LA-ICP-MS zircon U-Pb dating and geochemical characteristics of high Sr/Y-type granite from Xigela, eastern Qilian area
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摘要: 西格拉花岗岩体位于祁连东部的米屈花岗岩带上,空间上呈NW-NWW向展布,岩体由花岗闪长岩-花岗岩-正长岩组成,主要岩性为花岗闪长岩。LA-ICP-MS锆石U-Pb定年结果表明,西格拉花岗闪长岩存在两期岩浆作用,年龄分别为465.6±6.5Ma、443.2±4.8Ma,其中,前者与祁连洋俯冲极性发生转变的时限(~463Ma)相近,而后者与祁连洋闭合的时间(~445Ma)相似。早期淡色花岗闪长岩具正铕异常(δEu=2.44),晚期暗色花岗闪长岩则为弱负/正铕异常(δEu=0.94~1.32),两者均显示出高Si、Al,富Na贫K,富集Ba、Sr、LREE,高Sr/Y值,低Y、HREE含量,亏损HFSE(Nb、Ta、Ti、P)的特征,与Martin et al.(2005)划分的高硅埃达克岩(HSA)相似。其源区可能均残留石榴子石、普通角闪石及少量金红石,而斜长石则大量参与部分熔融过程,推测早期花岗闪长岩的源区深度可能超过50km;整体上,由早期→晚期反映出加厚地壳减薄、地幔组分贡献增强的趋势;两者可能均为加厚下地壳物质部分熔融的产物。Abstract: Xigela granite pluton, in the NW-NWW trending, locates in the Mi-Qu granite belt of eastern Qilian area. It is mainly composed of granodiorite-granite-syenite, and main lithology is granodiorite. U-Pb zircon dating by LA-ICP-MS yielded two group ages, including 465.6±6.5Ma and 443.2±4.8Ma.The former is similar to shift time (~463Ma) of Qilian Ocean's (QO) subduction polarity, and the later is consistent with closure time (~445Ma) of QO. Early stage granodiorite shows strong positive Eu anomalies (δEu=2.44), and later period granodiorite have a weak negative/positive Eu anomaly (δEu=0.94~1.32). In general, both granodiorites show characteristics of high Si, Al, Na, low K, HREE and Y content, enrichment of Ba, Sr, LREE, and high Sr/Y value, depletion in HFSE. These geochemical characteristics are similar to high silica adakites (HSA) divided by Martin et al. (2005). Both source regions may be residual garnet, hornblende, a small amount of rutile, while plagioclase heavily involved in the process of partial melting, implies the source depth of early magma might exceed 50km. Overall, its reflect crustal thinning and the contribution of mantle components enhanced from early to late. Two magma were probably produced by partial melting of the thickened lower crust.
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Key words:
- Granite /
- Zircon U-Pb chronology /
- Geochemical characteristics /
- Positive Eu anomaly /
- Qilian area
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[1] Anderson T. 2002. Correction of common lead in U-Pb analyses that do not report 204Pb. Chemical Geology, 192(1-2): 59-79
[2] Castillo PR, Janney PE and Solidum RU. 1999. Petrology and geochemistry of Camiguin Island, southern Philippines: Insights into the source of adakites and other lavas in a complex arc setting. Contrib. Mineral. Petrol., 134(1): 33-51
[3] Castillo PR. 2006. Review of adakite genesis. Chinese Science Bulletin, 51(6): 617-627 (in Chinese)
[4] Chen B, Zhai MG and Shao JA. 2002. Origin and significance of Mesozoic bath in north section of Taihang Mountain: Major and trace element of geochemical evidence. Science in China (Series D), 32(11): 896-907 (in Chinese)
[5] Chen QL. 2009. Petrology, zircon SHRIMP dating and genesis of Niuxinshan granitic body in North Qilian orogenic belt. Master Degree Thesis. Beijing: Capital Normal University (in Chinese with English summary)
