扬子克拉通北缘新元古代A型花岗岩的发现及大地构造意义

曹正琦; 蔡逸涛; 曾佐勋; 胡正祥; 陈静; 蒋幸福; 孙政权; 吴波; 刘成新; 郭盼

doi:10.3799/dqkx.2017.80

Volume 42 Issue 6

Jun. 2017

Turn off MathJax

Article Contents

Article Navigation > Earth Science > 2017 > 42(6): 957-943

Cao Zhengqi, Cai Yitao, Zeng Zuoxun, Hu Zhengxiang, Chen Jing, Jiang Xingfu, Sun Zhengquan, Wu Bo, Liu Chengxin, Guo Pan, 2017. Discovery of Neoproterozoic A-Type Granite in Northern Yangtze Craton and Its Tectonic Significance. Earth Science, 42(6): 957-943. doi: 10.3799/dqkx.2017.80

Citation:

Cao Zhengqi, Cai Yitao, Zeng Zuoxun, Hu Zhengxiang, Chen Jing, Jiang Xingfu, Sun Zhengquan, Wu Bo, Liu Chengxin, Guo Pan, 2017. Discovery of Neoproterozoic A-Type Granite in Northern Yangtze Craton and Its Tectonic Significance. Earth Science, 42(6): 957-943. doi: 10.3799/dqkx.2017.80

Citation:

Cao Zhengqi, Cai Yitao, Zeng Zuoxun, Hu Zhengxiang, Chen Jing, Jiang Xingfu, Sun Zhengquan, Wu Bo, Liu Chengxin, Guo Pan, 2017. Discovery of Neoproterozoic A-Type Granite in Northern Yangtze Craton and Its Tectonic Significance. Earth Science, 42(6): 957-943. doi: 10.3799/dqkx.2017.80

PDF( 4178 KB)

Discovery of Neoproterozoic A-Type Granite in Northern Yangtze Craton and Its Tectonic Significance

doi: 10.3799/dqkx.2017.80

1.
School of Earth Sciences, China University of Geosciences, Wuhan430074, China
2.
Hubei Institute of Geological Survey, Wuhan430034, China
3.
Nanjing Geological Survey Center, China Geological Survey, Nanjing210016, China
4.
College of Earth Sciences, East China Institute of Technology, Nanchang330013, China

Received Date: 2016-12-10
Publish Date: 2017-06-15

Abstract

Abstract

Researches on the Daleishan gneissic granites can constrain Neoproterozoic Rodinia supercontinent breakup in the northern margin of Yangtze craton. In this paper, zircon U-Pb dating, in-situ Lu-Hf isotope and whole-rock geochemical compositions analyses are presented for the Daleishan gneissic granites in the northern margin of the Yangtze craton. The results show that the Daleishan gneissic granites have high contents of SiO₂ (73.18%-77.40%) and alkali (8.07%-8.70%), but low contents of Al₂O₃ (12.11%-13.92%) and MgO (0.10%-0.34%), and display enrichment in Ga, Rb, Th, Zr, Hf but depletion in Nb, Sr, P, Ti, which indicates the post-orogenic A-type affinity. Zircons selected from two Daleishan gneissic granitic samples show typical oscillatory zone structure with high ratios of Th/U (greater than 0.5), exhibiting the magmatic zircon genesis. LA-ICP-MS (laser ablation inductively coupled plasma mass spectrometry) zircon U-Pb data from the two samples yield Neoproterozoic crystallization ages of 801.3±3.0 Ma (MSWD=0.62) and 796.1±6.3 Ma (MSWD=1.70), respectively, which are interpreted to represent the intrusion time. In-situ Hf isotopic compositions show that the two gneissic granitic samples have wide range of ε_Hf(t) values that are indicative of a heterogeneity property. ε_Hf(t) values of these zircon ranges from -7.5 to +8.0, with the positive ε_Hf(t) values, coinciding with the single phase model age (t_DM1) of the depleted mantle of (1 242-1 059 Ma), and the negative ε_Hf(t) values coinciding with two-phase model age (t_DM2) of the crustal of (1 636-1 981 Ma), suggesting that the oldest existing material in the region belongs to Paleoproterozoic (as old as 1 981 Ma). These data show that the source materials of the Daleishan A-type granites were usually derived from Palaeoproterozoic ancient crust. The magmatic source of the granites was originated from the crust-mantle migmatization, and the mantle composition could have been generated from the upwelling of the mantle magma in the extensional background. Combining with the pre-existing regional publications, it is proposed that the Daleishan A-type granite was formed at the crustal extensional background in the continental back-arc setting associated with the assembly-break up process of the Rodinia supercontinent.
- northern margin of Yangtze craton,
- Neoproterozoic,
- A-type granite,
- zircon U-Pb dating,
- Lu-Hf isotopic composition,
- petrology

