东昆仑沟里地区晚奥陶世花岗闪长岩地球化学特征及其对原特提斯洋演化的制约

陈加杰; 付乐兵; 魏俊浩; 田宁; 熊乐; 赵玉京; 张玉洁; 祁月清

doi:10.3799/dqkx.2016.129

Volume 41 Issue 11

Nov. 2016

Turn off MathJax

Article Contents

Article Navigation > Earth Science > 2016 > 41(11): 1863-1882

Chen Jiajie, Fu Lebing, Wei Junhao, Tian Ning, Xiong Le, Zhao Yujing, Zhang Yujie, Qi Yueqing, 2016. Geochemical Characteristics of Late Ordovician Granodiorite in Gouli Area, Eastern Kunlun Orogenic Belt, Qinghai Province: Implications on the Evolution of Proto-Tethys Ocean. Earth Science, 41(11): 1863-1882. doi: 10.3799/dqkx.2016.129

Citation:

Chen Jiajie, Fu Lebing, Wei Junhao, Tian Ning, Xiong Le, Zhao Yujing, Zhang Yujie, Qi Yueqing, 2016. Geochemical Characteristics of Late Ordovician Granodiorite in Gouli Area, Eastern Kunlun Orogenic Belt, Qinghai Province: Implications on the Evolution of Proto-Tethys Ocean. Earth Science, 41(11): 1863-1882. doi: 10.3799/dqkx.2016.129

Citation:

Chen Jiajie, Fu Lebing, Wei Junhao, Tian Ning, Xiong Le, Zhao Yujing, Zhang Yujie, Qi Yueqing, 2016. Geochemical Characteristics of Late Ordovician Granodiorite in Gouli Area, Eastern Kunlun Orogenic Belt, Qinghai Province: Implications on the Evolution of Proto-Tethys Ocean. Earth Science, 41(11): 1863-1882. doi: 10.3799/dqkx.2016.129

PDF( 4983 KB)

Geochemical Characteristics of Late Ordovician Granodiorite in Gouli Area, Eastern Kunlun Orogenic Belt, Qinghai Province: Implications on the Evolution of Proto-Tethys Ocean

doi: 10.3799/dqkx.2016.129

1.
Faculty of Earth Resources, China University of Geosciences, Wuhan 430074, China
2.
Qinghai Institute of Geology and Mineral Resources, Xining 810007, China
3.
No.8 Geological Team of Qinghai Nonferrous Metals Geological Exploration Bureau, Xining 810012, China

Received Date: 2016-02-01
Publish Date: 2016-11-15

Abstract

Abstract

The Aowade granodiorited in the east-end of Kunnan terrain, a part of Kunlun Orogenic belt, belongs to Proto-Tethyan tectonic domain. Detailed study of the granodiorite can offer important information to constrain the evolution of the Proto-Tethys Ocean. Detailer study of the granodiorite can offer important information to constrain the evolution of the Proto-Tethys Ocean. In this study, LA-ICP-MS zircon U-Pb dating yields a weighted mean age of 454±2 Ma for the intrusion. It is characterized by low K₂O/Na₂O (0.92-2.68) and Mg^# (39-43), and the A/CNK is between 1.00 and 1.03. The REE exhibits right-dipping patterns with negative anomalies of Eu/Eu^*(0.48-0.96) and high (La/Yb)_N ratios. LILE(Rb, Ba, K, La, Sr) is enriched in this intrusion, while HFSE(Nb, Ta, P, Ti) is depleted relative to the primitive mantle, and the concentrations of transition elements such as Cr and Ni are low. The ratios of Sr/Y (average of 55) are relatively high. All the samples have high initial ⁸⁷Sr/⁸⁶Sr values (0.705 9-0.706 3) and ε_Hf(t) (+5.4 to +9.2), but with relatively low ε_Nd(t)(-4.1 to -1.9) and old two stage model age (T_2DMNd=1.3-1.5 Ga). In combination with the lithology, geochemical signature and isotopic compositions of the intrusion, we propose that the Aowade granodiorite was derived from melting of the subducted oceanic crust with minor involvement of continent crust. The possible residual of the source region is garnet amphibolite. Fractional crystallization of pyroxene, amphibole and plagioclase may have also occurred during the evolution of magma. Integrating evidences from the geodynamic setting of the Aowade granodiorite, the ophiolites in the Kunzhong structure zone, and the metamorphic rocks, arc-related igneous rocks on either side of the Kunzhong structure zone, it is concluded that the Aowade granodiorite was formed during the subduction of Proto-Tethys Ocean, which further reveals the nature of bidirectional subduction of the Proto-Tethys in the Late Ordovician.
- low-Mg adakitic granodiorite,
- Late Ordovician,
- Kunzhong suture belt,
- Proto-Tethys Ocean,
- bidirectional subduction,
- eastern Kunlun,
- geochemistry

FullText(HTML)

References(128)

References

Atherton, M.P., Petford, N., 1993.Generation of Sodium-Rich Magmas from Newly Underplated Basaltic Crust.Nature, 362(6416):144-146.doi: 10.1038/362144a0

Blichert-Toft, J., Chauvel, C., Albarède, F., 1997.Separation of Hf and Lu for High-Precision Isotope Analysis of Rock Samples by Magnetic Sector-Multiple Collector ICP-MS.Contributions to Mineralogy and Petrology, 127(3):248-260.doi: 10.1007/s004100050278

Castillo, P.R., Janney, P.E., Solidum, R.U., 1999.Petrology and Geochemistry of Camiguin Island, Southern Philippines:Insights to the Source of Adakites and Other Lavas in a Complex Arc Setting.Contributions to Mineralogy and Petrology, 134(1):33-51.doi: 10.1007/s004100050467

Chen, G.C., Pei, X.Z., Li, R.B., et al., 2013.Zircon U-Pb Geochronology, Geochemical Characteristics and Geological Significance of Cocoe along Quartz Diorites Body from the Hongshuichuan Area in East Kunlun.Acta Geologica Sinica, 87(2):178-196(in Chinese with English abstract).

