全部 标题 作者
关键词 摘要

OALib Journal期刊
ISSN: 2333-9721
费用:99美元

查看量下载量

相关文章

更多...

华北埃达克质岩与克拉通破坏:实验岩石学和地球化学依据

, PP. 654-667

Keywords: 埃达克质岩,华北克拉通,地壳减薄,金红石,实验岩石学

Full-Text   Cite this paper   Add to My Lib

Abstract:

?华北埃达克质花岗岩和火山岩与岩石圈减薄时空一致性使得它们成为窥视克拉通破坏过程和机制的一个重要窗口.本文通过实验岩石学资料限定华北埃达克质岩石的主要源区岩石为中钾和高钾基性变质岩,并通过基性变质岩体系相平衡、长英质熔体TiO2溶解度、埃达克质岩石Nb/La随La/Yb变化规律等研究论证大别、胶东和克拉通北缘许多埃达克质岩石的源区存在残留金红石,岩浆形成深度超过50km,从而揭示华北克拉通破坏涉及超过15km的地壳厚度减薄或下地壳拆沉.

References

[1]  143 樊祺诚, 刘若新. 汉诺坝玄武岩中高温麻粒岩捕掳体. 科学通报, 1996, 41: 235-238
[2]  144 王清海, 许文良, 王冬艳, 等. 徐淮地区中生代深部地壳的物质组成及热状态-深源捕虏体证据. 大地构造与成矿学, 2003, 27: 362-371
[3]  145 Huang X L, Xu Y G, Liu D Y. Geochronology, petrology and geochemistry of the granulite xenoliths from Nushan, east China: Implication for a heterogeneous lower crust beneath the Sino-Korean Craton. Geochim Cosmochim Acta, 2004, 68: 127-149??
[4]  146 Watson E B, Harrison T M. Zircon saturation revisited: temperature and composition effects in a variety of crustal magma types. Earth Planet Sci Lett, 1983, 64: 295-304??
[5]  147 Miller C F, McDowell S M, Mapes R W. Hot and cold granites? Implications of zircon saturation temperatures and preservation of inheritance. Geology, 2003, 31: 529-532??
[6]  148 Watson E B, Harrison T M. Zircon thermometer reveals minimum melting conditions on earliest earth. Science, 2005, 308: 841-844??
[7]  149 Green T H, Pearson N J. Ti-rich accessory phase saturation in hydrous mafic-felsic compositions at high P, T. Chem Geol, 1986, 54: 185-201??
[8]  150 Ryerson F J, Watson E B. Rutile saturation in magmas: Implications for Ti-Nb-Ta depletion in island-arc basalts. Earth Planet Sci Lett, 1987, 86: 225-239??
[9]  12 Gao S, Rudnick R L, Xu W L, et al. Recycling deep cratonic lithosphere and generation of intraplate magmatism in the North China Craton. Earth Planet Sci Lett, 2008, 270: 41-53??
[10]  13 高山, 章军锋, 许文良, 等. 拆沉作用与华北克拉通破坏. 科学通报, 2009, 54: 1962-1973
[11]  14 Wu F Y, Walker R J, Ren X W, et al. Osmium isotopic constraints on the age of lithospheric mantle beneath northeastern China. Chem Geol, 2003, 196: 107-129??
[12]  15 Wu F Y, Walker R J, Yang Y H, et al. The chemical-temporal evolution of lithospheric mantle underlying the North China Craton. Geochim Cosmochim Acta, 2006, 70: 5013-5034??
[13]  16 吴福元, 徐义刚, 高山, 等. 华北岩石圈减薄与克拉通破坏研究的主要学术争论. 岩石学报, 2008, 24: 1145-1174
[14]  17 Liu Y S, Gao S, Kelemen P B, et al. Recycled crust controls contrasting source compositions of Mesozoic and Cenozoic basalts in the North China Craton. Geochim Cosmochim Acta, 2008, 72: 2349-2376??
[15]  18 Xu J F, Shinjo R, Defant M J, et al. Origin of Mesozoic adakitic intrusive rocks in the Ningzhen area of east China: Partial melting of delaminated lower continental crust? Geology, 2002, 30: 1111-1114
[16]  19 Xu W L, Gao S, Wang Q H, et al. Mesozoic crustal thickening of the eastern North China Craton: Evidence from eclogite xenoliths and petrologic implications. Geology, 2006, 34: 721-724??
