阿尔金环形山花岗片麻岩同位素年龄及成因研究
Isotopic age and genesis of the monzogranitic gneiss at the Huanxingshan in middle Altyn Tagh
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摘要: 阿尔金中段环形山二长花岗片麻岩LA-ICP-MS锆石U-Pb年龄为928±9Ma。岩石SiO2含量为72.26%~74.34%,全碱(Na2O＋K2O)为7.22%~8.32%,Al2O3含量为12.40%~13.51%,含量较高;MgO为0.43%~1.07%,FeOT为2.09%~2.43%,CaO为1.02%~2.03%,TiO2为0.19%~0.32%,含量较低。岩石FeOT/MgO比值为2.28~4.87和Al2O3/TiO2比值为40.4~69.0(均小于100)、CaO/Na2O比值为0.46~1.06(大于0.30)、K2O/Na2O比值为2.10~3.43(大于1),富集大离子亲石元素Rb、Th、K及La等,亏损Ba、Ta、Nb、Sr、P、Ti,Th/U比值为5.17~14.7、Zr/Hf比值为30.3~34.3,ΣREE总量平均为193×10-6,(La/Yb)N为3.89~5.00(小于10),δEu#值(平均值36.2),具有负Eu异常,显示其源岩区与泥质岩、基性岩的关系不大;0.4Abstract: The LA-ICP-MS zircon U-Pb isotopic dating on the Huanxingshan monzogranitic gneiss from the middle Altyn Tagh reveals a U-Pb mean age of 928±9Ma, which approximately represents the intrusive age of the granitic. Geochemical characteristics of major elements exhibit the granite with high SiO2 (72.26%~74.34%), Na2O+K2O (7.22%~8.32%) and Al2O3 (12.40%~13.51%) contents, and low MgO (0.43%~1.07%), FeOT (2.09%~2.43%), CaO (1.02%~2.03%) and TiO2 (0.19%~0.32%) contents. FeOT/MgO (2.28~4.87) and Al2O3/TiO2 (40.4~69.0) ratios are less than 100, while CaO/Na2O (0.46~1.06) and K2O/Na2O (2.10~3.43) ratios are more than 0.3 and 1, respectively. These characteristics are similar to values of typical S-type granite. Th/U and Zr/Hf are 5.17~14.7, 30.3~34.3. Additionally, the granitic gneisses are characterized by relative enrichment in Rb, Th, K, La, and depletion in Ba, Ta, Nb, Sr, P and Ti, which indicate monzogranitic gneiss may be product of Partial melting of sedimentary rocks. All the samples are slightly enriched in LREE with (La/Yb)N ratios ranging from 3.89 to 5.00 (less than 10). In the chondrite normalized REE patterns, all the granitic gneiss show clear negative Eu abnormalies (δEu# (36.2, in average), Sr/Ba (0.12~0.20) ratios and Eu depletion indicate that the primary magma was derived from partial melting of greywacke rather than muddy rock and basic rock, under temperature of ca.789~803℃ and pressure 0.8~1.6GPa. Based on all above element and isotope geochemistry, it is reasonably suggested that the Huanxingshan granite in Altyn Tagh was formed in a syn-collision tectonic setting at Early Neoproterozoic era.