Chen, H.W., Luo, Z.H., Mo, X.X., et al., 2006.SHRIMP Ages of Kayakedengtage Complex in the East Kunlun Mountains and Their Geological Implications.Acta Petrologica et Mineralogica, 25(1):25-32(in Chinese with English abstract). http://www.en.cnki.com.cn/Article_en/CJFDTotal-YSKW200601002.htm

Chen, L., Sun, Y., Pei, X.Z., et al., 2001.Northernmost Paleo-Tethyan Oceanic Basin in Tibet:Geochronological Evidence from ⁴⁰Ar/³⁹Ar Age Dating of Dur'ngoi Ophiolite.Chinese Science Bulletin, 46(14):1203-1205.doi: 10.1007/bf02900603

Chen, L., Sun, Y., Pei, X.Z., et al., 2003.Comprehensive Comparison of Paleo-Tethys Ophiolite and Its Geodynamic Significance—An Example from Dur'ngoi Ophiolite.Science in China (Series D), 33(12):1136-1142 (in Chinese with English abstract). http://kns.cnki.net/KCMS/detail/detail.aspx?filename=jdxk200312001&dbname=CJFD&dbcode=CJFQ

Chen, N.S., Sun, M., He, L., et al., 2002.Precise Timing of the Early Paleozoic Metamorphism and Thrust Deformation in the Eastern Kunlun Orogen.Chinese Science Bulletin, 47(13):1130-1133.doi: 10.1360/02tb9253

Chen, N.S., Sun, M., Wang, Q.Y., et al., 2008.U-Pb Dating of Zircon from the Central Zone of the East Kunlun Orogen and Its Implications for Tectonic Evolution.Science in China (Series D), 51(7):929-938.doi: 10.1007/s11430-008-0072-x

Chen, Y.X., Pei, X.Z., Li, R.B., et al., 2013.Zircon U-Pb Age, Geochemical Characteristics and Tectonic Significance of Metavolcanic Rocks from Naij Tal Group, East Section of East Kunlun.Earth Science Frontiers, 20(6):240-254 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-DXQY201306032.htm

Chen, Y.X., Pei, X.Z., Li, R.B., et al., 2014.Geochemical Characteristics and Tectonic Significance of Meta-Sedimentary Rocks from Naij Tal Group, Eastern Section of East Kunlun.Geoscience, 28(3):489-500 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-XDDZ201403005.htm

Chung, S.L., Liu, D.Y., Ji, J.Q., et al., 2003.Adakites from Continental Collision Zones:Melting of Thickened Lower Crust beneath Southern Tibet.Geology, 31(11):1021.doi: 10.1130/g19796.1

Crawford, A.J., Fall, T.J., Green, D.H., et al., 1989.Classification, Petrogenesis and Tectonic Setting of Boninites.Academic Division of Unwin Hyman Ltd., London.

Cui, M.H., Meng, F.C., Wu, X.K., 2011.Early Ordovician Island Arc of Qimantag Mountain, Eastern Kunlun:Evidences from Geochemistry, Sm-Nd Isotope and Geochronology of Intermediate-Basic Igneous Rocks.Acta Petrologica Sinica, 27(11):3365-3379 (in Chinese with English abstract). http://www.oalib.com/paper/1476111

Defant, M.J., Drummond, M.S., 1990.Derivation of Some Modern Arc Magmas by Melting of Young Subducted Lithosphere.Nature, 347(6294):662-665.doi: 10.1038/347662a0

Elburg, M.A., van Bergen, M.V., Hoogewerff, J., et al., 2002.Geochemical Trends across an Arc-Continent Collision Zone:Magma Sources and Slab-Wedge Transfer Processes below the Pantar Strait Volcanoes, Indonesia.Geochimica et Cosmochimica Acta, 66(15):2771-2789.doi: 10.1016/s0016-7037(02)00868-2

Feng, J.Y., Pei, X.Z., Yu, S.L., et al., 2010.The Discovery of the Mafic-Ultramafic Melange in Kekesha Area of Dulan County, East Kunlun Region, and Its LA-ICP-MS Zircon U-Pb Age.Geology in China, 37(1):28-38 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DIZI201001006.htm

Foley, S., Tiepolo, M., Vannucci, R., 2002.Growth of Early Continental Crust Controlled by Melting of Amphibolite in Subduction Zones.Nature, 417(6891):837-840.doi: 10.1038/nature00799

Gao, S., Rudnick, R.L., Yuan, H.L., et al., 2004.Recycling Lower Continental Crust in the North China Craton.Nature, 432(7019):892-897.doi: 10.1038/nature03162

Gao, X.F., Xiao, P.X., Xie, C.R., et al., 2010.Zircon LA-ICP-MS U-Pb Dating and Geological Significance of Bashierxi Granite in the Eastern Kunlun Area, China.Geological Bulletin of China, 29(7):1001-1008 (in Chinese with English abstract). https://www.researchgate.net/publication/289317698_Zircon_LA-ICP-MS_U-Pb_dating_and_geological_significance_of_Bashierxi_granite_in_the_eastern_kimlun_area_China