[6] Chen YX, Xia XH and Song SG. 2012. Decompression melting evidence of high silicon adakite in Silurian from west of North Qilian orogenic belt. Chinese Science Bulletin, 57(22): 2072-2085 (in Chinese)
[7] Chung SL, Liu DY, Ji JQ, Chu MM, Lee HY, Wen DJ, Lo CH, Lee TY, Qian Q and Zhang Q. 2003. Adakites from continental collision zones: Melting of thickened lower crust beneath southern Tibet. Geology, 31(11): 1021-1024
[8] Crofu F, Hanchar JM, Hoskin PWO and Kinny P. 2003. Atlas of zircon textures. Reviews in Mineralogy and Geochemistry, 53(1): 469-495
[9] Defant MJ and Drummond MS. 1990. Derivation of some modern arc magmas by melting of young subducted lithosphere. Nature, 347(6294): 662-665
[10] Deng JF, Mo XX, Zhao HL and Luo ZH. 1996. Continental Root: Key for Continental Dynamics. Beijing: Geological Publishing House (in Chinese with English abstract)
[11] Guo JJ and Lu SN. 1999. Collision of Chinese Neoproterozoic continental and Rodinia super continent. Geological Journal of China Universities, 5(2): 148-156 (in Chinese with English abstract)
[12] Gutscher MA, Maury R, Eissen JP and Bourdon E. 2000. Can slab melting be caused by flat subduction? Geology, 28(6): 535-538
[13] Hanchar JM and Miller CF. 1993. Zircon zonation patterns as revealed by cathodoluminescence and backscattered electron images: Implications for interpretation of complex crustal histories. Chemical Geology, 110(1-3): 1-13
[14] Hou ZQ, Gao YF, Qu XM, Rui ZY and Mo XX. 2004. Origin of adakitic intrusives generated during Mid-Miocene east-west extension in southern Tibet. Earth Planet. Sci. Lett., 220(1-2): 139-155
[15] Huang F and He YS. 2010. Partial melting of dry mafic lower continental crust: Significance for C-type adakite genesis. Chinese Science Bulletin, 55(13): 1255-1267 (in Chinese)
[16] Li CD, Zhang Q, Miao CL and Meng XF. 2004. Geochemistry, genesis and mineralization of Mesozoic high Sr-low Y and low Sr-low Y type granite in North Hebei. Acta Petrologica Sinica, 20(2): 269-284 (in Chinese with English abstract)
[17] Li DM. 2012. Genesis of adakite in Maozang temple from North Qilian area. Chinese Journal of Geology, 47(2): 347-359 (in Chinese with English abstract)
[18] Liu HT, Zhao MG, Liu JM and Sun SH. 2002. Mesozoic granite on the north margin of North China craton: Evidence from post collisional to anorogenic. Acta Petrologica Sinica, 18(4): 433-448 (in Chinese with English abstract)
[19] Liu QS, Gao S and Li YS. 2000. Magnetic structure of the continental crust as revealed by the Wutai-Jining crustal cross-section in the North China craton. Journal of Geodynamics, 29(1-2): 1-13
[20] Lonov DA, Priknodko VS and O'Reilly SY. 1995. Peridotite xenoliths in alkali basalts from the Sikhote-Alin, southeastern Siberia, Russia: Trace element signatures of mantle beneath a convergent continental margin. Chemical Geology, 120(3-4): 275-294
