大兴安岭南段维拉斯托高分异花岗岩体的成因与演化及其对Sn-(Li-Rb-Nb-Ta)多金属成矿作用的制约

张天福; 郭硕; 辛后田; 张云; 何鹏; 刘文刚; 张阔; 刘传宝; 王可祥; 张超

doi:10.3799/dqkx.2018.246

Volume 44 Issue 1

Jan. 2019

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Article Navigation > Earth Science > 2019 > 44(1): 248-267

Zhang Tianfu, Guo Shuo, Xin Houtian, Zhang Yun, He Peng, Liu Wengang, Zhang Kuo, Liu Chuanbao, Wang Kexiang, Zhang Chao, 2019. Petrogenesis and Magmatic Evolution of Highly Fractionated Granite and Their Constraints on Sn-(Li-Rb-Nb-Ta) Mineralization in the Weilasituo Deposit, Inner Mongolia, Southern Great Xing'an Range, China. Earth Science, 44(1): 248-267. doi: 10.3799/dqkx.2018.246

Citation:

Zhang Tianfu, Guo Shuo, Xin Houtian, Zhang Yun, He Peng, Liu Wengang, Zhang Kuo, Liu Chuanbao, Wang Kexiang, Zhang Chao, 2019. Petrogenesis and Magmatic Evolution of Highly Fractionated Granite and Their Constraints on Sn-(Li-Rb-Nb-Ta) Mineralization in the Weilasituo Deposit, Inner Mongolia, Southern Great Xing'an Range, China. Earth Science, 44(1): 248-267. doi: 10.3799/dqkx.2018.246

Citation:

Zhang Tianfu, Guo Shuo, Xin Houtian, Zhang Yun, He Peng, Liu Wengang, Zhang Kuo, Liu Chuanbao, Wang Kexiang, Zhang Chao, 2019. Petrogenesis and Magmatic Evolution of Highly Fractionated Granite and Their Constraints on Sn-(Li-Rb-Nb-Ta) Mineralization in the Weilasituo Deposit, Inner Mongolia, Southern Great Xing'an Range, China. Earth Science, 44(1): 248-267. doi: 10.3799/dqkx.2018.246

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Petrogenesis and Magmatic Evolution of Highly Fractionated Granite and Their Constraints on Sn-(Li-Rb-Nb-Ta) Mineralization in the Weilasituo Deposit, Inner Mongolia, Southern Great Xing'an Range, China

doi: 10.3799/dqkx.2018.246

1.
Tianjin Center of China Geological Survey, Tianjin 300170, China
2.
Inner Mongolia Tenth Geological Mineral Exporation Institute, Chifeng 024005, China
3.
Inner Mongolia Geology and Exporation Limited Corporation, Hohhot 010020, China

Received Date: 2018-04-22
Publish Date: 2019-01-15

Abstract

Abstract

In recent years, great breakthroughs have been made in the deep Sn-Li prospecting in the Weilasituo area of the southern of Great Xing'an Range. However, the genesis and evolution of deep hidden rock mass closely related to the mineralization has not been studied in depth. In this paper, this cancealed granite was selected as example for a detailed geochronological, geochemical and Sr-Nd-Hf isotopic composition study in order to elucidate their petrogenesis. LA-ICP-MS U-Pb zircon age for Weilasituo pluton was 130.7±0.5 Ma (MSWD=0.53), indicating that it was generated in Early Cretaceous. Chemically, Weilasituo granite is metaluminous-(weakly) peraluminous (A/CNK concentrated in the range of 1.02-1.08), which shows high contents of silica, alkalis and natrium, low abundances of calcium, magnesium, iron and extremely low P₂O₅(< 0.01%), with high Rb/Sr, Nb/Ta and low Zr/Hf ratios. They are also enriched in Cs, Rb, Th, U, Nb, Ta, Li, F and depleted in Ba, Sr, Ti, REE elements with low LREE/HREE ratios and obviously negative Eu abnormality (δEu=0.02-0.15). Zircon saturation temperatures (691-727℃) and Zr+Nb+Ce+Y contents of Weilasituo pluton are less than those of the low-limit values of the A-type granite. Integrated geological and geochemical data suggest that the pluton was highly fractionated I-type granite. The granite has positive ε_Nd(t)(+1.10-+3.75) and relatively high ε_Hf(t)(+4.2-+8.7) and young two-stage Nd and Hf model ages (T_(Nd)DM^C=607-829 Ma; T_(Hf)DM^C=627-914 Ma), suggesting that the rock was dominantly derived from the partial melting of a juvenile lower crust with a mass of mantle magma mixed into the crust, followed by fractional crystallization during magma ascent. The Sn-(rare-metal) mineralization of the pluton was controlled jointly both by high fractionation of the magma and fluid-melt interaction during the late stage. A complete magmatic-hydrothermal system was revealed by the Sn-(rare-metal) mineralization granite with the surrounding vein ore bodies.
- highly fractionated I-type granite,
- southern of Great Xing'an Range,
- Weilasituo deposit,
- zircon U-Pb dating,
- Nd-Hf isotopes,
- rare metal,
- geochemistry

