河北阜平平阳片麻状花岗岩及其成因
|
摘要
平阳片麻状花岗岩位于阜平复式穹状构造猴石顶倒转背斜的东部，出露面积大于40平方公里，为奥长花岗岩。岩体的西部似一穹状背斜，向东逐渐转变为两个向南倒转的次级背斜，总体上为向南倒转的复式背斜的核部，其产状及其面理构造与区域构造线完全一致。花岗岩在中北部与围岩呈侵入接触，其他部分主要由混合岩或混合质黑云斜长片麻岩过渡到变质表壳岩。平阳岩体岩性不很均匀，长英质集结体及团块、长英质“无根”脉很发育，暗色矿物(黑云母、角闪石、磁铁矿)分布不均匀，在岩体边缘及附近围岩中伟晶岩脉较为多见。平阳片麻状花岗岩之中存在以片麻岩为主的变质表壳岩残留层(体)，片麻理与岩体的片麻理协调一致，其产状继承了原岩的产状，尤其是在岩体的东部，使花岗岩的原地特征表现十分清楚。岩体中还广泛分布着各种类型的变质基性岩石包体(角闪质岩石和麻粒岩)和岩片，在东部具有明显的“成群成带”分布特点，边缘地带也较为多见。
平阳片麻状花岗岩主要由奥长石，石英和黑云母组成，含少量微斜长石，局部含少量角闪石，极少量白云母。具有典型的波状一齿状花岗变晶结构，补片状的反条纹长石多见，常见绢云母化、缝合线结构、乳滴状石英的交代穿孔结构。石英外形弯曲多变，波状消光明显。黑云母常见暗化边并有细粒磁铁矿析出等的深熔初期的岩相学现象。总体显示了交代、重熔成因的岩相学特点。
平阳片麻状花岗岩的化学成分是在区域混合岩化对岩石成分总体改造趋势的背景下，在黑云斜长片麻岩成分的基础上，通过黑云斜长片麻岩的深熔以及可能的变质脱水反应流体和深部流体的加入演变而成，富SiO_2、Na_2O以及Sr和Ba。花岗岩的不相容元素、REE和Sm-Nd同位素与片麻岩、变粒岩显示了系统性的演变，并具一定互补性。片麻岩等的深熔还使Sm／Nd发生轻微分馏，进而使花岗岩Nd同位素组成随Sm／Nd一起表现了明显的区域性变化。花岗岩Sm-Nd同位素模式年龄比片麻岩等要小约200Ma。根据副矿物和锆石，以及矿物温压计估算，并结合已有同位素测年数据，认为平阳片麻状花岗岩是在25亿年稍后，在造山作用中，伴随构造减压作用，与阜平群中一系列倒转褶皱形成的同时，由片麻岩等深熔而成。
Occurs to the eastern Houshiding overturned anticline of Fuping complex domal uplift, Pingyanggneissic granite, a trondhjemite looks like a domal anticline in the west part and becomes twosub-anticlines overturned to south in the east part. It is just the core of a multiple anticline aswhole and parallels including its gneissosity to the regional tectonic line. The granite has a belt oftransition composed of migmatite and migmatitic biotite gneiss between its body andmetamorphosed supracrustal rocks, but it exhibits magmatic features in center-north part andshows intrusive contact with wall rocks in some parts of its northern. Lithologic inhomogeneity ofgranite can be observed by the truth such as commonly occurred quartz-feldspathic lumps andblind ending Veins, uneven distributed dark minerals as well as pegmatite veins in its border.Within the granite particularly its eastern part, it is frequently met that gneiss which has itsoriginal occurrence, and granulite and amphibolite enclaves as well.
Pingyang gneissic granite which has wavy-hackly granoblastic texture mainly comprisesoligoclase, quartz and biotite, and also some microcline,hornblende and little muscovite.Characteristics of the metasomatic and re-melting petrography has been shown by metasomaticstructures of varieties, antiperthite of small sheets, quartz of various shapes with stronly wavyextinction and biotite with dark rim and fine magnetite presents along the rim..
The chemical composition of Pingyang gneissic granite with high contents of SiO_2,Na_2O,Sr andBa was inherited and developed from that of mainly biotite gneiss through anatexis under thebackground of regional migmatisation, it might also be introduced the fluid material from deep.Thus the comparatively and systematically variations of incompatible elements, REE and Sm-Ndisotopic ratios can be seen among granoblasite-gneiss-granite. Anatexis of gneisses resulted in aslightly fractionation of Sm/Nd and this in turn caused areal variation of Sm-Nd isotopic ratioswithin the granite. A deduction has been made that explains the gneissic granite was formed byanatexis of mainly gneisses in the time of overturned folding during the tectonic depressurizationperiod of the orogeny, these were happened at about 2.5Ga or later.
平阳片麻状花岗岩主要由奥长石，石英和黑云母组成，含少量微斜长石，局部含少量角闪石，极少量白云母。具有典型的波状一齿状花岗变晶结构，补片状的反条纹长石多见，常见绢云母化、缝合线结构、乳滴状石英的交代穿孔结构。石英外形弯曲多变，波状消光明显。黑云母常见暗化边并有细粒磁铁矿析出等的深熔初期的岩相学现象。总体显示了交代、重熔成因的岩相学特点。
平阳片麻状花岗岩的化学成分是在区域混合岩化对岩石成分总体改造趋势的背景下，在黑云斜长片麻岩成分的基础上，通过黑云斜长片麻岩的深熔以及可能的变质脱水反应流体和深部流体的加入演变而成，富SiO_2、Na_2O以及Sr和Ba。花岗岩的不相容元素、REE和Sm-Nd同位素与片麻岩、变粒岩显示了系统性的演变，并具一定互补性。片麻岩等的深熔还使Sm／Nd发生轻微分馏，进而使花岗岩Nd同位素组成随Sm／Nd一起表现了明显的区域性变化。花岗岩Sm-Nd同位素模式年龄比片麻岩等要小约200Ma。根据副矿物和锆石，以及矿物温压计估算，并结合已有同位素测年数据，认为平阳片麻状花岗岩是在25亿年稍后，在造山作用中，伴随构造减压作用，与阜平群中一系列倒转褶皱形成的同时，由片麻岩等深熔而成。
Occurs to the eastern Houshiding overturned anticline of Fuping complex domal uplift, Pingyanggneissic granite, a trondhjemite looks like a domal anticline in the west part and becomes twosub-anticlines overturned to south in the east part. It is just the core of a multiple anticline aswhole and parallels including its gneissosity to the regional tectonic line. The granite has a belt oftransition composed of migmatite and migmatitic biotite gneiss between its body andmetamorphosed supracrustal rocks, but it exhibits magmatic features in center-north part andshows intrusive contact with wall rocks in some parts of its northern. Lithologic inhomogeneity ofgranite can be observed by the truth such as commonly occurred quartz-feldspathic lumps andblind ending Veins, uneven distributed dark minerals as well as pegmatite veins in its border.Within the granite particularly its eastern part, it is frequently met that gneiss which has itsoriginal occurrence, and granulite and amphibolite enclaves as well.
Pingyang gneissic granite which has wavy-hackly granoblastic texture mainly comprisesoligoclase, quartz and biotite, and also some microcline,hornblende and little muscovite.Characteristics of the metasomatic and re-melting petrography has been shown by metasomaticstructures of varieties, antiperthite of small sheets, quartz of various shapes with stronly wavyextinction and biotite with dark rim and fine magnetite presents along the rim..
The chemical composition of Pingyang gneissic granite with high contents of SiO_2,Na_2O,Sr andBa was inherited and developed from that of mainly biotite gneiss through anatexis under thebackground of regional migmatisation, it might also be introduced the fluid material from deep.Thus the comparatively and systematically variations of incompatible elements, REE and Sm-Ndisotopic ratios can be seen among granoblasite-gneiss-granite. Anatexis of gneisses resulted in aslightly fractionation of Sm/Nd and this in turn caused areal variation of Sm-Nd isotopic ratioswithin the granite. A deduction has been made that explains the gneissic granite was formed byanatexis of mainly gneisses in the time of overturned folding during the tectonic depressurizationperiod of the orogeny, these were happened at about 2.5Ga or later.