FullText(HTML)

References(82)

References

Amelin, Y., Lee, D.C., Halliday, A.N., et al., 1999.Nature of the Earth Searliest Crust from Hafnium Isotopes in Single Detrital Zircons.Nature, (399):252-255. http://cat.inist.fr/?aModele=afficheN&cpsidt=1794955

Ao, W.H., Zhang, Y.K., Zhang, R.Y., et al., 2014.Neoproterozoic Crustal Accretion of the Northern Margin of Yangtze Plate:Constrains from Geochemical Characteristics, LA-ICP-MS Zircon U-Pb Chronology and Hf Isotopic Compositions of Trondhjemite from Zushidian Area, Harman Region.Geological Review, 60(6):1393-1408 (in Chinese with English abstract).

Cui, X.Z., Jiang, X.S., Wang, J., et al., 2012.Zircon Shrimp U-Pb Age of Jinkouhe Diabase Dykes in Ebian Area of Western Sichuan Province and Its Implications for the Breakup of Rodinia.Geological Bulletin of China, 31(7):1131-1141(in Chinese with English abstract).doi: 10.3969/j.issn.1671-2552.2012.07.013

Deng, Q., Wang, J., Wang, Z.J., et al., 2013.Zircon U-Pb Ages for Tuffs from the Dashigou and Sanlangpu Formations of the Xixiang Group in the Northern Margin of Yangtze Block and Their Geological Significance.Journal of Jilin University(Earth Science Edition), 43(3):797-808, 819(in Chinese with English abstract). https://www.researchgate.net/publication/257684885_Zircon_SHRIMP_U-Pb_geochronology_of_the_Neoproterozoic_Chengjiang_Formation_in_central_Yunnan_Province_SW_China_and_its_geological_significance

Diwu, C.R., Sun, Y., Liu, C.L., et al., 2007.Zircon U-Pb Ages and Hf Isotopes and Their Geological Significance of Yiyang TTG Gneisses from Henan Province, China.Acta Petrologica Sinica, 23(2):253-262(in Chinese with English abstract). https://www.researchgate.net/publication/280015308_Zircon_U-Pb_ages_and_Hf_isotopes_and_their_geological_significance_of_Yiyang_TTG_gneisses_from_Henan_province_China

Eby, G.N., 1992.Chemical Subdivision of the A-Type Granitoids:Petrogenetic and Tectonic Implications.Geology, 20:641-644. doi: 10.1130/0091-7613(1992)020<0641:CSOTAT>2.3.CO;2

Harrison, T.M., Blichert-Toft, J., Müller, W., et al., 2005.Heterogeneous Hadean Hafnium:Evidence of Continental Crust at 4.4 to 4.5 Ga.Science, 310(5756):1947-1950. doi: 10.1126/science.1117926

Jia, X.H., Wang, Q., Tang, G.J., 2009.A-Type Granites:Research Progress and Implications.Geotectonica et Metallogenia, 33(3):465-480 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DGYK200903020.htm

Jiang, X.F., Peng, S.B., Polat, A., et al., 2016.Geochemistry and Geochronology of Mylonitic Metasedimentary Rocks Associated with the Proterozoic Miaowan Ophiolite Complex, Yangtze Craton, China:Implications for Geodynamic Events.Precambrian Research, (279):37-56.doi: 10.1016/j.precamres.2016.04.004

Le Maitre, R.W., 1989.A Classification of Igneous Rocks and Glossary of Terms.Blackwell, Oxford, 193.