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References(95)

References

Blundy, J.D., Shimizu, N., 1991.Trace Element Evidence for Plagioclase Recycling in Calc-Alkaline Magmas.Earth and Planetary Science Letters, 102(2):178-197.https://doi.org/10.1016/0012-821x(91)90007-5 doi: 10.1016/0012-821X(91)90007-5

Boynton, W.V., 1984.Cosmochemistry of the Rare Earth Elements: Meteorite Studies.In: Henderson, P., ed., Developments in Geochemistry.Elsevier, Amsterdam, 63-144. https://arizona.pure.elsevier.com/en/publications/cosmochemistry-of-the-rare-earth-elements-meteorite-studies

Chen, B., Jahn, B.M., Tian, W., 2009.Evolution of the Solonker Suture Zone:Constraints from Zircon U-Pb Ages, Hf Isotopic Ratios and Whole-Rock Nd-Sr Isotope Compositions of Subduction-and Collision-Related Magmas and Forearc Sediments.Journal of Asian Earth Sciences, 34(3):245-257. https://doi.org/10.1016/j.jseaes.2008.05.007

Deering, C.D., Keller, B., Schoene, B., et al., 2016.Zircon Record of the Plutonic-Volcanic Connection and Protracted Rhyolite Melt Evolution.Geology, 44(4):267-270.https://doi.org/10.1130/g37539.1 doi: 10.1130/G37539.1

DePaolo, D.J., 1988.Neodymium Isotope Geochemistry.Spring-Verlag, New York.

Downes, H., Shaw, A., Williamson, B.J., et al., 1997.Sr, Nd and Pb Isotope Geochemistry of the Hercynian Granodiorites and Monzogranites, Massif Central, France.Chemical Geology, 136(1):99-122.https://doi.org/10.1016/S0009-2541(96)00141-6 http://www.sciencedirect.com/science/article/pii/S0009254197000600

Ewart, A., Griffin, W.L., 1994.Application of Proton-Microprobe Data to Trace-Element Partitioning in Volcanic Rocks.Chemical Geology, 117(1-4):251-284. https://doi.org/10.1016/0009-2541(94)90131-7

Gao, Y., Sun, Y., Zhao, Z., et al., 2017.⁴⁰Ar-³⁹Ar Dating of Muscovite from the Zhaojinggou Nb-Ta Polymetallic Deposit in Wuchuan County of Inner Mongolia and Its Geological Implications.Rock and Mineral Analysis, 36(5):551-558 (in Chinese with English abstract).

Geng, J.Z., Li, H.K., Zhang, J., et al., 2011.Zircon Hf Isotope Analysis by Means of LA-MC-ICP-MS.Geological Bulletin of China, 30(10):1508-1513 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-ZQYD201110005.htm

Griffin, W.L., Wang, X., Jackson, S.E., et al., 2002.Zircon Chemistry and Magma Mixing, SE China:In-Situ Analysis of Hf Isotopes, Tonglu and Pingtan Igneous Complexes.Lithos, 61(3-4):237-269.https://doi.org/10.1016/s0024-4937(02)00082-8 doi: 10.1016/S0024-4937(02)00082-8

Guo, G.J., 2016.Discussion on the Geological Characteristics and Genesis of the Weilasituo Tin Polymetallic Deposit in Inner Mongolia (Dissertation).China University of Geosciences, Beijing (in Chinese with English abstract).