引文
程裕淇、沈其韩、刘国惠、王泽九，1963，变质岩的一些基本问题和工作方法，中国工业出版社195页。
程裕淇，1987，关于混合岩和混合岩化作用的一些问题—对半个世纪以来某些基本问题的回顾，中国地质科学院院报，第16号，5-19。
程裕淇、高吉凤、万渝生，1996，河北平山晚太古代阜平群一些主要变质岩类深熔特征的初步研究，献给第三十届 国际地质大会地质科学论文集，中国经济出版社。
程裕淇、高吉凤、万渝生、马瑞，1998，河北平山阜平群两种岩石类型的初步熔融实验极其启示，中国地质，1998(3)：18-22。
程裕淇、高吉凤、万渝生，1999，论中国河北平山西北部新太古代阜平群一些变质岩类的深熔作用，前寒武纪地质学和变质岩石学(钱祥麟、游振东主编)，第30届国际地质大会论文集(17)：126-136。
程裕淇、万渝生、高吉凤，2000a，河北平山小觉地区阜平群变质作用和深熔作用同位素年代研究的初步报道，地质学报，2000(2)：30-37。
程裕淇、刘敦一、I．S．Williams、简平、庄育勋、高天山，2000b，大别山碧溪岭深色榴辉岩和片麻状花岗质岩石SHRIMP分析—晋宁期高压-超高压变质作用的同位素年代学依据，地质学报，2000(3)：193-205。
程裕淇、高吉凤、万渝生、马瑞，2000c，河北平山小觉地区新太古代阜平岩群中变质岩所显示深熔改造的一些岩相学特征，中国地质，2000(12)：14-16。
董申保，1999，五十年来中国花岗岩研究的回顾与展望，中国地质科学五十年(王鸿祯主编)，中国地质大学出版社，123-130页。
洪大卫，1994，花岗岩研究的最新进展及发展趋势，地学前缘，1(1-2)：79-86页。
高吉凤，1997，河北平山晚太古代阜平群中主要变质岩类及其深熔产物的稀土地球化学初步研究，岩石学报，1997(3)，418-426页。
关鸿、孙敏、徐平，1998，阜平杂岩中几种不同类型片麻岩的锆石激光探针等离子体质谱年代学研究，岩石学报，1998(11)：460-470。
李江海、钱祥麟，1994，恒山早前寒武纪地壳演化，山西科学技术出版社，116页。
李武显、董传石、周新民，1999，平潭和漳州深成杂岩中斜长石捕虏晶与岩浆混合作用，岩石学报，15(2)：286-290。
刘敦一、R．W．佩吉、W．康普斯顿、伍家善，1984，太行山-五台山区前寒武纪变质岩系同位素地质年代学研究，中国地质科学院院报，8：57-82页。
刘树文、梁海华、赵国春、华永刚、简安华，2000，太行山早前寒武纪杂岩的同位素年代学和地质事件，中国科学(D辑)，2000(1)：18-24。
刘树文，1996，阜平地区麻粒岩的P-T路径研究，高校地质学报，1996(2卷)：75-83。
刘福来、沈其韩、耿元生、徐学纯、马瑞，1997，麻粒岩相条件下熔融反应与矿物相转变机制的实验研究，地质学报，1997(3)：254-265。
马杏垣、游振东、谭应佳、蔡学林，1963，中国东部前寒武纪大地构造发展的样式，地质学报，1963(1)：27-52。
南京大学地质学系，1981，华南不同时代花岗岩类及其与成矿关系，1981，科学出版社，395页。
牛树银、陈路、许传诗等，1994，太行山区地壳演化及成矿规律，地震出版社，页。
钱祥麟、崔文元、王时麒，1985，内蒙、冀东太古界麻粒岩相岩带的演化，地质研究论文集，北京大学出版社，20-29页。
山西地层表编写组，1979，华北地区区域地层表，山西分册(一)，地质出版社，195-202页。
沈其韩、徐惠芬、张宗清、高吉凤、伍家善、吉成林，1992，中国早前寒武纪麻粒岩，地质出版社，237页。
沈其韩，1998，华北地台早前寒武纪条带状铁英岩地质特征和形成的地质背景，华北地台早前寒武纪地质研究论文集(程裕淇主编)，1-30。
孙敏、关鸿，阜平杂岩年龄及其地质意义：兼论前寒武高级变质地体的定年问题，岩石学报，2001，17(1)：145-156。
谭应佳、王方正、赵温霞，1993，太行山阜平隆起南部早前寒武纪地质-兼论太古宙地质若干问题及研究方法，中国地质大学出版社，161页。
万渝生，1987，雌山混合花岗岩及有关岩石的副矿物组合锆石特征及其地质意义，地质论评，1987(5)：229-236。
王江海、扬问华、吴金平，1994，鄂东北大别杂岩中混合岩形成的动力学机制，地质学报，1994(4)：308-323。
王凯怡、李继亮、刘如琦，1991，阜平片麻岩之成因，地质科学，1991(7)：254-266。
王凯怡、郝杰、周少平、Wilde，S．，Cawood，P．A．，单颗粒锆石离子探针质谱定年结果对五台造山事件的制约，科学通报，1997(12)：1295-1297。
王涛，2000，花岗岩混合成因研究及大陆动力学意义，岩石学报，2000，16(2)：161-168。
王联魁、朱为方、张绍力，1982，华南花岗岩两个成岩成矿系列的演化，地球化学，1982(4)，329-339页。
王德滋、周金城，1999；我国花岗岩研究的回顾与展望，岩石学报，15(2)：161-169页。
吴昌华、李惠民、钟长汀、左义成，2000，阜平片麻岩和湾子片麻岩的单颗粒锆石U-Pb年龄——阜平杂岩并非一统太古宙基地的年代学证据，前寒武纪研究进展，2000(3)：129-139。
吴澄宇、万渝生，1997，稀土元素地球化学与花岗质岩石的成因—应用与问题，岩石圈研究的现代方法(张炳熹等主编)，201-214页。
伍家善、耿元生、徐惠芬、金龙国、贺绍英、孙世伟，1989，阜平群变质地质，中国地质科学院地质研究所所刊，19，219页。
伍家善、耿元生、沈其韩、刘敦一、厉子龙、赵敦敏，1991，华北陆台早前寒武纪重大地质事件，地质出版社，115页。
伍家善、耿元生、沈其韩、万渝生、刘敦一、宋彪，1998，中朝古大陆太古宙地质特征及构造演化，地质出版社，212页。
徐夕生、周新民、O’Rreilly，S．Y．，唐红峰，1999，中国东南部下地壳物质与花岗岩成因探索，岩石学报，15(2)：217-223页。
徐克勤、胡受奚、孙明志、张景荣、叶俊，1983，论花岗岩的成因系列—以华南中生代花岗岩为例，地质学报，1983(2)：107-118页。
徐克勤、孙鼐、王德滋、胡受奚、刘英俊、季受元、1984，华南花岗岩成因与成矿，花岗岩地质和成矿关系(徐克勤、涂光炽主编)，江苏科学技术出版社，1-20页。
徐朝雷、徐有华、张平，1985，太行山区龙华河群的建立与否定，地球科学，1985(4)：151-158。
杨杰，1936，山西省五台山地质略述，中国地质学会会志，2，261页。
张春华等，1990，河北早前寒武纪变质作用，地质出版社。
张寿广、金龙国、肖庆辉，阜平太古宙穹状复合褶皱群的构造样式及变形史，中国 区域地质，1983(6)：97-110。
张西平，1999，深熔作用及有关问题，地球学报，1999，增刊，38-47。
张宗清、伍家善、叶笑江，1991，阜平群下部太古代变质岩石的REE、Rb-Sr和Sm-Nd年龄及其意义。地球化学，1991(2)：118-126。
郑海飞、谢鸿森、徐有生、宋茂双、张月明、王明再、徐惠刚，1995，高温高压下含水矿物对岩石熔点影响的实验研究，地质学报，1995(4)：326-335。
中国地质图(1：5000000)编辑委员会，1990，中国地质图(1：5000000)，地质出版社。
中国科学院贵阳地球化学研究所，1979，华南花岗岩类的地球化学，科学出版社，421页。
周新民、姚玉鹏、徐夕生，1992，浙东大巨山花岗岩中淬冷包体及其成因机制，岩石学报，8(3)：234-242页。
周珣若，1994；1994，花岗岩混合作用，地学前缘，1(1-2)：87-97页。
哈克，A．，1981，变质作用：岩石转变的研究(中译本)，地质出版社，373页。
J．迪迪埃，1981，花岗岩极其包体：包体与花岗岩成因的关系，中译本，姜胜章译，地质出版社，274页。
V．马莫，花岗岩岩石学与花岗岩问题，中译本，袁廷佐，吴荣庆译，地质出版社，255页。
Arth, J. G. and Hanson, G. N., 1972, Quartz diorites derivd by partial melting of eclogite or amphibolite at mantle depths, Contrib. Mineral. Petrol.,37, p. 161-174.
Arth, J. G. and Hanson, G. N.,1975, Geochemistry and origin of the early Precambrian crust of northeastern Minneresota, Geochim. Cosmochim. Acta, 39, p. 325-362.
Ashworth, J.R.,1985, Introduction, in: Ashworth et al(eds),Migmatites, Blackie, New York, p. 1-35.
Barbey, P., Brouand, M., Le Fort, P. AndPecher, A.,1996, Granite-migmatite genetic link: the example of the Manaslu granite and Tibeten Slab migmatites in central Nepal, Lithos, vol. 38, p. 63-79.
Barboza S.A. and Bergantz, G.W., 1996, Dynamic model of dehydration melting motivated by a natural analogue:applications to the Ivrea-Verbano zone, northern Italy, Transactions of the Royal Society of Edinburgh, 87, p23-31.
Barboza,S.A. and Bergantz,G.W.,2OOO,Metamorphism and anatexis in the mafic complex contact aureole, Ivrea Zone, northern Italy, J. Petrol., vol. 41, p. 1307-1327.