[21] Lu LZ and Lin Q. 2004. Petrogenesis of Rock. Changchun: Jinlin University Press (in Chinese)
[22] Ludwig KR. 2003. Isoplot 3.00: A Geochronological Toolkit for Microsoft Excel. Berkeley, California: Berkeley Geochronology Center
[23] Ma CQ, Li ZC, Ehlers C, Yang KG and Wang RJ. 1998. A post-collisional magmatic plumbing system: Mesozoic granitoid plutons from the Dabieshan high-pressure and ultrahigh-pressure metamorphic zone, east-central China. Lithos, 45(1-4): 431-456
[24] Ma CQ, Yu ZB, Zhang JY and Zhang C. 2006. Crustal root, orogenic heat and magmatism. Earth Science Frontiers, 13(2): 130-138 (in Chinese with English abstract)
[25] Macpherson CG, Dreher ST and Thirwall MF. 2006. Adakites without slab melting: High pressure processing of island arc magma, Mindanao, the Philippines. Earth Planet. Sci. Lett., 243(3-4): 581-593
[26] Martin H. 1995. The Archean grey gneisses and the genesis of the continental crust. In: Condie KC (ed.). The Archean Crustal Evolution. Amsterdam: Elsevier, 205-259
[27] Martin H. 1999. Adakite magmas: Modern analogues of Archaean granitoids. Lithos, 46(3): 411-429
[28] Martin H, Smiithies RH, Rapp R, Moyen JF and Champion D. 2005. An overview of adakite, tonalite-trondhjemite-granodiorite (TTG), and sanukitoid: Relationships and some implications for crustal evolution. Lithos, 79(1-2): 1-24
[29] Moyen JF. 2009. High Sr/Y and La/Yb ratios: The mean of the adakite signature. Lithos, 112(3-4): 556-574
[30] Pitcher WS. 1978. The anatomy of a batholith: President's anniversary address 1977. J. Geol. Soc., 135(2): 157-182
[31] Qian Q. 1998. Geodynamic environment of mafic and acidic suite. Earth Science Frontier, 5(3): 104-105 (in Chinese with English abstract)
[32] Qian Q, Zhong SL, Li TY and Wen DR. 2002. Genesis discussion and geochemical characteristics of Badaling basic rock and high Ba-Sr granite: Comparion among Mesozoic magmatic rocks from Huabei and Dabie area. Acta Petrologica Sinica, 18(3): 275-292 (in Chinese with English abstract)
[33] Qin HP, Wu CL, Wu XP, Lei M and Hou ZH. 2012. Zircon Lu-Hf isotopic characteristics and genesis of high Sr granite in Mangling area of Qinling Orogenic belt. Journal of Jinlin University (Earth Science Edition), (S1): 254-264 (in Chinese with English abstract)
[34] Rapp RP, Watson EB and Miller CF. 1991. Partial melting of amphibolite/eclogite and the origin of Archaean trondhjemites and tonalities. Precambrian Research, 51(1-4): 1-25
[35] Rapp RP, Shimizu N and Norman MD. 2003. Growth of early continental crust by partial melting of eclogite. Nature, 425(6958): 605-609
[36] Rubatto D and Gebauer D. 2000. Use of cathodoluminescence for U-Pb zircon dating by IOM Microprobe: Some examples from the western Alps. In: Pagel M, Barbin V, Blanc P and Ohnenstetter D (eds.). Cathodoluminescence in Geosciences. Berlin Heidelberg, Germany: Springer-Verlag, 373-400
