滇西吉义独蛇绿混杂岩的岩石地球化学特征、成因和构造环境探讨

何琦, 肖龙, 魏启荣, 倪平泽. 滇西吉义独蛇绿混杂岩的岩石地球化学特征、成因和构造环境探讨[J]. 岩石学报, 2009, 25(12): 3229-3240.
引用本文: 何琦, 肖龙, 魏启荣, 倪平泽. 滇西吉义独蛇绿混杂岩的岩石地球化学特征、成因和构造环境探讨[J]. 岩石学报, 2009, 25(12): 3229-3240.

滇西吉义独蛇绿混杂岩的岩石地球化学特征、成因和构造环境探讨

  • 加载中
  • [1]

    Abelson M,Baer G,Agnon A,Evidence from gabbros of the Troodos ophiolite for lateral magma transport along a slow-spreading mid-ocean ridge,Nature,2001.

    [2]

    Bloomer SH,Distribution and origin of igneous rocks from the landward slopes of the Mariana trench,Implications for its structure and evolution,Journal of Geophysical Research,1983.

    [3]

    Coleman RG,Ophiolites.Springer-Verlag,Berlin,Heidelberg,New York,1977.

    [4]

    Defant MJ,Drummond MS,Derivation of some modern arc magmas by melting of young subducted lithosphere,Nature,1990.

    [5]

    Ge MC,Feng QL,Xie CD,Geological Survey Party,CUG(China University of Geoscience).1:500000 Geological Map of Xiaruo Area,Yunnan Province.1 sheet,北京:地质出版社,2000.

    [6]

    Godard M,Jousselin D,Bodinier JL,Relationships between geochemistry and structure beneath a palaeo-spreading centre:A study of the mantle section in the Oman ophiolite,Earth and Planetary Science Letters,2000.

    [7]

    Han S,Jia XQ,Huang ZX,A preliminary geochemical and genetic study of Jinsha River ophiolites,Yunnan Province,Acta Petrologica et Mineralogica,1996.

    [8]

    Hawkins JW,Geology of supra-subduction zones:Implications for the origin of ophiolites,Geological Society of America,2003.

    [9]

    Hawkins JW,Londsdale PF,MacDongall JD,Volpe AM,Petrology of the axial ridge of the Mariana Trough backarc spreading center,Earth and Planetary Science Letters,1990.

    [10]

    Hou QY,Zhao ZD,Zhang HF,Indian Ocean-MORB-type isotopic signature of Yushigou ophiolite in North Qilian Mountains and its implications,Science in China(Series D),2005(6).

    [11]

    Ishiwatari A,Yanagida Y,Li YB,Ishii T,Haraguchi S,Koizumi K,Ichiyama Y and Umeka M,Dredge petrology of the boniniteand adakites-bearing Hahajima Seamount of the Ogasawara(Bonin)forearc:An ophiolite or a serpentinite seamount,Island Arc,2006.

    [12]

    Jian P,Wang XF,He LQ,Wang CS,U-Pb dating of anorthosite and plagiogranite from the Jinshajiang ophiolite belt,Acta Petrologica Sinica,1999(4).

    [13]

    Jian P,Liu DY,Sun XM,SHRIMP dating of the PermoCarboniferous Jinshajiang ophiolite,southwestern China:Geochronological constraints for the evolution of Paleo-Tethys,Journal of Asian Earth Sciences,2008(5-6).

    [14]

    Johnson LE,Fryer P,The first evidence for mid-oceanic ridge basalt-like lavas from the outer Mariana forearc,geochemistry,petrography,and tectonic implications,Earth and Planetary Science Letters,1990.

    [15]

    Ling WL,Gao S,Zheng HF,Sm-Nd isotopic geochronology of Kongling complex in Huangling region of Yangtze Craton,Chinese Science Bulletin,1998(1).

    [16]

    Metcalfe I,Gondwanaland dispersion,Asian accretion and evolution of eastern Tethys,Australian Journal of Earth Sciences,1996.

    [17]

    Miyashiro A,The Troodos ophiolite complex was probably formed in an island arc setting,Earth and Planetary Science Letters,1973.