Barker F., 1979, Trondhjemite:Definition, environment and hypotheses of origin, in: Barker F. (ed), Trondhjemites, dacites and related rocks. Elsevier, Amsterdam, p.1-12.
Barker, F. and Millard, H.T.,Jr.,1979, Geochemistry of the type trondhjemite and three associated rocks, Norway, in:Barker F. (ed), Trondhjemites, dacites and related rocks. Elsevier, Amsterdam, p. 517-529.
Bergantz, G. W. and Dawes, R. 1994, Aspects of magma generation and ascent in continental lithosphere, in: Ryan, M. P. (ed.), Magmatic systems, San Diego, CA: Academic Press, p291-317.
Brown, M.,1993, P-T-t evolution of orogenic belts and the causes of regional metamorphiism, J. geol. Soc., London, vol. 150, p. 227-241.
Brown, M.,1994, The generation, segregation, ascent and emplacement of granite magma: the migmatite-to-crustal ly-derived granite connection in thickened orogens, Earth Sci. Rev.,vol,36,p. 83-130.
Brown, M. and Dallmeyer, R. D., 1996, Rapid variscan exhumation and the role of magma in core complex formation:southern Brittany metamorphic belt, France, J. Metamorphic Geol., vol. 14, p.361-379.
Brown, M. and Rushmer, T., 1997, The role of deformation in the movement of granitic melt: views from the laboratort and the field, in: Holness(ed), Deformation-enhanced fluid transport in the Earth's and mantal, Chapman & Hall, London, p. 111-144.
Campbell, I. H. and Turner, J. S. , 1987, A laboratory investigation of assimilation at the top of a basltic magma chamber, J. Geol. , 95, pl55—172.
Carmichael, D. M., 1987, Induced stress and secondary mass trasfer: thermodynamic basis for the tendency toward constant-volume constraint in diffusion metasomatism, in:Helgeson(ed),Chemical transport in metasomatic processes, D. Reidel Publishing Company, p. 239-264.
Carswell, D. A. and O'Brien, P. J., 1993, Thermobarometetry and geotectonic significance of high-p granulite examples from the Moldanubian zone of the Bohemian massif in lower Austria, J. Petrol., 34, p. 427-459.
Castro, A., 1991, H-type (Hybrid) granitoids: a proposed revision of the granite type classification and nomenclature, Earth Sci. Rev. , vol, 31, p. 237-253.
Cheng, Y. Q., Gao,J. F. and Wan, Y. S., 1997, Notes on the anatexis of some metamorphic rock types of Late Archaean Fuping Group of Northwestern Pingshan, Hebei Province, China, in:X. L., Qian et al (eds),Proc.30~(th) Int'l. Geol. Congr., vol. 17, part II, p. 173-185.
Chappell, B. W. , 1996 , Magma mixing and the production of compositional variationwithin granite suites:evidence from the granites of southeastern Australia, J. Petrol, vol. 37, P. 449-470
Chappell, B. W. , White, A. J. R. and Wyborn, D., 1987, The importance of residual source material(restite) in granite petrogenesis., J. Petrol, vol. 28, p. 1111-1138.
Chappell, B. W. and White, A. J. R., 1992,I- and S-type granites in the Lachlan Fold Belt, Trans. Roy. Soc. Edinburgh: Earth Sci., 83,p.1-26.
Clarke, D. B., 1996, Two centuries after Hutton's 'Theory of the Earth': the status of granite science, Trans. Roy. Soc. Edinburgh: Earth Sci., 87, p. 353-359.
Clemens J. D., 1990, The granulite-granie connexion, in: Vielzeuf, D. and Vidal.Ph. (eds), Granulites and crustal evolution, Kluwer Academic Publishers, Dordrecht, p. 25-36.
Clements, J. D., Petford, N. and Mawer, C. K., 1997, Ascent mechanisms of granitic magmas: causes and consequenses, in: Holness(ed), Deformation-enhanced fluid transport in the Earth's and mantal, Chapman & Hall, London, p. 145-192.
Collins, W. J. , 1996, Lachlan Fold Belt granitoids: products of three-component mixing, Trans. Royal. Soc. Edinburgh: Earth Sci. 87, p. 171-181.
Compton, P., 1978, Rare earth evidence for the origin of the N k gneisses Buksef jorden region, southern West Greenland, Contrib. Minerl. Petrol., 66, p. 283-293.
Condie, K. C. and Harrison, N. M., 1976, Geochemistry of the Archean Bulawayan
Group, Midlands greenstone belt, Rhodesia, Precambrian Res., 3, p. 253-271.
Condie, K. C., 1982, Plate tectonics & crustal evolution(2ed), Pergramon Press, 310p.
Cullers, R. L. and Graf, J. L., 1984, Rare earth element in igneous rocks of the continental crust: intermediate and silicic rocks-ore petrogenesis, in; Henderson,P. (ed),Rare earth element geochemistry, Elsevier, Amsterdam, p. 275-316.
Davidson, J. P. , Tepley, F. J.III and Knesel, K. M. , 1998, Isotopic fingerprinting may provide insights into evolution of magmatic systems, EOS Transactions, Am. Geophy. Union 79, 185, 189, 193.
Drury, S. A., 1978, REE distributions in a high-grade Archean gneiss complex in Scotland: implications for the ancient sialic crust. Precambrian Res., 7, p. 237-257.
Drummond, M. S., Defant,M. J. and Kepezhinskas, P. K., 1996, Petrogenesis of slab-derived trondhjemite-tonalite-dacite/adakite magmas, Trans. Roy. Soc.Edinburgh: Earth Sci., 87, p. 205-215.
Ellis, D. J. , 1987, Origin and evolution of granulites in normal and thickened crust, Geol., 15, pl67-170.
England, P. C. and Thompson, A. B., 1984, Pressure-temperature-time paths of regional metamorphism I . Heat transfer during the evolution of regions of thickened continental crust, J. Petrol., 25, p. 894-928.
Fitzsimons, I. C. W., 1996, Metapelitic migmatites from Brattstrand Bluffs,East Antarctica-Metamorphism,melting and Exhumation of the mid crust, J. Petrol., vol. 37, p. 395-414.
Fountain D. M., Salisbury M. H., 1981, Exposed cross-sections through the continental crust:implications for crustal structure, petrology and evolution. Earth Planet. Sci. Lett. 56, 263-277.
Frey, F. A., Chappell, B. W. and Roy, S. D., 1978, Fractionation of Rare-earth elements in the Tuolumne Intrusive Series, Sierra Nevada batholith, California, Geology, 6, p. 239-242.
Giorgetti.G., Frezzotti,M. -L. E., Palmeri, R. And Burke, E. A. J., 1996, Role of fluids in migmatites:C02-H20 fluid inclusion in leucosomes from the Deep Freeze Range migmatites(Terra Nova Bay, Antarctica), J.metamorphic Geol., 1996,14, p. 303-317.
Glickson, A. Y., 1976, Trace element geochemistry and origin of early Precambrian acid igneous series, Barberton Mountain Land, Transvaal, Geochim. Cosmochim. Acta,40, p. 1261-1280.
Graessner, T. And Schenk, V., 2001, An exposed Hercynian deep crustal section in the Sila Massif of northern Calabria: mineral chemistry, petrology and a P-T path of granulite-facies metapelitic migmatites and metabasites, J. Petrol, vol. 42, p. 931-961.
Graham, C. M., Skelton, A. D. L., Bickle, M. And Cole,C.,1997, Lithological, structural and deformation controls on fluid flow during regional metamorphism, in: Holness(ed), Deformation-enhanced fluid transport in the Earth's and mantal, Chapman & Hall, London, p.196-226.
Greenwood, H. J., 1987, Fluid exchange between reaction bodies of rock, in:Helgeson(ed), Chemical transport in metasomatic processes, D. Reidel Publishing Company, p. 153-168.
Hanson, G. N. and Goldich, S. S., 1972, Early Precambrian rocks in the Saganaga Lake-Northern Light Lake Area, Minnesoda-Ontario, II. Petrogenesis. Geol. Soc. Am., Mem., 135, p. 179-192.
Hawkesworth, C. J. and van Calsteren , P. W. C., 1984, Radiogenic isotopes-some geological applications, in Henderson,P. (ed), Rare earth element geochemistry, Elsevier, Amsterdam, p. 375-422.
Holland, T. J. B. and Blundy, J. D., 1994, Non-ideal interactions in calci amphiboles and their bearing on amphibole plagioclase thermometry. Contrib. Mineral. Petrol., 116, p. 433-447.
Hutton, 1997, Theory of the Earth with proofs and illustrations, volIII, London. Johannes, W., 1985, The significance of experimental studies for the formation of migmatites, in: Ashworth et al(eds), Migmatites, Blackie, New York, p. 36-85. Johannes, W. and Holtz, F., 1996, Petrogenesis and experimental petrology of granitic rocks, Springer,335p.
John, B. E. and Stunitz, H., 1997, Magmatic fracturing and small-scale melt segregation during pluton emplacement: evidence from the Adamello massif (Italy), in: Holness(ed), Deformation-enhanced fluid transport in the Earth's and mantal, Chapman & Hall, London, p. 55-74.