Li, H.K., Lu, S.N., Chen, Z.H., et al., 2003.Zircon U-Pb Geochronology of Rift-Type Volcanic Rocks of the Yaolinghe Group in the South Qinling Orogen.Geological Bulletin of China, 22(10):775-781(in Chinese with English abstract).doi: 10.3969/j.issn.1671-2552.2003.10.005

Li, X.H., Zhou, H.W., Li, Z.X., et al., 2001.Zircon U-Pb Age and Petrochemical Characteristics of the Neoproterozoic Bimodal Volcanics from Western Yangtze Block.Geochimica, 30(4):315-322(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DQHX200104002.htm

Liu, X.C., Dong, S.W., Li, S.Z., et al., 2005.Timing of the Hongan Group in Hubei:Constraints from U-Pb Dating of Metagranitic Intrusions.Geology in China, 32(1):75-81(in Chinese with English abstract).doi: 10.3969/j.issn.1000-3657.2005.01.010

Liu, Y.S., Gao, S., Hu, Z.C., et al., 2009.Continental and Oceanic Crust Recycling-Induced Melt-Peridotite Interactions in the Trans-North China Orogen:U-Pb Dating, Hf Isotopes and Trace Elements in Zircons from Mantle Xenoliths.Journal of Petrology, 51(1-2):537-571.doi: 10.1093/petrology/egp082

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

Loiselle, M.C., Wones, D.R., 1979.Characteristics and Origin of Anorogenic Granites.Geological Society of America Abstracts, 11:468.

Lu, C.Z., Dong, C.W., Gu, M.G., et al., 2006.Discorery of the Neoproterozoic Daolinshan A-Type Granite in Zhejiang and Its Tectonic Implications.Geology in China, 33(5):1044-1051(in Chinese with English abstract).doi: 10.3969/j.issn.1000-3657.2006.05.013

Lu, S.N., 1998.A Review of Advance in the Research on the Neoproterozoic Rodinia Supercontinent.Geological Review, 44(5):489-495 (in Chinese with English abstract). http://en.cnki.com.cn/article_en/cjfdtotal-dzlp199805006.htm

Lu, S.N., Li, H.K., Chen, Z.H., et al., 2004.Relationship between Neoproterozoic Cratons of China and the Rodinia.Earth Science Frontiers, 11(2):515-523(in Chinese with English abstract). https://www.researchgate.net/publication/285862139_Relationship_between_Neoproterozoic_cratons_of_China_and_the_Rodinia

Ludwig, K.R., 2003.ISOPLOT 3.00:A Geochronological Toolkit for Microsoft Excel.Berkeley Geochronology Center, Berkeley, California, 39.

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

Middlemost, E.A.K., 1985.Magmas and Magmatic Rocks.Longman, London.

Niu, B.G., Fu, Y.L., Liu, Z.G., et al., 1994.Main Tectonothermal Events and ⁴⁰Ar/³⁹Ar Dating of the Tongbai-Dabie Mts.Acta Geoscientia Sinica, 1(2):20-32(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-DQXB4Z1.004.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

Peccerillo, A., Taylor, S.R., 1976.Geochemistry of Eocene Calc-Alkaline Volcanic Rocks from the Kastamonu Area, Northern Turkey.Contributions to Mineralogy and Petrology, 58(1):63-81.doi: 10.1007/bf00384745