[37] Song SG, Zhang LF, Niu YL, Song B and Liu DY. 2004. Tectonic evolution and continental subduction of Paleozoic plate in north margin of Tibet Plateau. Geological Bulletin of China, 23(9): 918-925 (in Chinese with English abstract)
[38] Song SG, Zhang LF, Niu YL, Su L, Song B and Liu DY. 2006. Evolution from oceanic subduction to continental collision: A case study from the Northern Tibetan Plateau based on geochemical and geochronological data. J. Petrol., 47(3): 435-455
[39] Song SG. 2009. Review of high pressure metamorphic in oceanic subduction zone of North Qilian. Geological Bulletin of China, 28(12): 1769-1778 (in Chinese with English abstract)
[40] Song SG, Li SG, Li XH, Niu YL and Zhang LF. 2012. Grenville-age orogenesis in the Qaidam-Qilian Block: The link between South China and Tarim. Precambrian Research, 220-221: 9-22
[41] Su JP, Zhang XH, Hu NG, Fu GM and Zhang HF. 2004. Geochemical characteristics and genesis of adakite in Yemananshan area, west section of Middle Qilian. Geology in China, 31(4): 365-371 (in Chinese with English abstract)
[42] Sun SS and McDonough WF. 1989. Chemical and isotopic systematics of oceanic basalts: Implications for mantle composition and processes. In: Saunders AD and Norry MJ (eds.). Magmatism in Oceanic Basins. Geological Society, London, Special Publications, 42(1): 313-345
[43] Tarney J and Jones CE. 1994. Trace element geochemistry of orogenic igneous rocks and crustal growth. J. Geol. Soc., 151(5): 855-868
[44] Tseng CY, Yang HY, Wan YS, Liu DY, Wen DJ, Lin TC and Tung KA. 2006. Finding of Neoproterozoic (~775Ma) magmatism recorded in metamorphic complexes from the North Qilian orogen: Evidence from SHRIMP zircon U-Pb dating. Chinese Science Bulletin, 51(8): 963-970
[45] Turner S, Arnaud N, Liu J, Rogers N, Hawkesworth C, Harris N, Kelley S, Van Calsteren P and Deng W. 1996. Post-collision, shoshonitic volcanism on the Tibetan Plateau: Implications for convective thinning of the lithosphere and the source of ocean island basalts. Journal of Petrology, 37(1): 45-71
[46] Wang FC, Wang SS, Li TD, Cai XJ and Zhao L. 2011. Preliminary study of granite classification and mineralization in Qilian area. Acta Petrologica Sinica, 27(12): 3823-3830 (in Chinese with English abstract)
[47] Wang JR, Guo YS, Fu SM, Chen JL, Qin XF, Zhang HP and Yang YJ. 2005. Discovery of Early Paleozoic adakite and its tectonic significance in Heishi mountain, Gansu Province. Acta Petrologica Sinica, 21(3): 977-985 (in Chinese with English abstract)
[48] Wang JR, Wu CJ, Cai ZH, Guo YS, Wu JC and Liu XH. 2006. Geodynamic and mineralization significance of high adakite in Yindongliang, east section of North Qilian area. Acta Petrologica Sinica, 22(11): 2655-2664 (in Chinese with English abstract)
[49] Wang JR, Wu JC and Jia ZL. 2008. Geodynamic implication of high Mg adakite in Sujiashan area, east section of North Qilian. Journal of Lanzhou University, 44(3): 16-22 (in Chinese with English abstract)