Knesel, K. M. and Davidson, J. P., 1996, Isotopic disequilibrium during melting of granite and implications for crustal contamination of magmas, Geology, v. 24, no. 3, p.243-246.
Knesel, K. M. , Davidson, J. P. and Duffield, W. A. , 1999, Open-system evolution of silicic magma by assimilation followed by recgarge: evidence from Sr isotopes in sanidine phenocrysts, Taylor Creek Rhyolite, NM. J. Petrol. , vol. 40, p. 773-786.
Kohn, M. J. and Spear, F. S., 1990, Two new geobarometers for garnet amphibolites, with applications to southeastern Vermont. Amer. Mineralogist, 75,p. 89-96.
Lambert, R. St. J. and Holland, J. G., 1976, Am tsoq gneiss geochemistry preliminary observations, in:Windley, B. F. (ed), The early history of the Earth, Wiley, New York, N. Y., p. 191-201.
Leak, B. E., 1990, Granite magmas, their sources, initiation and consequences of emplacement, J. Geol. Soc. Lond., 147, p. 579-589.
London, D., Morgan VI G. B., Babb, H. A. and Loomis, J. L., 1993, Behavior and effects of phosphorus in the system Na20-K20-A1203"Si02-P205-H20 at 200 Mpa(H20), Contrib. Mineral. Petrol., 113, p.450-465.
Maniar, P. D. and Piccoli, P. M.,, 1989, tectonic discrimination of granitoids, Geol. Soc. Am. Bull.,101, p. 635-643.
Martin, H., 1994, Archaean grey gneisses and continental crust origin, in: Condie(ed), Archaean crustal evolution, Elsevier, Amsterdam., p.205-259.
Masuda, A., Nakamura, N. and Tanaka, T., 1973, Fine structures of mutually normalised Rare-earth patterns of chondrites, Geochim. Cosmochim. Acta, 37,p. 239-248.
Mehnert,K. R., 1968, Migmatites, Elsevier Amsterdam, 393p.
Mogk,D. W., 1992, Ductile shearing and migmatization at mid-crustal level in an Archaean high-grade gneiss belt, northern Gallatin Range, Montana, USA., J. Metamorphic Geol., vol. 10, p. 427-438.
Montel, J. M., 1993, A model for monazite/melt equilibrium and application to the generation of granitic magmas, Chem. Geol., vol. 110, p. 127-146.
Nabelek, P. I.,1997, Quartz-sillimanite leucosomes in high-grade schists, Black Hills, South Dakota: A perspective on the mobility of Al in high-grade metamorphic rocks, Geol., vol. 25, p. 995-998
Nedelec, A., Minyem,D. and Barbey, P.,1993, High-P-high-T anatexis of Archaean tonalitic grey gneisses: the Eseka migmatites, Cameroon, Precamb. Res., vol. 62, p. 191-205.
Nekvasil,H. And Carroll, W., 1996, Experimental constraints on the compositional evolution of crustal magmas, Transactions of the Royal Society of Edinburgh: Earth Sciences,87,p. 139-146.
Neogi, S., Dasgupta, S. and Fukuoka, M., 1998, High P-T polymetamorphism, Dehydration melting, and generation of migmatites and granites in the Higher Himalayan Complex, Sikkim, India, J. Petrol., vol. 39, p61-99.
Norlan, E. U., Schert.H. -P. and Schreyer. W., 2000, Garnet-omphacite-phengite thermobarometry of eclogites from the coesite-bearing unit of the southern Dora-Maira Massif, Western Alps, Lithos, 52, p. 197-214.
Norton, D. L., 1987, Advective metasomatism, in:Helgeson(ed), Chemical transport in metasomatic processes, D. Reidel Publishing Company, p. 123-132.
Oconnor, J. T., 1965, A classification for quartz-rich igneous rock based on feldspar ratios, U.S. Geol. Surv. Prof. Paper 525B, B79-B84.
Ohr,M., Halliday, A. N. and Peacor, D. R., 1994, Mobility and fractionation of rare earth elements in argillaceous sediments: implications for dating diagenesis and low-grade metamorphism, Geoch. Et Cosmo ecta, vol. 58,p. 289-312.
Olsen, S. N., 1985, Mass balance in migmatites, in: Ashworth et al(eds), Migmatites, Blackie, New York, p. 145-179.
0'Nions, R. K. and Pankhursf, R. J., 1974, Rare-earth element distribution in Archean gneisses and anothosites, Godthab area, West Greenland, Earth Planet. Sci. Lett., 22, p. 328-338.
0'Nions, R. K. and Pankhursf, R. J., 1978, Early Archean rocks and geochemicalevolution of the earth's crust, Earth Planet. Sci. Lett., 38, p. 211-236.
Otamendi, J.E. and Patino Douce, A. E. , 2001, Partial melting of aluminous metagreywackes in the norther Sierra de Comechingones, Central Argentina, J. Petrol.,vol. 42,p1751-1772.
Patino Douce, A. E. and McCarthy, T. C., 1998, Melting of crustal rocks during continental collision and subduction, in:Hacker, B. R. and Liu, J. G. (ed), When continents collide: Geodynamics and geochemistry of ultrahigh-pressure rocks, Kluwer Academic Publishers, p. 27-55.
Pearce, J. A., 1983,Role of the sub-continental lithosphere in magma genesis at active continental margins, in: Hawkesworth C. J. and Norry M. J. (eds), Continental basalts and mantle xenoliths, Shiva, Nantwich, p. 230-249.
Petford, N., Clements, J.D. and Vigneresse,J. L.,1997, Application of information theory to the formation of granitic rocks, in: Bouchez et al(eds), Granite: from segregation of melt to emplacement fabrics, Kluwer Academic Publishers, p. 3-10.
Pichavant,M., Hammonda, T. And Scaillet, B., 1996, Control of redox state and Sr isotopic composition of granitic magmas: a critical evaluation of the role of souce rocks, Transactions of the Royal Society of Edinburgh: Earth Sciences, 87, p. 321-329.
Pitcher, W. S., 1997, The nature and origin of granite(2ed), Chapman & Hall,p387. Pupin, J. P.,1980,Zircon and granite petrology, Contrib. Mineral. Petrol.,73,p.207- 220.
Putnis, A. And McConnell, J. D. C.,1980, Principles of mineral behaviour, Blackwell Scientific Publications, 257p.
Rice, T. M. and Ferry, T. M., 1982, Buffering, infiltration, and the control of intensive variables during metamorphism, in: Ferry(ed), Charaterization of metamorphism through mineral equilibria, Mineralogical Soc. Am, p.263-326.
Rapp,R. P., Watson, E. B. and Miller,C. F., 1991, Partial melting of amphibolite/eclogite and the origin of Archaean trondhjemites and tonalites, Prec. Res., vol. 51, p. 1-25.
Read, H. H., 1957, The granite controversy, Thomas Murby & Co. Rollinson, H. R.,1993, Using geochemical data:evaluation, presentation, interpretation, Longman Scien. & Tech., p343.
Rushmer, T., 1996, Melt segregation in the lower crust: how have experiments help us?, Transactions of the Royal Society of Edinburgh: Earth Sciences, 87, p. 73-83.
Sawyer, E. W., 1991, Disequilibrium melting and the rate of melt-residium separation during migmatization of mafic rocks from the Grenvilli Front, Quebec, J. Petrol, vol. 32, p. 701-738.
Sawyer, E. W., 1996, Melt segregation and magma flow in migmatites: implications for the generation of granite magmas, Transactions of the Royal Society of Edinburgh: Earth Sciences, 87, p. 85-94.
Scaillet,B., Holtz,F. And Pichavant.M., 1997, Rheological properties of granitic magmas in their crystallization range, in: Bouchez et al(eds), Granite: from segregation of melt to emplacement fabrics, Kluwer Academic Publishers, p. 11-30.
Schmitt, A. K. , Emmermann, R. , Trumbull, R. B. , Buhn, B. and Henjes-Kunst, F. , 2000, Petrogenesis and Ar~(40)/Ar~(39) geochronology of the Brandberg Complex, Namibia: evidence for a major mantal contribution in metaluminous and peralkaline grnites, J. Petrol. , vol.41, p. 1207-1239.
Sederholm, J. J., 1967, Selected works, granites and migmatites, Oliver & Boyd. Simmons, E. C. and Hedge, C. E., 1978, Minor-element and Sr-isotope geochemistry of Tertiary stocks, Colorado mineral belt, Contrib. Mineral. Petrol., 67, p. 379-396.
Soderlund, U., 1996, Conventional U-Pb dating versus single-grain Pb evaporation dating of complex zircons from a pegmatite in the high-grade gneisses of southwestern Sweden, Lithos, vol. 38,p93-105.
Spear, F. S., 1989, Petrological determination of metamorphic pressure-temperature -time paths , in:Spear, F. S. and Peacock, S. M., (eds),Metamorphic pressure- temperature-time paths, Am. Geophys. Union Short Cours in Geology,7,p.1-55. Spear, F. S. and Florence, F. P., 1992, Thermobarometry in granulites:pitfalls and new approaches, Precambrian Res., 55, p. 209-241.