[17]  20 Xu Y G, Menzies M A, Vroon P, et al. Texture-temperature-geochemistry relationships in the upper mantle as revealed from spinel peridotite xenoliths from Wangqing, NE China. J Petrol, 1998, 39: 469-493??
[18]  21 Xu Y G. Thermo-tectonic destruction of the Archean lithospheric keel beneath the Sino-Korean Craton in China: Evidence, timing and mechanism. Phys Chem Earth, 2001, 26: 741-757
[19]  22 Xu Y G, Menzies M A, Thirlwall M F, et al. “Reactive” harzburgites from Huinan, NE China: Products of lithosphere-asthenosphere interaction during lithospheric thinning? Geochim Cosmochim Acta, 2003, 67: 487-505
[20]  25 Zheng J P, O’Reilly S Y, Griffin W L, et al. Relict refractory mantle beneath the eastern North China Block: Significance for lithosphere evolution. Lithos, 2001, 57: 43-66??
[21]  26 路凤香, 郑建平, 李伍平, 等. 中国东部显生宙地幔演化的主要样式: “蘑茹云”模型. 地学前缘, 2000, 7: 97-107
[22]  27 郑建平, 余淳梅, 路凤香, 等. 华北东部大陆地幔橄榄岩组成、年龄与岩石圈减薄. 地学前缘, 2007, 14: 87-97
[23]  28 Zheng J P, Griffin W L, O’Reilly S Y, et al. Mechanism and timing of lithospheric modification and replacement beneath the eastern North China Craton: Peridotitic xenoliths from the 100 Ma Fuxin basalts and a regional synthesis. Geochim Cosmochim Acta, 2007, 71: 5203-5225??
[24]  29 郑建平. 不同时空背景幔源物质对比与华北深部岩石圈破坏和增生置换过程. 科学通报, 2009, 54: 1990-2007
[25]  45 Xiong X L. Trace element evidence for the growth of early continental crust by melting of rutile-bearing hydrous eclogite. Geology, 2006, 34: 945-948??
[26]  46 Xiong X L, Keppler H, Audétat A, et al. Experimental constraints on rutile saturation during partial melting of metabasalt at the amphibolite to eclogite transition, with applications to TTG genesis. Amer Mineral, 2009, 94: 1175-1186??
[27]  47 Nair R, Chacko T. Role of oceanic plateaus in the initiation of subduction and origin of continental crust. Geology, 2008, 36: 583-586??
[28]  48 Zhai M G, Fan Q C, Zhang H F, et al. Lower crustal processes leading to Mesozoic lithospheric thinning beneath eastern North China: Underplating, replacement and delamination. Lithos, 2007, 96: 36-54??
[29]  49 张旗, 王焰. 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, 2001, 17: 236-244
[30]  50 Wu F Y, Yang J H, Wilde S A, et al. Geochronology, petrogenesis and tectonic implications of Jurassic granites in the Liaodong Peninsula, NE China. Chem Geol, 2005, 221: 127-156??
[31]  51 张旗, 王焰, 王元龙. 埃达克岩与构造环境. 大地构造与成矿学, 2003, 27: 101-108
[32]  52 张旗, 李承东, 王焰, 等. 中国东部中生代高Sr低Yb和低Sr高Yb型花岗岩: 对比及其地质意义. 岩石学报, 2005, 21: 1527-1537
[33]  53 张旗, 王焰, 熊小林, 等. 埃达克岩和花岗岩: 挑战与机遇. 北京: 中国大地出版社, 2008. 1-344
[34]  54 Wang Q, Xu J F, Zhao Z H, et al. Cretaceous high-potassium intrusive rocks in the Yueshan-Hongzhen area of east China: Adakites in an extensional tectonic regime within a continent. Geochem J, 2004, 38: 417-434
[35]  55 Wang Q, Zhao Z H, Bao Z W, et al. Geochemistry and petrogenesis of the Tongshankou and Yinzu adakitic intrusive rocks and the associated porphyry copper-molybdenum mineralization in southeast Hubei, east China. Resourc Geol, 2004, 54: 137-152??