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Key words:
- Isotopic chronology /
- Geochemistry /
- Monzogranitic gneiss /
- Altyn Tagh
[1] Alther R, Holl A, Hegner E, Langer C and Kreuzer H. 2000. High-potassium, calc-alkaline I-type plutonism in the European Variscides: Northern Vosges (France) and northern Schwarzwald (Germany). Lithos, 50(1-3): 51-73
[2] Anderson JL. 1996. Status of thermobarometry in granitic batholiths. Transactions of the Royal Society of Edinburgh: Earth Sciences, 87(1-2): 125-138
[3] Andersen T. 2002. Correction of common lead in U-Pb analyses that do not report 204Pb. Chem. Geol., 192(1-2): 59-79
[4] Barth MG, McDonough WF and Rndnick RI. 2000. Tracking the budget of Nb and Ta in the continental crust. Chem. Geol., 165(3-4): 197-213
[5] Batchelor RA and Bowden P. 1985. Petrogenietic interpretation of granitiod rock series using multicationic paramelters. Chem. Geol., 48(1-4): 43-55
[6] Belousova EA, griffiu WL and O'Reilly SY. 2006. Zircon crystal morphology, trace element signatures and Hf isotope compositions, a tool for petrogenetic modelong: Examples from eastern Australian granitoids. J. Petrol., 47: 329-353
[7] Calvin FM, McDowell SM and Mapes RW. 2003. Hot and cold granites implications of zircon saturation temperatures and preservation of inheritance. Geology, 31(6): 529-532
[8] Cao YT, Liu L, Wang C, Yang WQ and Zhu XH. 2010. Geochemical, zircon U-Pb dating and Hf isotope compositions studies for Tatelekebulake granite in South Altyn Tagh. Acta Petrologica Sinica, 26(11): 3259-3271 (in Chinese with English abstract)
[9] Castillo PR. 2006. An overview of adakite petrogenesis. Chinese Science Bulletin, 51(3): 257-268
[10] Che ZC, Liu L, Luo JH et al. 1995. Discovery and occurrence of high pressure metapelitic rocks from Altun Mountain areas, Xinjiang Autonomous Region. Chinese Science Bulletin, 40(14): 1298-1300 (in Chinese)
[11] Che ZC, Liu L and Luo JH. 2002. Regional Tectonics of China and Its Adjacent Areas. Beijing: Science Press, 354-386 (in Chinese)
[12] Defant MJ and Drummond MS. 1990. Derivation of some modern arc magmas by melting of young subducted lithosphere. Nature, 347(6294): 662-665
[13] Dostal J and Chatterjee AK. 2000. Contrasting behaviour of Nb/Ta and Zr/Hf ratios in a peraluminous granitic pluton Nova Scotia, Canada. Chem. Geol., 163(1-4): 207-218
[14] Ferry JM and Watson EB. 2007. New thermodynamic models and revised calibrations for the Ti-in-zircon and Zr-in-rutile thermometers. Contributions to Mineralogy and Petrology, 154(4): 429-437
[15] Gao S, Luo TC, Zhang BR, Zhang HF, Han YW, Zhao ZD and Hu YK. 1998. Chemical composition of the continental crust as revealed by studies in East China. Geochimica et Cosmochimica Acta, 62(11): 1959-1975
[16] Gehrels GE, Yin A and Wang XF. 2003. Magmatic history of the northeastern Tibetan Plateau. Journal of Geophysical Research, 108(B9): doi: 10.1029/2002JB001876
[17] Guo JJ, Zhao FQ and Li HK. 1999. Jinningian collisional granite belt in the eastern sector of the Central Qilian massif and its implication. Acta Geoscientia Sinica, 20(1): 10-15 (in Chinese with English abstract)