Spear, F. S. , and Parrish, R. R. , 1996, Petrology and cooling rates of the Valhalla Complex, British Columbia, Canada, J. Petrol. , vol. 37, p. 733-765. Streckeisen, A. L., 1976, To each plutonic rock its proper name, Earth Sci. Rev. ,12, p. 1-33.
Tarney, S. R., Ewart,A. and Drury, S. A., 1979, geochemistry of Archean trondhjemitic and tonalitic gneisses from Scotland and East Greenland, in: Barker, F. (ed), Trondhjemites, dacites and related rocks. Elsevier, Amsterdam,p.275-300.
Taylor, S. R. and McLennen, S. M., 1985, The continental crust:its composition and evolution, Blackwell,Oxford.
Taylor, S. R. 和 McLennan, S. M., 1996, 大陆地壳的演化, 科学, .1996(5): 38-43.
Tepley, F. J. III, Davidson, J. P. and Clynne.M. A. , 1999, Magamatic interactions recorded in plagioclase phenocrysts of Chaos Crags, Lassen Volcanic Center, California, J. Petrol. , vol.40, p. 787-806.
Tepley, F. J. III, Davidson, J. P. , Tilling, R.I. and Arth, J. G. , 2000, Magma mixing, recharge and eruption histories recorded in plagioclase phenocrysts from El Chichon volcano, Mexico, J. Petrol. , vol.41, p.1397-1411.
Thompson, A. B. and England, P. C., 1984, Pressure-temperature-time paths of regional metamorphism II. Their inference and interpretation using mineral assemblages in metamorphic rocks, J. Petrol., vol. 25, p. 929-955.
Thompson, A. B.,1996, Fertility of crustal rocks during anatexis, Transactions of the Royal Society of Edinburgh: Earth Sciences, 87, p. 1-10.
Touret, J. And Olsen, S. N., 1985, Fluid inclusion in migmatites, in: Ashworth et al(eds), Migmatites, Blackie, New York, p. 36-85.
Tuttle, 0. F. and Bowen, N. L., 1958, Origin of granite in the light of experimental studies, Geol. Soc.Am. Memoir. No. 74.
Vielzeuf,D., Clemens, J. D., Pin, C. and Moinet, E. 1990, granites, granulites, and crustal differentiation, in: Vielzeuf.D. and Vidal,Ph. (eds), Granulites and crustal evolution, Kluwer Academic Publishers, Dordrecht, p. 59-85.
Vielzeuf,D. and Montel, T. M., 1994, Partial melting of metagreywackes, Part I. Fluid-absent experiments and phase relationships, Contrib. Mineral. Petrol., vol. 117, p. 375-393.
Walker, J. D. , Martin, M. W. , Bowring, S. A. , Searle, M. P. , Waters, D. J. and Hodges, K. V. , 1999, Metamorphism, melting, and extension: age constrains from the High Himalayan Slab of southeast Zanskar and northwest Lahaul, J. Geol. vol. 107, p. 473-495.
Winkler, H. G. F.,1979, Petrogenesis of metamorphic rocks(5ed), Springer Verlag, 348p
Wolf, M.B. and Wyllie, P. J., 1994, Dehydration-melting of amphibolite at 10 Kbar: the effects of temprature and time, Contrib. Mineral. Petrol, vol. 115, p. 369-383.
Wyllie, P. J., 1983, Experimental studies on biotite-and muscovite-granites and some crustal magmatic sources, in: Atherton et al(eds), Migmatites, melting and metamorphism, Shiva Publishing Limited, p. 12-26.
Wyllie, P. J., 1983, Experimental and thermal constrains on the deep-seated parentage of some granitoid magmas in subduction zones, in: Atherton et al(eds), Migmatites, melting and metamorphism, Shiva Publishing Limited, p. 37-54.
Yardley, B.W.D.,1994, The solution chemistry of metamorphic fluids,地学前缘(中国地质大学，北京)1994 (1-2): 27-39.
Zhao, G. C., Wilde, S. A., Cawood, P.A. and Lu, L.Z.,2000, Petrology and P-T path of the Fuping mafic granulites: implications for tectonic evolution of the central zone of the North China craton, J. metamorphic Geol.,18, p. 375-391.
程裕淇，1987，关于混合岩和混合岩化作用的一些问题—对半个世纪以来某些基本问题的回顾，中国地质科学院院报，第16号，5-19。
程裕淇、高吉凤、万渝生，1996，河北平山晚太古代阜平群一些主要变质岩类深熔特征的初步研究，献给第三十届 国际地质大会地质科学论文集，中国经济出版社。
程裕淇、高吉凤、万渝生、马瑞，1998，河北平山阜平群两种岩石类型的初步熔融实验极其启示，中国地质，1998(3)：18-22。
程裕淇、高吉凤、万渝生，1999，论中国河北平山西北部新太古代阜平群一些变质岩类的深熔作用，前寒武纪地质学和变质岩石学(钱祥麟、游振东主编)，第30届国际地质大会论文集(17)：126-136。
程裕淇、万渝生、高吉凤，2000a，河北平山小觉地区阜平群变质作用和深熔作用同位素年代研究的初步报道，地质学报，2000(2)：30-37。
程裕淇、刘敦一、I．S．Williams、简平、庄育勋、高天山，2000b，大别山碧溪岭深色榴辉岩和片麻状花岗质岩石SHRIMP分析—晋宁期高压-超高压变质作用的同位素年代学依据，地质学报，2000(3)：193-205。
程裕淇、高吉凤、万渝生、马瑞，2000c，河北平山小觉地区新太古代阜平岩群中变质岩所显示深熔改造的一些岩相学特征，中国地质，2000(12)：14-16。
董申保，1999，五十年来中国花岗岩研究的回顾与展望，中国地质科学五十年(王鸿祯主编)，中国地质大学出版社，123-130页。
洪大卫，1994，花岗岩研究的最新进展及发展趋势，地学前缘，1(1-2)：79-86页。
高吉凤，1997，河北平山晚太古代阜平群中主要变质岩类及其深熔产物的稀土地球化学初步研究，岩石学报，1997(3)，418-426页。
关鸿、孙敏、徐平，1998，阜平杂岩中几种不同类型片麻岩的锆石激光探针等离子体质谱年代学研究，岩石学报，1998(11)：460-470。
李江海、钱祥麟，1994，恒山早前寒武纪地壳演化，山西科学技术出版社，116页。
李武显、董传石、周新民，1999，平潭和漳州深成杂岩中斜长石捕虏晶与岩浆混合作用，岩石学报，15(2)：286-290。
刘敦一、R．W．佩吉、W．康普斯顿、伍家善，1984，太行山-五台山区前寒武纪变质岩系同位素地质年代学研究，中国地质科学院院报，8：57-82页。
刘树文、梁海华、赵国春、华永刚、简安华，2000，太行山早前寒武纪杂岩的同位素年代学和地质事件，中国科学(D辑)，2000(1)：18-24。
刘树文，1996，阜平地区麻粒岩的P-T路径研究，高校地质学报，1996(2卷)：75-83。
刘福来、沈其韩、耿元生、徐学纯、马瑞，1997，麻粒岩相条件下熔融反应与矿物相转变机制的实验研究，地质学报，1997(3)：254-265。
马杏垣、游振东、谭应佳、蔡学林，1963，中国东部前寒武纪大地构造发展的样式，地质学报，1963(1)：27-52。
南京大学地质学系，1981，华南不同时代花岗岩类及其与成矿关系，1981，科学出版社，395页。
牛树银、陈路、许传诗等，1994，太行山区地壳演化及成矿规律，地震出版社，页。
钱祥麟、崔文元、王时麒，1985，内蒙、冀东太古界麻粒岩相岩带的演化，地质研究论文集，北京大学出版社，20-29页。
山西地层表编写组，1979，华北地区区域地层表，山西分册(一)，地质出版社，195-202页。
沈其韩、徐惠芬、张宗清、高吉凤、伍家善、吉成林，1992，中国早前寒武纪麻粒岩，地质出版社，237页。
沈其韩，1998，华北地台早前寒武纪条带状铁英岩地质特征和形成的地质背景，华北地台早前寒武纪地质研究论文集(程裕淇主编)，1-30。
孙敏、关鸿，阜平杂岩年龄及其地质意义：兼论前寒武高级变质地体的定年问题，岩石学报，2001，17(1)：145-156。
谭应佳、王方正、赵温霞，1993，太行山阜平隆起南部早前寒武纪地质-兼论太古宙地质若干问题及研究方法，中国地质大学出版社，161页。
万渝生，1987，雌山混合花岗岩及有关岩石的副矿物组合锆石特征及其地质意义，地质论评，1987(5)：229-236。
王江海、扬问华、吴金平，1994，鄂东北大别杂岩中混合岩形成的动力学机制，地质学报，1994(4)：308-323。
王凯怡、李继亮、刘如琦，1991，阜平片麻岩之成因，地质科学，1991(7)：254-266。
王凯怡、郝杰、周少平、Wilde，S．，Cawood，P．A．，单颗粒锆石离子探针质谱定年结果对五台造山事件的制约，科学通报，1997(12)：1295-1297。
王涛，2000，花岗岩混合成因研究及大陆动力学意义，岩石学报，2000，16(2)：161-168。
王联魁、朱为方、张绍力，1982，华南花岗岩两个成岩成矿系列的演化，地球化学，1982(4)，329-339页。
王德滋、周金城，1999；我国花岗岩研究的回顾与展望，岩石学报，15(2)：161-169页。
吴昌华、李惠民、钟长汀、左义成，2000，阜平片麻岩和湾子片麻岩的单颗粒锆石U-Pb年龄——阜平杂岩并非一统太古宙基地的年代学证据，前寒武纪研究进展，2000(3)：129-139。
吴澄宇、万渝生，1997，稀土元素地球化学与花岗质岩石的成因—应用与问题，岩石圈研究的现代方法(张炳熹等主编)，201-214页。
