华北中部造山带五台-恒山地区古元古代变质作用与构造演化

魏春景

doi:10.3799/dqkx.2018.002

Volume 43 Issue 1

Jan. 2018

Turn off MathJax

Article Contents

Article Navigation > Earth Science > 2018 > 43(1): 24-43

Wei Chunjing, 2018. Paleoproterozoic Metamorphism and Tectonic Evolution in Wutai-Hengshan Region, Trans-North China Orogen. Earth Science, 43(1): 24-43. doi: 10.3799/dqkx.2018.002

Citation:

Wei Chunjing, 2018. Paleoproterozoic Metamorphism and Tectonic Evolution in Wutai-Hengshan Region, Trans-North China Orogen. Earth Science, 43(1): 24-43. doi: 10.3799/dqkx.2018.002

Wei Chunjing, 2018. Paleoproterozoic Metamorphism and Tectonic Evolution in Wutai-Hengshan Region, Trans-North China Orogen. Earth Science, 43(1): 24-43. doi: 10.3799/dqkx.2018.002

Citation:

Wei Chunjing, 2018. Paleoproterozoic Metamorphism and Tectonic Evolution in Wutai-Hengshan Region, Trans-North China Orogen. Earth Science, 43(1): 24-43. doi: 10.3799/dqkx.2018.002

PDF( 8577 KB)

Paleoproterozoic Metamorphism and Tectonic Evolution in Wutai-Hengshan Region, Trans-North China Orogen

doi: 10.3799/dqkx.2018.002

Wei Chunjing

The Key Laboratory of Orogenic Belts and Crustal Evolution, Ministry of Education; School of Earth and Space Sciences, Peking University, Beijing 100871, China

Received Date: 2017-08-22
Publish Date: 2018-01-15

Abstract

Abstract

The tempo-spatial distribution and tectonic attribute of the Paleoproterozoic orogens of the North China Craton (NCC) are strongly controversial. One model argues that three times of continental collision occurred sequentially during the period of 1.85-1.95 Ga in the NCC, resulted in the formation of three Paleoproterozoic orogens, i.e. the Khondalite belt, Jiao-Liao-Ji belt and the Trans-North China orogen (TNCO). The other model contests that the above three orogens may have experienced the same long-lived evolutional history within the period of 1.80-1.98 Ga, suggesting particular hot subduction and collision in Paleoproterozoic. Summarizing the recent advances of the study on metamorphism in the Wutai-Hengshan region, this paper presents the time and tectonic attribute of the Paleoproterozoic orogeny. The main litho-structural units in the Wutai-Hengshan region include the Hengshan complex, Wutai complex and Hutuo Group. The Hengshan and Wutai complexes are recognized to have undergone two phases of metamorphism. The first phase was identified to be a medium-pressure type, which was attributed to resulting from a crust thickening orogeny related to the closure of back-arc basins due to continental collision. A progressive metamorphic series can be revealed, including, from south to north, the low-amphibolite facies of the lower Wutai Group and the southern part of the south Hengshan complex, the high-amphibolite facies of the northern part of the south Hengshan complex and the high-pressure granulite facies of the north Hengshan complex, with their pressure peak conditions corresponding to a geothermal gradient of~15℃/km. With increasing in metamorphic grade, the peak ages from metamorphic zircons show a decreasing trend, which are~1.95 Ga, ~1.92 Ga and~1.85 Ga for the low-amphibolite, high-amphibolite and granulite facies rocks respectively. This is because zircon growth during metamorphism depends on the behaviors of fluids and melts, which results in that metamorphic zircons tend to record the time of the peak stages for metamorphism under subsolidus conditions, but to date the retrograde stage with melt crystallization during metamorphism under suprasolidus conditions. As a result, the pressure peak stage of the medium-pressure type metamorphism is determined to be~1.95 Ga, also equivalent to the peak stage of the crust-thickening orogeny. Due to gravity isostasy in the thickening crust region, metamorphic rocks may exhume from deep crust to middle crust, displaying as the post-peak isothermal decompression (ITD) to 0.5-0.7 GPa in P-T paths, and suggested from the 'white eye socket' textures formed by the decomposition of peak garnet under fluid-absent conditions. The metamorphic zircon ages of 1.92 Ga from the high-amphibolite facies rocks of the northern part of the south Hengshan complex were interpreted to represent the decompression of medium-pressure rocks, also constraining the termination of the first-phase orogeny. The second phase of metamorphism is inferred to be a low-pressure type, resulted from deformation within-plate, and displaying as the formation of equilibrium assemblages that overprinted the exhumed medium-pressure rocks triggered by compressional shearing and fluid infiltration. The Zhujiafang shearing belt could be a high-strain zone produced in this within-plate deformation, which also records a clockwise P-T path, but indicating limited crustal thickening. The second phase of metamorphism and deformation was constrained to occur mainly at~1.85 Ga. The sinistral strike-slip of the Zhujiafang shearing belt may have resulted in the uplifting of the north Hengshan granulite terranes. Two phases of metamorphism and deformation were proposed to have occurred within the period of 1.80-1.96 Ga in the Wutai-Hengshan region, which could be significant for discussing the Paleoproterozoic orogenic evolution from the other domains in the NCC.
- metamorphism,
- P-T path,
- Hengshan complex,
- Wutai complex,
- tectonic evolution,
- Trans-North China orogen,
- petrology