    [18]

    Mo XX,Lu FX,Sheng SY,Sanjiang Tethyan Volcanism and Related Mineralization,北京:地质出版社,1993.

    [19]

    Mo XX,Sheng SY,Zhu QW,Volcanics,Ophiolite and Mineralization of Middle-Southern Part in Sanjiang Area of Southwestern China,北京:地质出版社,1998.

    [20]

    Pan GT,Chen ZL,Li XZ,Geological-Tectonic Evolution in the Eastern Tethys,北京:地质出版社,1997.

    [21]

    Pearce JA,The role of sub-continental lithosphere in magma genesis at destructive plate margins,Nantwich,Shiva,1983.

    [22]

    Pearce JA,Lippard SJ,Roberts S,Characteristics and tectonic significance of supra-subduction zone ophiolites,Geological Society of London Special Publication,Blackwell Scientific Publications,1984.

    [23]

    Qi L,Hu J,Gregoire DC,Determination of trace dements in granites by inductively coupled plasma mass spectrometry,Talanta,2000.

    [24]

    Shervais JW,Island are and ocean crust ophiolites,contrasts in the petrology,geochemistry and tectonic style of ophiolite assemblages in the California Coast Ranges,Geological Survey Department of Cyprus,1990.

    [25]

    Stern RJ,Bloomer SH,Lin PH,Submarine arc volcanism in the southern Maria arc as an ophiolite analogue,Tectonophysics,1989.

    [26]

    Su L,Song SG,Zhou DW,Petrogenesis of Songshugou dunite body in the Qinling orogenic belt,Central China:Constraints from geochemistry and melt inclusions,Science in China(Series D),2005(8).

    [27]

    Sun SS,McDonough WF,Chemical and isotopic systematics of ocean basalts:Implications for mantle composition and processes,Special Publication of Geological Society of London,1989.

    [28]

    Sun XM,Nie ZT,Liang DY,Determination of sedmentary enviroments and tectonic significance of silicolites in Jinsha River belt,NW Yunnan,Geological Review,1995(2).

    [29]

    Sun XM,Zhang BM,Nie ZT,Formation age and environment of ophiolite and ophiolitic melange in the Jinshajiang belt,northwestern Yunnan,Geological Review,1997.

    [30]

    Wang LQ,Pan GT,Li DM,The spatio-temperal framework and geological evolution of the Jinshajiang arc-basin systems,Acta Geologica Sinica,1999(3).

    [31]

    Wang PS,Petrochemistry of the ophiolite-associated lavas in Deqin,Yunnan,Contribution to the Geology of the Qinghai-Xizang(Tibet)Plateau,1985.

    [32]

    Wang XF,Metcalfe I,Jian P,The Jinshajiang suture zone:Tectono-stratigraphic subdivision and revision of age,Science in China(Series D),1999(1).

    [33]

    Wang XF,Metcalfe I,Jian P,He LQ and Wang CS,The Jinshajiang-Ailaoshan Suture Zone,China:Tectonostratigraphy,age and evolution,Journal of Asian Earth Sciences,2000(6).

    [34]

    Wilson M,Igneous Petrogenesis,London:Unwin Hyroan,1989.

    [35]

    Winchester JA,Floyed PA,Geochemical discrimination of different magmas series and their differentiation products using immobile elements,Chemical Geology,1977.

    [36]

    Wood DA,The application of a Th-Hf-Ta diagram to problems of tectonomagmatic classification of basaltic lavas of the British Tertiary volcanic province,Earth and Planetary Science Letters,1980.

    [37]

    Wu HR,Discovery of Early Carboniferous deep-sea sediments from the Jinsha Belt,NW Yunnan,Scientia Geologica Sinica,1993.

    [38]

    Xiao L,He Q,Pirajno F,Ni PZ Du JX and Wei QR,Possible correlation between a mantle plume and the evolution of Paleo-Tethys Jinshajiang Ocean:Evidence from a volcanic rifted margin in the Xiaru-Tuoding area,Yunnan,SW China,Lithos,2008(1-4).