Peng, S.B., Kusky, T.M., Jiang, X.F., et al., 2012.Geology, Geochemistry, and Geochronology of the Miaowan Ophiolite, Yangtze Ctaton:Implications for South Chinas Amalgamation History with Rodinia Supercontinent.Gondwana Research, 21(2012):577-594. https://www.researchgate.net/publication/251666408_Geology_geochemistry_and_geochronology_of_the_Miaowan_ophiolite_Yangtze_craton_Implications_for_South_China%27s_amalgamation_history_with_the_Rodinian_supercontinent

Peng, S.B., Liu, S.F., Lin, M.S., et al., 2016a.Early Paleozoic Subduction in Cathaysia (Ⅰ):New Evidence from Nuodong Ophiolite.Earth Science, 41(5):765-778 (in Chinese with English abstract). https://www.researchgate.net/publication/305144667_Early_paleozoic_subduction_in_Cathaysia_I_New_evidence_from_Nuodong_Ophiolite

Peng, S.B., Liu, S.F., Lin, M.S., et al., 2016b.Early Paleozoic Subduction in Cathaysia(Ⅱ):New Evidence from the Dashuang High Magnesian-Magnesian Andesite.Earth Science, 41(6):931-947(in Chinese with English abstract). http://www.en.cnki.com.cn/Article_en/CJFDTOTAL-DQKX201606003.htm

Pitcher, W.S., 1993.The Nature and Origin of Granite.Blackie Academic and Professional, Chapman and Hall, London.

Qi, L., Hu, J., Gregoire, D.C., 2000.Determination of Trace Elements in Granites by Inductively Coupled Plasma-Mass Spectrometry.Talanta, 51:507-513. doi: 10.1016/S0039-9140(99)00318-5

Sun, S.S., McDonough, W.F., 1989.Chemical and Isotopic Systematics of Oceanic Basalts:Implications for Mantle Composition and Processes.Geological Society, London, Special Publications, 42(1):313-345.doi: 10.1144/gsl.sp.1989.042.01.19

Wang, D.Z., Zhao, G.T., Qiu, J.S., 1995.The Tectonic Constraint on the Late Mesozoic A-Type Granitoids in Eastern China.Geological Journal of Universities, 1(2):13-21 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-GXDX502.001.htm

Wang, M.X., Wang, Y., Zhao, J.H., 2012.Zircon U-Pb Dating and Hf-O Isotopes of the Zbouan Ultramafic Intrusion in the Northern Margin of the Yangtze Block, SW China:Constraints on the Nature of Mantle Source and Timing of the Supercontinent Rodinia Breakup.Chinese Science Bulletin, 57(34):3283-3294(in Chinese). http://mall.cnki.net/magazine/Article/JXTW201307012.htm

Wang, Q., Zhao, Z.H., Xiong, X.L., 2000.The Ascertainment of Late-Yanshanian A-Type Granite in Tongai-Dabie Orogenic Belt.Acta Petrologica et Mineralogica, 19(4):297-306(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-YSKW200004001.htm

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.doi: 10.1007/bf00402202

Wu, Y.B., Zheng, Y.F., 2004.Genesis of Zircon and Its Constraints on Interpretation of U-Pb Age.Chinese Science Bulletin, 49(16):1586-1604(in Chinese with English abstract). https://www.researchgate.net/profile/Yong-Fei_Zheng/publication/225204011_Genesis_of_zircon_and_its_constraints_on_interpretation_of_U-Pb_age/links/53fe74800cf21edafd151294.pdf

Xu, B., 2001.Recent Study of the Rodinia Supercontinent Evolution and Its Main Goal.Geological Science and Technology Information, 20(1):15-19(in Chinese with English abstract).doi: 10.3969/j.issn.1000-7849.2001.01.003

Xu, X.Y., Xia, L.Q., Chen, J.L., et al., 2009.Zircon U-Pb Dating and Geochemical Study of Volcanic Rocks from Sunjiahe Formation of Xixiang Group in Northern Margin of Yangtze Plate.Acta Petrologica Sinica, 25(12):3309-3326 (in Chinese with English abstract). https://www.researchgate.net/publication/288701911_Zircon_U-Pb_dating_and_geochemical_study_of_volcanic_rocks_from_Sunjiahe_Formation_of_Xixiang_Group_in_northern_margin_of_Yangtze_Plate

