闽西南龙岩地区印支期天宫山花岗岩体成因

康丛轩; 周延; 宗雯; 范飞鹏; 李凤春; 孙建东; 吕劲松

doi:10.3799/dqkx.2017.602

Volume 43 Issue 12

Dec. 2018

Turn off MathJax

Article Contents

Article Navigation > Earth Science > 2018 > 43(12): 4621-4637

Kang Congxuan, Zhou Yan, Zong Wen, Fan Feipeng, Li Fengchun, Sun Jiandong, Lü Jinsong, 2018. Petrogenesis of Tiangongshan Indosinian Granites in Longyan Area, Southwest Fujian. Earth Science, 43(12): 4621-4637. doi: 10.3799/dqkx.2017.602

Citation:

Kang Congxuan, Zhou Yan, Zong Wen, Fan Feipeng, Li Fengchun, Sun Jiandong, Lü Jinsong, 2018. Petrogenesis of Tiangongshan Indosinian Granites in Longyan Area, Southwest Fujian. Earth Science, 43(12): 4621-4637. doi: 10.3799/dqkx.2017.602

Citation:

Kang Congxuan, Zhou Yan, Zong Wen, Fan Feipeng, Li Fengchun, Sun Jiandong, Lü Jinsong, 2018. Petrogenesis of Tiangongshan Indosinian Granites in Longyan Area, Southwest Fujian. Earth Science, 43(12): 4621-4637. doi: 10.3799/dqkx.2017.602

PDF( 5868 KB)

Petrogenesis of Tiangongshan Indosinian Granites in Longyan Area, Southwest Fujian

doi: 10.3799/dqkx.2017.602

1.
Nanjing Center of Geological Survey, China Geological Survey, Nanjing 210016, China
2.
School of Earth Sciences and Engineering, Hohai University, Nanjing 210016, China
3.
Geological Survey of Jiangsu Province, Nanjing 210018, China
4.
Testing Center of Shandong Bureau, China Metallurgy and Geology Bureau, Jinan 250014, China

Received Date: 2017-12-19
Publish Date: 2018-12-15

Abstract

Abstract

The research of petrogenesis about Tiangongshan Indosinian granites have great significance on the magmatic evolution and dynamic process in Southwest Fujian. The Tiangongshan pluton is dominated by syenogranite. Previous studies obtained the K-Ar age of 146-149 Ma from its granites, while U-Pb zircon analyses yielded consistent age of 233±2.0 Ma and 230±2.8 Ma by LA-ICP-MS in our study, indicating that the pluton was formed in Late Triassic and Indosinian tectonic movement. The granites are characterized by high silicon and alkali (σ=1.21-2.55, A/CNK=0.97-1.73), belonging to quasi aluminum to peraluminous calc-alkaline series. The granites have high ΣREE and relative accumulation of LREE, and are deficient in Al₂O₃ and Sr, and rich in Y and Yb, showing obvious micrographic texture with relatively high negative Eu anomaly and moderately negative to weak positive Ce anomaly; the granites are depleted in LILE and enriched in HFSE.The Tiangongshan pluton has the characteristics of A-type granite with high Ga/Al value. Its w (P₂O₅) averages on 0.02%, lower than that of highly fractionated S-type granite, w (Na₂O) on average of 2.93%, higher than that of highly fractionated S-type granite, and w (TFeO) on average of 1.15%, higher than that of highly fractionated I-type granite.The average saturation temperature of zircon is 729.8℃.The ε_Hf(t) all is negative (-5.29 to -10.69), suggesting possible material sources from the lower crustal material of Paleoproterozoic. The magma of the diagenetic stage, derived from partial melting of the crustal material, is crust-derived aluminous A-type granite formed in the syn-collisional settings. Through the stage of Indosinian collisional-compressional orogeny, the Paleoproterozoic lower crustal material of the pluton initially melted. Stretched by Indosinian tectonic movements, part of the mantle material was involved in the underplating.
- Tiangongshan granite,
- Indosinian,
- U-Pb age of zircon,
- rock formation cause,
- Lu-Hf isotope,
- geochemistry

