期刊网首页  /  联系我们  /  English
高级检索
{{news.title}}

中国东部富钾埃达克岩成因的实验约束

downloadPDF
文章导航 > 岩石学报 > 2002 > 18(3): 293-302

上一篇

下一篇

RobertP.PAPP 肖龙 等. 中国东部富钾埃达克岩成因的实验约束[J]. 岩石学报, 2002, 18(3): 293-302.
引用本文: RobertP.PAPP 肖龙 等. 中国东部富钾埃达克岩成因的实验约束[J]. 岩石学报, 2002, 18(3): 293-302.
shu
Rapp R P,Xiao L and Shimizu N. 2002. 1. Department of Geosciences and Mineral Physics Institute,State University of New York,Stony Brook,New York 11794 2100,USA2. Guangzhou Institute of Geochemistry,Chinese Academy of Sciences,Wushan,Guangzhou 510640,China3. Woods Hole Oceanographic Institution,Woods,Hole,Massachusetts 02543,USA. Experimental constraints on the origin of potassium-rich adakites in eastern China.[J]. Acta Petrologica Sinica, 2002, 18(3): 293-302.
Citation: Rapp R P,Xiao L and Shimizu N. 2002. 1. Department of Geosciences and Mineral Physics Institute,State University of New York,Stony Brook,New York 11794 2100,USA2. Guangzhou Institute of Geochemistry,Chinese Academy of Sciences,Wushan,Guangzhou 510640,China3. Woods Hole Oceanographic Institution,Woods,Hole,Massachusetts 02543,USA. Experimental constraints on the origin of potassium-rich adakites in eastern China.[J]. Acta Petrologica Sinica, 2002, 18(3): 293-302.
shu

中国东部富钾埃达克岩成因的实验约束

    • [1]DepartmentofGeosciencesandMineralPhysicsInstitute,StateUniversityofNewYork,StonyBrook,NewYork11794－2100,USA [2]中国科学院广州地球化学研究所，广州510640,StateUniversityofNewYork,StonyBrook,NewYork11794－2100,USA

  • 基金项目:

    the grant of the National Science F oundation of the United States:Petrogenesis of Archean Granitoidsand Implications for the Geochemical Evolution of Cratonic Lithosphere( EAR-0 0 0 3 63 8)

Experimental constraints on the origin of potassium-rich adakites in eastern China.

    摘要
  • Adakite在地球化学上具明显特征的火山岩和深成花岗岩类岩石，见于洋内岛孤环境和大陆孤，如安底斯孤。在洋内岛孤，由热的消减的大洋岩石圈熔融形成（叫做“板片熔融”），而在大陆孤，熔融曾发生在构造或岩浆加厚的下地壳底（叫做“下地壳熔融”）。在这两种产状环境中，adakite的鲜明地球化学特征被认为是起因子，一种不同程度含水的变质基性原岩在足够深度上的部分熔融，这里的足够深度是指可使石榴子石在残余结晶组合（即石榴角闪石和/或榴辉石的残余）中保持稳定的深度。“原始”或“母”adakite熔体一旦形成，便可能在其向上运移和侵位上地壳期间受到同化作用（或是地幔，或是大陆物质）和结晶分异作用的改造。中国东部晚中生代（早中白垩世，160-110Ma）的adakite,与见于同一地区和其它地方的钠质adakite相比，通常富含钾(K2O)和其它大离子亲石元素（如Ba,Th,U），有较低的Na2O/K2O比值（-1.0-1.1）,类似于玄武岩在石榴角闪岩-榴辉岩相含水熔融实验中所产生adakite熔体，要么是由洋壳板片熔融所形成，要么是由不同成分的玄武质下地壳原岩部分熔融所形成。尽管有些成分差异，它们的总体化学特征仍然可将中国东部的富钾花岗岩类岩石定均adakite。我们把这些富钾的adakite的独特化学行特征，归因于成分来源的特殊性，或adakite母岩浆遭受了同化混染和结晶分异(AFC)作用的改造。虽然中国东部与消减带环境明显不同这一点表明，那里的adakite可由板块底部侵位的（岩浆加厚的）镁铁质下地壳部分熔融所形成，但燕山运动期间中国东部存在“平坦”俯冲的地球动力学环境是可能被排除的。
    • HTML全文
  • 加载中
    • 参考文献(54)
  • [1]

    ［1］Atherton M P and Petford N. 1993. Generation of sodium-rich magmas from newly underplated basaltic crust. Nature, 362:144-146

    [2]