[18] Harris NBW and Inger S. 1992. Trace element modelling of pelite-derived granites. Contributions to Mineralogy and Petrology, 110(1): 46-56
[19] Hermann LM, Bowins R and Crocket J. 1990. The chemical composition of igneous zircon suites: Implications for geochemical tracer studies. Geochimica et Cosmochimica Acta, 54(6): 1597-1607
[20] Hoskin PWO and Schaltegger U. 2003. The composition of zircon and igneous and metamorphic petrogenesis. Reviews in Mineralogy and Geochemistry, 53(1): 27-62
[21] Kang L, Liu L, Cao YT, Wang C, Yang WQ and Liang S. 2013. Geochemistry, zircon U-Pb age and its geological significance of the gneissic granite from the eastern segment of the Tatelekebulake composite granite in the south Altyn Tagh. Acta Petrologica Sinica, 29(9): 3039-3048 (in Chinese with English abstract)
[22] Li HK, Lu SN, Zhao FQ, Li HM, Yu HF and Zheng JK. 1999a. Geochronological framework of the Neoproterozoic major geological events in the northern margin of the Qaidam basin. Geoscience, 13(2): 224-225 (in Chinese with English abstract)
[23] Li HK, Lu SN, Zhao FQ, Yu HF and Zheng JK. 1999b. Determination and significance of the coesite eclogite on the Yuqia River on the north margin of the Qaidam basin. Geoscience, 13(1): 43-49 (in Chinese with English abstract)
[24] Liu L, Che ZC, Luo JH, Wang Y and Gao JZ. 1996. Recognition and implication of eclogite in the western Altun Mountains, Xinjiang. Chinese Science Bulletin, 41(14): 1458-1488 (in Chinese)
[25] Liu L, Che ZC, Wang Y, Luo JH and Chen DL. 1999. The petrological character and geotectonic setting of high Pressure metamorphic rock belts in Altun Mountains. Acta Petrologica Sinica, 15(1):57-64 (in Chinese with English abstract)
[26] Liu L, Sun Y, Che ZC, Luo JH, Chen DL, Wang Y, Zhang AD, Chen L, Xiao PX and Wang YH. 2002. Discovery of ultra-high pressure magnesite bearing garnet Iherzolite (>3.8GPa) in the Altyn Tagh, Northwest China. Chinese Science Bulletin, 47(9): 657-662 (in Chinese)
[27] Liu L, Sun Y, Luo JH, Wang Y, Chen DL and Zhang AD. 2003. Ultra-high pressure metamorphism of granitic gneiss in the Yinggelisayi area, Altun Mountains, NW China. Science in China (Series D), 33(12): 1184-1192 (in Chinese)
[28] Liu L, Wang C, Cao YT, Chen DL, Kang L, Yang WQ and Zhu XH. 2012. Geochronology of multi-stage metamorphic events: Constraints on episodic zircon growth from the UHP eclogite in the South Altyn, NW China. Lithos, 136-139: 10-26
[29] Liu XM, Yuan HL, Hattendorf B, Günther D, Chen L and Hu SH. 2002. Analysis of 42 major and trace elements in glass standard reference materials by 193nm La-ICPMS. Acta Petrologica Sinica, 18(3): 408-418 (in Chinese with English abstract)
[30] Liu YS, Yu HF, Xin HT, Lu SN, Xiu QY and Li Q. 2009. Tectonic units division and Precambrian significant geological events in Altyn Tagh Mountain, China. Geological Bulletin of China, 28(10): 1430-1438 (in Chinese with English abstract)
[31] Lu FX and Sang LK. 2002. Petrology. Beijing: Geological Publishing House, 82-94 (in Chinese)
[32] Lu SN. 1998. A review of advance in the research on the Neoproterozoic Rodinia supercontinent. Geological Review, 44(5): 489-495 (in Chinese with English abstract)