Griffin, W.L., Belousova, E.A., Shee, S.R., et al., 2004.Archean Crustal Evolution in the Northern Yilgarn Craton:U-Pb and Hf-Isotope Evidence from Detrital Zircons.Precambrian Research, 131(3-4):231-282.doi: 10.1016/j.precamres.2003.12.011

Hofmann, A.W., 1988.Chemical Differentiation of the Earth:The Relationship between Mantle, Continental Crust, and Oceanic Crust.Earth and Planetary Science Letters, 90(3):297-314.doi: 10.1016/0012-821x(88)90132-x

Hu, Z.C., Liu, Y.S., Gao, S., et al., 2012.Improved in Situ Hf Isotope Ratio Analysis of Zircon Using Newly Designed X Skimmer Cone and Jet Sample Cone in Combination with the Addition of Nitrogen by Laser Ablation Multiple Collector ICP-MS.Journal of Analytical Atomic Spectrometry, 27(9):1391-1399.doi: 10.1039/c2ja30078h

Jia, L.H., Meng, F.C., Feng, H.B., 2014.Fluid Activity during Eclogite-Facies Peak Metamorphism:Evidence from a Quartz Vein in Eclogite in the East Kunlun, NW China.Acta Petrologica Sinica, 30(8):2339-2350 (in Chinese with English abstract). https://www.researchgate.net/publication/286130156_Eclogite-facies_peak_fluid_activity_Evidence_from_the_British_East_Kunlun_eclogite_rock_veins

Jia, Y.R., 2013.Petrogenesis and Tectonic Implications of Qiukesu Granite Pluton and Its Enclaves in the Western Kunlun Orogen Belt, NW China (Dissertation).Nanjing University, Nanjing (in Chinese with English abstract). https://www.researchgate.net/publication/287527260_Discovery_of_the_Middle_Devonian_A-type_granite_from_the_Eastern_Kunlun_Orogen_and_its_tectonic_implications

Li, R.B., Pei, X.Z., Li, Z.C., et al., 2015.Geochemistry and Zircon U-Pb Geochronology of Granitic Rocks in the Buqingshan Tectonic Mélange Belt, Northern Tibet Plateau, China and Its Implications for Prototethyan Evolution.Journal of Asian Earth Sciences, 105:374-389.doi: 10.1016/j.jseaes.2015.02.004

Li, R.B., Pei, X.Z., Li, Z.C., et al., 2015.Geological and Geochemical Features of Delisitannan Basalts and Their Petrogenesis in Buqingshan Tectonic Mélange Belt, Southern Margin of East Kunlun Orogen.Earth Science, 40(7):1148-1162(in Chinese with English abstract). https://www.researchgate.net/publication/282730051_Geological_and_geochemical_features_of_delisitannan_basalts_and_their_petrogenesis_in_Buqingshan_tectonic_Melange_belt_southern_margin_of_East_Kunlun_Orogen

Li, X., Yuan, W.M., Hao, N.N., et al., 2014.Characteristics and Tectonic Setting of Granite in Wulonggou Area, East Kunlun Mountains.Globle Geology, 33(2):275-288 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-SJDZ201402004.htm

Li, Z.C., Pei, X.Z., Liu, Z.Q., et al., 2013.Geochronology and Geochemistry of the Gerizhuotuo Diorites from the Buqingshan Tectonic Mélange Belt in the Southern Margin of East Kunlun and Their Geologic Implications.Acta Geologica Sinica, 87(8):1089-1103(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-DZXE201308006.htm

Liu, B., 2011.Petrology, Zircon U-Pb Geochronology, and Petrogenesis of Early Devonian Yuejinshan Intrusive Complex in the Eastern Kunlun Orogen(Dissertation).China University of Geosciences, Wuhan (in Chinese with English abstract). https://www.researchgate.net/publication/287527260_Discovery_of_the_Middle_Devonian_A-type_granite_from_the_Eastern_Kunlun_Orogen_and_its_tectonic_implications

Liu, B, Ma, C.Q., Guo, P., et al., 2013a.Discovery of the Middle Devonian A-Type Granite from the Eastern Kunlun Orogen and Its Tectonic Implications.Earth Science, 38(5):947-962 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-DQKX201305005.htm

Liu, B, Ma, C.Q., Jiang, H.A., et al., 2013b.Early Paleozoic Tectonic Transition from Ocean Subduction to Collisional Orogeny in the Eastern Kunlun Region:Evidence from Huxiaoqin Mafic Rocks.Acta Petrologica Sinica, 29(6):2093-2106 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-YSXB201306018.htm

Liu, J.L., Sun, F.Y, Li, L., et al., 2015.Geochronology, Geochemistry and Hf Isotopes of Gerizhuotuo Complex Intrusion in West of Anyemaqen Suture Zone.Earth Science, 40(6):965-981(in Chinese with English abstract). https://www.researchgate.net/publication/282233403_Geochronology_geochemistry_and_Hf_isotopes_of_gerizhuotuo_complex_intrusion_in_west_of_anyemaqen_suture_zone

Liu, Y.S., Hu, Z.C., Gao, S., et al., 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. doi: 10.1016/j.chemgeo.2008.08.004

Liu, Y.S., Hu, Z.C., Zong, K.Q., et al., 2010.Reappraisement and Refinement of Zircon U-Pb Isotope and Trace Element Analyses by LA-ICP-MS.Chinese Science Bulletin, 55(15):1535-1546. doi: 10.1007/s11434-010-3052-4

Liu, Z.Q., Pei, X.Z., Li, R.B., et al., 2011.LA-ICP-MS Zircon U-Pb Geochronology of the Two Suites of Ophiolites at the Buqingshan Area of the A'nyemaqen Orogenic Belt in the Southern Margin of East Kunlun and Its Tectonic Implication.Acta Geologica Sinica, 85(2):185-194(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DZXE201102005.htm

Long, X.P., 2004.The Research of Zircon Chronology in Orogenic Belts—A Case Study in Jinshuikou Zone(Dissertation).Jilin University, Changchun (in Chinese with English abstract).