    ［2］Barnes C G, Barnes M A and Kistler R W. 1992. Petrology of the Caribou Mountainpluton, Klamath Mountains, California. Journal of Petrol., 33: 95-124

    [3]

    ［3］Barnes C G, Petersen S W, Kistler R W, Murray R and Kays M A. 1996. Source andtectonic implications of tonalite-trondhjemite magmatism in the Klamath Mountains.Contrib. Mineral. Petrol., 123: 40-60

    [4]

    ［4］Barth M G, Foley S F and Horn I. 2002. Partial melting in Archean subduction zones:constraints from experimentally determined trace element partition coefficients betweeneclogitic minerals and tonalitic melts under upper mantle conditions. Precambrian Res.,113: 323-340

    [5]

    ［5］Beate B, Monzier M, Spikings R, Cotton J, Silva J, Bourdon E and Eissen J-P. 2001. Mio-Pliocene adakite generation related to flat subduction in southern Ecuador: theQuimsacocha volcanic center. Earth Planet. Sci. Lett., 192: 561-570

    [6]

    ［6］Castillo P R, Janney P E and Solidum R U. 1999. Petrology and geochemistry ofCamiguin Island, southern Philippines: insights to the source of adakites and other lavasin a complex arc setting. Contrib. Mineral. Petrol., 134: 33-51

    [7]

    ［7］Defant M J and Drummond M S. 1990. derivation of some modern arc magmas by meltingof young subducted lithosphere. Nature, 347: 662-665

    [8]

    ［8］Gutscher M-A, Maury R, Eissen J-P and Bourdon E. 2000. Can slab melting be causedby flat subduction?. Geology, 28: 535-538

    [9]

    ［9］Gutscher M-A, Olivet J-L, Aswlanian D, Eissen J-P and Maury R. 1999. The "lostInca Plateau": cause of flat subduction beneath Peru? Earth Planet. Sci. Lett., 171:335-341

    [10]

    ［10］Johnston A D. 1986. Anhydrous P-T phase relations of near-primary high-aluminabasalt from the South Sandwich Islands: Implications for the origin of island arcs andtonalite-trondhjemite series rocks. Contrib. Mineral. Petrol., 92: 368-382

    [11]

    ［11］Kay R W. 1978. Aleutian magnesian andesites: melts from subducted Pacific oceancrust. Jour. Volcan. Geothermal Research, 4: 117-132

    [12]

    ［12］Kay S M, Ramos V A and Marquez M. 1993. Evidence in Cerro Pampa volcanic rocks forslab melting prior to ridge-trench collision in southern South America. Journal ofGeology, 101: 703-714

    [13]

    ［13］Kerrick D M and Connolly J A D. 2001. Metamorphic devolatilization of subductedoceanic metabasalts: implications for seismicity, arc magmatism and volatile recycling.Earth Planet. Sci. Lett.. 189: 19-29

    [14]

    ［14］Kepezhinkas P K, Defant M J and Drummond M S. 1995. Na metasomatism in theisland-arc mantle by slab melt-peridotite interaction: evidence from mantle xenoliths inthe North Kamchatka Arc. Journal of Petrology, 36: 1505-1527

    [15]

    ［15］Kimura G, Takahashi M and Kono M. 1990. Mesozoic collision-extrusion tectonics ineastern Asia. Tectonophysics, 181: 15-23

    [16]

    ［16］Li WP, Li XH and Lu FX. 2001. Genesis and geological significance for thr middleJurassic high Sr and low Y type volcanic rocks in Fuxin area of west Liaoning,northeastern China. Acta Petrologica Sinica, 17(4):523-532 (in Chinese with Englishabstract)

    [17]

    ［17］Lopez S and Castro A. 2001. Determination of the fluid-absent solidus andsupersolidus phase relationships of MORB-derived amphibolites in the range 4-14 kbar.American Mineral., 86: 1396-1403

    [18]

    ［18］Molnar P and England P. 1995. Temperatures in zones of steady-state underthrustingof young oceanic lithosphere. Earth Planet. Sci. Lett., 131: 57-70

    [19]

    ［19］Morris P A. 1995. Slab melting as an explanation of Quaternary volcanism andaseismicity in southwest Japan. Geology, 23: 395-398

    [20]

    ［20］Muir R J, Weaver S D, Bradshaw J D, Eby G N and Evans J A. 1995. The CretaceousSeparation Point batholith, New Zealand: granitoid magmas formed by melting of maficlithosphere. Journal. Geol. Soc. London, 152: 689-701

    [21]

