秦岭山阳-柞水地区燕山期中酸性侵入岩地球化学特征、锆石U-Pb年龄及Lu-Hf同位素组成

吴发富, 王宗起, 闫臻, 陈雷, 夏长玲, 郭延辉, 彭远民. 秦岭山阳-柞水地区燕山期中酸性侵入岩地球化学特征、锆石U-Pb年龄及Lu-Hf同位素组成[J]. 岩石学报, 2014, 30(2): 451-471.
引用本文: 吴发富, 王宗起, 闫臻, 陈雷, 夏长玲, 郭延辉, 彭远民. 秦岭山阳-柞水地区燕山期中酸性侵入岩地球化学特征、锆石U-Pb年龄及Lu-Hf同位素组成[J]. 岩石学报, 2014, 30(2): 451-471.
WU FaFu, WANG ZongQi, YAN Zhen, CHEN Lei, XIA ChangLing, GUO YanHui, PENG YuanMin. Geochemical characteristics, zircons U-Pb ages and Lu-Hf isotopic composition of the Yanshanian intermediate-acidic plutons in the Shanyang-Zhashui areas, Qinling Orogenic Belt.[J]. Acta Petrologica Sinica, 2014, 30(2): 451-471.
Citation: WU FaFu, WANG ZongQi, YAN Zhen, CHEN Lei, XIA ChangLing, GUO YanHui, PENG YuanMin. Geochemical characteristics, zircons U-Pb ages and Lu-Hf isotopic composition of the Yanshanian intermediate-acidic plutons in the Shanyang-Zhashui areas, Qinling Orogenic Belt.[J]. Acta Petrologica Sinica, 2014, 30(2): 451-471.

秦岭山阳-柞水地区燕山期中酸性侵入岩地球化学特征、锆石U-Pb年龄及Lu-Hf同位素组成

  • 基金项目:

    本文受国家科技支撑计划课题(2011BAB04B05、2006BAB01A11)和国家自然科学基金项目(41172178、40772137)联合资助.

Geochemical characteristics, zircons U-Pb ages and Lu-Hf isotopic composition of the Yanshanian intermediate-acidic plutons in the Shanyang-Zhashui areas, Qinling Orogenic Belt.

  • 秦岭山阳-柞水地区广泛出露燕山期中酸性花岗(斑)岩体,并有大量与其相关的斑岩-矽卡岩型Cu-Mo-Fe、Cu-Au-Fe矿化。LA-ICP-MS锆石U-Pb测年结果表明,与矿化密切相关的斑岩体形成于144.6~141.5Ma。岩石地球化学分析结果表明,这些花岗(斑)岩体SiO2含量为55.73%~67.80%,K2O含量为2.52%~6.40%,Na2O含量为1.94%~5.19%,Al2O3含量为14.61%~16.10%,FeOT含量为2.1%~9.0%,MgO含量为1.32%~5.52%,主体显高钾钙碱性准铝质特征。A/CNK2O5与SiO2负相关,Mg#平均为49,含有角闪石、黑云母、榍石、磁铁矿等矿物,属I型花岗岩类;稀土元素分异明显,无明显Eu异常;富集K、Rb、Sr、Ba等大离子亲石元素,Nb、Ta、Ti、P和Hf等高场强元素亏损,属后碰撞型花岗岩。岩体的锆石εHf(t)为-4.5~+1.78,平均为-0.87,表明其岩浆源区为地壳物质的熔融岩浆与幔源岩浆的混合,且以地壳熔融成份为主;Hf同位素二阶段模式年龄(tDM2)为1479~1084Ma,表明其壳源源区物质可能形成于中晚元古代(1.4~1.0Ga)。
  • 加载中
  • [1]

    Amelin Y, Lee DC, Halliday AN and Pidgeon RT. 1999. Nature of the Earth's earliest crust from hafnium isotopes in single detrital zircons. Nature, 399(6733): 252-255

    [2]

    Batchelor RA and Bowden P. 1985. Petrogenetic interpretation of granitoids rock series using multicationic parameters. Chemical Geology, 48(1-4): 43-55