[36]  56 Wang Q, Xu J F, Jian P, et al. Petrogenesis of adakitic porphyries in an extensional tectonic setting, dexing, South China: Implications for the genesis of porphyry copper mineralization. J Petrol, 2006, 47: 119-144
[37]  57 Wang Q, Wyman D A, Xu J F, et al. Petrogenesis of Cretaceous adakitic and shoshonitic igneous rocks in the Luzong area, Anhui Province (eastern China): Implications for geodynamics and Cu-Au mineralization. Lithos, 2006, 89: 424-446??
[38]  58 Wang Q, Wyman D A, Xu J F, et al. Partial melting of thickened or delaminated lower crust in the middle of eastern China: Implications for Cu-Au mineralization. J Geol, 2007, 115: 149-161??
[39]  59 Wang Q, Wyman D A, Xu J F, et al. Early Cretaceous adakitic granites in the Northern Dabie Complex, central China: Implications for partial melting and delamination of thickened lower crust. Geochim Cosmochim Acta, 2007, 71: 2609-2636??
[40]  60 王强, 赵振华, 熊小林, 等. 底侵玄武质下地壳的熔融: 来自安徽沙溪adakite质富钠石英闪长玢岩的证据. 地球化学, 2001, 30: 353-362
[41]  61 李伍平, 李献华, 路风香. 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, 2001, 17: 523-532
[42]  62 刘红涛, 孙世华, 刘建明, 等. 华北克拉通北部边缘中生代高锶花岗岩类: 地球化学与源区性质. 岩石学报, 2002, 18: 257-274
[43]  63 陈斌, 翟明国, 邵济安. 太行山北段中生代岩基的成因和意义: 主要和微量元素地球化学证据. 中国科学D辑: 地球科学, 2002, 32: 896-907
[44]  64 Chen B, Jahn B M, Arakawa Y, et al. Petrogenesis of the Mesozoic intrusive complexes from the southern Taihang Orogen, North China Craton: Elemental and Sr-Nd-Pb isotopic constraints. Contrib Mineral Petrol, 2004, 148: 489-501??
[45]  65 李承东, 张旗, 苗来成, 等. 冀北中生代高Sr低Y和低Sr低Y型花岗岩: 地球化学、成因及其与成矿作用的关系. 岩石学报, 2004, 20: 269-284
[46]  66 蔡剑辉, 阎国翰, 牟保磊, 等. 北京房山岩体锆石U-Pb年龄和Sr、Nd、Pb同位素与微量元素特征及成因探讨. 岩石学报, 2005, 21: 776-788
[47]  67 Xu W L, Wang Q H, Wang D Y, et al. Mesozoic adakitic rocks from the Xuzhou-Suzhou area, eastern China: Evidence for partial melting of delaminated lower continental crust. J Asian Earth Sci, 2006, 27: 230-240??
[48]  68 Guo F, Fan W M, Li C W. Geochemistry of late Mesozoic adakites from the Sulu belt, eastern China: Magma genesis and implications for crustal recycling beneath continental collisional orogens. Geol Mag, 2006, 143: 1-13
[49]  69 Hou M L, Jiang Y H, Jiang S Y, et al. Contrasting origins of late Mesozoic adakitic granitoids from the northwestern Jiaodong Peninsula, east China: Implications for crustal thickening to delamination. Geol Mag, 2007, 144: 619-631??
[50]  70 黄华, 高山, 胡兆初, 等. 辽西彰武地区中生代高镁安山岩地球化学及其对新生代下地壳拆沉作用的指示. 中国科学D辑: 地球科学, 2007, 37: 1287-1300
[51]  71 Jiang N, Liu Y S, Zhou W G, et al. Derivation of Mesozoic adakitic magmas from ancient lower crust in the North China Craton. Geochim Cosmochim Acta, 2007, 71: 2591-2608??
[52]  72 Yang W, Li S G. Geochronology and geochemistry of the Mesozoic volcanic rocks in Western Liaoning: Implications for lithospheric thinning of the North China Craton. Lithos, 2008, 102: 88-117??
[53]  73 Huang F, Li S G, Dong F, et al. High-Mg adakitic rocks in the Dabie orogen, central China: Implications for foundering mechanism of lower continental crust. Chem Geol, 2008, 255: 1-13??