Xu, Y., Yang, K.G., Polat, A., et al., 2016.The 860 Ma Mafic Dikes and Granitoids from the Northern Margin of the Yangtze Block, China:A Record of Oceanic Subduction in the Early Neoproterozoic.Precambrian Research, 275:310-331.doi: 10.1016/j.precamres.2016.01.021

Xue, H.M., Ma, F., 2013.Detrital-Zircon Geochronology from the Metasedimentary Rocks of the Suizhou Group in the Southern Foot of the Tongbaishan Orogen and Their Geological Significance.Acta Petrologica Sinica, 29(2):564-580(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-YSXB201302016.htm

Yang, W.R., Wang, G.C., Jian, P., 2000.Study on the Tectono-Chronology of the Dabie Orogenic Belt.China University of Geosciences Press, Wuhan, 533(in Chinese).

Yang, W.R., Yang, K.G., Liu, Z.M., et al., 1999.Caledonian Tectono-Thermal Event in Tongbai-Dabie Orogenic Belt and Its Significance.Earth Science Frontiers, 6(4):247-253(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DXQY199904011.htm

Zhang, J.Y., Ma, C.Q., She, Z.B., et al., 2007.The Early Paleozoic Tiefosi Syn-Collisional Granite in the Northern Dabie Orogen:Geochronological and Geochemical Constraints.Science in China (Series D), 37(1):1-9(in Chinese). http://www.academia.edu/15502406/The_Early_Paleozoic_Tiefosi_syn-collisional_granite_in_the_northern_Dabie_Orogen_Geochronological_and_geochemical_constraints

Zhang, Q., Ran, H., Li, C.D., 2012.A-Type Granite:What is the Essence? Acta Petrologica et Mineralogica, 31(4):621-626(in Chinese with English abstract).doi: 10.3969/j.issn.1000-6524.2012.04.014

Zhang, S.M., Jiang, G.L., Liu, K.F., et al., 2014.Evolution of Neoproterozoic-Mesozoic Sedimentary Basins in Qinling-Dabie Orogenic Belt.Earth Scicnce, 39(8):1185-1199(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-DQKX201408019.htm

Zhang, Y.Z., Wang, Y.J., Guo, X.F., et al., 2015.Geochronology and Geochemistry of Cihua Neoproterozoic High-Mg Andesites in Jiangnan Orogen and Their Tectonic Implications.Earth Science, 40(11):1781-1795 (in Chinese). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DQKX201511001.htm

Zhao, J.H., Zhou, M.F., 2008.Neoproterozoic Adakitic Plutons in the Northern Margin of the Yangtze Block, China:Partial Melting of a Thickened Lower Crust and Implications for Secular Crustal Evolution.Lithos, 104(1-4):231-248.doi: 10.1016/j.lithos.2007.12.009

Zhao, J.H., Zhou, M.F., 2009.Secular Evolution of the Neoproterozoic Lithospheric Mantle underneath the Northern Margin of the Yangtze Block, South China.Lithos, 107(3-4):152-168.doi: 10.1016/j.lithos.2008.09.017

Zhao, Z.H., Xiong, X.L., Wang, Q., et al., 2008.Some Aspects on Geochemistry of Nb and Ta.Geochimica, 37(4):304-320(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DQHX200804004.htm

Zheng, Y.F., 2003, Neoproterozoic Magmatic Activity and Global Change.Chinese Science Bulletin, 48(16):1639-1656(in Chinese). doi: 10.1360/03wd0342

Zhou, J.B., Li, X.H., Ge, W.C., et al., 2007.Geochronology, Mantle Source and Geological Implications of Neoproterozoic Ultramafic Rocks from Yuanbaoshan Area of Northern Guangxi.Geological Science and Technology Information, 26(1):11-18(in Chinese with English abstract).doi: 10.3969/j.issn.1000-7849.2007.01.002