Lu, S.N., Yu, H.F., Zhao, F.Q., 2002.Cambrian Geology in the Northern Part of the Tibetan Plateau.Geological Press, Beijing (in Chinese).

Ludwig, K.R., 2012.User's Manual for Isoplot 3.75—A Geochronological Toolkit for Microsoft Excel.Berkeley Geochronology Center Special Publication, Berkeley.

Maniar, P., D., Piccoli, P.M., 1989.Tectonic Discrimination of Granitoids.Geological Society of America Bulletin, 101(5):635-643.doi:10.1130/0016-7606(1989)101<0635:tdog>2.3.co;2

Matte, P., Tapponnier, P., Arnaud, N., et al., 1996.Tectonics of Western Tibet, between the Tarim and the Indus.Earth and Planetary Science Letters, 142(3-4):311-330.doi: 10.1016/0012-821x(96)00086-6

Mattern, F., Schneider, W., Li, Y., et al., 1996.A Traverse through the Western Kunlun (Xinjiang, China):Tentative Geodynamic Implications for the Paleozoic and Mesozoic.Geologische Rundschau, 85(4):705-722.doi: 10.1007/bf02440106

Meng, F.C., Cui, M.H., Wu, X.K., et al., 2013.Magmatic and Metamorphic Events Recorded in Granitic Gneisses From the Qimantag, East Kunlun Mountains, Northwest China.Acta Petrologica Sinica, 29(6):2107-2122 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-YSXB201306019.htm

Meng, F.C., Zhang, J.X., Cui, M.H., 2013.Discovery of Early Paleozoic Eclogite from the East Kunlun, Western China and Its Tectonic Significance.Gondwana Research, 23(2):825-836.doi: 10.1016/j.gr.2012.06.007

Mo, X.X., Luo, Z.H., Deng, J.F., et al., 2007.Granitoids and Crustal Growth in the East-Kunlun Orogenic Belt.Geological Journal of China Universities, 13(3):403-414(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-GXDX200703005.htm

Pearce, J.A., Harris, N.B.W., Tindle, A.G., 1984.Trace Element Discrimination Diagrams for the Tectonic Interpretation of Granitic Rocks.Journal of Petrology, 25(4):956-983.doi: 10.1093/petrology/25.4.956

Rollinson, H.R., 1993.Using Geochemical Data:Evaluation, Presentation, Interpretation.Longman Group UK Ltd., New York.

Rapp, R.P., Shimizu, N., Norman, M.D., 2003.Growth of Early Continental Crust by Partial Melting of Eclogite.Nature, 425(6958):605-609.doi: 10.1038/nature02031

Rapp, R.P., Shimizu, N., Norman, M.D., et al., 1999.Reaction Between Slab-Derived Melts and Peridotite in the Mantle Wedge:Experimental Constraints at 3.8 GPa.Chemical Geology, 160(4):335-356.doi: 10.1016/S0009-2541(99)00106-0

Ren, J.H., Liu, Y.Q., Feng, Q., et al., 2009.LA-ICP-MS U-Pb Zircon Dating and Geochemical Characteristics of Diabase-Dykes from the Qingshuiquan Area, Eastern Kunlun Orogenic Belt.Acta Petrologica Sinica, 25(5):1135-1145 (in Chinese with English abstract). http://www.oalib.com/paper/1471628

Rudnick, R.L., Gao, S., 2003.Composition of the Continental Crust.In:Rudnick, R.L., ed., The Crust.Elsevier-Pergamon, Oxford.

Salters, V.J.M., Hart, S.R., 1989.The Hafnium Paradox and the Role of Garnet in the Source of Mid-Ocean-Ridge Basalts.Nature, 342(6248):420-422.doi: 10.1038/342420a0

Schmitz, M.D., Vervoort, J.D., Bowring, S.A., et al., 2004.Decoupling of the Lu-Hf and Sm-Nd Isotope Systems during the Evolution of Granulitic Lower Crust Beneath Southern Africa.Geology, 32(5):405.doi: 10.1130/g20241.1

Söderlund, U., Patchett, P.J., Vervoort, J.D., et al., 2004.The ¹⁷⁶Lu Decay Constant Determined by Lu-Hf and U-Pb Isotope Systematics of Precambrian Mafic Intrusions.Earth and Planetary Science Letters, 219(3-4):311-324.doi: 10.1016/s0012-821x(04)00012-3

Sun, S.S., McDonough, W.F., 1989.Chemical and Isotopic Systematics of Oceanic Basalt:Implications for Mantle Composition and Processes.In:Saunders, A.D., Norry, M.J., eds., Magmatism in the Ocean Basins.Geological Society Special Publications, London, 42:313-345.doi: 10.1144/gsl.sp.1989.042.01.19

Sun, Y., Pei, X.Z., Ding, S.P., et al., 2009.Halagatu Magma Mixing Granite in the East Kunlun Mountains—Evidence from Zircon U-Pb Dating.Acta Geologica Sinica, 83(7):1000-1010(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DZXE200907009.htm

Tatsumi, Y., 1995.Subduction Zone Magmatism.Blackwell Publishing House, Boston.