[54]  74 Liu S, Hu R Z, Gao S, et al. Zircon U-Pb age, geochemistry and Sr-Nd-Pb isotopic compositions of adakitic volcanic rocks from Jiaodong, Shandong Province, Eastern China: Constraints on petrogenesis and implications. J Asian Earth Sci, 2009, 35: 445-458??
[55]  75 葛小月, 李献华, 陈志刚, 等. 中国东部燕山期高Sr低Y型中酸性火成岩的地球化学特征及成因: 对中国东部地壳厚度的制约. 科学通报, 2002, 47: 474-480
[56]  76 李伍平, 李献华. 燕山造山带中段中晚侏罗世中酸性火山岩的成因及其意义. 岩石学报, 2004, 20: 501-510
[57]  77 李晓勇, 郭锋, 范蔚茗, 等. 北京西山东岭台组粗面质火山岩地球化学: 下地壳熔融成因. 大地构造与成矿学, 2004, 28: 155-164
[58]  78 王焰, 张旗. 八达岭花岗杂岩的组成,地球化学特征及其意义. 岩石学报, 2001, 17: 533-540
[59]  93 Ling M X, Wang F Y, Ding X, et al. Cretaceous ridge subduction along the lower Yangtze river belt, eastern China. Econ Geol, 2009, 104: 303-321??
[60]  94 Xiong X L, Xia B, Xu J F, et al. Na depletion in modern adakites via melt/rock reaction within the sub-arc mantle. Chem Geol, 2006, 229: 273-292??
[61]  95 Douce A E P. Vapor-absent melting of tonalite at 15-32 kbar. J Petrol, 2005, 46: 275-290
[62]  96 Singh J, Johannes W. Dehydration melting of tonalites. Part II. Composition of melts and solids. Contrib Mineral Petrol, 1996, 125: 26-44??
[63]  97 Singh J, Johannes W. Dehydration melting of tonalites. Part I. Beginning of melting. Contrib Mineral Petrol, 1996, 125: 16-25??
[64]  98 Skjerlie K P, Johnston A D. Fluid-absent melting behavior of an F-rich tonalitic gneiss at mid-crustal pressures: Implications for the generation of anorogenic granites. J Petrol, 1993, 34: 785-815
[65]  99 Skjerlie K P, Johnston A D. Vapor-absent melting at 10 kbar of a biotite- and amphibole-bearing tonalitic gneiss: Implications for the generation of A-type granites. Geology, 1992, 20: 263-266??
[66]  100 Watkins J, Clemens J, Treloar P. Archaean TTGs as sources of younger granitic magmas: Melting of sodic metatonalites at 0.6-1.2 GPa. Contrib Mineral Petrol, 2007, 154: 91-110
[67]  101 Gardien V, Thompson A B, Ulmer P. Melting of biotite + plagioclase+ quartz gneisses: The role of H2O in the stability of amphibole. J Petrol, 2000, 41: 651-666??
[68]  102 Douce A E P, Beard J S. Dehydration-melting of biotite gneiss and quartz amphibolite from 3 to 15 kbar. J Petrol, 1995, 36: 707-738
[69]  103 Castro A, Corretge L G, El-Biad M, et al. Experimental constraints on hercynian anatexis in the Iberian Massif, Spain. J Petrol, 2000, 41: 1471-1488
[70]  104 Vielzeuf D, Montel J M. Partial melting of metagreywackes. Part I. Fluid-absent experiments and phase relationships. Contrib Mineral Petrol, 1994, 117: 375-393??
[71]  105 Montel J M, Vielzeuf D. Partial melting of metagreywackes, Part II. Compositions of minerals and melts. Contrib Mineral Petrol, 1997, 128: 176-196??
[72]  106 Douce A E P, Beard J S. Effects of P, f(O2) and Mg/Fe ratio on dehydration melting of model metagreywackes. J Petrol, 1996, 37: 999-1024
[73]  107 Casco A G, Haissen F, Castro A, et al. Synthesis of staurolite in melting experiments of a natural metapelite: Consequences for the phase relations in low-temperature pelitic migmatites. J Petrol, 2003, 44: 1727-1757??