    [3]

    Blichert-Toft J and Albarède F. 1997. The Lu-Hf isotope geochemistry of chondrites and the evolution of the mantle-crust system. Earth and Planetary Science Letters, 148(1-2): 243-258

    [4]

    Chappell BW. 1999. Aluminum saturation in I-and S-type granites and the characterization of fractionated haplogranites. Lithos, 46(3): 535-551

    [5]

    Chen YJ, Li C, Zhang J, Li Z and Wang HH. 2000. Sr and Q isotopic characteristics of porphyries in the Qinling molybdenum deposit belt and their implication to genetic mechanism and type. Science in China (Series D), 43(Suppl.): 82-94

    [6]

    Collins WJ, Beams SD, White AJR. et al. 1982. Nature and origin of A-type granites with particular reference to southeastern Australia. Contributions to Mineralogy and Petrology, 80(2): 189-200

    [7]

    Cui JT and Zhao CY. 1998. The geological characteristic of ring-mottled granite in Dongjiangkou and Zhashui masses, Shaanxi Province. Geology of Shaanxi, 16(1): 51-57(in Chinese with English abstract)

    [8]

    Cui JT, Zhao CY and Wang JC. 1999. The rock-lineage units classification and evolution of Dongjiangkou and Zhashui rock bodies in southern Qinling. Geology of Shaanxi, 17(2): 7-15(in Chinese with English abstract)

    [9]

    Elhlou S, Belousova E, GriffinWL, Pearson NJ and O'Reilly SY. 2006. Trace element and isotopic composition of GJ-red zircon standard by laser ablation. Geochimica et Cosmochimica Acta, 70(18): A158

    [10]

    Gong HJ, Zhu LM, Sun BY, Li B and Guo B. 2009a. Zircon U-Pb ages and Hf isotope characteristics and their geological significance of the Shahewan, Caoping and Zhashui granitic plutons in the South Qinling orogen. Acta Petrologica Sinica, 25(2): 248-264(in Chinese with English abstract)

    [11]

    Gong HJ, Zhu LM, Sun BY, Li B, Guo B and Wang JQ. 2009b. Zircon U-Pb ages and Hf isotopic composition of the Dongjiangkou granitic pluton and its mafic enclaves in the South Qinling terrain. Acta Petrologica Sinica, 25(11): 3029-3042(in Chinese with English abstract)

    [12]

    Griffin WL, Wang X, Jackson SE, Pearson SE, O'Reilly SY and Zhou XM. 2002. Zircon chemistry and magma mixing, SE China: In-situ analysis of Hf isotopes, Tonglu and Pingtan igneous compexes. Lithos, 61(3-4): 237-269

    [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]

    Hoskin PWO and Black LP. 2000. Metamorphic zircon formation by solid-state recrystallization of protolith igneous zircon. Journal of Metamorphic Geology, 18(4): 423-439

    [15]

    Hou KJ, Li YH, Zou TR, Qu XM, Shi YR and Xie GQ. 2007. Laser ablation-MC-ICP-MS technique for Hf isotope microanalysis of zircon and its geological applications. Acta Petrologica Sinica, 23(10): 2595-2604(in Chinese with English abstract)

    [16]

    Hou KJ, Li YH and Tian YR. 2009. In situ U-Pb zircon dating using laser ablation-multⅡon couting-ICP-MS. Mineral Deposits, 28(4): 481-492 (in Chinese with English abstract)

    [17]

    Hu JM, Cui JT, Meng QR and Zhao CY. 2004. The U-Pb age of zircons separated from the Zhashui granite in Qinling Orogen and its significance. Geological Review, 50(3): 323-329(in Chinese with English abstract)

    [18]

    Jiang YH, Jin GD, Liao SY, Qing Z and Peng Z. 2010. Geochemical and Sr-Nd-Hf isotopic constraints on the origin of Late Triassic granitoids from the Qinling orogen, central China: Implications for a continental arc to continent-continent collision. Lithos, 117(3-4): 183-197