[50] Wang Q, Zhao ZH and Xiong XL. 2001. Melt of underplating basaltic lower crust: Evidence from Na enriched quartz diorite porphyrite in Shaxi, Anhui Provence. Geochimica, 30(4): 353-362 (in Chinese with English abstract)
[51] Wang Q, Zhao ZH, Bai ZH, Xiong XL, Yang HJ, Xu JF, Bao ZW and Wang YX. 2003. Carboniferous adakite and Nb enriched arc basalt in Alataoshan area, Xinjiang Province: Crustal plate melt and mantle peridotite interaction growth. Chinese Science Bulletin, 48(12): 1312-1349 (in Chinese)
[52] Wang Y and Cheng SH. 2007. Genesis relationship between partial melting of dry eclogite and petrogenesis of C type adakite. Geological Review, 53(2): 198-206 (in Chinese with English abstract)
[53] Wang Y and Cheng SH. 2009. Discussion on relationship between C type adakite and mineralization in eastern China. Acta Mineralogica Sinica, 29(Suppl.1): 27-28 (in Chinese with English abstract)
[54] Wang Y and Cheng SH. 2010. C type adakite: Based on a misunderstanding concept? Bulletin of Mineralogy, Petrology and Geochemistry, 29(3): 284-292 (in Chinese with English abstract)
[55] Winther TK and Newton RC. 1991. Experimental melting of anhydrous low-K tholeiite: Evidence on the origin of Archaean cratons. Bull. Geol. Soc. Den., 39: 213-228
[56] Wu CL, Yao SZ, Yang JS, Zeng LS, Chen SY, Li HB, Qi XX, Wooden JL and Mazdab FK. 2006. Paleozoic granite evidence of double direction subduction in North Qilian. Geology in China, 33(6): 1197-1208 (in Chinese with English abstract)
[57] Wu CL, Xu XY, Gao QM, Li XM, Lei M, Gao YH, Frost RB and Wooden JL. 2010. Magmatism and tectonic evolution of Early Paleozoic granite of North Qilian. Acta Petrologica Sinica, 26 (4):1027-1044 (in Chinese with English abstract)
[58] Wu CL, Gao YH, Frost BR, Robinson PT, Wooden JL, Wu SP, Chen QL and Lei M. 2011. An Early Paleozoic double-subduction model for the North Qilian oceanic plate: Evidence from zircon SHRIMP dating of granites. International Geology Review, 53(2): 157-181
[59] Wu FY, Li XH, Yang JH and Zheng YF. 2007. Preliminary study on the origin of granite. Acta Petrologica Sinica, 23(6):1217-1238 (in Chinese with English abstract)
[60] Wu YB and Zheng YF. 2004. Zircon genesis and its constraints on interpretation of U-Pb age. Chinese Science Bulletin, 49(16): 1589-1601 (in Chinese)
[61] Xia LQ, Xia ZC and Xu XY. 1996. Genesis of Marine Facies Volcano Rock. Beijing: Geological Publishing House (in Chinese with English abstract)
[62] Xiong XL, Adam J and Green TH. 2005. Rutile stability and rutile/melt HFSE partitioning during partial melting of hydrous basalt: Implications for TTG genesis. Chem. Geol., 218(3-4): 339-359
[63] Xiong XL, Liu XC, Zhu ZM, Li Y, Xiao WS, Song MS, Zhang X and Wu JH. 2011. Adakite and craton destruction of North China: Basis on experimental petrology and geochemistry. Science in China (series D), 41(5): 654-667 (in Chinese)
[64] Xu WL, Wang QH, Wang DY, Guo JH and Pei FP. 2006. Mesozoic adakitic rocks from the Xuzhou-Suzhou area, eastern China: Evidence for partial melting of delaminated lower continental crust. J. Asian Earth Sci., 27(4): 454-464