    [39]

    Xie J,Zhu BQ,Chang XY,Geochemical characteristics of basic-intermediate volcanic rocks from Jinshajiaag Belt in Northwestern Yuunan,China,Bulletin of Mineralogy Petrology and Geochemistry,2005(4).

    [40]

    Xu JF,Castillo PR,Li XH,MORB-type rocks from the PaleoTethyan Mian-Lueyang northern ophiolite in the Qinling Mountains,central China:Implications for the source of the low ~(206)Pb/~(204)Pb and high ~(143)Nd/~(144)Nd mantle component in the Indian Ocean,Earth and Planetary Science Letters,2002(3-4).

    [41]

    Xu JF,Zhang BR,Han YW,Geochemistry of the Mian-Lue ophiolites in the Qinling Mountains,central China:Constraints on the evolution of the Qinling orogenic belt and collision of the North and South China Cratons,Journal of Asian Earth Sciences,2008.

    [42]

    Zhang Q,Zhang KW,Li DZ,Mafic-Ultramafic Rocks in the Hengduan Mountains Region,北京:科学出版社,1992.

    [43]

    Zhang Q,Zhou GQ,Ophiolites of China,北京:科学出版社,2001.

    [44]

    Zhong DL,The Paleo-Tethyan Orogenic Belts,Western Yunnan and Sichuan Provinces,北京:科学出版社,1998.

    [45]

    Zindler A,Hart SR,Chemical geodynamies,Annual Review of Earth and Planetary Sciences,1986.

    [46]

    葛孟春,冯庆来,谢德凡,中国地质大学(武汉)滇西北区域地质调查队,云南1:5万霞若幅地质图(1张),北京:地质出版社,2000.

    [47]

    韩松,贾秀勤,黄忠祥,云南金沙江蛇绿岩的地球化学特征及其成因的初步研究,岩石矿物学杂志,1996(3).

    [48]

    侯青叶.赵志丹.张宏飞.张本仁.陈岳龙 北祁连玉石沟蛇绿岩印度洋MORB型同位素组成特征及其地质意义[J].中国科学D辑2005(8)

    [49]

    简平.汪啸风.何龙清.王传尚 金沙江蛇绿岩中斜长岩和斜长花岗岩的U-Pb年龄及地质意义 [J].-岩石学报1999(4)

    [50]

    凌文黎,高山,郑海飞,周炼,赵祖斌,扬子克拉通黄陵地区崆岭杂岩Sm-Nd同位素地质年代学研究,科学通报,1998(1).

    [51]

    莫宣学,路凤香,沈上越,三江特提斯火山作用与成矿,北京:地质出版社,1993.

    [52]

    莫宣学,沈上越,朱勤文,三江中南段火山岩-蛇绿岩与成矿,北京:地质出版社,1998.

    [53]

    潘桂棠,陈智梁,李兴振,东特提斯地质构造形成演化,北京:地质出版社,1997.

    [54]

    苏犁.宋述光.周鼎武 秦岭造山带松树沟纯橄岩体成因: 地球化学和岩浆包裹体的制约[J].中国科学D辑2005(1)

    [55]

    孙晓猛.聂泽同.梁定益 滇西北金沙江带硅质岩沉积环境的确定及大地构造意义 [J].-地质论评1995(2)

    [56]

    孙晓猛.张保民.聂泽同.梁定益 滇西北金沙江带蛇绿岩、蛇绿混杂岩形成环境及时代 [J].-地质论评1997(2)

    [57]

    王立全,潘桂棠,李定谋,徐强,林仕良,金沙江弧-盆系时空结构及地史演化,地质学报,1999(3).

    [58]

    王培生,云南德钦蛇绿岩中基性熔岩的岩石化学特征初步研究,北京:地质出版社,1985.

    [59]

    汪啸风.Ian Metcalfe.简平.何龙清.王传尚 金沙江缝合带构造地层划分及时代厘定 [J].-中国科学D辑1999(4)

    [60]

    吴浩若,滇西北金沙江带早石炭世深海沉积的发现,地质科学,1993(4).

  • 加载中
计量
  • 文章访问数:  6358
  • PDF下载数:  5983
  • 施引文献:  0
出版历程
刊出日期:  2009-12-31

目录