    [19]

    Johannes W and Holtz F. 1996. Petrogenesis and Experimental Petrology of Granitic Rocks. Berlin: Springer, 1-254

    [20]

    Kay RW and Kay SM. 1991. Creation and destruction of lower continental crust. Geologische Rundschau, 80(2): 259-278

    [21]

    Li CY, Liu YW, Zhu BQ, Feng YM and Wu HQ. 1978. Tectonic evolution of Qinling and Qilian Mountains. Northwestern Geology, 4: 1-12 (in Chinese)

    [22]

    Li XH, Li WX and Li ZX. 2007. On the genetic classification and tectonic implications of the Early Yanshanian granitoids in the Nanling Range, South China. Chinese Science Bulletin, 52(14): 1873-1885

    [23]

    Li XZ, Yan Z and Lu XX. 1993. Granitoids of Mt. Qinling-Dabieshan. Beijing: Geological Publishing House, 1-218(in Chinese with English abstract)

    [24]

    Liu SW, Li QG, Tian W, Wang ZQ, Yang PT, Wang W, Bai X and Guo RR. 2011. Petro-genesis of Indosinian granitoids in middle-segment of south Qinling tectonic belt: Constraints from Sr-Nd isotopic systematics. Acta Geologica Sinica, 85(3): 610-628

    [25]

    Liu SW, Yang PT, Li QG, Wang ZQ, Zhang WY and Wang W. 2011. Indosinian granitoids and orogenic processes in the middle segment of the Qinling orogen, China. Journal of Jilin University (Earth Science Edition), 41(6): 1928-1943(in Chinese with English abstract)

    [26]

    Liu YS, Hu ZC, Gao S, GÜnther D, Xu J, Gao C and Chen H. 2008. In situ analysis of major and trace elements of anhydrous minerals by LA-ICP-MS without applying an internal standard. Chemical Geology, 257(1-2): 34-43

    [27]

    Lu XX, Dong Y, Chang QL, Xiao QH, Li XB and Wang XX. 1996. Indosinian Shahewan rapakivi granite in Qinling and its dynamic significance. Science in China (Series D), 39(3): 266-272

    [28]

    Lu XX, Wei XD, Xiao QH, Zhang ZQ, Li HM and Wang W. 1999. Geochronological studies of rapakivi granites in Qinling and its geological implications. Geological Journal of China Universities, 5(4): 372-377(in Chinese with English abstract)

    [29]

    Lu XX, Wang XX, Xiao QH and Xing ZY. 2007. Comparison of Qinling-Kunlun orogenic-type rapakivi granite with world typical rapakivi granite. Geological Science and Technology Information, 26(1): 1-10(in Chinese with English abstract)

    [30]

    Maniar PD and Piccoli PM. 1989. Tectonic discrimination of granitoids. Geological Society of America Bulletin, 101(5): 635-643

    [31]

    Nasdala L, Hofmeister W, Norberg N, Martinson JM. Corfu F, Dorr W, Kamo SL. Kennedy AK, Kronz A, Reiners PW, Frei D, Kosler J, Wan YS, Gotze J, Hager T, Kroner A and Valley JW. 2008. Zircon M257: A homogeneous natural reference material for the ion microprobe U-Pb analysis of zircon. Geostandards and Geoanalytical Research, 32(3): 247-265

    [32]

    Niu BG, He ZJ, Ren JS, Wang J and Deng P. 2006. SHRIMP U-Pb ages of zircon from the intrusion in the western Douling-Xiaomaoling uplift and their geological significances. Geological Review, 52(6): 826-835 (in Chinese with English abstract)

    [33]

    Pearce JA. 1996. Sources and settings of granitic rocks. Episodes, 19(4): 120-125

    [34]

    Peccerillo A and Taylor SR. 1976. Geochemistry of Eocene calc-alkaline volcanic rocks from the Kastamonu area, Northern Turkey. Contributions to Mineralogy and Petrology, 58(1): 63-81

    [35]