[33] Lu SN. 2002. Preliminary Study of Precambrian Geology in the North Tibet Qinghai Plateau. Beijing: Geological Publishing House, 35-117 (in Chinese)
[34] Lu YF. 2004. GeoKit: A geochemical toolkit for Microsoft Excel. Geochimica, 33(5): 459-464 (in Chinese with English abstract)
[35] Mei HL, Li HM, Lu SN, Yu HF, Zuo YC and Li C. 1999. The age and origin of the Liuyuan granitoid, northwestern Gansu. Acta Petrologica et Mineralogica, 18(1): 14-17 (in Chinese with English abstract)
[36] Maniar PD and Piccoli PM. 1989. Tectonic discrimination of granitoids. Geological Society of America Bulletin, 101(5): 635-643
[37] Pearce JA, Harris NBW and Andrew GT. 1984. Trace element discrimination diagrams for the tectonic interpretation of granitic rocks. Journal of Petrology, 25(4): 959-983
[38] 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
[39] Rickwood PC. 1989. Boundary lines within petrologic diagrams which use oxides of major and minor elements. Lithos, 22(4): 247-263
[40] Rubatto D. 2002. Zircon trace element geochemistry: Partitioning with garnet and the link between U-Pb ages and metamorphism. Chemical Geology, 184(1-2): 123-138
[41] Rudnick RL and Fountain DM. 1995. Natureand composition of the continental crust: A lower crustal perspective. Rev. Geophys., 33(3): 267-309
[42] Song SG, Su L, 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
[43] Sun JM, Ma ZP, Tang Z and Li XM. 2012. LA-ICP-MS zircon dating of the Yumuquan magma mixing granite in the southern Altyn Tagh and its tectonic significance. Acta Geologica Sinica, 86(2): 247-257 (in Chinese with English abstract)
[44] 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 the Ocean Basins. Geological Society, London, Special Publications, 42(1): 313-345
[45] Sylverster PJ. 1998. Post-collisional strongly peraluminous granites. Lithos, 45(1-4): 29-44
[46] Taylor SR and Mclemann SM. 1985. The Continental Crust: Its Composition of Melts and Evolution. Blackwell: Oxford Press, 1-312
[47] Turner G, Harrison TM, Holland G, Moizsis SJ and Gilmour J. 2004. Extinct 244Pu in ancient zircons. Science, 306(5693): 89-91
[48] Vavra G, Gebauer D, Schmid R and Compston W. 1996. Multiple zircon growth and recrystallization during polyphase Late Carboniferous to Triassic metamorphism in granulites of the Ivrea Zone (SouthernAlps): An ion microprobe (SHRIMP) study. Contrib. Mineral Petrol., 122(4): 337-358
[49] Vavra G, Schmid R and Gebauer D. 1999. Internal morphology, habit and U-Th-Pb microanalysis of amphibolites togranulite facies zircons: Geochronology of the Ivrea Zone (SouthernAlps). Contrib. Mineral. Petrol., 134(4): 380-404
[50] Wang C, Liu L, Che ZC, Chen DL, Zhang AD and Luo JH. 2006. U-Pb Geochronology and tectonic setting of the granitic gneiss in Jianggaleisayi eclogite belt, the southern edge of Altyn Tagh. Geological Journal of China Universities, 12(1): 74-82 (in Chinese with English abstract)
[51] Wang C, Liu L, Zhang AD, Yang WQ and Cao YT. 2008. Geochemistry and petrography of Early Paleozoic Yusupuleke Tagh rapakivi-textured granite complex, South Altyn: An example for magma mixing. Acta Petrologica Sinica, 24(12): 2809-2819 (in Chinese with English abstract)