Guo, L.X., Liu, J.M., Zeng, Q.D., 2018.Fluid Inclusion Characteristics of the Weilasituo Sn Polymetallic Ore Deposit, Inner Mongolia, China.Earth Science Frontiers, 25(1):168-181 (in Chinese with English abstract). http://d.old.wanfangdata.com.cn/Periodical/dxqy201801012

Harrison, T.M., Watson, E.B., 1984.The Behavior of Apatite during Crustal Anatexis:Equilibrium and Kinetic Considerations.Geochimica et Cosmochimica Acta, 48(7):1467-1477.https://doi.org/10.1016/0016-7037(84)90403-4 doi: 10.1016-0016-7037(84)90403-4/

Hong, D.W., Wang, S.G., Xie, X.L., et al., 2000.Genesis of Positive ε_Nd(t) Granitoids in the Da Hinggan Mts-Mongolia Orogenic Belt and Growth Continental Crust.Earth Science Frontiers, 7(2):441-456 (in Chinese with English abstract). http://en.cnki.com.cn/article_en/cjfdtotal-dxqy200002016.htm

Irber, W., 1999.The Lanthanide Tetrad Effect and Its Correlation with K/Rb, Eu/Eu^*, Sr/Eu, Y/Ho, and Zr/Hf of Evolving Peraluminous Granite Suites.Geochimica et Cosmochimica Acta, 63(3-4):489-508.https://doi.org/10.1016/s0016-7037(99)00027-7 doi: 10.1016/S0016-7037(99)00027-7

Irvine, T.N., Baragar, W.R.A., 1971.A Guide to the Chemical Classification of the Common Volcanic Rocks.Canadian Journal of Earth Sciences, 8(5):523-548. https://doi.org/10.1139/e71-055

Ishiyama, D., Sato, R., Mizuta, T., et al., 2008.Characteristic Features of Tin-Iron-Copper Mineralization in the Anle-Huanggangliang Mining Area, Inner Mongolia, China.Resource Geology, 51(4):377-392.https://doi.org/10.1111/j.1751-3928.2001.tb00109.x doi: 10.1111/j.1751-3928.2001.tb00109.x/pdf

Jiang, S.H., Liang, Q.L., Liu, Y.F., et al., 2012.Zircon U-Pb Ages of the Magmatic Rocks Occurring in and around the Dajing Cu-Ag-Sn Polymetallic Deposit of Inner Mongolia and Constrains to the Ore-Forming Age.Acta Petrologica Sinica, 28(2):495-513 (in Chinese with English abstract). http://d.old.wanfangdata.com.cn/Periodical/ysxb98201202012

Keppler, H., 1993.Influence of Fluorine on the Enrichment of High Field Strength Trace Elements in Granitic Rocks.Contributions to Mineralogy and Petrology, 114(4):479-488.https://doi.org/10.1007/bf00321752 doi: 10.1007/BF00321752

Li, J.K., Wang, C.H., Feng, W.J., et al., 2017.A Granite Pegmatite Type Lithium Mica Deposit was Found in the Northwest of Yunnan.Mineral Deposits, 36(6):1453-1455 (in Chinese).

Liao, Z., Wang, Y.W., Wang, J.B., et al., 2014.In-Situ LA-MC-ICP-MS Cassiterite U-Pb Dating of Dajing Sn Polymetallic Deposit and Its Significance.Mineral Deposits, 33(S1):421-422 (in Chinese). http://en.cnki.com.cn/Article_en/CJFDTOTAL-YSXB201403024.htm

Liu, C.S., Chen, X.M., Chen, P.R., et al., 2003.Subdivision, Discrimination Criteria and Genesis for A-Type Rock Suites.Geological Journal of China Universities, 9(4):573-591 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-GXDX200304010.htm

Liu, J.J., Xing, Y.L., Wang, J.P., et al., 2010.Discovery of Falkmanite from the Bairendaba Superlarge Ag-Pb-Zn Polymetallic Deposit, Inner Mongolia and Its Origin Significance.Journal of Jilin University (Earth Science Edition), 40(3):565-572 (in Chinese with English abstract). http://en.cnki.com.cn/article_en/cjfdtotal-ccdz201003013.htm