    Qin JF, Lai SC and Li YF. 2005. Petrogenesis and geological significance of Yangba granodiorites from Bikou area, north margin of Yangtze Plate. Acta Petrologica Sinica, 21(3): 697-710(in Chinese with English abstract)

    [36]

    Qin JF, Lai SC and Li YF. 2007. Genesis of the Indosinian Guangtoushan adakitic biotite plagiogranite in the Mianxian-Lueyang (Mianlue) suture, South Qinling, China, and its tectonic implications. Geological Bulletin of China, 26(4): 466-471(in Chinese with English abstract)

    [37]

    Qin JF, Lai SC, Grapes, Diwu CR, Ju YJ and Li YF. 2009. Geochemical evidence for origin of magma mixing for the Triassic monzonitic granite and its enclaves at Mishuling in the Qinling orogeny (central China). Lithos, 112(3-4): 259-276

    [38]

    Qin JF. 2010. Petrogenesis and geodynamic implications of the Late-Triassic granitoids from the Qinling Orogenic Belt. Ph. D. Dissertation. Xi'an: Northwest University, 1-266(in Chinese with English summary)

    [39]

    Qin JF, Lai SC, Grapes R. Diwu CR, Ju YJ and Li YF. 2010. Origin of Late Triassic high-Mg adakitic granitoid rocks from the Dongjiangkou area, Qinling orogen, central China: Implication for subduction of continent crust. Lithos, 120(3-4): 347-367

    [40]

    Rapp RP. 1997. Heterogeneous source regions for Archean granitoids. In: deWit MJ and Ashwal LD (eds.). Greenstone Belts. Oxford: Oxford University Press, 35-37

    [41]

    Rapp RP, Shimizn N, Norman MD and Applegate GS. 1999. Reaction between slab-derived melt and peridotite in the mantle wedge: Experimental constraints at 3.8Gpa. Chemical Geology, 160(4): 335-356

    [42]

    Rudnick RL. 1995. Making continental crust. Nature, 378(6557): 571-578

    [43]

    Scherer E, MÜnker C and Mezger K. 2001. Calibration of the Lutetium-hafnium clock. Science, 293(5530): 683-687

    [44]

    Shan RJ and Yan Z. 1988. Granites of Qinling-Dabashan Mountains. Wuhan: China University of Geosciences Press, 1-229(in Chinese)

    [45]

    Sisson TW, Ratajeski K and Hankins WB. 2005. Voluminous granitic magmas from common basaltic sources. Contributions to Mineralogy and Petrology, 148(6): 635-661

    [46]

    Slama J, Kosler J, Condon DJ, Crowley JL, Gerdes A, Hanchar JM, Horstwood MSA, Morris GA, Nasdala L, Norberg N, Schaltegger U, Schoene B, Tubrett MN and Whitehouse MJ. 2008. Plesovice zircon: A new natural reference material for U-Pb and Hf isotopic microanalysis. Chemical Geology, 249(1-2): 1-35

    [47]

    Sun SS and MeDonough 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: 313-345

    [48]

    Tian W, Dong SB, Chen MM and Zhu WP. 2009. "Mantle signature" on the Indosinian granitoid belt in south Qinling, Central China. Earth Science Frontiers, 16(2): 119-128 (in Chinese with English abstract)

    [49]

    Vervoort JD and Blicher-Toft J. 1999. Evolution of the depleted mantle: Hf isotope evidence from juvenile rocks through time. Geochimica et Cosmochimica Acta, 63(3-4): 533-556

    [50]

    Wan YW. 1980. Mineralization characteristics and ore deposit model of intermediate-acid granitoid porphyry from Shanyang region. Regional Characteristics of Qinling, (3): 1-36(in Chinese)

    [51]

    Wang J, Li X, Lai SC and Qin JF. 2008. Petrogenesis of the Early Triassic Xichahe and Wulong plutons in the South Qinling Mountains and their tectonic significance. Geology in China, 35(2): 207-216(in Chinese with English abstract)

    [52]