[52] Wang C, Liu L, Yang WQ, Zhu XH, Cao YT, Kang L, Chen SF, Li RS and He SP. 2013. Provenance and ages of the Altyn complex in Altyn Tagh: Implications for the Early Neoproterozoic evolution of northwestern China. Precambrian Research, 230: 193-208
[53] Wang ZG, Yu XY and Zhao ZH. 1989. Rare Earth Element Geochemistry. Beijing: Science Press, 223-224 (in Chinese)
[54] Watson EB and Harrison TM. 1983. Zircon saturation revisited: Temperature and composition effects in a variety of crustal magma types. Earth and Planetary Science Letters, 64(2): 295-304
[55] Watson EB, Wark DA and Thomas JB. 2006. Crystallization thermometers for zircon and rutile. Contributions to Mineralogy and Petrology, 151(4): 413-433
[56] Whitehouse MJ and Platt JP. 2003. Dating high-grade metamorphism: Constraints from rare-earth elements in zircon and garnet. Contrib. Mineral. Petrol., 145(1): 61-74
[57] Wilde SA, Vallev JW, Peck WH and Graham CM. 2001. Evidence from detrital zircons for the existence of continental crust and oceans on the Earth 4.4Ga ago. Nature, 409(6817): 175-178
[58] Wright JB. 1969. A simple alkalinity ratio and its application to questions of non-orogenic granite genesis. Geological Magazine, 106(4): 370-384
[59] Wu FY, Li XH, Yang JH and Zheng YF. 2007. Discussions on the petrogenesis of granites. Acta Petrologica Sinica, 23(6): 1217-1238 (in Chinese with English abstract)
[60] Wu LR. 1985. Mesozoic granites in East China. Acta Petrologica Sinica, 1(1): 1-10 (in Chinese with English abstract)
[61] Wu SP, Wu CL and Chen QL. 2007. Characteristics and tectonic setting of the Tula aluminous A-type granite at the south side of the Altyn Tagh fault, NW China. Geological Bulletin of China, 26(10): 1385-1392 (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. Chemical Geology, 218(3-4): 339-359
[63] Yang DB, Xu WL, Wang QH, Pei FP and Ji WQ. 2006. Petrogenesis of Late Jurassic Jingshan granite in Bengbu uplift, Anhui Province: Constraints from geochemistry and Hf isotope of zircons. Acta Petrologica Sinica, 22(12): 2923-2932 (in Chinese with English abstract)
[64] Yang JS, Xu ZQ, Li HB, Wu CL, Cui JW, Zhang JX and Chen W. 1998. Discovery of eclogite in the North Qaidam Mountain in West China. Chinese Science Bulletin, 43(14): 1544-1549 (in Chinese)
[65] Yang WQ, Liu L, Ding HB, Xiao PX, Cao YT and Kang L. 2012. Geochemistry, geochronology and zircon Hf isotopes of the Dimunalike granite in South Altyn Tagn and its geological significance. Acta Petrologica Sinica, 28(12): 4139-4150 (in Chinese with English abstract)
[66] Yu HF, Lu SN, Mei HL, Zhao FQ, Li HK and Li HM. 1999. Characteristics of Neo-proterozoic eclogite granite zones and deep level ductile shear zone in western China and their significance for continental reconstruction. Acta Petrologica Sinica, 15(4): 532-538 (in Chinese with English abstract)
[67] Yu HF, Lu SN, Liu YS, Xiu QY and Li Q. 2002. Composition of the Altyn Tagh formation-complex and its tectonic signification. Geological Bulletin of China, 21(12): 834-840 (in Chinese with English abstract)