Liu, R.L., Wu, G., Li, T.G., et al., 2018a.LA-ICP-MS Cassiterite and Zircon U-Pb Ages of the Weilasituo Tin-Polymetallic Deposit in the Southern Great Xing'an Range and Their Geological Significance.Earth Science Frontiers, 25(5):183-201 (in Chinese with English abstract). http://d.old.wanfangdata.com.cn/Periodical/dxqy201805012

Liu, R.L., Wu, G., Chen, G.Z., et al., 2018b.Characteristics of Fluid Inclusions and H-O-C-S-Pb Isotopes of Weilasituo Sn-Polymetallic Deposit in Southern Da Hinggan Mountains.Mineral Deposit, 37(2):199-224 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-KCDZ201802001.htm

Liu, W.G., Li, G.Z., Liu, H., 2018.Micro-Fluorite Sample Digestion Technology and High Precision Thermionic Mass Spectrometry Determination for Sm-Nd Isotopes.Acta Geoscientica Sinica, 39(1):119-124 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-DQXB201801014.htm

Liu, W.G., Liu, H., Li, G.Z., 2017.The Application of Ion Exchang Resins in Sr-Nd Isotopic Assay of Geological Samples.Acta Geologica Sinica, 91(11):2584-2592 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-DZXE201711013.htm

Liu, Y.F., 2009.Metallogenic Study of Bairendaba Ag Polymetallic Deposit in Hexigten Banner.Inner Mongolia (Dissertation).Chinese Academy of Geological Sciences, Beijing (in Chinese with English abstract).

Liu, Y.F., Fan, Z.Y, Jiang, H.C., et al., 2014.Genesis of the Weilasituo-Bairendaba Porphyry-Hydrothermal Vein Type System in Inner Mongolia, China.Acta Geologica Sinica, 88(12):2373-2385 (in Chinese with English abstract).

Liu, Y.F., Jiang, S.H., Bagas, L., 2016.The Genesis of Metal Zonation in the Weilasituo and Bairendaba Ag-Zn-Pb-Cu-(Sn-W) Deposits in the Shallow Part of a Porphyry Sn-W-Rb System, Inner Mongolia, China.Ore Geology Reviews, 75:150-173. https://doi.org/10.1016/j.oregeorev.2015.12.006

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

Manning, D.A.C., 1981.The Effect of Fluorine on Liquidus Phase Relationships in the System Qz-Ab-Or with Excess Water at 1 kb.Contributions to Mineralogy and Petrology, 76(2):206-215.https://doi.org/10.1007/bf00371960 doi: 10.1007/BF00371960

McDonough, W.F., Sun, S.S., 1995.The Composition of the Earth.Chemical Geology, 120(3-4):223-253. https://doi.org/10.1016/0009-2541(94)00140-4

Mei, W., Lü, X.B., Tang, R.K., et al., 2015.Ore-Forming Fluids and Its Evolution of Bairendaba-Weilasituo Deposits in West Slope of Southern Great Xing'an Range.Earth Science, 40(1):145-162 (in Chinese with English abstract).https://doi.org/10.3799/dqkx.2015.010 http://en.cnki.com.cn/Article_en/CJFDTotal-DQKX201501010.htm

Middlemost, E.A.K., 1994.Naming Materials in the Magma/Igneous Rock System.Earth-Science Reviews, 37(3-4):215-224. https://doi.org/10.1016/0012-8252(94)90029-9

Ouyang, H.G., Mao, J.W., Santosh, M., et al., 2013.Anatomy of a Large Ag-Pb-Zn Deposit in the Great Xing'an Range, Northeast China:Metallogeny Associated with Early Cretaceous Magmatism.International Geology Review, 55(4):411-429. https://doi.org/10.1080/00206814.2012.719690

Pan, X.F., Guo, L.J., Wang, S., et al., 2009.Laser Microprobe Ar-Ar Dating of Biotite from the Weilasituo Cu-Zn Polymetallic Deposit in Inner Mongolia.Acta Petrologica et Mineralogica, 28(5):473-479 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-YSKW200905007.htm