FullText(HTML)

References(92)

References

Amelin, Y., Lee, D.C., Halliday, A.N., et al., 1999.Nature of the Earth's Earliest Crust from Hafnium Isotopes in Single Detrital Zircons.Nature, 399(6733):252-255. doi: 10.1038/20426

Anderson, T., 2002.Correction of Common Lead in U-Pb Zircon Ages that do not Report ²⁰⁴Pb.Chemical Geology, 192:59-79. doi: 10.1016/S0009-2541(02)00195-X

Belousova, E.A., Griffin, W.L., O'Reilly, S.Y., 2005.Zircon Crystal Morphology, Trace Element Signatures and Hf Isotope Composition as a Tool for Petrogenetic Modelling:Examples from Eastern Australian Granitoids.Journal of Petrology, 47(2):329-353. https://doi.org/10.1093/petrology/egi077

Belousova, E., Griffin, W., O'Reilly, S.Y., et al., 2002.Igneous Zircon:Trace Element Composition as an Indicator of Source Rock Type.Contributions to Mineralogy and Petrology, 143(5):602-622. https://doi.org/10.1007/s00410-002-0364-7

Chappell, B.W., White, A.J.R., 1974.Two Contrasting Granite Types.Pacific Geol., 8:173-174. http://d.old.wanfangdata.com.cn/NSTLQK/NSTL_QKJJ027419645/

Chen, P.R., Kong, X.G., Wang, Y.X., et al., 1999.Rb-Sr Isotopic Dating and Significance of Early Yanshanian Bimodal Volcanic-Inrusive Complex from South Jiangxi Province.Geological Journal of China Universities, 5(4):378-383 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-GXDX199904002.htm

Chen, Y.C., Wang, D.H., Xu, Z.G., et al., 2014.Outline of Regional Metallogeny of Ore Deposits Associated with the Mesozoic Magmatism in South China.Geotectonica et Metallogenia, 38(2):219-229 (in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ddgzyckx201402002

Collins, W.J., Beams, S.D., White, A.J.R., 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. https://doi.org/10.1007/bf00374895

Deng, J.F., Feng, Y.F., Di, Y.J., et al., 2016.The Intrusive Spatial Temporal Evolutional Framework in the Southeast China.Geological Review, 62(1):3-16 (in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dzlp201601002

Deng, X.G., Chen, Z.G., Li, X.H., et al., 2004.SHRIMP U-Pb Zircon Dating of the Darongshan-Shiwandashan Granitoid Belt in Southeastern Guangxi, China.Geological Review, 50(4):426-432 (in Chinese with English abstract). http://d.old.wanfangdata.com.cn/Periodical/OA000005441

Eby, G.N., 1990.The A-Type Granitoids:A Review of Their Occurrence and Chemical Characteristics and Speculations on Their Petrogenesis.Lithos, 26(1-2):115-134. https://doi.org/10.1016/0024-4937(90)90043-z

Eby, G.N., 1992.Chemical Subdivision of the A-Type Granitoids:Petrogenetic and Tectonic Implications.Geology, 20(7):641.https://doi.org/10.1130/0091-7613(1992)020<0641:csotat>2.3.co;2 doi: 10.1130/0091-7613(1992)020<0641:csotat>2.3.co;2

Ferry, J.M., Watson, E.B., 2007.New Thermodynamic Models and Revised Calibrations for the Ti-in-Zircon and Zr-in-Rutile Thermometers.Contributions to Mineralogy and Petrology, 154(4):429-437. https://doi.org/10.1007/s00410-007-0201-0