    ［21］Pan GQ, Lu XC and Yu HB. 2001. Petrological and geochemical characteristics ofMesozoic adakite from Northern Huaiyang and discussion on its genesis. Acta PetrologicaSinica, 17, 541-550 (in Chinese with English abstract)

    [22]

    ［22］Peacock S M, Rushmer T and Thompson A B. 1994. Partial melting of subductingoceanic crust. Earth Planet. Sci. Lett., 121: 227-244

    [23]

    ［23］Petford N and Atherton M P. 1996. Na-rich partial melts from newly underplatedbasaltic crust: the Cordillera Blanca Batholith, Peru. Journal of Petrology, 37: 1491-1521

    [24]

    ［24］Petford N and Gallagher K. 2001. Partial melting of mafic (amphibolitic) lowercrust by periodic influx of basaltic magma. Earth Planet. Sci. Lett., 193: 483-499

    [25]

    ［25］Rapp R P, Watson E B and Miller C F. 1991. Partial melting of amphibolite/eclogiteand the origin of Archean trondhjemites and tonalites. Precambrian Res., 51: 1-25

    [26]

    ［26］Rapp R P. 1995. The amphibole-out phase boundary in partially-melted metabasalt,its control over liquid fraction and composition, and source permeability. Jour. Geophys.Res., 100: 15601-15610

    [27]

    ［27］Rapp R P and Watson E B. 1995. Dehydration melting of metabasalt at 8-32 kbar:implications for continental growth and crust-mantle recycling. Journal of Petrol., 36:891-931

    [28]

    ［28］Rapp R P, Shimizu N, Norman M D and Applegate G S. 1999. Reaction betweenslab-derived melts and peridotite in the mantle wedge: experimental constraints at 3.8GPa. Chemical Geol., 160: 335-356

    [29]

    ［29］Sajona F G, Bellon H, Maury R C, Pubellier M, Cotton J and Rangin C. 1994. Magmatic response to abrupt changes in geodynamic settings: Pliocene-Quaternarycalc-alkaline and Nb-enriched lavas from Mindanao (Philippines). Tectonophysics, 237:47-72

    [30]

    ［30］Schmidt M W and Poli S. 1998. Experimentally based water budgets for dehydratingslabs and consequences for arc magma generation. Earth Planet. Sci. Lett., 163: 361-379

    [31]

    ［31］Sen C and Dunn T. 1994. Dehydration melting of a basaltic composition amphiboliteat 1.5 and 2.0 GPa: implications for the origin of adakites. Contrib. Mineral. Petrol.,117: 394-409

    [32]

    ［32］Smithies R H. 2000. The Archean tonalite-trondhjemite-granodiorite (TTG) series isnot an analogue of Cenozoic adakite. Earth Planet. Sci. Lett., 182: 115-125

    [33]

    ［33］Stern C R and Killian R. 1996. Role of the subducted slab, mantle wedge andcontinental crust in the generation of adakites from the Andean Austral Volcanic Zone.Contrib. Mineral. Petrol., 123: 263-281

    [34]

    ［34］Vielzeuf D and Schmidt M W. 2001. Melting relations in hydrous systems revisited:application to metapelites, metagreywackes, and metabasalts. Contrib. Mineral. Petrol.,141: 251-267

    [35]

    ［35］Wang Q, Xu JF, Zhao ZH, Wang RJ, Qiu JX and Bao ZW. 2001. The petrogenesis andgeodynamic significance of HREE depleted granitoids during Yanshan period in the DabieMountains. Acta Petrologica Sinica, 17: 551-564 (in Chinese with English abstract)

    [36]

    ［36］Wang Y and Zhang Q. 2001. A granitoid complex from Badaling area, North China:composition, geochemical characteristics and its implications. Acta Petrologica Sinica,17: 533-540 (in Chinese with English abstract)

    [37]

    ［37］Wang YL, Zhang Q and Wang Y. 2001. Geochemical characteristics of volcanic rocksfrom Ningwu area, and its significance. Acta Petrologica Sinica, 17: 565-575 (in Chinesewith English abstract)

    [38]

    ［38］Wareham C D, Millar I L and Vaughan A P M. 1997. The genration of sodic granitemagmas, western Palmer Land, Antarctic Peninsula. Contrib. Mineral. Petrol., 141: 81-96

    [39]

    ［39］Winther K T and Newton R C. 1991. Experimental melting of hydrous low-K tholeiite:evidence on the origin of Archean cratons. Bull. Geol. Soc. Denmark, 39: 213-228