Ren, S.K., Walshe, J.L., Paterson, R.G., et al., 1995.Magmatic and Hydrothermal History of the Porphyry-Style Deposits of the Ardlethan Tin Field, New South Wales, Australia.Economic Geology, 90(6):1620-1645. https://doi.org/10.2113/gsecongeo.90.6.1620

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.https://doi.org/10.1016/s0012-821x(04)00012-3 doi: 10.1016/S0012-821X(04)00012-3

Sylvester, P.J., 1989.Post-Collisional Alkaline Granites.The Journal of Geology, 97(3):261-280. https://doi.org/10.1086/629302

Tang, R.K., Lü, X.B., Cao, X.F., et al., 2014.Mineralogy and Metallogenic Mechanism of Weilasituo and Bairendaba Deposit, Inner Mongolia, China.Earth Science, 39(6):671-686 (in Chinese with English abstract).https://doi.org/10.3799/dqkx.2014.063

Vidal, P., Bernard-Griffiths, J., Cocherie, A., et al., 1984.Geochemical Comparison between Himalayan and Hercynian Leucogranites.Physics of the Earth and Planetary Interiors, 35(1-3):179-190. https://doi.org/10.1016/0031-9201(84)90041-4

Wang, F.X., Bagas, L., Jiang, S.H., et al., 2017.Geological, Geochemical, and Geochronological Characteristics of Weilasituo Sn-Polymetal Deposit, Inner Mongolia, China.Ore Geology Reviews, 80:1206-1229. https://doi.org/10.1016/j.oregeorev.2016.09.021

Wang, G.Z., 2002.Bao Gaigou Tin Deposit-A Hight Temperature Hydrothermal Deposit of Albitite and Biotite Quartzite Types.Geology and Prospecting, 38(2):42-45 (in Chinese with English abstract). http://www.cqvip.com/Main/Detail.aspx?id=6112687

Wang, J.B., Wang, Y.W., Wang, L.J., et al., 2001.Tin-Polymetallic Mineralization in the Southern Part of the Da Hinggan Mountains, China.Resource Geology, 51(4):283-291.https://doi.org/10.1111/j.1751-3928.2001.tb00102.x doi: 10.1111/rge.2001.51.issue-4

Wang, X.Y., Hou, Q.Y., Wang, J., et al., 2013.SHRIMP Geochronology and Hf Isotope of Zircons from Granitoids of the Weilasituo Deposit in Inner Mongolia.Geoscience, 27(1):67-78 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-XDDZ201301007.htm

Wang, Y.X., Zhao, Z.H., 1997.Geochemistry and Origin of the Baerzhe REE Nb-Be-Zr Superlarge Deposit.Geochimica, 26(1):25-26 (in Chinese with English abstract).

Whalen, J.B., Currie, K.L., Chappell, B.W., 1987.A-Type Granites:Geochemical Characteristics, Discrimination and Petrogenesis.Contributions to Mineralogy and Petrology, 95(4):407-419.https://doi.org/10.1007/bf00402202 doi: 10.1007/BF00402202

Wu, F.Y., Li, X.H., Yang, J.H., et al., 2007.Discussions on the Petrogenesis of Granites.Acta Petrologica Sinica, 23(6):1217-1238 (in Chinese with English abstract).

Wu, F.Y., Liu, X.C., Ji, W.Q., et al., 2017.Highly Fractionated Granites:Recognition and Research.Science in China (Series D), 47(7):745-765 (in Chinese). http://d.old.wanfangdata.com.cn/Periodical/dizhixb201708010

Xiao, W.J., Windley, B.F., Hao, J., et al., 2003.Accretion Leading to Collision and the Permian Solonker Suture, Inner Mongolia, China:Termination of the Central Asian Orogenic Belt.Tectonics, 22(6):1069.https://doi.org/10.1029/2002tc001484 doi: 10.1029/2002TC001484/abstract

Xiao, W.J., Zhang, L.C., Qin, K.Z., et al., 2004.Paleozoic Accretionary and Collisional Tectonics of the Eastern Tianshan (China):Implications for the Continental Growth of Central Asia.American Journal of Science, 304(4):370-395. https://doi.org/10.2475/ajs.304.4.370

Yang, J.H., Wu, F.Y., Shao, J.A., et al., 2006.Constraints on the Timing of Uplift of the Yanshan Fold and Thrust Belt, North China.Earth and Planetary Science Letters, 246(3-4):336-352. https://doi.org/10.1016/j.epsl.2006.04.029

Yang, W.B., Shan, Q., Zhao, Z.H., et al., 2011.Petrogenic and Metallogenic Action of the Alkaline Granitoids in Baerzhe Area:A Comparison between Mineralized and Barren Plutons.Journal of Jilin University (Earth Science Edition), 41(6):1689-1704 (in Chinese with English abstract).