Tatsumi, Y., 2001.Geochemical Modeling of Partial Melting of Subducting Sediments and Subsequent Melt-Mantle Interaction:Generation of High-Mg Andesites in the Setouchi Volcanic Belt, Southwest Japan.Geology, 29(4):323.doi:10.1130/0091-7613(2001)029<0323:gmopmo>2.0.co;2

Tatsumi, Y., Hanyu, T., 2003.Geochemical Modeling of Dehydration and Partial Melting of Subducting Lithosphere:Toward a Comprehensive Understanding of High-Mg Andesite Formation in the Setouchi Volcanic Belt, SW Japan.Geochemistry, Geophysics, Geosystems, 4(9):1-19.doi: 10.1029/2003gc000530

Vervoort, J.D., Patchett, P.J., Blichert-Toft, J., et al., 1999.Relationships between Lu-Hf and Sm-Nd Isotopic Systems in the Global Sedimentary System.Earth and Planetary Science Letters, 168(1-2):79-99. doi: 10.1016/s0012-821x(99)00047-3

Wang, G., Sun, F.Y., Li, B.Y., et al., 2014.Zircon U-Pb Geochronology and Geochemistry of Diorite in Xiarihamu Ore District from East Kunlun and Its Geological Significance.Journal of Jilin University(Earth Science Edition), 44(3):876-891 (in Chinese with English abstract). https://www.researchgate.net/publication/286738911_Zircon_U-Pb_geochronology_and_geochemistry_of_diorite_in_Xiarihamu_ore_district_from_east_Kunlun_and_its_geological_significance

Wang, Q., Xu, J.F., Zhao, Z.H., et al., 2001.The Petrogenesis and Geodynamic Significances of HREE Depleted Granitoids during Yanshan Period in the Dabie Mountains.Acta Petrologica Sinica, 17(4):551-564 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-YSXB200104005.htm

Wang, Q., Xu, J.F., Zhao, Z.H., et al., 2008.Tectonic Setting and Associated Rock Suites of Adakitic Rocks.Bulletin of Mineralogy Petrology & Geochemistry, 27(4):344-350 (in Chinese with English abstract). http://en.cnki.com.cn/article_en/cjfdtotal-kydh200804005.htm

Wang, X.X., Hu, N.G., Wang, T., et al., 2012.Late Ordovician Wanbaogou Granitoid Pluton from the Southern Margin of the Qaidam Basin:Zircon SHRIMP U-Pb Age, Hf Isotope and Geochemistry.Acta Petrologica Sinica, 28(9):2950-2962 (in Chinese with English abstract). http://www.oalib.com/paper/1474273

Wison, M., 1989.Igneous Petrogenesis.Unwim Hyman, London.

Workman, R.K., Hart, S.R., 2005.Major and Trace Element Composition of the Depleted MORB Mantle (DMM).Earth and Planetary Science Letters, 231(1-2):53-72.doi: 10.1016/j.epsl.2004.12.005

Xia, R., Qing, M., Wang, C.M., 2014.The Genesis of the Ore-Bearing Porphyry of the Tuoketuo Porphyry Cu-Au(Mo) Deposit in the East Kunlun, Qinghai Province:Constraints from Zircon U-Pb Geochronological and Geochemistry.Journal of Jilin University(Earth Science Edition), 44(5):1502-1524 (in Chinese with English abstract). https://www.researchgate.net/publication/286654334_The_genesis_of_the_ore-bearing_porphyry_of_the_Tuoketuo_porphyry_Cu-AuMo_deposit_in_the_East_Kunlun_Qinghai_Province_Constraints_from_zircon_U-Pb_geochronological_and_geochemistry

Xiong, F.H., Ma, C.Q., Jiang, H.A., et al., 2016.Geochronology and Petrogenesis of Triassic High-K Calc-Alkaline Granodiorites in the East Kunlun Orogen, West China:Juvenile Lower Crustal Melting during Post-Collisional Extension.Journal of Earth Science, 26(3):474-490. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=zddy201603012&dbname=CJFD&dbcode=CJFQ

Xiong, F.H., 2014.Spatial-Temporal Pattern, Petrogenesis and Geological Implications of Paleo-Tethyan Granitoids in the East Kunlun Orogenic Belt (Eastern Segment)(Dissertation).China University of Geosciences, Wuhan (in Chinese with English abstract).

Xiong, F.H., Ma, C.Q., Zhang, J.Y., et al., 2011.LA-ICP-MS Zircon U-Pb Dating, Elements and Sr-Nd-Hf Isotope Geochemistry of the Early Mesozoic Mafic Dyke Swarms in East Kunlun Orogenic Belt.Acta Petrologica Sinica, 27(11):3350-3364 (in Chinese with English abstract). http://www.oalib.com/paper/1476006

Xiong, F.H., Ma, C.Q., Zhang, J.Y., et al., 2012.The Origin of Mafic Microgranular Enclaves and Their Host Granodiorites from East Kunlun, Northern Qinghai-Tibet Plateau:Implications for Magma Mixing during Subduction of Paleo-Tethyan Lithosphere.Mineralogy and Petrology, 104(3-4):211-224. doi: 10.1007/s00710-011-0187-1

Xu, J.F., Shinjo, R., Defant, M.J., et al., 2002.Origin of Mesozoic Adakitic Intrusive Rocks in the Ningzhen Area of East China:Partial Melting of Delaminated Lower Continental Crust? Geology, 30(12):1111.doi:10.1130/0091-7613(2002)030<1111:oomair>2.0.co;2