敖文昊, 张宇昆, 张瑞英, 等, 2014.新元古代扬子北缘地壳增生事件:来自汉南祖师店奥长花岗岩地球化学、锆石LA-ICP-MS U-Pb年代学和Hf同位素证据.地质论评, 60(6):1393-1408. http://www.cnki.com.cn/Article/CJFDTOTAL-DZLP201406020.htm

崔晓庄, 江新胜, 王剑, 等, 2012.川西峨边地区金口河辉绿岩脉SHRIMP锆石U-Pb年龄及其对Rodinia裂解的启示.地质通报, 31(7):1131-1141. http://www.cnki.com.cn/Article/CJFDTOTAL-ZQYD201207014.htm

邓奇, 王剑, 汪正江, 等, 2013.扬子北缘西乡群大石沟组和三郎铺组凝灰岩锆石U-Pb年龄及其地质意义.吉林大学学报(地球科学版), 43(3):797-808, 819. http://www.cnki.com.cn/Article/CJFDTOTAL-CCDZ201303016.htm

第五春荣, 孙勇, 林慈銮, 等, 2007.豫西宜阳地区TTG质片麻岩锆石U-Pb定年和Hf同位素地质学.岩石学报, 23(2):253-262. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200702007.htm

贾小辉, 王强, 唐功建, 2009.A型花岗岩的研究进展及意义.大地构造与成矿学, 33(3):465-480. http://www.cnki.com.cn/Article/CJFDTOTAL-DGYK200903020.htm

李怀坤, 陆松年, 陈志宏, 等, 2003.南秦岭耀岭河群裂谷型火山岩锆石U-Pb年代学.地质通报, 22(10):775-781. doi: 10.3969/j.issn.1671-2552.2003.10.005

李献华, 周汉文, 李正祥, 等, 2001.扬子块体西缘新元古代双峰式火山岩的锆石U-Pb年龄和岩石化学特征.地球化学, 30(4):315-322. http://www.cnki.com.cn/Article/CJFDTOTAL-DQHX200104002.htm

刘晓春, 董树文, 李三忠, 等, 2005.湖北红安群的时代:变质花岗质侵入体U-Pb定年提供的制约.中国地质, 32(1):75-81. http://www.cnki.com.cn/Article/CJFDTOTAL-DIZI200501010.htm

卢成忠, 董传万, 顾明光, 等, 2006.浙江道林山新元古代A型花岗岩的发现及其构造意义.中国地质, 33(5):1044-1051. http://www.cnki.com.cn/Article/CJFDTOTAL-DIZI200605014.htm

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. http://www.cnki.com.cn/Article/CJFDTOTAL-DZLP199805006.htm

陆松年, 李怀坤, 陈志宏, 等, 2004.新元古时期中国古大陆与罗迪尼亚超大陆的关系.地学前缘, 11(2):515-523. http://www.cnki.com.cn/Article/CJFDTOTAL-DXQY200402029.htm

牛宝贵, 富云莲, 刘志刚, 等, 1994.桐柏-大别山主要构造热事件及⁴⁰Ar/³⁹Ar地质定年研究.地球学报, 1(2):20-32.

彭松柏, 刘松峰, 林木森, 等, 2016a.华夏早古生代俯冲作用(Ⅰ):来自糯洞蛇绿岩的新证据.地球科学, 41(5):765-778. http://www.earth-science.net/WebPage/Article.aspx?id=3295

彭松柏, 刘松峰, 林木森, 等, 2016b.华夏早古生代俯冲作用(Ⅱ):大爽高镁-镁质安山岩新证据.地球科学, 41(6):931-947. http://www.earth-science.net/WebPage/Article.aspx?id=3309

王德滋, 赵广涛, 邱检生, 1995.中国东部晚中生代A型花岗岩的构造制约.高校地质学报, 1(2):13-21. http://www.cnki.com.cn/Article/CJFDTOTAL-GXDX502.001.htm