Frost, C.D., Ronald Frost, B., 1997.Reduced Rapakivi-Type Granites:The Tholeiite Connection.Geology, 25(7):647.https://doi.org/10.1130/0091-7613(1997)025<0647:rrtgtt>2.3.co;2 doi: 10.1130/0091-7613(1997)025<0647:rrtgtt>2.3.co;2

Gilder, S.A., Gill, J., Coe, R.S., et al., 1996.Isotopic and Paleomagnetic Constraints on the Mesozoic Tectonic Evolution of South China.Journal of Geophysical Research(Solid Earth), 101(B7):16137-16154. https://doi.org/10.1029/96jb00662

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

Guo, C.L., Zheng, J.H., Lou, F.S., et al., 2012.Petrography, Genetic Types and Geological Dynamical Settings of the Indosinian Granitoids in South China.Geotectonica et Metallogenia, 36(3):457-472 (in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ddgzyckx201203020

Hoskin, P.W.O., 2003.The Composition of Zircon and Igneous and Metamorphic Petrogenesis.Reviews in Mineralogy and Geochemistry, 53(1):27-62. https://doi.org/10.2113/0530027

Jian, P., Cheng, Y.Q., Liu, D.Y., 2001.Petrographical Study of Metamorphic Zircon:Basic Roles in Interpretation of U-Pb Age of High Grade Metamorphic Rocks.Earth Science Frontiers, 8(3):183-191 (in Chinese with English abstract).

Kang, C.X., Zhou, Y., Fan, F.P., et al., 2017.Geochemical Characteristic, Zircon U-Pb Ages, and Lu-Hf Isotopic Compositions of the Yongfu Pluton in Longyan, Fujian Province.Geotectonica et Metallogenia, 41(5):960-973 (in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ddgzyckx201705012

Kemp, A.I.S., Wormald, R.J., Whitehouse, M.J., et al., 2005.Hf Isotopes in Zircon Reveal Contrasting Sources and Crystallization Histories for Alkaline to Peralkaline Granites of Temora, Southeastern Australia.Geology, 33(10):797. https://doi.org/10.1130/g21706.1

King, P.L., White, A.J.R., Chappell, B.W., et al., 1997.Characterization and Origin of Aluminous A-Type Granites from the Lachlan Fold Belt, Southeastern Australia.Journal of Petrology, 38(3):371-391. https://doi.org/10.1093/petroj/38.3.371

Li, R.B., Pei, X.Z., Ding, S.P., et al., 2009.LA-ICP-MS Zircon U-Pb Dating of the Pipasi Basic Volcanic Rocks within the Mian-Lue Tectonic Zone in the Southern Margin of West Qinling and Its Geological Implication.Acta Geologica Sinica, 83(11):1612-1623 (in Chinese with English abstract).

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://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=gxdzxb200304011

Liu, Y., Deng, J., Wang, Z.L., et al., 2014.Zircon U-Pb Age Lu-Hf Isotopes and Petrogeochemistry of the Monzogranites from Xincheng Gold Deposit, Northwestern Jiaodong Peninsula, China.Acta Petrologica Sinica, 30(9):2559-2573 (in Chinese with English abstract). http://d.old.wanfangdata.com.cn/Periodical/ysxb98201409009

Loiselle, M., Wones, D., 1979.Characteristics and Origin of Anorogenic Granites.Geological Society of America, 11(7):468. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=9108a701005035f04fb9accc13dc243b

Ludwig, K.R., 2008.Isoplot 3.0-A Geochronological Tool Kit for Microsoft Excel.Berkeley Geochronology Center, Berkeley.

Mao, J.R., Li, Z.L., Ye, H.M., 2014.Mesozoic Tectono-Magmatic Activities in South China:Retrospect and Prospect.Science in China (Series D:Earth Sciences), 44(12):2593-2617 (in Chinese with English abstract). doi: 10.1007/s11430-014-5006-1

Mao, J.R., Xu, N.Z., Hu, Q., et al., 2004.The Mesozoic Rock-Forming and Ore-Forming Processes and Tectonic Environment Evolution in Shanghang-Datian Region, Fujian.Acta Petrologica Sinica, 20(2):285-296 (in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ysxb98200402010

Middlemost, E.A.K., 1985.Magmas and Magmatic Rocks: An Introduction to Igneous Petrology.Longman, London.