Xu, Q.L., Sun, F.Y., Li, B.Y., et al., 2014.Geochronological Dating, Geochemical Characteristics and Tectonic Setting of the Granite-Porphyry in the Mohexiala Silver Polymetallic Deposit, Eastern Kunlun Orogenic Belt.Geotectonica et Metallogenia, 38(2):421-433 (in Chinese with English abstract). http://www.researchgate.net/publication/290762194_Geochronological_dating_geochemical_characteristics_and_tectonic_setting_of_the_granite-porphyry_in_the_Mohexiala_silver_polymetallic_deposit_eastern_Kunlun_Orogenic_belt

Xu, Z.Q., Yang, J.S., Jiang, M., et al., 2001.Deep Structure and Lithospheric Shear Faults in the East Kunlun-Qiangtang Region, Northern Tibetan Plateau.Science in China (Series D), 44(S1):1-9.doi: 10.1007/bf02911965

Xu, Z.Q., 2007.The Mechanism of Collage, Collision and Uplift of the Qinghai-Tibet Plateau, an Orogenic Plateau.Geology Publishing House, Beijing (in Chinese).

Yang, J.S., Robinson, P.T., Jiang, C.F., et al., 1996.Ophiolites of the Kunlun Mountains, China and Their Tectonic Implications.Tectonophysics, 258(1-4):215-231.doi: 10.1016/0040-1951(95)00199-9

Yin, H.F., Zhang, K.X., Chen, N.S., et al., 2000.The Report on the Regional Geological Survey of Donggeicuonahu.China University of Geosciences Press, Wuhan (in Chinese).

Yu, N., Jin, W., Ge, W.C., et al., 2005.Geochemical Study on Peraluminous Granite from Jinshuikou in East Kunlun.Global Geology, 24(2):123-128 (in Chinese with English abstract). https://www.researchgate.net/publication/285330320_Geochemical_study_on_peraluminous_granite_from_Jinshuikou_in_East_Kunlun

Zhang, G., 2012.Research on Geological Characteristics, Ages and Geological Significance of the Halagatu Granitic Rocks in East Segment of the East Kunlun Orogen (Dissertation).Chang'an University, Xi'an (in Chinese with English abstract). doi: 10.1007%2Fs11430-015-5151-1

Zhang, J.X., Meng, F.C., Wan, Y.S., et al., 2003.Early Paleozoic Tectono-Thermal Event of the Jinshuikou Group on the Southern Margin of Qaidam:Zircon U-Pb SHRIMP Age Evidence.Geological Bulletin of China, 22(6):397-404(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-ZQYD200306003.htm

Zhang, J.Y., Ma, C.Q., Xiong, F.H., et al., 2014.Early Paleozoic High-Mg Diorite-Granodiorite in the Eastern Kunlun Orogen, Western China:Response to Continental Collision and Slab Break-Off.Lithos, 210-211:129-146.doi: 10.1016/j.lithos.2014.10.003

Zhang, Y.L., Zhang, X.J., Hu, D.G., et al., 2010.SHRIMP Zircon U-Pb Ages of Rhyolite from the Nachitai Group in the East Kulun Orogenic Belt.Journal of Geomechanics, 16(1):21-27 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DZLX201001004.htm

Zhao, K.D., Jiang, S.Y., Sun, T., et al., 2006.The Hf-Nd Isotopes Decoupling of Indosinian Granite and Its Implication on Petrogenesis, Western of Nanling.National Symposium on Petrology and Geodynamics.Nanjing (in Chinese).

Zhao, Z.M., Ma, H.D., Wang, B.Z., et al., 2008.The Evidence of Intrusive Rocks about Collision-Orogeny during Early Devonian in Eastern Kunlun Area.Geological Review, 54(1):47-56 (in Chinese with English abstract). http://en.cnki.com.cn/article_en/cjfdtotal-dzlp200801007.htm

Zhao, T.Y., Qian, X., Feng, Q.L., 2016.Geochemistry, Zircon U-Pb Age and Hf Isotopic Constraints on the Petrogenesis of the Silurian Rhyolites in the Loei Fold Belt and Their Tectonic Implications.Journal of Earth Science, 26(3):391-402. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=zddy201603005&dbname=CJFD&dbcode=CJFQ

Zhu, Y.H., Lin, Q.X., Jia, C.X., et al., 2006.SHRIMP Zircon U-Pb Age and Significance of Early Paleozoic Volcanic Rocks in East Kunlun Orogenic Belt, Qinghai Province, China.Science in China (Series D), 49(1):88-96.doi: 10.1007/s11430-004-5317-8

Zhu, Y.H., Zhang, K.X., Chen, N.S., et al., 1999.Determination of Different Ophiolitic Belts in Eastern Kunlun Orogenic Belt and Its Tectonic Significance.Earth Science, 24(2):26-30 (in Chinese with English abstract).