[74]  108 Hermann J, Spandler C J. Sediment melts at sub-arc depths: An experimental study. J Petrol, 2008, 49: 717-740
[75]  109 Skjerlie K P, Johnston A D. Vapour-absent melting from 10 to 20 kbar of crustal rocks that contain multiple hydrous phases: Implications for anatexis in the deep to very deep continental crust and active continental margins. J Petrol, 1996, 37: 661-691??
[76]  110 Liu J, Bohlen S R, Ernst W G. Stability of hydrous phases in subducting oceanic crust. Earth Planet Sci Lett, 1996, 143: 161-171??
[77]  111 Winther K T, Newton R C. Experimental melting of hydrous low-K tholeiite: Evidence on the origin of Archaean cratons. Bull Geol Soc Denmark, 1991, 39: 213-228
[78]  112 Winther K T. An experimentally based model for the origin of tonalitic and trondhjemitic melts. Chem Geol, 1996, 127: 43-59??
[79]  113 Rushmer T. Partial melting of two amphibolites: Contrasting experimental results under fluid-absent conditions. Contrib Mineral Petrol, 1991, 107: 41-59??
[80]  114 Rushmer T. Experimental high-pressure granulites: Some applications to natural mafic xenolith suites and Archean granulite terranes. Geology, 1993, 21: 411-414??
[81]  115 Wolf M B, Wyllie P J. Dehydration-melting of amphibolite at 10 kbar: The effects of temperature and time. Contrib Mineral Petrol, 1994,115: 369-383??
[82]  116 Rapp R P, Watson E B. Dehydration Melting of Metabasalt at 8-32 kbar: Implications for continental growth and crust-mantle recycling. J Petrol, 1995, 36: 891-931
[83]  117 Springer W, Seck H A. Partial fusion of basic granulites at 5 to 15 kbar: Implications for the origin of TTG magmas. Contrib Mineral Petrol, 1997, 127: 30-45??
[84]  118 Lopez S, Castro A. Determination of the fluid-absent solidus and supersolidus phase relationships of MORB-derived amphibolites in the range 4-14 kbar. Am Miner, 2001, 86: 1396-1403
[85]  151 Clemens J D. Water contents of intermediate to silicic magmas. Lithos, 1984, 17: 273-287??
[86]  152 Defant M J, Drummond M S. Derivation of some modern arc magmas by melting of young subducted lithosphere. Nature, 1990, 347: 662-665??
[87]  153 Prowatke S, Klemme S. Effect of melt composition on the partitioning of trace elements between titanite and silicate melt. Geochim Cosmochim Acta, 2005, 69: 695-709??
[88]  154 Klemme S, Günther D, Hametner K, et al. The partitioning of trace elements between ilmenite, ulvospinel, armalcolite and silicate melts with implications for the early differentiation of the moon. Chem Geol, 2006, 234: 251-263??
[89]  1 陈国达. 中国地台“活化区”的实例并着重讨论华夏古陆问题. 地质学报, 1956, 36: 239-272
[90]  2 Fan W M, Menzies M A. Destruction of aged lower lithosphere and accretion of asthenosphere mantle beneath eastern China. Geotect Metall, 1992, 16: 171-180
[91]  3 Fan W M, Zhang H F, Baker J, et al. On and off the North China Craton: Where is the Archean keel? J Petrol, 2000, 41: 933-950