Yao, L., Lü, Z.C., Ye, T.Z., et al., 2017.Zircon U-Pb Age, Geochemical and Nd-Hf Isotopic Characteristics of Quartz Porphyry in the Baiyinchagan Sn Polymetallic Deposit, Inner Mongolia, Southern Great Xing'an Range, China.Acta Petrologica Sinica, 33(10):3183-3199 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-YSXB201710014.htm

Zhai, D.G., Liu, J.J., Li, J.M., et al., 2016.Geochronological Study of Weilasituo Porphyry Type Sn Deposit in Inner Monglia and Its Geological Significance.Mineral Deposits, 35(5):1011-1022 (in Chinese with English abstract). http://www.en.cnki.com.cn/Article_en/CJFDTotal-KCDZ201605009.htm

Zhai, D.G., Liu, J.J., Yang, Y.Q., et al., 2012.Petrogenetic and Metallogentic Ages and Tectonic Setting of the Huanggangliang Fe-Sn Deposit, Inner Mongolia.Acta Petrologica et Mineralogica, 31(4):513-523 (in Chinese with English abstract). http://d.wanfangdata.com.cn/Periodical/yskwxzz201204004

Zhang, T.F., Sun, L.X., Zhang, Y., et al., 2016.Geochemical Characteristics of the Jurassic Yan'an and Zhiluo Formations in the Northern Margin of Ordos Basin and Their Paleoenvironmental Implications.Acta Geologica Sinica, 90(12):3454-3472 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DZXE201612013.htm

Zhao, Y.M., Zhang, D.Q., 1997.Metallogenic Regularity and Prospective Evaluation of Copper-Polymetallic Deposits in Daxing'anling and Its Adjacent Areas.Seismological Press, Beijing (in Chinese).

Zhou, Z.H., Lü, L.S., Feng, J.R., et al., 2010.Molybdenite Re-Os Ages of Huanggang Skarn Sn-Fe Deposit and Their Geological Significance, Inner Mongolia.Acta Petrologica Sinica, 26(3):667-679 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-YSXB201003003.htm

Zhou, Z.H., Mao, J.W., Lyckberg, P., 2012.Geochronology and Isotopic Geochemistry of the A-Type Granites from the Huanggang Sn-Fe Deposit, Southern Great Hinggan Range, NE China:Implication for Their Origin and Tectonic Setting.Journal of Asian Earth Sciences, 49:272-286. https://doi.org/10.1016/j.jseaes.2012.01.015

Zhu, X.Y., Zhang, Z.H., Fu, X., et al., 2016.Geological and Geochemical Characteristics of the Weilasito Sn-Zn Deposit, Inner Mongolia.Geology in China, 43(1):188-208 (in Chinese with English abstract). http://www.en.cnki.com.cn/Article_en/CJFDTotal-DIZI201601014.htm

Zong, K.Q., Klemd, R., Yuan, Y., et al., 2017.The Assembly of Rodinia:The Correlation of Early Neoproterozoic (ca.900 Ma) High-Grade Metamorphism and Continental Arc Formation in the Southern Beishan Orogen, Southern Central Asian Orogenic Belt (CAOB).Precambrian Research, 290:32-48.https://doi.org/10.1016/j.precamres.2016.12.010 http://adsabs.harvard.edu/abs/2017PreR..290...32Z

高允, 孙艳, 赵芝, 等, 2017.内蒙古武川县赵井沟铌钽多金属矿床白云母⁴⁰Ar-³⁹Ar同位素年龄及地质意义.岩矿测试, 36(5):551-558. http://d.old.wanfangdata.com.cn/Periodical/ykcs201705013