[65] Yu FS, Qi JF, Wang CY and Zhang J. 2001. Geological characteristic and forming environment of Neoproterozoic volcano rocks in eastern section of North Qilian area. Geotectonica et Metallogenia, 25(1): 74-82 (in Chinese with English abstract)
[66] Yu FS, Wang CY and Du GM. 2002. Geochronological evidence of Neoprotereozoic volcano rock in eastern section of North Qilian. Geology in China, 29(4): 360-363 (in Chinese with English abstract)
[67] Zhang HF, Zhai MG, He ZF, Peng P and Xu BL. 2004. Geochemical significance of high Sr granite in Kunyu mountain of Jiaodong area. Acta Petrologica Sinica, 20(3): 369-379 (in Chinese with English abstract)
[68] Zhang HF, Zhai MG, Tong Y, Peng P, Xu BL and Guo JH. 2006. Genesis of high Ba-Sr granite in Sanfoshan area of Jiaodong. Geological Review, 52(1): 43-51 (in Chinese with English abstract)
[69] Zhang Q, Qian Q, Wang EQ, Wang Y, Zhao TP, Hao J and Guo GJ. 2001. Eastern plateau of China in Late Yanshan period: Implication from adakite. Chinese Journal of Geology, 36(2): 248-255 (in Chinese with English abstract)
[70] Zhang Q, Wang Y and Wang YL. 2003. Adakite and tectonic environment. Geotectonica et Metallogenia, 27(2):101-108 (in Chinese with English abstract)
[71] Zhang Q, Wang Y, Li CD, Jin WJ and Jia XQ. 2006a. Granite classification based on pressure. Geological Bulletin of China, 25(11):1274-1278 (in Chinese with English abstract)
[72] Zhang Q, Wang Y, Li CD, Wang YL, Jin WJ and Jia XQ. 2006b. Sr-Yb classification of granite and its geological significance. Acta Petrologica Sinica, 22(9): 2249-2269 (in Chinese with English abstract)
[73] Zhang Q. 2008. Review and prospect on adakite research. Geology in China, 35(1): 33-39 (in Chinese with English abstract)
[74] Zhang Q, Jin WJ, Li CD and Wang YL. 2010. Third discussion on Sr-Yb classification of granite: Application. Acta Petrologica Sinica, 26(12): 3431-3455 (in Chinese with English abstract)
[75] Zhang Q, Jin WJ, Li CD, Wang Y and Wang YL. 2011. Discussion on relationship between granite and crustal thickness. Geotectonica et Metallogenia, 35(2): 259-269 (in Chinese with English abstract)
[76] Zheng YF, Wu YB, Chen FK, Gong B, Li L and Zhao ZF. 2004. Zircon U-Pb and oxygen isotope evidence for a large-scale 18O depletion event in igneous rocks during the Neoproterozoic. Geochimica et Cosmochimica Acta, 68(20): 4145-4165
[77] Castillo PR. 2006. 埃达克岩成因回顾. 科学通报, 51(6): 617-627
[78] 陈斌, 翟明国, 邵济安. 2002. 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),32(11):896-907
[79] 陈其龙. 2009. 北祁连牛心山岩体岩石学、锆石SHRIMP定年及其成因. 硕士学位论文. 北京: 首都师范大学
[80] 陈育晓, 夏小洪, 宋述光. 2012. 北祁连山西段志留纪高硅埃达克岩: 洋壳减压熔融的证据. 科学通报, 57(22): 2072-2085
[81] 邓晋福, 莫宣学, 赵海玲, 罗照华. 1996. 中国大陆根-柱构造——大陆动力学的钥匙. 北京: 地质出版社
[82] 马昌前, 佘振兵, 张金阳, 张超. 2006. 地壳根、造山热与岩浆作用. 地学前缘, 13(2): 130-138
[83] 郭进京, 陆松年. 1999. 中国新元古代大陆拼合与Rodinia超大陆. 高校地质学报, 5(2): 148-156