[92]  4 Griffin W L, O’Reilly S Y, Ryan C G. Composition and thermal structure of the lithosphere beneath South Africa, Siberia and China: Proton microprobe studies. In: Abstract of International Symposium on Cenozoic Volcanic Rocks and Deep-seated Xenoliths of China and Its Environs, Beijing, 1992. 65-66
[93]  5 Menzies M A, Fan W M, Zhang M. Palaeozoic and Cenozoic lithoprobes and the loss of >120 km of Archaean lithosphere, Sino-Korean Craton, China. In: Prichard H M, Alabaster T, Harris N B W, et al, eds. Magmatic Processes and Plate Tectonics. Geol Soc Spec Pub, 1993, 76: 71-78??
[94]  6 邓晋福, 莫宣学, 赵海玲, 等. 中国东部岩石圈根/去根作用与大陆“活化”-东亚型大陆动力学模式研究计划. 现代地质, 1994, 8: 349-356
[95]  7 邓晋福, 赵海玲, 莫宣学, 等. 中国大陆根-柱构造-大陆动力学的钥匙. 北京: 地质出版社, 1996. 110
[96]  8 Gao S, Luo T C, Zhang B R, et al. Chemical composition of the continental crust as revealed by studies in East China. Geochim Cosmochim Acta, 1998, 62: 1959-1975??
[97]  9 Gao S, Zhang B R, Jin Z M, et al. How mafic is the lower continental crust? Earth Planet Sci Lett, 1998, 16: 101-117
[98]  10 Gao S, Rudnick R L, Carlson R W, et al. Re-Os evidence for replacement of ancient mantle lithosphere beneath the North China Craton. Earth Planet Sci Lett, 2002, 198: 307-322??
[99]  11 Gao S, Rudnick R L, Yuan H L, et al. Recycling lower continental crust in the North China Craton. Nature, 2004, 432: 892-897??
[100]  23 徐义刚, 李洪颜, 庞崇进, 等. 论华北克拉通破坏的时限. 科学通报, 2009, 54: 1974-1989
[101]  24 郑建平. 中国东部地幔置换作用与中新生带岩石圈减薄. 武汉: 中国地质大学出版社, 1999. 126
[102]  30 周新华. 中国东部中新生代岩石圈转型与减薄研究若干问题. 地学前缘, 2006, 13: 50-64
[103]  31 Xu X S, Griffin W L, O’Reilly S Y, et al. Re-Os isotopes of sulfides in mantle xenoliths from eastern China: Progressive modification of lithospheric mantle. Lithos, 2008, 102: 43-64??
[104]  32 Zhang J J, Zheng Y F, Zhao Z F. Geochemical evidence for interaction between oceanic crust and lithospheric mantle in the origin of Cenozoic continental basalts in east-central China. Lithos, 2009, 110: 305-326??
[105]  33 郑永飞, 吴福元. 克拉通岩石圈的生长和再造. 科学通报, 2009, 54: 1945-1949
[106]  34 张宏福, 周新华, 范蔚茗, 等. 华北东南部中生代岩石圈地幔性质、组成、富集过程及其形成机理. 岩石学报, 2005, 21: 443-454
[107]  35 张宏福. 橄榄岩-熔体的相互作用: 岩石圈地幔组成转变的重要方式. 地学前缘, 2006, 13: 65-74
[108]  36 张宏福. 橄榄岩-熔体相互作用: 克拉通型岩石圈地幔能够被破坏之关键. 科学通报, 2009, 54: 2008-2026
[109]  37 Zhang H F, Sun M, Zhou X H, et al. Mesozoic lithosphere destruction beneath the North China Craton: Evidence from major, trace element and Sr-Nd-Pb isotope studies of Fangcheng basalts. Contrib Mineral Petrol, 2002, 144: 241-253??
[110]  38 Zhang H F. Transformation of lithospheric mantle through peridotite-melt reaction: A case of Sino-Korean Craton. Earth Planet Sci Lett, 2005, 237: 768-780??
[111]  39 Zhang H F, Goldstein S, Zhou X H, et al. Evolution of subcontinental lithospheric mantle beneath eastern China: Re-Os isotopic evidence from mantle xenoliths in Paleozoic kimberlites and Mesozoic basalts. Contrib Mineral Petrol, 2008, 155: 271-293??
[112]  40 牛耀龄. 玄武岩浆起源和演化的一些基本概念以及对中国东部中-新生代基性火山岩成因的新思路. 高校地质学报, 2005, 11: 9-46
[113]  41 朱日祥, 郑天愉. 华北克拉通破坏机制与古元古代板块构造体系. 科学通报, 2009, 54: 1950-1961