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

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. https://doi.org/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. https://doi.org/10.1007/bf00384745

Qiu, J.S., Li, Z., Liu, L., et al., 2012.Petrogenesis of the Zhangpu Composite Granite Pluton in Fujian Province:Constraints from Zircon U-Pb Ages, Elemental Geochemistry and Nd-Hf Isotopes.Acta Geologica Sinica, 86(4):561-576 (in Chinese with English abstract). http://www.cnki.com.cn/Article/CJFDTotal-DZXE201204003.htm

Rowley, D.B., Ziegler, A.M., Gyou, N., et al., 1989.Comment and Reply on "Mesozoic Overthrust Tectonics in South China".Geology, 17(4):384. doi: 10.1130/0091-7613(1989)017<0384:CAROMO>2.3.CO;2

Sláma, J., Košler, J., Condon, D.J., et al., 2008.Plešovice Zircon-A New Natural Reference Material for U-Pb and Hf Isotopic Microanalysis.Chemical Geology, 249(1-2):1-35. https://doi.org/10.1016/j.chemgeo.2007.11.005

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. https://doi.org/10.1144/gsl.sp.1989.042.01.19

Turner, S.P., Foden, J.D., Morrison, R.S., 1992.Derivation of Some A-Type Magmas by Fractionation of Basaltic Magma:An Example from the Padthaway Ridge, South Australia.Lithos, 28(2):151-179. https://doi.org/10.1016/0024-4937(92)90029-x

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. https://doi.org/10.1016/s0012-821x(99)00047-3

Wang, Q., Zhao, Z.H., Xiong, X.L., 2000.The Ascertainment of Late-Yanshanian A-Type Granite in Tongbai-Dabie Orogenic Belt.Acta Petrologica et Mineralogica, 19(4):297-306 (in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=yskwxzz200004002

Wang, Y.J., Fan, W.M., Guo, F., et al., 2003.Geochemistry of Mesozoic Mafic Rocks Adjacent to the Chenzhou-Linwu Fault, South China:Implications for the Lithospheric Boundary between the Yangtze and Cathaysia Blocks.International Geology Review, 45(3):263-286. https://doi.org/10.2747/0020-6814.45.3.263

Wang, Y.J., Fan, W.M., Peng, T.P., et al., 2004.Elemental and Sr-Nd Isotopic Systematics of the Early Mesozoic Volcanic Sequence in Southern Jiangxi Province, South China:Petrogenesis and Tectonic Implications.International Journal of Earth Sciences, 94(1):53-65. https://doi.org/10.1007/s00531-004-0441-4

Wang, Z.L., Gong, Q.J., Sun, X., et al., 2012.LA-ICP-MS Zircon U-Pb Geochronology of Quartz Porphyry from the Niutougou Gold Deposit in Songxian County, Henan Province.Acta Geologica Sinica (English Edition), 86(2):370-382. https://doi.org/10.1111/j.1755-6724.2012.00666.x

Watson, E.B., Harrison, T.M., 1983.Zircon Saturation Revisited:Temperature and Composition Effects in a Variety of Crustal Magma Types.Earth and Planetary Science Letters, 64(2):295-304. https://doi.org/10.1016/0012-821x(83)90211-x

Watson, E.B., Wark, D.A., Thomas, J.B., 2006.Crystallization Thermometers for Zircon and Rutile.Contributions to Mineralogy and Petrology, 151(4):413-433. https://doi.org/10.1007/s00410-006-0068-5

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

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). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ysxb98200706001

Wu, S.P., Wang, M.Y., Qi, K.J., 2007.Present Situation of Researches on A-Type Granites:A Review.Acta Petrologica et Mineralogica, 26(1):57-66 (in Chinese with English abstract).