伍家善、耿元生、徐惠芬、金龙国、贺绍英、孙世伟，1989，阜平群变质地质，中国地质科学院地质研究所所刊，19，219页。
伍家善、耿元生、沈其韩、刘敦一、厉子龙、赵敦敏，1991，华北陆台早前寒武纪重大地质事件，地质出版社，115页。
伍家善、耿元生、沈其韩、万渝生、刘敦一、宋彪，1998，中朝古大陆太古宙地质特征及构造演化，地质出版社，212页。
徐夕生、周新民、O’Rreilly，S．Y．，唐红峰，1999，中国东南部下地壳物质与花岗岩成因探索，岩石学报，15(2)：217-223页。
徐克勤、胡受奚、孙明志、张景荣、叶俊，1983，论花岗岩的成因系列—以华南中生代花岗岩为例，地质学报，1983(2)：107-118页。
徐克勤、孙鼐、王德滋、胡受奚、刘英俊、季受元、1984，华南花岗岩成因与成矿，花岗岩地质和成矿关系(徐克勤、涂光炽主编)，江苏科学技术出版社，1-20页。
徐朝雷、徐有华、张平，1985，太行山区龙华河群的建立与否定，地球科学，1985(4)：151-158。
杨杰，1936，山西省五台山地质略述，中国地质学会会志，2，261页。
张春华等，1990，河北早前寒武纪变质作用，地质出版社。
张寿广、金龙国、肖庆辉，阜平太古宙穹状复合褶皱群的构造样式及变形史，中国 区域地质，1983(6)：97-110。
张西平，1999，深熔作用及有关问题，地球学报，1999，增刊，38-47。
张宗清、伍家善、叶笑江，1991，阜平群下部太古代变质岩石的REE、Rb-Sr和Sm-Nd年龄及其意义。地球化学，1991(2)：118-126。
郑海飞、谢鸿森、徐有生、宋茂双、张月明、王明再、徐惠刚，1995，高温高压下含水矿物对岩石熔点影响的实验研究，地质学报，1995(4)：326-335。
中国地质图(1：5000000)编辑委员会，1990，中国地质图(1：5000000)，地质出版社。
中国科学院贵阳地球化学研究所，1979，华南花岗岩类的地球化学，科学出版社，421页。
周新民、姚玉鹏、徐夕生，1992，浙东大巨山花岗岩中淬冷包体及其成因机制，岩石学报，8(3)：234-242页。
周珣若，1994；1994，花岗岩混合作用，地学前缘，1(1-2)：87-97页。
哈克，A．，1981，变质作用：岩石转变的研究(中译本)，地质出版社，373页。
J．迪迪埃，1981，花岗岩极其包体：包体与花岗岩成因的关系，中译本，姜胜章译，地质出版社，274页。
V．马莫，花岗岩岩石学与花岗岩问题，中译本，袁廷佐，吴荣庆译，地质出版社，255页。
Arth, J. G. and Hanson, G. N., 1972, Quartz diorites derivd by partial melting of eclogite or amphibolite at mantle depths, Contrib. Mineral. Petrol.,37, p. 161-174.
Arth, J. G. and Hanson, G. N.,1975, Geochemistry and origin of the early Precambrian crust of northeastern Minneresota, Geochim. Cosmochim. Acta, 39, p. 325-362.
Ashworth, J.R.,1985, Introduction, in: Ashworth et al(eds),Migmatites, Blackie, New York, p. 1-35.
Barbey, P., Brouand, M., Le Fort, P. AndPecher, A.,1996, Granite-migmatite genetic link: the example of the Manaslu granite and Tibeten Slab migmatites in central Nepal, Lithos, vol. 38, p. 63-79.
Barboza S.A. and Bergantz, G.W., 1996, Dynamic model of dehydration melting motivated by a natural analogue:applications to the Ivrea-Verbano zone, northern Italy, Transactions of the Royal Society of Edinburgh, 87, p23-31.
Barboza,S.A. and Bergantz,G.W.,2OOO,Metamorphism and anatexis in the mafic complex contact aureole, Ivrea Zone, northern Italy, J. Petrol., vol. 41, p. 1307-1327.
Barker F., 1979, Trondhjemite:Definition, environment and hypotheses of origin, in: Barker F. (ed), Trondhjemites, dacites and related rocks. Elsevier, Amsterdam, p.1-12.
Barker, F. and Millard, H.T.,Jr.,1979, Geochemistry of the type trondhjemite and three associated rocks, Norway, in:Barker F. (ed), Trondhjemites, dacites and related rocks. Elsevier, Amsterdam, p. 517-529.
Bergantz, G. W. and Dawes, R. 1994, Aspects of magma generation and ascent in continental lithosphere, in: Ryan, M. P. (ed.), Magmatic systems, San Diego, CA: Academic Press, p291-317.
Brown, M.,1993, P-T-t evolution of orogenic belts and the causes of regional metamorphiism, J. geol. Soc., London, vol. 150, p. 227-241.
Brown, M.,1994, The generation, segregation, ascent and emplacement of granite magma: the migmatite-to-crustal ly-derived granite connection in thickened orogens, Earth Sci. Rev.,vol,36,p. 83-130.
Brown, M. and Dallmeyer, R. D., 1996, Rapid variscan exhumation and the role of magma in core complex formation:southern Brittany metamorphic belt, France, J. Metamorphic Geol., vol. 14, p.361-379.
Brown, M. and Rushmer, T., 1997, The role of deformation in the movement of granitic melt: views from the laboratort and the field, in: Holness(ed), Deformation-enhanced fluid transport in the Earth's and mantal, Chapman & Hall, London, p. 111-144.
Campbell, I. H. and Turner, J. S. , 1987, A laboratory investigation of assimilation at the top of a basltic magma chamber, J. Geol. , 95, pl55—172.
Carmichael, D. M., 1987, Induced stress and secondary mass trasfer: thermodynamic basis for the tendency toward constant-volume constraint in diffusion metasomatism, in:Helgeson(ed),Chemical transport in metasomatic processes, D. Reidel Publishing Company, p. 239-264.
Carswell, D. A. and O'Brien, P. J., 1993, Thermobarometetry and geotectonic significance of high-p granulite examples from the Moldanubian zone of the Bohemian massif in lower Austria, J. Petrol., 34, p. 427-459.
Castro, A., 1991, H-type (Hybrid) granitoids: a proposed revision of the granite type classification and nomenclature, Earth Sci. Rev. , vol, 31, p. 237-253.
Cheng, Y. Q., Gao,J. F. and Wan, Y. S., 1997, Notes on the anatexis of some metamorphic rock types of Late Archaean Fuping Group of Northwestern Pingshan, Hebei Province, China, in:X. L., Qian et al (eds),Proc.30~(th) Int'l. Geol. Congr., vol. 17, part II, p. 173-185.
Chappell, B. W. , 1996 , Magma mixing and the production of compositional variationwithin granite suites:evidence from the granites of southeastern Australia, J. Petrol, vol. 37, P. 449-470
Chappell, B. W. , White, A. J. R. and Wyborn, D., 1987, The importance of residual source material(restite) in granite petrogenesis., J. Petrol, vol. 28, p. 1111-1138.
Chappell, B. W. and White, A. J. R., 1992,I- and S-type granites in the Lachlan Fold Belt, Trans. Roy. Soc. Edinburgh: Earth Sci., 83,p.1-26.
Clarke, D. B., 1996, Two centuries after Hutton's 'Theory of the Earth': the status of granite science, Trans. Roy. Soc. Edinburgh: Earth Sci., 87, p. 353-359.
Clemens J. D., 1990, The granulite-granie connexion, in: Vielzeuf, D. and Vidal.Ph. (eds), Granulites and crustal evolution, Kluwer Academic Publishers, Dordrecht, p. 25-36.
Clements, J. D., Petford, N. and Mawer, C. K., 1997, Ascent mechanisms of granitic magmas: causes and consequenses, in: Holness(ed), Deformation-enhanced fluid transport in the Earth's and mantal, Chapman & Hall, London, p. 145-192.
Collins, W. J. , 1996, Lachlan Fold Belt granitoids: products of three-component mixing, Trans. Royal. Soc. Edinburgh: Earth Sci. 87, p. 171-181.
