,Liu JM,Hu JM,Song B,Liu J and Wu H.2010.Geochronology,geochemistry and tectonic setting of the Late Paleozoic-Early Mesozoic magmatism in the northern margin of the North China Block:A preliminary review.Acta Petrologica et Mineralogica,29(6):824-842(in Chinese with English abstract)
Zhang SH,Zhao Y,Davis G A,Ye H and Wu F.2014.Temporal and spatial variations of Mesozoic magmatism and deformation in the North China craton:Implications for lithospheric thinning and decratonization.Earth-Science Reviews,131:49-87
Zhang SH,Zhao Y,Liu JM and Hu ZC.2016.Different sources involved in generation of continental arc volcanism:The CarboniferousPermian volcanic rocks in the northern margin of the North China block.Lithos,240-243:382-401
Zhang XH,Mao Q,Zhang H and Wilde SA.2008.A Jurassic peraluminous leucogranite from Yiwulüshan,western Liaoning,North China craton:Age,origin and tectonic significance.Geological Magazine,145(3):305-320
Zhao QY.2010.Origin and tectonic setting of Late Paleozoic-Early Mesozoic granites in Daqingshan district,Inner Mongolia.Ph.D.Dissertation.Changchun:Jilin University(in Chinese with English summary)
Zhao ZH.1988.A preliminary report on the tetrad REE effect in granites.Geology and Geochemistry,(1):71-72(in Chinese)
Zhao ZH,Masuda A and Shabani MB.1992.Tetrad effects of rare-earth elements in rare-metal granites.Geochimica,(3):221-233(in Chinese with English abstract)
Zhao ZH.2016.Principles of Trace Element Geochemistry.2nded.Beijing:Science Press,115-118(in Chinese)
Zheng K.2016.Genesis of garnet-bearing granite and tectonic implications within Kangbao County,North Hebei Province.Master Degree Thesis.Chengdu:Chengdu University of Technology(in Chinese with English summary)
Zhou JC and Wang XL.2005.Experimental and Theoretical Petrology.Beijing:Geological Publishing House,1-256(in Chinese)
Zhou ZB,Pei FP,Wang ZW,Cao HH,Xu WL,Wang ZJ and Zhang Y.2017.Using detrital zircons from Late Permian to Triassic sedimentary rocks in the south-eastern Central Asian Orogenic Belt(NE China)to constrain the timing of the final closure of the Paleo-Asian Ocean.Journal of Asian Earth Sciences,144:82-109
ГрабежевAИ,叶德隆.1984.稀有金属矿化花岗岩专属性的地球化学标志.地质科技情报,(2):74-81
常海亮.1985.香花岭岩黄玉斑晶中熔融包裹体的研究.中国地质科学院宜昌地质矿产研究所文集,(9):33-40