Wu, Y.B., Zheng, Y.F., 2004.Genesis of Zircon and Its Constraints on Interpretation of U-Pb Age.Chinese Science Bulletin, 49(15):1554-1569. https://doi.org/10.1007/bf03184122

Xu, B.L., Yan, G.H., Zhang, C., et al., 1998.Petrological Subdivision and Source Material of A-Type Granites.Earth Science Frontiers, 5(3):113-124 (in Chinese with English abstract).

Xu, X.B., Li, Y., Xue, D.J., et al., 2014.Deformation Characteristics and Geochronological Constraints of Late Mesozoic Extensional Structures in Quanzhou, Fujian Province.Earth Science, 39(1):45-63 (in Chinese with English abstract). http://d.old.wanfangdata.com.cn/Periodical/dqkx201401005

Xu, X.B., Zhang, Y.Q., Jia, D., et al., 2009.Early Mesozoic Geotectonic Processes in South China.Geology in China, 36(3):573-593 (in Chinese with English abstract). http://d.old.wanfangdata.com.cn/Periodical/zgdizhi200903007

Xu, X.S., O'Reilly, S.Y., Griffin, W.L., et al., 2003.Enrichment of Upper Mantle Peridotite:Petrological, Trace Element and Isotopic Evidence in Xenoliths from SE China.Chemical Geology, 198(3-4):163-188. https://doi.org/10.1016/s0009-2541(03)00004-4

Yang, J.H., Wu, F.Y., Chung, S.L., et al., 2006a.A Hybrid Origin for the Qianshan A-Type Granite, Northeast China:Geochemical and Sr-Nd-Hf Isotopic Evidence.Lithos, 89(1-2):89-106. https://doi.org/10.1016/j.lithos.2005.10.002

Yang, J.H., Wu, F.Y., Wilde, S.A., et al., 2006b.Tracing Magma Mixing in Granite Genesis:In Situ U-Pb Dating and Hf-Isotope Analysis of Zircons.Contributions to Mineralogy and Petrology, 153(2):177-190. https://doi.org/10.1007/s00410-006-0139-7

Zhang, C.S., Su, H.M., Yu, M., et al., 2012.Zircon U-Pb Age and Nd-Sr-Pb Isotopic Characteristics of Dayang-Juzhou Granite in Longyan, Fujian Province and Its Geological Significance.Acta Petrologica Sinica, 28(1):225-242 (in Chinese with English abstract). http://d.old.wanfangdata.com.cn/Periodical/ysxb98201201017

Zhang, K.X., Pan, G.T., He, W.H., et al., 2015.New Division of Tectonic-Strata Superregion in China.Earth Science, 40(2):206-233 (in Chinese with English abstract). https://doi.org/10.3799/dqkx.2015.016

Zhang, Q., 2013.The Criteria and Discrimination for A-Type Granites:A Reply to the Question Put forward by Wang Yang and Some Other Persons for A-Type Granite:What is the Essence?.Acta Petrologica et Mineralogica, 32(2):267-274 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-YSKW201302014.htm

Zhang, Q., Pan, G.Q., Li, C.D., et al., 2007.Are Discrimination Diagrams always Indicative of Correct Tectonic Settings of Granites? Some Crucial Questions on Granite Study (3).Acta Petrologica Sinica, 23(11):2683-2698 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-YSXB200711003.htm

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). http://d.old.wanfangdata.com.cn/OAPaper/oai_doaj-articles_8c2890609571b9a5f39733c2b59b003c

Zhang, W.L., Hua, R.M., Wang, R.C., et al., 2004.Single Zircon U-Pb Isotopic Age of the Wuliting Granite in Dajishan Area of Jiangxi, and Its Geological Implication.Acta Geologica Sinica, 78(3):352-358 (in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dizhixb200403008