Compton, P., 1978, Rare earth evidence for the origin of the N k gneisses Buksef jorden region, southern West Greenland, Contrib. Minerl. Petrol., 66, p. 283-293.
Condie, K. C. and Harrison, N. M., 1976, Geochemistry of the Archean Bulawayan
Group, Midlands greenstone belt, Rhodesia, Precambrian Res., 3, p. 253-271.
Condie, K. C., 1982, Plate tectonics & crustal evolution(2ed), Pergramon Press, 310p.
Cullers, R. L. and Graf, J. L., 1984, Rare earth element in igneous rocks of the continental crust: intermediate and silicic rocks-ore petrogenesis, in; Henderson,P. (ed),Rare earth element geochemistry, Elsevier, Amsterdam, p. 275-316.
Davidson, J. P. , Tepley, F. J.III and Knesel, K. M. , 1998, Isotopic fingerprinting may provide insights into evolution of magmatic systems, EOS Transactions, Am. Geophy. Union 79, 185, 189, 193.
Drury, S. A., 1978, REE distributions in a high-grade Archean gneiss complex in Scotland: implications for the ancient sialic crust. Precambrian Res., 7, p. 237-257.
Drummond, M. S., Defant,M. J. and Kepezhinskas, P. K., 1996, Petrogenesis of slab-derived trondhjemite-tonalite-dacite/adakite magmas, Trans. Roy. Soc.Edinburgh: Earth Sci., 87, p. 205-215.
Ellis, D. J. , 1987, Origin and evolution of granulites in normal and thickened crust, Geol., 15, pl67-170.
England, P. C. and Thompson, A. B., 1984, Pressure-temperature-time paths of regional metamorphism I . Heat transfer during the evolution of regions of thickened continental crust, J. Petrol., 25, p. 894-928.
Fitzsimons, I. C. W., 1996, Metapelitic migmatites from Brattstrand Bluffs,East Antarctica-Metamorphism,melting and Exhumation of the mid crust, J. Petrol., vol. 37, p. 395-414.
Fountain D. M., Salisbury M. H., 1981, Exposed cross-sections through the continental crust:implications for crustal structure, petrology and evolution. Earth Planet. Sci. Lett. 56, 263-277.
Frey, F. A., Chappell, B. W. and Roy, S. D., 1978, Fractionation of Rare-earth elements in the Tuolumne Intrusive Series, Sierra Nevada batholith, California, Geology, 6, p. 239-242.
Giorgetti.G., Frezzotti,M. -L. E., Palmeri, R. And Burke, E. A. J., 1996, Role of fluids in migmatites:C02-H20 fluid inclusion in leucosomes from the Deep Freeze Range migmatites(Terra Nova Bay, Antarctica), J.metamorphic Geol., 1996,14, p. 303-317.
Glickson, A. Y., 1976, Trace element geochemistry and origin of early Precambrian acid igneous series, Barberton Mountain Land, Transvaal, Geochim. Cosmochim. Acta,40, p. 1261-1280.
Graessner, T. And Schenk, V., 2001, An exposed Hercynian deep crustal section in the Sila Massif of northern Calabria: mineral chemistry, petrology and a P-T path of granulite-facies metapelitic migmatites and metabasites, J. Petrol, vol. 42, p. 931-961.
Graham, C. M., Skelton, A. D. L., Bickle, M. And Cole,C.,1997, Lithological, structural and deformation controls on fluid flow during regional metamorphism, in: Holness(ed), Deformation-enhanced fluid transport in the Earth's and mantal, Chapman & Hall, London, p.196-226.
Greenwood, H. J., 1987, Fluid exchange between reaction bodies of rock, in:Helgeson(ed), Chemical transport in metasomatic processes, D. Reidel Publishing Company, p. 153-168.
Hanson, G. N. and Goldich, S. S., 1972, Early Precambrian rocks in the Saganaga Lake-Northern Light Lake Area, Minnesoda-Ontario, II. Petrogenesis. Geol. Soc. Am., Mem., 135, p. 179-192.
Hawkesworth, C. J. and van Calsteren , P. W. C., 1984, Radiogenic isotopes-some geological applications, in Henderson,P. (ed), Rare earth element geochemistry, Elsevier, Amsterdam, p. 375-422.
Holland, T. J. B. and Blundy, J. D., 1994, Non-ideal interactions in calci amphiboles and their bearing on amphibole plagioclase thermometry. Contrib. Mineral. Petrol., 116, p. 433-447.
Hutton, 1997, Theory of the Earth with proofs and illustrations, volIII, London. Johannes, W., 1985, The significance of experimental studies for the formation of migmatites, in: Ashworth et al(eds), Migmatites, Blackie, New York, p. 36-85. Johannes, W. and Holtz, F., 1996, Petrogenesis and experimental petrology of granitic rocks, Springer,335p.
John, B. E. and Stunitz, H., 1997, Magmatic fracturing and small-scale melt segregation during pluton emplacement: evidence from the Adamello massif (Italy), in: Holness(ed), Deformation-enhanced fluid transport in the Earth's and mantal, Chapman & Hall, London, p. 55-74.
Knesel, K. M. and Davidson, J. P., 1996, Isotopic disequilibrium during melting of granite and implications for crustal contamination of magmas, Geology, v. 24, no. 3, p.243-246.
Knesel, K. M. , Davidson, J. P. and Duffield, W. A. , 1999, Open-system evolution of silicic magma by assimilation followed by recgarge: evidence from Sr isotopes in sanidine phenocrysts, Taylor Creek Rhyolite, NM. J. Petrol. , vol. 40, p. 773-786.
Kohn, M. J. and Spear, F. S., 1990, Two new geobarometers for garnet amphibolites, with applications to southeastern Vermont. Amer. Mineralogist, 75,p. 89-96.
Lambert, R. St. J. and Holland, J. G., 1976, Am tsoq gneiss geochemistry preliminary observations, in:Windley, B. F. (ed), The early history of the Earth, Wiley, New York, N. Y., p. 191-201.
Leak, B. E., 1990, Granite magmas, their sources, initiation and consequences of emplacement, J. Geol. Soc. Lond., 147, p. 579-589.
London, D., Morgan VI G. B., Babb, H. A. and Loomis, J. L., 1993, Behavior and effects of phosphorus in the system Na20-K20-A1203"Si02-P205-H20 at 200 Mpa(H20), Contrib. Mineral. Petrol., 113, p.450-465.
Maniar, P. D. and Piccoli, P. M.,, 1989, tectonic discrimination of granitoids, Geol. Soc. Am. Bull.,101, p. 635-643.
Martin, H., 1994, Archaean grey gneisses and continental crust origin, in: Condie(ed), Archaean crustal evolution, Elsevier, Amsterdam., p.205-259.
Masuda, A., Nakamura, N. and Tanaka, T., 1973, Fine structures of mutually normalised Rare-earth patterns of chondrites, Geochim. Cosmochim. Acta, 37,p. 239-248.
Mehnert,K. R., 1968, Migmatites, Elsevier Amsterdam, 393p.
Mogk,D. W., 1992, Ductile shearing and migmatization at mid-crustal level in an Archaean high-grade gneiss belt, northern Gallatin Range, Montana, USA., J. Metamorphic Geol., vol. 10, p. 427-438.
Montel, J. M., 1993, A model for monazite/melt equilibrium and application to the generation of granitic magmas, Chem. Geol., vol. 110, p. 127-146.
Nabelek, P. I.,1997, Quartz-sillimanite leucosomes in high-grade schists, Black Hills, South Dakota: A perspective on the mobility of Al in high-grade metamorphic rocks, Geol., vol. 25, p. 995-998
Nedelec, A., Minyem,D. and Barbey, P.,1993, High-P-high-T anatexis of Archaean tonalitic grey gneisses: the Eseka migmatites, Cameroon, Precamb. Res., vol. 62, p. 191-205.
Nekvasil,H. And Carroll, W., 1996, Experimental constraints on the compositional evolution of crustal magmas, Transactions of the Royal Society of Edinburgh: Earth Sciences,87,p. 139-146.
Neogi, S., Dasgupta, S. and Fukuoka, M., 1998, High P-T polymetamorphism, Dehydration melting, and generation of migmatites and granites in the Higher Himalayan Complex, Sikkim, India, J. Petrol., vol. 39, p61-99.
Norlan, E. U., Schert.H. -P. and Schreyer. W., 2000, Garnet-omphacite-phengite thermobarometry of eclogites from the coesite-bearing unit of the southern Dora-Maira Massif, Western Alps, Lithos, 52, p. 197-214.
Norton, D. L., 1987, Advective metasomatism, in:Helgeson(ed), Chemical transport in metasomatic processes, D. Reidel Publishing Company, p. 123-132.
Oconnor, J. T., 1965, A classification for quartz-rich igneous rock based on feldspar ratios, U.S. Geol. Surv. Prof. Paper 525B, B79-B84.
Ohr,M., Halliday, A. N. and Peacor, D. R., 1994, Mobility and fractionation of rare earth elements in argillaceous sediments: implications for dating diagenesis and low-grade metamorphism, Geoch. Et Cosmo ecta, vol. 58,p. 289-312.