耿建珍, 李怀坤, 张健, 等, 2011.锆石Hf同位素组成的LA-MC-ICPMS测定.地质通报, 30(10):1508-1513. doi: 10.3969/j.issn.1671-2552.2011.10.004

郭贵娟, 2016.内蒙古维拉斯托锡多金属矿床地质特征及成因探讨(硕士学位论文).北京: 中国地质大学. http://cdmd.cnki.com.cn/Article/CDMD-11415-1016184693.htm

郭理想, 刘建明, 曾庆栋, 等, 2018.内蒙古维拉斯托锡多金属矿流体包裹体特征.地学前缘, 25(1):168-181. http://d.old.wanfangdata.com.cn/Periodical/dxqy201801012

洪大卫, 王式洸, 谢锡林, 等, 2000.兴蒙造山带正ε_Nd(t)值花岗岩的成因和大陆地壳生长.地学前缘, 7(2):441-456. doi: 10.3321/j.issn:1005-2321.2000.02.012

江思宏, 梁清玲, 刘翼飞, 等, 2012.内蒙古大井矿区及外围岩浆岩锆石U-Pb年龄及其对成矿时间的约束.岩石学报, 28(2):495-513. http://d.old.wanfangdata.com.cn/Periodical/ysxb98201202012

李建康, 王成辉, 冯文杰, 等, 2017.滇西北发现花岗伟晶岩型铁锂云母矿床.矿床地质, 36(6):1453-1455. http://d.old.wanfangdata.com.cn/Periodical/kcdz201706013

廖震, 王玉往, 王京彬, 等, 2014.内蒙古大井锡多金属矿床锡石LA-MC-ICP-MS U-Pb测年及其意义.矿床地质, 33(S1):421-422. http://d.old.wanfangdata.com.cn/Conference/8450485

刘昌实, 陈小明, 陈培荣, 等, 2003.A型岩套的分类、判别标志和成因.高校地质学报, 9(4):573-591. doi: 10.3969/j.issn.1006-7493.2003.04.011

刘家军, 邢永亮, 王建平, 等, 2010.内蒙拜仁达坝超大型Ag-Pb-Zn多金属矿床中针硫锑铅矿的发现与成因意义.吉林大学学报(地球科学版), 40(3):565-572. http://d.old.wanfangdata.com.cn/Periodical/cckjdxxb201003012

刘瑞麟, 武广, 李铁刚, 等, 2018a.大兴安岭南段维拉斯托锡多金属矿床LA-ICP-MS锡石和锆石U-Pb年龄及其地质意义.地学前缘, 25(5):183-201. http://d.old.wanfangdata.com.cn/Periodical/dxqy201805012

刘瑞麟, 武广, 陈公正, 等, 2018b.大兴安岭南段维拉斯托锡多金属矿床流体包裹体和同位素特征.矿床地质, 37(2):199-224. http://d.old.wanfangdata.com.cn/Periodical/kcdz201802001

刘文刚, 李国占, 刘卉, 等, 2018.微量萤石样品消解技术及其Sm-Nd同位素高精度热离子质谱法测试.地球学报, 39(1):119-124. http://d.old.wanfangdata.com.cn/Periodical/dqxb201801013

刘文刚, 刘卉, 李国占, 等, 2017.离子交换树脂在地质样品Sr-Nd同位素测定中的应用.地质学报, 91(11):2584-2592. doi: 10.3969/j.issn.0001-5717.2017.11.013

刘翼飞, 2009.内蒙古克什克腾旗拜仁达坝银多金属矿床成因研究(硕士学位论文).北京: 中国地质科学院. http://cdmd.cnki.com.cn/Article/CDMD-82501-2010024373.htm

刘翼飞, 樊志勇, 蒋胡灿, 等, 2014.内蒙古维拉斯托-拜仁达坝斑岩-热液脉状成矿体系研究.地质学报, 88(12):2373-2385. http://d.old.wanfangdata.com.cn/Periodical/dizhixb201412016

梅微, 吕新彪, 唐然坤, 等, 2015.大兴安岭南段西坡拜仁达坝-维拉斯托矿床成矿流体特征及其演化.地球科学, 40(1):145-162. http://earth-science.net/WebPage/Article.aspx?id=3022