陈国超, 裴先治, 李瑞保, 等, 2013.东昆仑洪水川地区科科鄂阿龙岩体锆石U-Pb年代学、地球化学及其地质意义.地质学报, 87(2):178-196. http://www.cnki.com.cn/Article/CJFDTOTAL-DZXE201302006.htm

谌宏伟, 罗照华, 莫宣学, 等, 2006.东昆仑喀雅克登塔格杂岩体的SHRIMP年龄及其地质意义.岩石矿物学杂志, 25(1):25-32. http://www.cnki.com.cn/Article/CJFDTOTAL-YSKW200601002.htm

陈亮, 孙勇, 裴先治, 等, 2003.古特提斯蛇绿岩的综合对比及其动力学意义——以德尔尼蛇绿岩为例.中国科学(D辑), 33(12):1136-1142. doi: 10.3321/j.issn:1006-9267.2003.12.002

陈有炘, 裴先治, 李瑞保, 等, 2013.东昆仑东段纳赤台岩群变火山岩锆石U-Pb年龄、地球化学特征及其构造意义.地学前缘, 20(6):240-254. http://www.cnki.com.cn/Article/CJFDTOTAL-DXQY201306032.htm

陈有炘, 裴先治, 李瑞保, 等, 2014.东昆仑东段纳赤台岩群变沉积岩地球化学特征及构造意义.现代地质, 28(3):489-500. http://www.cnki.com.cn/Article/CJFDTOTAL-XDDZ201403005.htm

崔美慧, 孟繁聪, 吴祥珂, 2011.东昆仑祁漫塔格早奥陶世岛弧:中基性火成岩地球化学、Sm-Nd同位素及年代学证据.岩石学报27(11):3365-3379. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201111017.htm

冯建赟, 裴先治, 于书伦, 等, 2010.东昆仑都兰可可沙地区镁铁－超镁铁质杂岩的发现及其LA-ICP-MS锆石U-Pb年龄.中国地质, 37(1):28-38. http://www.cnki.com.cn/Article/CJFDTOTAL-DIZI201001006.htm

高晓峰, 校培喜, 谢从瑞, 等, 2010.东昆仑阿牙克库木湖北巴什尔希花岗岩锆石LA-ICP-MS U-Pb定年及其地质意义.地质通报, 29(7):1001-1008. http://www.cnki.com.cn/Article/CJFDTOTAL-ZQYD201007007.htm

贾丽辉, 孟繁聪, 冯惠彬, 2014.榴辉岩相峰期流体活动:来自东昆仑榴辉岩石英脉的证据.岩石学报, 30(8):2339-2350. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201408016.htm

贾儒雅, 2013. 西昆仑造山带丘克苏花岗岩与暗色微粒包体岩石成因及其构造意义(硕士学位论文). 南京: 南京大学. http://cdmd.cnki.com.cn/Article/CDMD-10284-1013191626.htm

李瑞保, 裴先治, 李佐臣, 等, 2015.东昆仑南缘布青山构造混杂带得力斯坦南MOR型玄武岩地质、地球化学特征及岩石成因.地球科学, 40 (7):1148-1162. http://www.cnki.com.cn/Article/CJFDTOTAL-DQKX201507004.htm

李希, 袁万明, 郝娜娜, 等, 2014.东昆仑五龙沟花岗岩特征及其构造背景.世界地质, 33(2):275-288. http://www.cnki.com.cn/Article/CJFDTOTAL-SJDZ201402004.htm

李佐臣, 裴先治, 刘战庆, 等, 2013.东昆仑南缘布青山构造混杂岩带哥日卓托闪长岩体年代学、地球化学特征及其地质意义.地质学报, 87(8):1089-1103. http://www.cnki.com.cn/Article/CJFDTOTAL-DZXE201308006.htm

刘彬, 2011. 东昆仑跃进山早泥盆世侵入杂岩体岩石学、锆石U-Pb年代学及岩石成因(硕士学位论文). 武汉: 中国地质大学. http://cdmd.cnki.com.cn/Article/CDMD-10491-1011175515.htm

刘彬, 马昌前, 郭盼, 等, 2013a.东昆仑中泥盆世A型花岗岩的确定及其构造意义.地球科学, 38(5):947-962. http://earth-science.net/WebPage/Article.aspx?id=2780

刘彬, 马昌前, 蒋红安, 等, 2013b.东昆仑早古生代洋壳俯冲与碰撞造山作用的转换:来自胡晓钦镁铁质岩石的证据.岩石学报, 29(6):2093-2106. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201306018.htm

刘金龙, 孙丰月, 李良, 等, 2015.青海阿尼玛卿蛇绿混杂岩带西段哥日卓托杂岩体年代学、地球化学及Hf同位素.地球科学, 40(6):965-981. http://earth-science.net/WebPage/Article.aspx?id=3101

刘战庆, 裴先治, 李瑞保, 等, 2011.东昆仑南缘阿尼玛卿构造带布青山地区两期蛇绿岩的LA-ICP-MS锆石U-Pb定年及其构造意义.地质学报, 85(2):185-194. http://www.cnki.com.cn/Article/CJFDTOTAL-DZXE201102005.htm

龙晓平, 2004. 造山带锆石年代学研究——以金水口地区为例(硕士学位论文). 长春: 吉林大学. http://cdmd.cnki.com.cn/article/cdmd-10183-2004100390.htm

陆松年, 于海峰, 赵凤清, 2002.青藏高原北部前寒武纪地质初探.北京:地质出版社.