Olsen, S. N., 1985, Mass balance in migmatites, in: Ashworth et al(eds), Migmatites, Blackie, New York, p. 145-179.
0'Nions, R. K. and Pankhursf, R. J., 1974, Rare-earth element distribution in Archean gneisses and anothosites, Godthab area, West Greenland, Earth Planet. Sci. Lett., 22, p. 328-338.
0'Nions, R. K. and Pankhursf, R. J., 1978, Early Archean rocks and geochemicalevolution of the earth's crust, Earth Planet. Sci. Lett., 38, p. 211-236.
Otamendi, J.E. and Patino Douce, A. E. , 2001, Partial melting of aluminous metagreywackes in the norther Sierra de Comechingones, Central Argentina, J. Petrol.,vol. 42,p1751-1772.
Patino Douce, A. E. and McCarthy, T. C., 1998, Melting of crustal rocks during continental collision and subduction, in:Hacker, B. R. and Liu, J. G. (ed), When continents collide: Geodynamics and geochemistry of ultrahigh-pressure rocks, Kluwer Academic Publishers, p. 27-55.
Pearce, J. A., 1983,Role of the sub-continental lithosphere in magma genesis at active continental margins, in: Hawkesworth C. J. and Norry M. J. (eds), Continental basalts and mantle xenoliths, Shiva, Nantwich, p. 230-249.
Petford, N., Clements, J.D. and Vigneresse,J. L.,1997, Application of information theory to the formation of granitic rocks, in: Bouchez et al(eds), Granite: from segregation of melt to emplacement fabrics, Kluwer Academic Publishers, p. 3-10.
Pichavant,M., Hammonda, T. And Scaillet, B., 1996, Control of redox state and Sr isotopic composition of granitic magmas: a critical evaluation of the role of souce rocks, Transactions of the Royal Society of Edinburgh: Earth Sciences, 87, p. 321-329.
Pitcher, W. S., 1997, The nature and origin of granite(2ed), Chapman & Hall,p387. Pupin, J. P.,1980,Zircon and granite petrology, Contrib. Mineral. Petrol.,73,p.207- 220.
Putnis, A. And McConnell, J. D. C.,1980, Principles of mineral behaviour, Blackwell Scientific Publications, 257p.
Rice, T. M. and Ferry, T. M., 1982, Buffering, infiltration, and the control of intensive variables during metamorphism, in: Ferry(ed), Charaterization of metamorphism through mineral equilibria, Mineralogical Soc. Am, p.263-326.
Rapp,R. P., Watson, E. B. and Miller,C. F., 1991, Partial melting of amphibolite/eclogite and the origin of Archaean trondhjemites and tonalites, Prec. Res., vol. 51, p. 1-25.
Read, H. H., 1957, The granite controversy, Thomas Murby & Co. Rollinson, H. R.,1993, Using geochemical data:evaluation, presentation, interpretation, Longman Scien. & Tech., p343.
Rushmer, T., 1996, Melt segregation in the lower crust: how have experiments help us?, Transactions of the Royal Society of Edinburgh: Earth Sciences, 87, p. 73-83.
Sawyer, E. W., 1991, Disequilibrium melting and the rate of melt-residium separation during migmatization of mafic rocks from the Grenvilli Front, Quebec, J. Petrol, vol. 32, p. 701-738.
Sawyer, E. W., 1996, Melt segregation and magma flow in migmatites: implications for the generation of granite magmas, Transactions of the Royal Society of Edinburgh: Earth Sciences, 87, p. 85-94.
Scaillet,B., Holtz,F. And Pichavant.M., 1997, Rheological properties of granitic magmas in their crystallization range, in: Bouchez et al(eds), Granite: from segregation of melt to emplacement fabrics, Kluwer Academic Publishers, p. 11-30.
Schmitt, A. K. , Emmermann, R. , Trumbull, R. B. , Buhn, B. and Henjes-Kunst, F. , 2000, Petrogenesis and Ar~(40)/Ar~(39) geochronology of the Brandberg Complex, Namibia: evidence for a major mantal contribution in metaluminous and peralkaline grnites, J. Petrol. , vol.41, p. 1207-1239.
Sederholm, J. J., 1967, Selected works, granites and migmatites, Oliver & Boyd. Simmons, E. C. and Hedge, C. E., 1978, Minor-element and Sr-isotope geochemistry of Tertiary stocks, Colorado mineral belt, Contrib. Mineral. Petrol., 67, p. 379-396.
Soderlund, U., 1996, Conventional U-Pb dating versus single-grain Pb evaporation dating of complex zircons from a pegmatite in the high-grade gneisses of southwestern Sweden, Lithos, vol. 38,p93-105.
Spear, F. S., 1989, Petrological determination of metamorphic pressure-temperature -time paths , in:Spear, F. S. and Peacock, S. M., (eds),Metamorphic pressure- temperature-time paths, Am. Geophys. Union Short Cours in Geology,7,p.1-55. Spear, F. S. and Florence, F. P., 1992, Thermobarometry in granulites:pitfalls and new approaches, Precambrian Res., 55, p. 209-241.
Spear, F. S. , and Parrish, R. R. , 1996, Petrology and cooling rates of the Valhalla Complex, British Columbia, Canada, J. Petrol. , vol. 37, p. 733-765. Streckeisen, A. L., 1976, To each plutonic rock its proper name, Earth Sci. Rev. ,12, p. 1-33.
Tarney, S. R., Ewart,A. and Drury, S. A., 1979, geochemistry of Archean trondhjemitic and tonalitic gneisses from Scotland and East Greenland, in: Barker, F. (ed), Trondhjemites, dacites and related rocks. Elsevier, Amsterdam,p.275-300.
Taylor, S. R. and McLennen, S. M., 1985, The continental crust:its composition and evolution, Blackwell,Oxford.
Taylor, S. R. 和 McLennan, S. M., 1996, 大陆地壳的演化, 科学, .1996(5): 38-43.
Tepley, F. J. III, Davidson, J. P. and Clynne.M. A. , 1999, Magamatic interactions recorded in plagioclase phenocrysts of Chaos Crags, Lassen Volcanic Center, California, J. Petrol. , vol.40, p. 787-806.
Tepley, F. J. III, Davidson, J. P. , Tilling, R.I. and Arth, J. G. , 2000, Magma mixing, recharge and eruption histories recorded in plagioclase phenocrysts from El Chichon volcano, Mexico, J. Petrol. , vol.41, p.1397-1411.
Thompson, A. B. and England, P. C., 1984, Pressure-temperature-time paths of regional metamorphism II. Their inference and interpretation using mineral assemblages in metamorphic rocks, J. Petrol., vol. 25, p. 929-955.
Thompson, A. B.,1996, Fertility of crustal rocks during anatexis, Transactions of the Royal Society of Edinburgh: Earth Sciences, 87, p. 1-10.
Touret, J. And Olsen, S. N., 1985, Fluid inclusion in migmatites, in: Ashworth et al(eds), Migmatites, Blackie, New York, p. 36-85.
Tuttle, 0. F. and Bowen, N. L., 1958, Origin of granite in the light of experimental studies, Geol. Soc.Am. Memoir. No. 74.
Vielzeuf,D., Clemens, J. D., Pin, C. and Moinet, E. 1990, granites, granulites, and crustal differentiation, in: Vielzeuf.D. and Vidal,Ph. (eds), Granulites and crustal evolution, Kluwer Academic Publishers, Dordrecht, p. 59-85.
Vielzeuf,D. and Montel, T. M., 1994, Partial melting of metagreywackes, Part I. Fluid-absent experiments and phase relationships, Contrib. Mineral. Petrol., vol. 117, p. 375-393.
Walker, J. D. , Martin, M. W. , Bowring, S. A. , Searle, M. P. , Waters, D. J. and Hodges, K. V. , 1999, Metamorphism, melting, and extension: age constrains from the High Himalayan Slab of southeast Zanskar and northwest Lahaul, J. Geol. vol. 107, p. 473-495.
Winkler, H. G. F.,1979, Petrogenesis of metamorphic rocks(5ed), Springer Verlag, 348p
Wolf, M.B. and Wyllie, P. J., 1994, Dehydration-melting of amphibolite at 10 Kbar: the effects of temprature and time, Contrib. Mineral. Petrol, vol. 115, p. 369-383.
Wyllie, P. J., 1983, Experimental studies on biotite-and muscovite-granites and some crustal magmatic sources, in: Atherton et al(eds), Migmatites, melting and metamorphism, Shiva Publishing Limited, p. 12-26.
Wyllie, P. J., 1983, Experimental and thermal constrains on the deep-seated parentage of some granitoid magmas in subduction zones, in: Atherton et al(eds), Migmatites, melting and metamorphism, Shiva Publishing Limited, p. 37-54.
Yardley, B.W.D.,1994, The solution chemistry of metamorphic fluids,地学前缘(中国地质大学，北京)1994 (1-2): 27-39.
Zhao, G. C., Wilde, S. A., Cawood, P.A. and Lu, L.Z.,2000, Petrology and P-T path of the Fuping mafic granulites: implications for tectonic evolution of the central zone of the North China craton, J. metamorphic Geol.,18, p. 375-391.
© 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 |