[84] 黄方, 何永胜. 2010. 干的基性大陆下地壳部分熔融: 对C型埃达克岩成因的制约. 科学通报, 55(13): 1255-1267
[85] 李承东, 张旗, 苗来成, 孟宪锋. 2004. 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, 20(2): 269-284
[86] 李大民. 2012. 甘肃北祁连毛藏寺埃达克岩及其成因类型. 地质科学, 47(2): 347-359
[87] 刘红涛, 翟明国, 刘建明, 孙世华. 2002. 华北克拉通北缘中生代花岗岩: 从碰撞后到非造山. 岩石学报, 18(4): 433-448
[88] 卢良兆, 林强. 2004. 成因岩石学. 长春: 吉林大学出版社
[89] 钱青. 1998. 双峰式火山岩套形成的地球动力学环境. 地学前缘, 5(3): 104-105
[90] 钱青, 钟孙霖, 李通艺, 温大任. 2002. 八达岭基性岩和高Ba-Sr花岗岩地球化学特征及成因探讨: 华北和大别-苏鲁造山带中生代岩浆岩的对比. 岩石学报, 18(3): 275-292
[91] 秦海鹏, 吴才来, 武秀萍, 雷敏, 侯振辉. 2012. 秦岭蟒岭高Sr花岗岩的锆石Lu-Hf同位素特征及其成因. 吉林大学学报(地球科学版), (S1): 254-264
[92] 宋述光, 张立飞, 牛耀龄, 宋彪, 刘敦一. 2004. 青藏高原北缘早古生代板块构造演化和大陆俯冲. 地质通报, 23(9): 918-925
[93] 宋述光. 2009. 北祁连山古大洋俯冲带高压变质岩研究评述. 地质通报, 28(12): 1769-1778
[94] 苏建平, 张新虎, 胡能高, 付国民, 张海峰. 2004. 中祁连西段野马南山埃达克质花岗岩的地球化学特征及成因. 中国地质, 31(4): 365-371
[95] 王方成, 汪双双, 李泰德, 蔡晓菊, 赵磊. 2011. 祁连山花岗岩分类及找矿方向初探. 岩石学报, 27(12): 3823-3830
[96] 王金荣, 郭原生, 付善明, 陈建林, 秦秀峰, 张洪培, 杨永均. 2005. 甘肃黑石山早古生代埃达克质岩的发现及其构造动力学意义. 岩石学报, 21(3): 977-985
[97] 王金荣, 吴春俊, 蔡郑红, 郭原生, 吴继承, 刘晓煌. 2006. 北祁连山东段银硐粱早古生代高镁埃达克岩: 地球动力学及成矿意义. 岩石学报, 22(11): 2655-2664
[98] 王金荣, 吴继承, 贾志磊. 2008. 北祁连山东段苏家山高Mg埃达克岩地球动力学意义. 兰州大学学报(自然科学版), 44(3): 16-22
[99] 王强, 赵振华, 熊小林. 2001. 底侵玄武质下地壳的熔融: 来自安徽沙溪埃达克质富钠石英闪长玢岩的证据. 地球化学, 30(4): 353-362
[100] 王强, 赵振华, 白正华, 熊小林, 杨厚钧, 许继峰, 包志伟, 王一先. 2003. 新疆阿拉套山石炭纪埃达克岩、富Nb岛弧玄武质岩: 板片熔体与地幔橄榄岩相互作用及地壳生长. 科学通报, 48(12): 1342-1349
[101] 汪洋, 程素华. 2007. 干的榴辉岩部分熔融与C型埃达克岩成因的关系. 地质论评, 53(2): 198-206
[102] 汪洋, 程素华. 2009. 浅议"C型埃达克岩"与中国东部中生代金属成矿作用的关系. 矿物学报, 29(S1): 27-28
[103] 汪洋, 程素华. 2010. "C型埃达克岩": 一个基于误解的概念？矿物岩石地球化学通报, 29(3): 284-292
[104] 吴才来, 姚尚志, 杨经绥, 曾令森, 陈松永, 李海兵, 戚学祥, Wooden JL, Mazdab FK. 2006. 北祁连洋早古生代双向俯冲的花岗岩证据. 中国地质, 33(6): 1197-1208
[105] 吴才来, 徐学义, 高前明, 李向民, 雷敏, 郜源红, Frost RB, Wooden JL. 2010. 北祁连早古生代花岗质岩浆作用及构造演化. 岩石学报, 26(4): 1027-1044
[106] 吴福元, 李献华, 杨进辉, 郑永飞. 2007. 花岗岩成因研究的若干问题. 岩石学报, 23(6): 1217-1238
[107] 吴元保, 郑永飞. 2004. 锆石成因矿物学研究及其对U-Pb年龄解释的制约. 科学通报, 49(16): 1589-1601
[108] 夏林圻, 夏祖春, 徐学义. 1996. 北祁连山海相火山岩岩石成因. 北京: 地质出版社
[109] 熊小林, 刘星成, 朱志敏, 朱志敏, 李元, 肖万生, 宋茂双, 张生, 吴金花. 2011. 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. 中国科学(D辑), 41(5): 654-667
[110] 于福生, 漆家福, 王春英, 张军. 2001. 北祁连东段新元古代火山岩的发现及其特征和形成环境. 大地构造与成矿学, 25(1): 74-82
[111] 于福生, 王春英, 杜国民. 2002. 北祁连山东段新元古代火山岩的年代学证据. 中国地质, 29(4): 360-363
[112] 张华锋, 翟明国, 何中甫, 彭澎, 许保良. 2004. 胶东昆嵛山杂岩中高锶花岗岩地球化学成因及其意义. 岩石学报, 20(3): 369-379
[113] 张华锋, 翟明国, 童英, 彭澎, 许保良, 郭敬辉. 2006. 胶东半岛三佛山高Ba-Sr花岗岩成因. 地质论评, 52(1): 43-51
[114] 张旗, 钱青, 王二七, 王焰, 赵太平, 郝杰, 郭光军. 2001. 燕山中晚期的中国东部高原: 埃达克岩的启示. 地质科学, 36(2): 248-255
[115] 张旗, 王焰, 王元龙. 2003. 埃达克岩与构造环境. 大地构造与成矿学, 27(2): 101-108
[116] 张旗, 王焰, 李承东, 金惟俊, 贾秀勤. 2006a. 花岗岩按照压力的分类. 地质通报, 25(11): 1274-1278
[117] 张旗, 王焰, 李承东, 王元龙, 金惟俊, 贾秀勤. 2006b. 花岗岩的Sr-Yb分类及其地质意义. 岩石学报, 22(9): 2249-2269
[118] 张旗. 2008. 埃达克岩研究的回顾和前瞻. 中国地质, 35(1): 33-39
[119] 张旗, 金惟俊, 李承东, 王元龙. 2010. 三论花岗岩按照Sr-Yb的分类: 应用. 岩石学报, 26(12): 3431-3455
[120] 张旗, 金惟俊, 李承东, 王焰, 王元龙. 2011. 花岗岩与地壳厚度关系探讨. 大地构造与成矿学, 35(2): 259-269
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