[68] Yu SY, Zhang JX, del Real PG, Zhao XL, Hou KJ, Gong JH and Li YS. 2013. The Grenvillian orogeny in the Altun-Qilian-North Qaidam mountain belts of northern Tibet Plateau: Constraints from geochemical and zircon U-Pb age and Hf isotopic study of magmatic rocks. Journal of Asian Earth Sciences, 73: 372-395
[69] Yuan HL, Wu FY, Gao S, Liu XM, Xu P and Sun DY. 2003. La-ICP-MS zircon U-Pb age and REE of Cenozoic pluton in NE China. Chinese Science Bulletin, 48(14): 1511-1520 (in Chinese)
[70] Zhang JX, Zhang ZM, Xu ZQ, Yang JS and Cui JW. 1999. The ages of U-Pb and Sm-Nd for eclogite from the western segment of Altyn Tagh tectonic belt. Chinese Science Bulletin, 44(10): 1109-1112 (in Chinese)
[71] Zhang JX, Zhang ZM, Xu ZQ, Yang JS and Cui JW. 2001. Petrology and geochronology of eclogites from the western segment of the Altyn Tagh, northwestern China. Lithos, 56(2-3): 187-206
[72] Zhang JX, Yang JS, Xu ZQ, Meng FC, Li HB and Shi RD. 2002. Evidence for UHP metamorphism of eclogites from the Altun Mountains. Chinese Science Bulletin, 47(9): 751-755
[73] Zhang JX, Yang JS and Xu ZQ. 2002. Evidence for the ultrahigh pressure metamorphism in Altyn eclogite. Chinese Science Bulletin, 47(3): 231-234 (in Chinese)
[74] Zhang JX and Meng FC. 2005. Sapphirine bearing high pressure mafic granulite and its implications in the South Altyn Tagh. Chinese Science Bulletin, 50(3):265-269
[75] Zhang JX, Meng FC and Mattinson CG. 2007. Progress, controversies and challenge of studies on South Altyn Tagh-North Qaidam HP/UHP metamorphic belt. Geological Journal of China Universities, 13(3): 56-545
[76] Zhang JX, Mattinson CG, Meng FC, Wan YS and Tung K. 2008. Polyphase tectonothermal history recorded in granulitized gneisses from the North Qaidam HP/UHP metamorphic terrane, Western China: Evidence from zircon U-Pb geochronology. Geological Society of America Bulletin, 120(5-6): 732-749
[77] Zhang JX, Meng FC and Yu SY. 2010. Two contrasting HP/LT and UHP metamorphic belts: Constraint on Early Paleozoic orogeny in Qilian-Altun orogen. Acta Petrologica Sinica, 26(7): 1967-1992 (in Chinese with English abstract)
[78] Zhang JX, Li HK, Meng FC, Xiang ZQ, Yu SY and Li JP. 2011. Polyphase tectonothermal events recorded in "metamorphic basement" from the Altyn Tagh, the southeastern margin of the Tarim basin, western China: Constraintfrom U-Pb zircon geochronology. Acta Petrologica Sinica, 27(1): 23-46 (in Chinese with English abstract)
[79] Zhang Q, Wang Y, Li CD, Wang YL, Jin WJ and Jia XQ. 2006. Granite classification on the basis of Sr and Yb contents and its implications. Acta Petrologica Sinica, 22(9): 2249-2269 (in Chinese with English abstract)
[80] Zhang Q, Jin WJ, Li CD and Wang YL. 2010. Revisiting the new classification of granitic rocks based on whole-rock Sr and Yb contents: Index. Acta Petrologica Sinica, 26(4): 985-1015 (in Chinese with English abstract)
[81] Zhao ZH, Wang ZG, Chu TR and Zeng TGZ. 1991. The REE, isotopic composition of O, Pb, Sr, Nd and diagenetic model of granitoids in Altai region. Bulletin of Mineralogy, Petrology and Geochemistry, 24(3): 176-178 (in Chinese with English abstract)