    Wang XX, Wang T, Ilmari H and Lu XX. 2005. Genesis of mafic enclaves from rapakivi-textured granites in the Qinling and its petrological significance: Evidence of elements and Nd, Sr isotopes. Acta Petrologica Sinica, 21(3): 935-946(in Chinese with English abstract)

    [53]

    Wang ZQ, Wang T, Yan Z and Yan QR. 2002. Late Paleozoic forearc accretionary piggyback type basin system in the South Qinling, Central China. Regional Geology of China, 21(8-9): 456-464(in Chinese with English abstract)

    [54]

    Wang ZQ, Yan QR, Yan Z, Wang T, Jiang CF, Gao LD, Li QG, Chen JL, Zhang YL, Liu P, Xie CL and Xiang ZJ. 2009. New division of the main tectonic units of the Qinling Orogenic Belt, Central China. Acta Geologica Sinica, 83(11): 1527-1546(in Chinese with English abstract)

    [55]

    Wolf MB and Wyllie PJ. 1992. The formation of tonalitic liquids during the vapor-absent partial melting of amphibolite at 10kbar. Eos, 70: 506-518

    [56]

    Wu FY, Yang YH, Xie LW, Yang JH and Xu P. 2006. Hf isotopic compositions of the standard zircons and baddeleyites used in U-Pb geochronology. Chemical Geology, 234(1-2): 105-126

    [57]

    Xie GQ, Ren T, Li JB, Wang RT, Xia CL, Guo YH, Dai JZ and Shen ZC. 2012. Zircon U-Pb age and Petrogenesis of ore-bearing granitoids for the Chigou Cu-Mo deposit from the Zhashan basin, Shaanxi Province. Acta Petrologica Sinica, 28(1): 15-26(in Chinese with English abstract)

    [58]

    Yan Z. 1985. Granite from Shaanxi Province. Xi'an: Xi'an Jiaotong University Press, 1-321(in Chinese)

    [59]

    Yan Z, Wang ZQ, Yan QR, Wang T, Xiao WJ, Li JL, Han FL, Chen JL and Yang YC. 2006. Devonian sedimentary environments and provenance of the Qinling Orogen: Constraints on Late Paleozoic southward accretionary tectonics of the North China Craton. International Geology Review, 48(7): 585-618

    [60]

    Yan Z, Wang ZQ, Wang T, Yan QR, Xiao WJ, Li JL, Han FL and Chen JL. 2007. Tectonic setting of Devonian sediments in the Qinling orogen: Constraints from detrital modes and geochemistry of clastic rocks. Acta Petrologica Sinica, 23(5): 1023-1042(in Chinese with English abstract)

    [61]

    Yan Z, Wang ZQ, Yan QR, Wang T and Guo XQ. 2012. Geochemical constraints on the provenance and depositional setting of the Devonian Liuling Group, East Qinling Mountains, Central China: Implications for the tectonic evolution of the Qinling orogenic belt. Journal of Sedimentary Research, 82(1): 9-20

    [62]

    Yogodzinski CM, Kay RW, Volynets ON, Koloskov AV and Bolynets ON. 1995. Magnesian andesite in the western Aleutian Komandorsky region: Implications for slab melting and processes in the mantle wedge. Geological Society of America Bulletin, 107(5): 505-519

    [63]

    Zhang BR, Chen DX, Li ZJ et al. 1989. Region Geochemistry of Shanyang-Zhashui Metallogenic Belt, Shaanxi Province. Wuhan: Press of China University of Geosciences, 1-221(in Chinese with English abstract)

    [64]

    Zhang CL, Wang T and Wang XX. 2008. Origin and tectonic setting of the Early Mesozoic granitoids in Qinling Orogenic Belt. Geological Journal of China Universities, 14(3): 304-316 (in Chinese with English abstract)

    [65]

    Zhang HF, Zhang BR, Ling WL, Gao S and Ouyang JP. 1997. Late Proterozoic crustal accretion of South Qinling: Na isotopic study from granitic rocks. Geochimica, 26(5): 16-24 (in Chinese with English abstract)