[114]  42 Liu Y S, Gao S, Jin S Y, et al. Geochemistry of lower crustal xenoliths from Neogene Hannuoba basalt, North China Craton: Implications for petrogenesis and lower crustal composition. Geochim Cosmochim Acta, 2001, 65: 2589-2604??
[115]  43 Zheng J P, Sun M, Lu F X, et al. Mesozoic lower crustal xenoliths and their significance in lithospheric evolution beneath the Sino-Korea. Tectonophysics, 2003, 361: 37-60 ??
[116]  44 Xiong X L, Adam J, Green T H. Rutile stability and rutile/melt HFSE partitioning during partial melting of hydrous basalt: Implications for TTG genesis. Chem Geol, 2005, 218: 339-359??
[117]  79 杨进辉, 朱美妃, 刘伟, 等. 胶东地区郭家岭花岗闪长岩的地球化学特征及成因. 岩石学报, 2003, 19: 692-700
[118]  80 张华锋, 翟明国, 童英, 等. 胶东半岛三佛山高Ba-Sr花岗岩成因. 地质论评, 2006, 52: 43-53
[119]  81 张华锋, 翟明国, 何中甫, 等. 胶东昆箭山杂岩中高银花岗岩地球化学成因及其意义. 岩石学报, 2004, 20: 369-380
[120]  82 袁洪林, 柳小明, 刘勇胜, 等. 北京西山晚中生代火山岩U-Pb锆石年代学及地球化学研究. 中国科学D辑: 地球科学, 2005, 35: 821-836
[121]  83 Zhao Z F, Zheng Y F, Wei C S, et al. Post-collisional granitoids from the Dabie Orogen in China: Zircon U-Pb age, element and O isotope evidence for recycling of subducted continental crust. Lithos, 2007, 93: 248-272??
[122]  84 Xiao L, Clemens J D. Origin of potassic (C-type) adakite magmas: Experimental and field constraints. Lithos, 2007, 95: 399-414??
[123]  85 Xu H J, Ma C Q, Ye K. Early cretaceous granitoids and their implications for the collapse of the Dabie Orogen, eastern China: SHRIMP zircon U-Pb dating and geochemistry. Chem Geol, 2007, 240: 238-259??
[124]  86 马昌前, 杨坤光, 明厚利, 等. 大别山中生代地壳从挤压转向伸展的时间: 花岗岩的证据. 中国科学D辑: 地球科学, 2003, 33: 817-827
[125]  87 肖龙, Rapp R P, 许继峰, 等. 深部过程对埃达克质岩石成分的制约. 岩石学报, 2004, 20: 219-228
[126]  88 张宏福、邵济安. 辽西义县组火山岩: 拆沉作用还是岩浆混合作用的产物? 岩石学报, 2008, 24: 37-48
[127]  89 Guo F, Nakamuru E, Fan W M, et al. Generation of Palaeocene adakitic andesites by magma mixing; Yanji Area, NE China. J Petrol, 2007, 48: 661-692??
[128]  90 Guo F, Fan W M, Wang Y J, et al. Origin of early Cretaceous calc-alkaline lamprophyres from the Sulu orogen in eastern China: Implications for enrichment processes beneath continental collisional belt. Lithos, 2004, 78: 291-305??
[129]  91 Castillo P R. An overview of adakite petrogenesis. Chin Sci Bull, 2006, 51: 257-268??
[130]  92 Yang J H, Wu F Y, Wilde A S, et al. Mesozoic decratonization of the North China Block. Geology, 2008, 36: 467-470??
[131]  119 Skjerlie K P. The fluid-absent partial melting of a zoisite-bearing quartz eclogite from 10 to 32 Gpa: Implications for melting in thickened continental crust and for subduction-zone processes. J Petrol, 2002, 43: 291-314??
[132]  120 Sen C, Dunn T. Dehydration melting of a basaltic composition amphibolite at 1.5 and 2.0 GPa: Implications for the origin of adakites. Contrib Mineral Petrol, 1994, 117: 394-409
[133]  121 周文戈, 谢鸿森, 刘永刚, 等. 2.0 GPa块状斜长角闪岩部分熔融-时间和温度的影响. 中国科学D辑: 地球科学, 2005, 35: 320-332
[134]  122 郑建平, 孙敏, 路凤香, 等. 信阳基性麻粒捕虏体及其华北南缘早中生代下地壳性质. 岩石学报, 2005, 21: 91-98
[135]  123 邵济安, 韩庆军, 李惠民. 华北克拉通早中生代麻粒岩捕虏体的发现. 中国科学D辑: 地球科学, 2000, 30: 148-153