Zhang, Y.Q., Xu, X.B., Jia, D., et al., 2009.Deformation Record of the Change from Indosinian Collision-Related Tectonic System to Yanshanian Subduction-Related Tectonic System in South China during the Early Mesozoic.Earth Science Frontiers, 16(1):234-247 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DXQY200901033.htm

Zhao, J.L., Qiu, J.S., Li, Z., et al., 2012.Petrogenesis of the Taiwushan Granite Pluton in Fujian Province:Constraints from Zircon U-Pb Ages and Hf Isotopes.Acta Petrologica Sinica, 28(12):3938-3950 (in Chinese with English abstract). http://d.old.wanfangdata.com.cn/Periodical/ysxb98201212012

Zhao, X.L., Mao, J.R., Ye, H.M, et al., 2009.The Geochemical Characteristics of Biotite and Its Petrogenesis Implication in the Caixi Pluton and Sifang Pluton from Shanghang Area of Fujian Province.Bulletin of Mineralogy, Petrology and Geochemistry, 28(2):162-168 (in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=kwysdqhxtb200902010

陈培荣, 孔兴功, 王银喜, 等, 1999.赣南燕山早期双峰式火山-侵入杂岩的Rb-Sr同位素定年及意义.高校地质学报, 5(4):378-383. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=QK199900178513

陈毓川, 王登红, 徐志刚, 等, 2014.华南区域成矿和中生代岩浆成矿规律概要.大地构造与成矿学, 38(2):219-229. http://d.old.wanfangdata.com.cn/Periodical/ddgzyckx201402002

邓晋福, 冯艳芳, 狄永军, 等, 2016.华南地区侵入岩时空演化框架.地质论评, 62(1):3-16. http://d.old.wanfangdata.com.cn/Periodical/dzlp201601002

邓希光, 陈志刚, 李献华, 等, 2004.桂东南地区大容山-十万大山花岗岩带SHRIMP锆石U-Pb定年.地质论评, 50(4):426-432. doi: 10.3321/j.issn:0371-5736.2004.04.014

郭春丽, 郑佳浩, 楼法生, 等, 2012.华南印支期花岗岩类的岩石特征、成因类型及其构造动力学背景探讨.大地构造与成矿学, 36(3):457-472. doi: 10.3969/j.issn.1001-1552.2012.03.020

简平, 程裕淇, 刘敦一, 2001.变质锆石成因的岩相学研究——高级变质岩U-Pb年龄解释的基本依据.地学前缘, 8(3):183-191. doi: 10.3321/j.issn:1005-2321.2001.03.022

康丛轩, 周延, 范飞鹏, 等, 2017.福建龙岩永福岩体锆石U-Pb年龄、地球化学特征及Lu-Hf同位素组成.大地构造与成矿学, 41(5):960-973. http://d.old.wanfangdata.com.cn/Periodical/ddgzyckx201705012

李瑞保, 裴先治, 丁仨平, 等, 2009.西秦岭南缘勉略带琵琶寺基性火山岩LA-ICP-MS锆石U-Pb年龄及其构造意义.地质学报, 83(11):1612-1623. doi: 10.3321/j.issn:0001-5717.2009.11.006

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

刘跃, 邓军, 王中亮, 等, 2014.胶西北新城金矿床二长花岗岩岩石地球化学、锆石U-Pb年龄及Lu-Hf同位素组成.岩石学报, 30(9):2559-2573. http://d.old.wanfangdata.com.cn/Periodical/ysxb98201409009

毛建仁, 厉子龙, 叶海敏, 2014.华南中生代构造-岩浆活动研究:现状与前景.中国科学(D辑:地球科学), 44(12):2593-2617. http://www.cnki.com.cn/Article/CJFDTotal-JDXK201412001.htm

毛建仁, 许乃政, 胡青, 等, 2004.福建省上杭-大田地区中生代成岩成矿作用与构造环境演化.岩石学报, 20(2):285-296. http://d.old.wanfangdata.com.cn/Periodical/ysxb98200402010