FullText(HTML)

References(97)

References

Bai, J., 1986.The Early Precambrian Geology of Wutaishan.Tianjin Science and Technology Press, Tianjin (in Chinese).

Chen, B., Liu, S.W., Wang, R., et al., 2006.Nd-Sr Isotopic Geochemistry of the Late Archean-Paleoproterozoic Granitoids in the Lüliang-Wutai Terrain, North China Craton, and Implications for Petrogenesis.Acta Geologica Sinica (English Edition), 80(6):834-843. https://doi.org/10.1111/j.1755-6724.2006.tb00306.x

Du, L.L., Yang, C.H., Guo, J.H., et al., 2010.The Age of the Base of the Paleoproterozoic Hutuo Group in the Wutai Mountains Area, North China Craton:SHRIMP Zircon U-Pb Dating of Basaltic Andesite.Chinese Science Bulletin, 55(3):246-254 (in Chinese). doi: 10.1007/s11434-009-0690-5

Du, L.L., Yang, C.H., Ren, L.D., et al., 2009.Petrology, Geochemistry and Petrogenesis of the Metabasalts of the Hutuo Group, Wutai Mountain, Shanxi, China.Geological Bulletin of China, 28(7):867-876 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-ZQYD200907008.htm

Du, L.L., Yang, C.H., Wang, W., et al., 2011.The Re-Examination of the Age and Stratigraphic Subdivision of the Hutuo Group in the Wutai Mountains Area, North China Craton:Evidences from Geology and Zircon U-Pb Geochronology.Acta Petrologica Sinica, 27(4):1037-1055 (in Chinese with English abstract). http://www.oalib.com/paper/1475349

Du, L.L., Yang, C.H., Wang, W., et al., 2013.Paleoproterozoic Rifting of the North China Craton:Geochemical and Zircon Hf Isotopic Evidence from the 2 137 Ma Huangjinshan A-Type Granite Porphyry in the Wutai Area.Journal of Asian Earth Sciences, 72:190-202. https://doi.org/10.1016/j.jseaes.2012.11.040

Guiraud, M., Powell, R., Rebay, G., 2001.H₂O in Metamorphism and Unexpected Behaviour in the Preservation of Metamorphic Mineral Assemblages.Journal of Metamorphic Geology, 19(4):445-454. https://doi.org/10.1046/j.0263-4929.2001.00320.x

Guo, J.H., Zhai, M.G., Li, Y.G., et al., 1999.Metamorphism, Pt Paths and Tectonic Significance of Garnet Amphibolite and Granulite from Hengshan, North China Craton.Scientia Geologica Sinica, 34(3):311-325 (in Chinese with English abstract). doi: 10.1007/BF03187002

Jia, X.M., 2007.Study on the Mineralogy and Chronology of the Nianzigou Rutile Ore Deposit in Daixian County, Shanxi Province (Dissertation).China University of Geosciences, Beijing (in Chinese with English abstract).