[136]  124 黄小龙, 徐义刚, 储雪蕾, 等. 华北地台部分麻粒岩地体及包体的地球化学特征对比. 岩石矿物学杂志, 2001, 20: 318-328
[137]  125 刘勇胜, 高山, 骆庭川. 华北克拉通麻粒岩的地球化学特征及其对太古宙下地壳组成的指示意义. 地质地球化学, 1999, 27: 40-46
[138]  126 沈其韩, 耿元生. 冀西北太古宙条带状麻粒岩的岩石学和地球化学特征. 岩石学报, 1996, 12: 247-260
[139]  127 张宗清, 沈其韩, 耿元生, 等. 赤城伙房村和崇礼上新营变质岩的地球化学特征、年龄及其区域地壳形成时间. 岩石学报, 1996, 12: 315-328
[140]  128 刘勇胜, 高山, 王选策, 等. 太古宙-元古宙界限基性火山岩Nb/Ta比值变化及其对地球Nb/Ta平衡的指示意义. 中国科学D辑: 地球科学, 2004, 34: 1002-1014
[141]  129 Kogiso T, Hirschmann M M. Partial melting experiments of bimineralic eclogite and the role of recycled mafic oceanic crust in the genesis of ocean island basalts. Earth Planet Sci Lett, 2006, 249: 188-199??
[142]  130 Pertermann M, Hirschmann M M. Anhydrous partial melting experiments on MORB-like eclogite: Phase relations, phase compositions and mineral-melt partitioning of major elements at 2-3 GPa. J Petrol, 2003, 44: 2173-2201
[143]  131 Spandler C, Yaxley G, Green D H, et al. Phase relations and melting of anhydrous K-bearing eclogite from 1200 to 1600℃ and 3 to 5 GPa. J Petrol, 2008, 49: 771-795
[144]  132 王超, 金振民, 高山, 等. 华北克拉通岩石圈破坏的熔体-橄榄岩反应机制: 实验约束. 中国科学D辑: 地球科学, 2010, 40: 541-555
[145]  133 Lambert I B, Wyllie P J. Melting of gabbro (quartz eclogite) with excess water to 35 kilobars, with geological applications. J Geol, 1972, 80: 693-708??
[146]  134 Green T H. Anatexis of mafic crust and high pressure crystallization of andesite. In: Thorpe R S, ed. Andesites. New York: John Wiley, 1982. 465-487
[147]  135 Ernst W G, Liu J. Experimental phase-equilibrium study of Al- and Ti-contents of calcic amphibole in MORB-A semiquantitative thermobarometer. Am Miner, 1998, 83: 952-969
[148]  136 Prouteau G, Scaillet B, Pichavant M, et al. Evidence for mantle metasomatism by hydrous silicic melts derived from subducted oceanic crust. Nature, 2001, 410: 197-200??
[149]  137 Schmidt M W, Vielzeuf D, Auzanneau E. Melting and dissolution of subducting crust at high pressures: The key role of white mica. Earth Planet Sci Lett, 2004, 228: 65-84??
[150]  138 Forneris J F, Holloway J R. Phase equilibria in subducting basaltic crust: Implications for H2O release from the slab. Earth Planet Sci Lett, 2003, 214: 187-201??
[151]  139 Kessel R, Ulmer P, Pettke T, et al. The water-basalt system at 4 to 6 GPa: Phase relations and second critical endpoint in a K-free eclogite at 700 to 1400℃. Earth Planet Sci Lett, 2005, 237: 873-892??
[152]  140 Klimm K, Blundy J D, Green T H. Trace element partitioning and accessory phase saturation during H2O-saturated melting of basalt with implications for subduction zone chemical fluxes. J Petrol, 2008, 49: 523-553??
[153]  141 Schmidt M W, Poli S. Experimentally based water budgets for dehydrating slabs and consequences for arc magma generation. Earth Planet Sci Lett, 1998, 163: 361-379??
[154]  142 张旗, 王焰, 王元龙. 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, 2001, 17: 236-344

Full-Text

Contact Us

service@oalib.com

QQ:3279437679

WhatsApp +8615387084133