    [66]

    Zhang HF, Parrish R, Zhang L Xu WC, Yuan HL, Gao S and Crowley QG. 2007. A-type granite and adakitic magmatism association in Songpan Garze fold belt, eastern Tibetan Plateau: Implication for lithospheric delamination. Lithos, 97(3-4): 323-335

    [67]

    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)

    [68]

    Zhang YL. 2002. Geological features and the metallogentic conditions of acid-intermediate acid small rock bodies in Xiaohekou area of Shanyang County, Shaanxi Province. Shaanxi Geology, 20(2): 27-38(in Chinese with English abstract)

    [69]

    Zhang ZQ, Zhang GW, Tang SH and Lu XX. 1999. Age of the Shahewan rapakivi granite in the Qinling orogen, China, and its constraints on the end time of the main orogenic stage of this orogen. Chinese Science Bulletin, 44(21): 2001-2004

    [70]

    崔建堂, 赵长缨. 1998. 东江口、柞水岩体环斑花岗岩地质特征. 陕西地质, 16(1): 51-57

    [71]

    崔建堂, 赵长缨, 王炬川. 1999. 南秦岭东江口、柞水岩体岩石谱系单位划分及演化. 陕西地质, 17(2): 7-15

    [72]

    弓虎军, 朱赖民, 孙博亚, 李犇, 郭波. 2009a. 南秦岭沙河湾、曹坪和柞水岩体锆石U-Pb年龄、Hf同位素特征及其地质意义. 岩石学报, 25(2): 248-264

    [73]

    弓虎军, 朱赖民, 孙博亚, 李犇, 郭波, 王建其. 2009b. 南秦岭地体东江口花岗岩及其基性包体的锆石U-Pb年龄和Hf同位素组成. 岩石学报, 25(11): 3029-3042

    [74]

    侯可军, 李延河, 邹天人, 曲晓明, 石玉若, 谢桂青. 2007. LA-MC-ICP-MS锆石Hf同位素的分析方法及地质应用. 岩石学报, 23(10): 2595-2604

    [75]

    侯可军, 李延河, 田有荣. 2009. LA-MC-ICP-MS锆石微区原位U-Pb定年技术. 矿床地质, 28(4): 481-492

    [76]

    胡健民, 崔建堂, 孟庆任, 赵长缨. 2004. 秦岭柞水岩体锆石U-Pb年龄及其地质意义. 地质论评, 50(3): 323-329

    [77]

    李春昱, 刘仰文, 朱宝清, 冯益民, 吴汉泉. 1978. 秦岭及祁连山构造发展史. 西北地质, 4: 1-12

    [78]

    李献华, 李武显, 李正祥. 2007. 再论南岭燕山早期花岗岩的成因类型与构造意义. 科学通报, 52(9): 981-991

    [79]

    李先梓, 严阵, 卢欣祥. 1993. 秦岭-大别山花岗岩. 北京: 地质出版社, 1-218

    [80]

    刘树文, 杨朋涛, 李秋根, 王宗起, 张万益, 王伟. 2011. 秦岭中段印支期花岗质岩浆作用与造山过程. 吉林大学学报(自然科学版), 41(6): 1928-1943

    [81]

    卢欣祥, 董有, 常秋岭, 肖庆辉, 李晓波, 王晓霞. 1996. 秦岭印支期沙河湾奥长环斑花岗岩及其动力学意义. 中国科学(D辑), 26(3): 244-248

    [82]

    卢欣祥, 尉向东, 肖庆辉, 张宗清, 李惠民, 王卫. 1999. 秦岭环斑花岗岩的年代学研究及其意义. 高校地质学报, 5(4): 372-377

    [83]

    卢欣祥, 王晓霞, 肖庆辉, 邢作云. 2007. 秦岭-昆仑造山型环斑花岗岩与世界典型环斑花岗岩的对比. 地质科技情报, 26(1): 1-10

    [84]