[82] 曹玉亭, 刘良, 王超, 杨文强, 朱小辉. 2010. 阿尔金南缘塔特勒克布拉克花岗岩的地球化学特征、锆石U-Pb定年及Hf同位素组成. 岩石学报, 26(11): 3259-3271
[83] 车自成, 刘良, 罗金海等. 1995. 阿尔金山地区高压变质泥质岩石的发现及其产出环境. 科学通报, 40(14): 1298-1300
[84] 车自成, 刘良, 罗金海. 2002. 中国及其邻区区域大地构造学. 北京: 科学出版社, 354-386
[85] 郭进京, 赵风清, 李怀坤. 1999. 中祁连东段晋宁期碰撞型花岗岩及其地质意义. 地球学报, 20(1): 10-15
[86] 康磊, 刘良, 曹玉亭, 王超, 杨文强, 梁莎. 2013. 阿尔金南缘塔特勒克布拉克复式花岗质岩体东段片麻状花岗岩的地球化学特征、锆石U-Pb定年及其地质意义. 岩石学报, 29(9): 3039-3048
[87] 李怀坤, 陆松年, 赵风清, 李惠民, 于海峰, 郑健康. 1999a. 柴达木北缘新元古代重大地质事件年代格架. 现代地质, 13(2): 224-225
[88] 李怀坤, 陆松年, 赵风清, 于海峰, 郑健康. 1999b. 柴达木盆地北缘鱼卡河含柯石英榴辉岩的确定及其意义. 现代地质, 13(1): 43-49
[89] 刘良, 车自成, 罗金海, 王焰, 高章鉴. 1996. 阿尔金山西段榴辉岩的确定及其地质意义. 科学通报, 41(14): 1458-1488
[90] 刘良, 车自成, 王焰, 罗金海, 陈丹玲. 1999. 阿尔金高压变质岩带的特征及其构造意义. 岩石学报, 15(1):57-64
[91] 刘良, 孙勇, 车自成, 罗金海, 陈丹玲, 王焰, 张安达, 陈亮, 肖培喜, 王永和. 2002. 阿尔金发现超高压(>3.8GPa)石榴二辉橄榄岩. 科学通报, 47(9): 657-662
[92] 刘良, 孙勇, 罗金海, 王焰, 陈丹玲, 张安达. 2003. 阿尔金英格利萨依花岗质片麻岩超高压变质. 中国科学(D辑), 33(12): 1184-1192
[93] 柳小明, 高山, 袁洪林, Hattendorf B, Günther D, 陈亮, 胡圣红. 2002. 193nm LA-ICP-MS对国际地质标准参考物质中42种主量和微量元素的分析. 岩石学报, 18(3): 408-418
[94] 刘永顺, 于海峰, 辛后田, 陆松年, 修群业, 李铨. 2009. 阿尔金山地区构造单元划分和前寒武纪重要地质事件. 地质通报, 28(10): 1430-1438
[95] 路凤香, 桑隆康. 2002. 岩石学. 北京: 地质出版社, 82-94
[96] 陆松年. 1998. 新元古时期Rodinia超大陆研究进展述评. 地质论评, 44(5): 489-495
[97] 陆松年. 2002. 青藏高原北部前寒武纪地质初探. 北京: 地质出版社, 35-117
[98] 路远发. 2004. Geokit: 一个用VBA构建的地球化学工具软件包. 地球化学, 33(5): 459-464
[99] 梅华林, 李惠民, 陆松年, 于海峰, 左义成, 李铨. 1999. 甘肃柳园地区花岗质岩石时代及成因. 岩石矿物学杂志, 18(1): 14-17
[100] 孙吉明, 马中平, 唐卓, 李向民. 2012. 阿尔金南缘鱼目泉岩浆混合花岗岩LA-ICP-MS 测年与构造意义. 地质学报, 86(2): 247-257
[101] 王超, 刘良, 车自成, 陈丹玲, 张安达, 罗金海. 2006. 阿尔金南缘榴辉岩带中花岗片麻岩的时代及构造环境探讨. 高校地质学报, 12(1): 74-82
[102] 王超, 刘良, 张安达, 杨文强, 曹玉亭. 2008. 阿尔金造山带南缘岩浆混合作用: 玉苏普阿勒克塔格岩体岩石学和地球化学证据. 岩石学报, 24(12): 2809-2819
[103] 王中刚, 于学元, 赵振华. 1989. 稀土元素地球化学. 北京: 科学出版社, 223-224
[104] 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
[105] 吴利仁. 1985. 中国东部中生代花岗岩类. 岩石学报, 1(1): 1-10
[106] 吴锁平, 吴才来, 陈其龙. 2007. 阿尔金断裂南侧吐拉铝质A型花岗岩的特征及构造环境. 地质通报, 26(10): 1385-1392
[107] 杨德彬, 许文良, 王清海, 裴福萍, 纪伟强. 2006. 安徽蚌埠荆山晚侏罗世花岗岩岩体成因——来自地球化学和锆石Hf同位素的制约. 岩石学报, 22(12): 2923-2932
[108] 杨经绥, 许志琴, 李海兵, 吴才来, 崔军文, 张建新, 陈文. 1998. 柴北缘大柴旦榴辉岩的发现及区域构造意义. 科学通报, 43(14): 1544-1549
[109] 杨文强, 刘良, 丁海波, 校培喜, 曹玉亭, 康磊. 2012. 南阿尔金迪木那里克花岗岩地球化学、锆石U-Pb年代学与Hf同位素特征及其构造地质意义. 岩石学报, 28(12): 4139-4150
[110] 于海峰, 陆松年, 梅华林, 赵风清, 李怀坤, 李惠民. 1999. 中国西部新元古代榴辉岩-花岗岩带和深层次韧性剪切带特征及其大陆再造意义. 岩石学报, 15(4): 532-538
[111] 于海峰, 陆松年, 刘永顺, 修群业, 李铨. 2002. "阿尔金山岩群"的组成及其构造意义. 地质通报, 21(12): 834-840
[112] 袁洪林,吴福元,高山,柳小明,徐平,孙德有. 2003. 东北地区新生代侵入体的锆石激光探针U-Pb测定与稀土元素成分分析.科学通报, 48(14): 1511-1520
[113] 张建新, 张泽明, 许志琴, 杨经绥, 崔军文. 1999. 阿尔金构造带西段榴辉岩的Sm-Nd及U-Pb年龄——阿尔金构造带中加里东期山根存在的证据. 科学通报, 44(10): 1109-1112
[114] 张建新, 杨经绥, 许志琴. 2002. 阿尔金榴辉岩中超高压变质作用证据. 科学通报, 47(3): 231-234
[115] 张建新, 孟繁聪, 于胜尧. 2010. 两条不同类型的HP/LT和UHP变质带对祁连-阿尔金早古生代造山作用的制约. 岩石学报, 26(7): 1967-1992
[116] 张建新, 李怀坤, 孟繁聪, 相阵群, 于胜尧, 李金平. 2011. 塔里木盆地东南缘(阿尔金山)"变质基底"记录的多期构造热事件: 锆石U-Pb年代学的制约. 岩石学报, 27(1): 23-46
[117] 张旗, 王焰, 李承东, 王元龙, 金惟俊, 贾秀勤. 2006. 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, 金惟俊, 李承东, 王元龙. 2010. 再论花岗岩按照Sr-Yb的分类: 标志. 岩石学报, 26(4): 985-1015
[119] 赵振华, 王中刚, 雏天人, 增田彰正. 1991. 阿尔泰花岗岩类型与成岩模型的REE及O、Pb、Sr、Nd同位素组成依据. 矿物岩石地球化学通报, 24(3): 176-178
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