王梦玺, 王焰, 赵军红, 2012.扬子板块北缘周庵超镁铁质岩体锆石U/Pb年龄和Hf-O同位素特征:对源区性质和Rodinia超大陆裂解时限的约束.科学通报, 57(34):3283-3294. http://www.cnki.com.cn/Article/CJFDTOTAL-KXTB201234009.htm

王强, 赵振华, 熊小林, 2000.桐柏-大别造山带燕山晚期A型花岗岩的厘定.岩石矿物学杂志, 19(4):297-306. http://www.cnki.com.cn/Article/CJFDTOTAL-YSKW200004001.htm

吴元保, 郑永飞, 2004.锆石成因矿物学研究及其对U-Pb年龄解释的制约.科学通报, 49(16):1589-1604. doi: 10.3321/j.issn:0023-074X.2004.16.002

徐备, 2001.Rodinia超大陆构造演化研究的新进展和主要目标.地质科技情报, 20(1):15-19. http://www.cnki.com.cn/Article/CJFDTOTAL-DZKQ200101002.htm

徐学义, 夏林圻, 陈隽璐, 等, 2009.扬子地块北缘西乡群孙家河组火山岩形成时代及元素地球化学研究.岩石学报, 25(12):3309-3326. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200912020.htm

薛怀民, 马芳, 2013.桐柏山造山带南麓随州群变沉积岩中碎屑锆石的年代学及其地质意义.岩石学报, 29(2):564-580. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201302016.htm

杨巍然, 杨坤光, 刘忠明, 等, 1999.桐柏-大别造山带加里东期构造热事件及其意义.地学前缘, 6(4):247-253. http://www.cnki.com.cn/Article/CJFDTOTAL-DXQY199904011.htm

杨巍然, 王国灿, 简平, 2000.大别造山带构造年代学.武汉:中国地质大学出版社, 533.

张金阳, 马昌前, 佘振兵, 等, 2007.大别造山带北部铁佛寺早古生代同碰撞型花岗岩:地球化学和年代学证据.中国科学(D辑), 37(1):1-9. http://www.cnki.com.cn/Article/CJFDTOTAL-JDXK200701000.htm

张旗, 冉皞, 李承东, 2012.A型花岗岩的实质是什么?岩石矿物学杂志, 31(4):621-626. http://www.cnki.com.cn/Article/CJFDTOTAL-YSKW201302014.htm

张思敏, 姜高磊, 柳坤峰, 等, 2014.秦岭-大别新元古代-中生代沉积盆地演化.地球科学, 39(8):1185-1199. http://www.earth-science.net/WebPage/Article.aspx?id=2926

张玉芝, 王岳军, 郭小飞, 等, 2015.江南中段慈化地区新元古代高镁安山岩的厘定及其构造意义.地球科学, 40(11):1781-1795. http://www.earth-science.net/WebPage/Article.aspx?id=3185

赵振华, 熊小林, 王强, 等, 2008.铌与钽的某些地球化学问题.地球化学, 37(4):304-320. http://www.cnki.com.cn/Article/CJFDTOTAL-DQHX200804004.htm

郑永飞, 2003.新元古代岩浆活动与全球变化.科学通报, 48(16):1639-1656. http://www.cnki.com.cn/Article/CJFDTOTAL-KXTB200316000.htm

周继彬, 李献华, 葛文春, 等, 2007.桂北元宝山地区超镁铁岩的年代、源区及其地质意义.地质科技情报, 26(1):11-18. http://www.cnki.com.cn/Article/CJFDTOTAL-DZKQ200701001.htm

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(12) / Tables(5)

Get Citation

PDF

XML

Article views (4893) PDF downloads(78)

Discovery of Neoproterozoic A-Type Granite in Northern Yangtze Craton and Its Tectonic Significance

doi: 10.3799/dqkx.2017.80

Abstract

References

Proportional views

Catalog

通讯作者: 陈斌, bchen63@163.com

Proportional views

Export File

Citation

Format

Content