    牛宝贵, 何政军, 任纪舜, 王军, 邓平. 2006. 秦岭地区陡岭-小磨岭隆起西段几个岩体的SHRIMP锆石U-Pb测年及其地质意义. 地质论评, 52(6): 826-835

    [85]

    秦江锋, 赖绍聪, 李永飞. 2005. 扬子板块北缘碧口地区阳坝花岗闪长岩体成因研究及其地质意义. 岩石学报, 21(3): 697-710

    [86]

    秦江锋, 赖绍聪, 李永飞. 2007. 南秦岭勉县-略阳缝合带印支期光头山埃达克质花岗岩的成因及其地质意义. 地质通报, 26(4): 466-471

    [87]

    秦江锋. 2010. 秦岭造山带晚三叠世花岗岩类成因机制及其动力学背景. 博士学位论文. 西安:西北大学, 1-266

    [88]

    尚瑞钧, 严阵. 1988. 秦巴花岗岩. 武汉: 中国地质大学出版社, 1-229

    [89]

    田伟, 董申保, 陈咪咪, 朱文萍. 2009. 南秦岭印支期花岗岩带的"地幔印记". 地学前缘, 16(2): 119-128

    [90]

    万义文. 1980. 山阳一带中酸性斑岩体的成矿特点与成矿模式. 秦岭区测, (3): 1-36

    [91]

    王娟, 李鑫, 赖绍聪, 秦江锋. 2008. 印支期南秦岭西茬河、五龙岩体成因及构造意义. 中国地质, 35(2): 207-216

    [92]

    王晓霞, 王涛, Ilmari H, 卢欣祥. 2005. 秦岭环斑结构花岗岩中暗色包体的岩浆混合成因及岩石学意义——元素和Nd、Sr同位素地球化学证据. 岩石学报, 21(3): 935-946

    [93]

    王宗起, 王涛, 闫臻, 闫全人. 2002. 秦岭晚古生代弧前增生的背驮型盆地体系. 地质通报, 21(8-9): 456-464

    [94]

    王宗起, 闫全人, 闫臻, 王涛, 姜春发, 高联达, 李秋根, 陈隽璐, 张英利, 刘平, 谢春林, 向忠金. 2009. 秦岭造山带主要大地构造单元的新划分. 地质学报, 83(11): 1527-1546

    [95]

    谢桂青, 任涛, 李剑斌, 王瑞廷, 夏长玲, 郭延辉, 代军治, 申志超. 2012. 陕西柞山盆地池沟铜钼矿区含矿岩体的锆石年龄和岩石成因. 岩石学报, 28(1): 15-26

    [96]

    闫臻, 王宗起, 王涛, 闫全人, 肖文交, 李继亮, 韩芳林, 陈隽璐. 2007. 秦岭造山带泥盆系形成构造环境: 来自碎屑岩组成和地球化学方面的约束. 岩石学报, 23(5): 1023-1042

    [97]

    严阵. 1985. 陕西省花岗岩. 西安: 西安交通大学出版社, 1-321

    [98]

    张本仁, 陈德兴, 李泽九等. 1989. 陕西柞水山阳成矿带区域地球化学. 武汉: 中国地质大学出版社, 1-221

    [99]

    张成立, 王涛, 王晓霞. 2008. 秦岭造山带早中生代花岗岩成因及其构造环境. 高校地质学报, 14(3): 304-316

    [100]

    张宏飞, 张本仁, 凌文黎, 高山, 欧阳建平. 1997. 南秦岭新元古代地壳增生事件: 花岗质岩石钕同位素示踪. 地球化学, 26(5): 16-24

    [101]

    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

    [102]

    张银龙. 2002. 陕西省山阳县小河口地区酸性-中酸性岩体地质特征及其成矿地质条件分析. 陕西地质, 20(2): 27-38

  • 加载中
计量
  • 文章访问数:  6772
  • PDF下载数:  7298
  • 施引文献:  0
出版历程
收稿日期:  2013-02-06
修回日期:  2013-08-11
刊出日期:  2014-02-28

目录