莫宣学, 罗照华, 邓晋福, 等, 2007.东昆仑造山带花岗岩及地壳生长.高校地质学报, 13(3):403-414. http://www.cnki.com.cn/Article/CJFDTOTAL-GXDX200703005.htm

孟繁聪, 崔美慧, 吴祥珂, 等, 2013.东昆仑祁漫塔格花岗片麻岩记录的岩浆和变质事件.岩石学报, 29(6):2107-2122. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201306019.htm

任军虎, 柳益群, 冯乔, 等, 2009.东昆仑清水泉辉绿岩脉地球化学及LA-ICP-MS锆石U-Pb定年.岩石学报, 25(5):1135-1145. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200905008.htm

孙雨, 裴先治, 丁仨平, 等, 2009.东昆仑哈拉尕吐岩浆混合花岗岩:来自锆石U-Pb年代学的证据.地质学报, 83(7):1000-1010. http://www.cnki.com.cn/Article/CJFDTOTAL-DZXE200907009.htm

王冠, 孙丰月, 李碧乐, 等, 2014.东昆仑夏日哈木矿区闪长岩锆石U-Pb年代学、地球化学及其地质意义.吉林大学学报(地球科学版), 44(3):876-891. http://www.cnki.com.cn/Article/CJFDTOTAL-CCDZ201403014.htm

王强, 许继锋, 赵振华, 等, 2001.大别山燕山期亏损重稀土元素花岗岩类的成因及动力学意义.岩石学报, 17(4):551-564. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200104005.htm

王强, 许继峰, 赵振华, 等, 2008.埃达克质岩的构造背景与岩石组合.矿物岩石地球化学通报, 27(4):344-350. http://www.cnki.com.cn/Article/CJFDTOTAL-KYDH200804005.htm

王晓霞, 胡能高, 王涛, 等, 2012.柴达木盆地南缘晚奥陶世万宝沟花岗岩:锆石SHRIMP U-Pb年龄、Hf同位素和元素地球化学.岩石学报, 28(9):2950-2962. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201209023.htm

熊富浩, 2014. 东昆仑造山带东段古特提斯域花岗岩类时空分布、岩石成因及其地质意义(博士学位论文). 武汉: 中国地质大学. http://cdmd.cnki.com.cn/Article/CDMD-10491-1014340842.htm

熊富浩, 马昌前, 张金阳, 等, 2011.东昆仑造山带早中生代镁铁质岩墙群LA-ICP-MS锆石U-Pb定年、元素和Sr-Nd-Hf同位素地球化学.岩石学报, 27(11):3350-3364. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201111016.htm

夏锐, 卿敏, 王长明, 2014.青海东昆仑托克妥Cu-Au(Mo)矿床含矿斑岩成因:锆石U-Pb年代学和地球化学约束.吉林大学学报(地球科学版), 44(5):1502-1524. http://www.cnki.com.cn/Article/CJFDTOTAL-CCDZ201405011.htm

许庆林, 孙丰月, 李碧乐, 等, 2014.东昆仑莫河下拉银多金属矿床花岗斑岩年代学、地球化学特征及其构造背景.大地构造与成矿学, 38(2):421-433. http://www.cnki.com.cn/Article/CJFDTOTAL-DGYK201402021.htm

许志琴, 2007.造山的高原——青藏高原的地体拼合、碰撞造山及隆升机制.北京:地质出版社.

殷鸿福, 张克信, 陈能松, 等, 2000.中华人民共和国区域地质调查报告冬给措纳湖幅.武汉:中国地质大学出版社.

余能, 金巍, 葛文春, 等, 2005.东昆仑金水口过铝花岗岩的地球化学研究.世界地质, 24(2):123-128. http://www.cnki.com.cn/Article/CJFDTOTAL-SJDZ200502004.htm

张刚, 2012. 东昆仑造山带东段哈拉尕吐花岗岩体地质特征、形成时代及地质意义(硕士学位论文). 西安: 长安大学. http://cdmd.cnki.com.cn/Article/CDMD-10710-1013017533.htm

张建新, 孟繁聪, 万渝生, 2003.柴达木盆地南缘金水口群的早古生代构造热事件:锆石U-Pb SHRIMP年龄证据.地质通报, 22(6):397-404. http://www.cnki.com.cn/Article/CJFDTOTAL-ZQYD200306003.htm

张耀玲, 张绪教, 胡道功, 等, 2010.东昆仑造山带纳赤台群流纹岩SHRIMP锆石U-Pb年龄.地质力学学报, 16(1):21-27. http://www.cnki.com.cn/Article/CJFDTOTAL-DZLX201001004.htm

赵葵东, 蒋少涌, 孙涛, 等, 2006. 南岭西段印支期花岗岩Hf-Nd同位素解耦现象及岩石成因意义. 南京: 2006年全国岩石学与地球动力学研讨会. http://cpfd.cnki.com.cn/Article/CPFDTOTAL-ZGDJ200611002253.htm

赵振明, 马华东, 王秉璋, 等, 2008.东昆仑早泥盆世碰撞造山的侵入岩证据.地质论评, 54(1):47-56. http://www.cnki.com.cn/Article/CJFDTOTAL-DZLP200801007.htm

朱云海, 张克信, 陈能松, 等, 1999.东昆仑造山带不同蛇绿岩带的厘定及其构造意义.地球科学, 24(2):26-30. http://earth-science.net/WebPage/Article.aspx?id=776

Relative Articles

Supplements(0)

Cited By

Proportional views

Proportional views

通讯作者: 陈斌, bchen63@163.com

1.
沈阳化工大学材料科学与工程学院沈阳 110142

Figures(11) / Tables(5)

Get Citation

PDF

XML

Article views (5055) PDF downloads(51)

Geochemical Characteristics of Late Ordovician Granodiorite in Gouli Area, Eastern Kunlun Orogenic Belt, Qinghai Province: Implications on the Evolution of Proto-Tethys Ocean

doi: 10.3799/dqkx.2016.129

Abstract

References

Proportional views

Catalog

通讯作者: 陈斌, bchen63@163.com

Proportional views

Export File

Citation

Format

Content