董少花,毕献武,胡瑞忠,陈佑纬.2014.湖南瑶岗仙复式花岗岩岩石成因及与钨成矿关系.岩石学报,30(9):2749-2765
范文博.2017.华北克拉通北缘丰宁地区中生代花岗岩类岩石成因研究.博士学位论文.北京:中国科学院大学
郭春丽,曾令森,高利娥,苏红中,马星华,尹冰.2017.福建河田高分异花岗岩的矿物和全岩地球化学找矿标志研究.地质学报,91(8):1796-1817
李献华,李武显,李正祥.2007.再论南岭燕山早期花岗岩的成因类型与构造意义.科学通报,52(9):981-991
李玉静,王玉芳,徐国新,李智斌,齐云飞,孙金龙,赵丙刚,张勃,越悦.2018.冀东分水岭岩体锆石U-Pb年代学、地球化学特征及地质意义.地质学报,92(9):1904-1917
刘昌实,王汝成,舒良树,陈小明,黄小龙.2002.陆内S型花岗岩的形成与演化.见:王德滋,周新民编.中国东南部晚中生代花岗质火山-侵入杂岩成因与地壳演化.北京:科学出版社,93-135
刘红涛,翟明国,刘建明,孙世华.2002.华北克拉通北缘中生代花岗岩:从碰撞后到非造山.岩石学报,18(4):433-448
刘建忠,刘喜山,张福勤,李树勋,李桂林,欧阳自远.2000.辽宁阜新-锦州地区花岗杂岩特征及成因.地质地球化学,28(4):65-74
刘勇胜.2014.LA-ICP-MS/LA-MC-ICP-MS数据处理软件ICPMSDataCal(V9.5)使用手册
刘志超.2013.喜马拉雅然巴淡色花岗岩时代与成因.博士学位论文.北京:中国科学院大学
吕科,王勇,肖剑.2011.西华山复式花岗岩株地球化学特征及构造环境探讨.东华理工大学学报(自然科学版),34(2):117-128
孟庆鹏,贺元凯,张文,吴泰然,郑荣国,徐操,张昭昱.2013.华北板块北缘古大洋闭合时间的限定---来自四子王旗西后壕子同碰撞花岗岩的证据.地质通报,32(11):1749-1759
孙德有,铃木和博,吴福元,路孝平.2005.吉林省南部荒沟山地区中生代花岗岩CHIME定年.地球化学,34(4):1-10
孙景贵,连长云.1997.辽西地区花岗岩的形成时代.辽宁地质,(1):24-29
孙涛,周新民,陈培荣,李惠民,周红英,王志成,沈渭洲.2003.南岭东段中生代强过铝花岗岩成因及其大地构造意义.中国科学(地球科学),33(12):1209-1218
王季亮,李丙泽,周德星,姚士臣,李枝荫.1994.河北省中酸性岩体地质特征及其与成矿关系.北京:地质出版社,60-64
王汝成,吴福元,谢磊,刘小驰,王佳敏,杨雷,赖文,刘晨.2017.藏南喜马拉雅淡色花岗岩稀有金属成矿作用初步研究.中国科学(地球科学),47(8):871-880
王鑫琳,张臣,刘树文,舒桂明.2007.河北康保地区花岗岩独居石电子探针定年.岩石学报,23(4):817-822
王秀萍,李睿,杨志猛,冯义生,王凯红.2005.辽宁省清源县放牛沟含榴白云母花岗岩地质特征及构造环境探讨.吉林地质,24(3):1-4
吴福元,刘志超,刘小驰,纪伟强.2015.喜马拉雅淡色花岗岩.岩石学报,31(1):1-36
吴福元,刘小驰,纪伟强,王佳敏,杨雷.2017.高分异花岗岩的识别与研究.中国科学(地球科学),47(7):745-765
夏卫华,陈紫英.1984.黄玉、石英中熔浆包裹体的发现及其在华南钽铌花岗岩成因上的意义.地球科学(武汉地质学院学报),(2):79-83
夏卫华,章锦统,冯志文,陈紫英.1989.南岭花岗岩型稀有金属矿床地质.武汉:中国地质大学出版社,90-115
叶德隆,邰道乾,任迎新.1987.河北兴隆M111稀有金属花岗岩体地质和岩石学特征.地球科学(武汉地质学院学报),12(3):265-275,333
叶德隆,任迎新,邰道乾.1991.河北兴隆M111稀有金属花岗岩体地球化学和矿化特征研究.现代地质,5(1):13-23
张臣,韩宝福.2004.华北北部武川-康保地区中元古代晚期花岗岩类基本特征及其构造意义.岩石学报,20(3):433-438
张青伟,刘正宏,柴社立,徐仲元,徐学纯.2011.内蒙古乌拉特中旗乌兰地区含石榴石花岗岩锆石U-Pb年龄及地质意义.吉林大学学报(地球科学版),41(3):745-752
张拴宏,赵越,刘建民,胡健民,宋彪,刘健,吴海.2010.华北地块北缘晚古生代-早中生代岩浆活动期次、特征及构造背景.岩石矿物学杂志,29(6):824-842
赵庆英.2010.内蒙古大青山地区晚古生代-早中生代花岗岩成因及其形成构造环境.博士学位论文.长春:吉林大学
赵振华.1988.花岗岩中发现稀土元素四重分布效应的初步报道.地质地球化学,(1):71-72
赵振华,增田彰正,夏巴尼MB.1992.稀有金属花岗岩的稀土元素四分组效应.地球化学,(3):221-233
赵振华.2016.微量元素地球化学原理.第2版.北京:科学出版社,115-118
郑坤.2016.冀北康保石榴花岗岩成因及大地构造意义.硕士学位论文.成都:成都理工大学
周金城,王孝磊.2005.实验及理论岩石学.北京:地质出版社,1-256
© 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 |