邱检生, 李真, 刘亮, 等, 2012.福建漳浦复式花岗岩体的成因:锆石U-Pb年代学、元素地球化学及Nd-Hf同位素制约.地质学报, 86(4):561-576. doi: 10.3969/j.issn.0001-5717.2012.04.003

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. doi: 10.3969/j.issn.1000-6524.2000.04.002

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

吴锁平, 王梅英, 戚开静, 2007.A型花岗岩研究现状及其述评.岩石矿物学杂志, 26(1):57-66. doi: 10.3969/j.issn.1000-6524.2007.01.009

许保良, 阎国翰, 张臣, 等, 1998.A型花岗岩的岩石学亚类及其物质来源.地学前缘, 5(3):113-124. doi: 10.3321/j.issn:1005-2321.1998.03.011

徐先兵, 李源, 薛德杰, 等, 2014.福建泉州晚中生代伸展构造变形特征与年代学制约.地球科学, 39(1):45-63. http://earth-science.net/WebPage/Article.aspx?id=2828

徐先兵, 张岳桥, 贾东, 等, 2009.华南早中生代大地构造过程.中国地质, 36(3):573-593. doi: 10.3969/j.issn.1000-3657.2009.03.007

张承帅, 苏慧敏, 于淼, 等, 2012.福建龙岩大洋-莒舟花岗岩锆石U-Pb年龄和Sr-Nd-Pb同位素特征及其地质意义.岩石学报, 28(1):225-242. http://d.old.wanfangdata.com.cn/Periodical/ysxb98201201017

张克信, 潘桂棠, 何卫红, 等, 2015.中国构造-地层大区划分新方案.地球科学, 40(2):206-233. http://earth-science.net/WebPage/Article.aspx?id=3179

张旗, 2013.A型花岗岩的标志和判别——兼答汪洋等对"A型花岗岩的实质是什么"的质疑.岩石矿物学杂志, 32(2):267-274. doi: 10.3969/j.issn.1000-6524.2013.02.014

张旗, 潘国强, 李承东, 等, 2007.花岗岩构造环境问题:关于花岗岩研究的思考之三.岩石学报, 23(11):2683-2698. doi: 10.3969/j.issn.1000-0569.2007.11.002

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. doi: 10.3969/j.issn.1000-6524.2012.04.014

张文兰, 华仁民, 王汝成, 等, 2004.江西大吉山五里亭花岗岩单颗粒锆石U-Pb同位素年龄及其地质意义探讨.地质学报, 78(3):352-358. doi: 10.3321/j.issn:0001-5717.2004.03.008

张岳桥, 徐先兵, 贾东, 等, 2009.华南早中生代从印支期碰撞构造体系向燕山期俯冲构造体系转换的形变记录.地学前缘, 16(1):234-247. doi: 10.3321/j.issn:1005-2321.2009.01.026

赵姣龙, 邱检生, 李真, 等, 2012.福建太武山花岗岩体成因:锆石U-Pb年代学与Hf同位素制约.岩石学报, 28(12):3938-3950. http://d.old.wanfangdata.com.cn/Conference/7863327

赵希林, 毛建仁, 叶海敏, 等, 2009.福建省上杭地区晚中生代花岗质岩体黑云母的地球化学特征及成因意义.矿物岩石地球化学通报, 28(2):162-168. doi: 10.3969/j.issn.1007-2802.2009.02.010

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(13) / Tables(6)

Get Citation

PDF

XML

Article views (4710) PDF downloads(25)

Petrogenesis of Tiangongshan Indosinian Granites in Longyan Area, Southwest Fujian

doi: 10.3799/dqkx.2017.602

Abstract

References

Proportional views

Catalog

通讯作者: 陈斌, bchen63@163.com

Proportional views

Export File

Citation

Format

Content