潘小菲, 郭利军, 王硕, 等, 2009.内蒙古维拉斯托铜锌矿床的白云母Ar/Ar年龄探讨.岩石矿物学杂志, 28(5):473-479. doi: 10.3969/j.issn.1000-6524.2009.05.007

唐然坤, 吕新彪, 曹晓峰, 等, 2014.内蒙古维拉斯托-拜仁达坝矿床矿石特征及成矿机理.地球科学, 39(6):671-686. http://earth-science.net/WebPage/Article.aspx?id=2874

王国政, 2002.宝盖沟锡矿:黑英岩钠长岩型高温热液矿床.地质与勘探, 38(2):42-45. http://d.old.wanfangdata.com.cn/Periodical/dzykt200202010

王新宇, 侯青叶, 王瑾, 等, 2013.内蒙古维拉斯托矿床花岗岩类SHRIMP年代学及Hf同位素研究.现代地质, 27(1):67-78. doi: 10.3969/j.issn.1000-8527.2013.01.007

王一先, 赵振华, 1997.巴尔哲超大型稀土铌铍锆矿床地球化学和成因.地球化学, 26(1):25-26. http://www.cqvip.com/Main/Detail.aspx?id=2561982

吴福元, 李献华, 杨进辉, 等, 2007.花岗岩成因研究的若干问题.岩石学报, 23(6):1217-1238. doi: 10.3969/j.issn.1000-0569.2007.06.001

吴福元, 刘小驰, 纪伟强, 等, 2017.高分异花岗岩的识别与研究.中国科学(D辑), 47(7):745-765. http://www.cnki.com.cn/Article/CJFDTOTAL-JDXK201707001.htm

杨武斌, 单强, 赵振华, 等, 2011.巴尔哲地区碱性花岗岩的成岩和成矿作用:矿化和未矿化岩体的比较.吉林大学学报(地球科学版), 41(6):1689-1704. http://d.old.wanfangdata.com.cn/Periodical/cckjdxxb201106005

姚磊, 吕志成, 叶天竺, 等, 2017.大兴安岭南段内蒙古白音查干Sn多金属矿床石英斑岩的锆石U-Pb年龄、地球化学和Nd-Hf同位素特征及地质意义.岩石学报, 33(10):3183-3199. http://d.old.wanfangdata.com.cn/Periodical/ysxb98201710014

翟德高, 刘家军, 李俊明, 等, 2016.内蒙古维拉斯托斑岩型锡矿床成岩、成矿时代及其地质意义.矿床地质, 35(5):1011-1022. http://d.old.wanfangdata.com.cn/Periodical/kcdz201605009

翟德高, 刘家军, 杨永强, 等, 2012.内蒙古黄岗梁铁锡矿床成岩、成矿时代与构造背景.岩石矿物学杂志, 31(4):513-523. doi: 10.3969/j.issn.1000-6524.2012.04.004

张天福, 孙立新, 张云, 等, 2016.鄂尔多斯盆地北缘侏罗纪延安组、直罗组泥岩微量元素、稀土元素地球化学特征及其古沉积环境意义.地质学报, 90(12):3454-3472. doi: 10.3969/j.issn.0001-5717.2016.12.013

赵一鸣, 张德全, 1997.大兴安岭及其邻区铜多金属矿床成矿规律与远景评价.北京:地震出版社.

周振华, 吕林素, 冯佳睿, 等, 2010.内蒙古黄岗矽卡岩型锡铁矿床辉钼矿Re-Os年龄及其地质意义.岩石学报, 26(3):667-679. http://www.cqvip.com/QK/94579X/201003/1003850648.html

祝新友, 张志辉, 付旭, 等, 2016.内蒙古赤峰维拉斯托大型锡多金属矿的地质地球化学特征.中国地质, 43(1):188-208. doi: 10.3969/j.issn.1000-3657.2016.01.014

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Petrogenesis and Magmatic Evolution of Highly Fractionated Granite and Their Constraints on Sn-(Li-Rb-Nb-Ta) Mineralization in the Weilasituo Deposit, Inner Mongolia, Southern Great Xing'an Range, China

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