    [40]

    ［40］Xiong XL, Zhao ZH, Bai ZH, Mei HJ, Xu JF and Wang Q. 2001. Origin of Awulaleadakitic sodium-rich rocks in western Tianshan: Constraints for Nd and Sr isotopiccompositions. Acta Petrologica Sinica, 17: 514-522 (in Chinese with English abstract)

    [41]

    ［41］Xu JF, Wang Q and Yu X-Y. 2000. Geochemistry of high_Mg andesites and adakiticandesite from the Sanchasi block of the Mian-Lue ophiolitic m閘ange in the QinlingMountains, central China: Evidence of partial melting of the subducted Paleo-Tethyancrust. Geochemical Jour., 34: 359-377

    [42]

    ［42］Xu JF, Mei H, Yu X, Bai Z, Niu H, Chen F, Zhen Z and Wang Q. 2001. Adakitesrelated to subduction in the northern margin of Junggar arc for the Late Paleozoic:Products of slab melting. Chinese Science Bull., 46: 1312-1316

    [43]

    ［43］Xu JF, Wang Q, Xu YG, Zhao ZH and Xiong XL. 2001. Geochemistry of Anjishanintermediate-acid intrusive rocks in Ningzhen area: Constraint to origin of the magma withHREE and Y depletion. Acta Petrologica Sinica, 17: 576-584 (in Chinese with Englishabstract)

    [44]

    ［44］Zhang Q, Wang Y, Qian Q, Yang J, Wang Y L, Zhao T P and Guo GJ. 2001. Thecharacteristics and tectono-metallogenic significance of the adakites in Yanshan periodfrom eastern China. Acta Petrologica Sinica, 17: 236-244 (in Chinese with Englishabstract)

    [45]

    ［45］Zhang Q, Wang Y and Wang YL. 2001. Preliminary study on the components of thelower crust in east China plateau during Yanshanian Period: Constraints on Sr and Ndisotopic compositions of adakite-like rocks. Acta Petrologica Sinica, 17, 505-513 (inChinese with English abstract)

    [46]

    ［46］李伍平,李献华,路凤香. 2001. 辽西中侏罗世高Sr低Y型火山岩的成因及其地质意义.岩石学报, 17(4):523-532

    [47]

    ［47］潘国强,陆现彩,于航波. 2001. 北淮阳中生代adakite岩石地球化学特征及成因讨论.岩石学报, 17(4):541-550

    [48]

    ［48］王强,许继锋,赵振华,王人镜,邱家骧,包志伟. 2001.大别山燕山期亏损重稀土元素花岗岩类的成因及动力学意义.岩石学报, 17(4):551-564

    [49]

    ［49］王焰,张旗. 2001.八达岭花岗杂岩的组成、地球化学特征及其意义. 岩石学报,17(4):533-540

    [50]

    ［50］王元龙,张旗,王焰. 2001. 宁芜火山岩的地球化学特征及其意义.岩石学报, 17(4):565-575

    [51]

    ［51］熊小林,赵振华,白正华,梅厚钧,许继峰,王强. 2001.西天山阿吾拉勒埃达克质岩石成因: Nd和Sr同位素组成的限制.岩石学报, 17(4):514-522

    [52]

    ［52］许继峰,王强,徐义刚,赵振华,熊小林. 2001.宁镇地区中生代安基山中酸性侵入岩的地球化学:亏损重稀土和钇的岩浆产生的限制. 岩石学报, 17(4):576-584

    [53]

    ［53］张旗,王焰,钱青,杨进辉,王元龙,赵太平,郭光军. 2001.中国东部燕山期埃达克岩的特征及其构造-成矿意义. 岩石学报,17(2):236-244

    [54]

    ［54］张旗,王焰,王元龙. 2001. 燕山期中国东部高原下地壳组成初探:埃达克质岩Sr、Nd同位素制约.岩石学报, 17(4):505-513

    • 相关文章
  • 施引文献
  • 资源附件(0)
  • 加载中
WeChat 点击查看大图
计量
  • 文章访问数:  6849
  • PDF下载数:  7332
  • 施引文献:  0
出版历程
刊出日期:  2002-08-31

目录

    返回

    地址：北京9825信箱/北京朝阳区北土城西路19号邮编：100029

    电话：(010) 82998205/82998135/82998137 邮箱：ysxb@mail.iggcas.ac.cn

    版权所有 © 2009-2023 岩石学报 京ICP备05029136号-23

    本系统由 北京仁和汇智信息技术有限公司开发