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

Kelsey, D.E., Powell, R., 2011.Progress in Linking Accessory Mineral Growth and Breakdown to Major Mineral Evolution in Metamorphic Rocks:A Thermodynamic Approach in the Na₂O-CaO-K₂O-FeO-MgO-Al₂O₃-SiO₂-H₂O-TiO₂-ZrO₂ System.Journal of Metamorphic Geology, 29(1):151-166. https://doi.org/10.1111/j.1525-1314.2010.00910.x

Kröner, A., Wilde, S.A., Li, J.H., et al., 2005a.Age and Evolution of a Late Archean to Paleoproterozoic Upper to Lower Crustal Section in the Wutaishan/Hengshan/Fuping Terrain of Northern China.Journal of Asian Earth Sciences, 24(5):577-595. https://doi.org/10.1016/j.jseaes.2004.01.001

Kröner, A., Wilde, S.A., O'Brien, P.J., et al., 2005b.Field Relationships, Geochemistry, Zircon Ages and Evolution of a Late Archean to Paleoproterozoic Lower Crustal Section in the Hengshan Terrain of Northern China.Acta Geologica Sinica (English Edition), 79(5):605-629.

Kröner, A., Wilde, S.A., Zhao, G.C., et al., 2006.Zircon Geochronology and Metamorphic Evolution of Mafic Dykes in the Hengshan Complex of Northern China:Evidence for Late Palaeoproterozoic Extension and Subsequent High-Pressure Metamorphism in the North China Craton.Precambrian Research, 146(1-2):45-67. https://doi.org/10.1016/j.precamres.2006.01.008

Li, Q.G., Liu, S.W., Wang, Z.Q., et al., 2008.Contrasting Provenance of Late Archean Metasedimentary Rocks from the Wutai Complex, North China Craton:Detrital Zircon U-Pb, Whole-Rock Sm-Nd Isotopic, and Geochemical Data.International Journal of Earth Sciences, 97(3):443-458. https://doi.org/10.1007/s00531-007-0170-6

Liu, C.H., Zhao, G.C., Sun, M., et al., 2011.U-Pb and Hf Isotopic Study of Detrital Zircons from the Hutuo Group in the Trans-North China Orogen and Tectonic Implications.Gondwana Research, 20(1):106-121. https://doi.org/10.1016/j.gr.2010.11.016

Liu, S.W., Pan, Y.M., Xie, Q.L., et al., 2004.Archean Geodynamics in the Central Zone, North China Craton:Constraints from Geochemistry of Two Contrasting Series of Granitoids in the Fuping and Wutai Complexes.Precambrian Research, 130(1-4):229-249. https://doi.org/10.1016/j.precamres.2003.12.001

Liu, S.W., Zhao, G.C., Wilde, S.A., et al., 2006.Th-U-Pb Monazite Geochronology of the Lüliang and Wutai Complexes:Constraints on the Tectonothermal Evolution of the Trans-North China Orogen.Precambrian Research, 148(3-4):205-225. https://doi.org/10.1016/j.precamres.2006.04.003

Lu, S.N., Li H.K., Tian, Y.Q., 2003.Preliminary Study of Giant-Crystal Garnet-Gedrite Rocks in Hengshan Mountain, Shanxi Province.Geological Survey and Research, 26(1):15-20, 26 (in Chinese with English abstract). https://www.deepdyve.com/lp/elsevier/metamorphic-evolution-and-zircon-ages-of-garnet-orthoamphibole-rocks-mUm1BC7Occ

Miao, P.S., Zhang, Z.F., Zhang, J.Z., et al., 1999.Paleoproterozoic Stratigraphic Sequence in the Wutai Mountain Area.Regional Geology of China, 18(4):405-413 (in Chinese with English abstract). doi: 10.1007/s11434-009-0615-3

Miyashiro, A., 1994.Metamorphic Petrology.UCL Press Limited, London.

O'Brien, P.J., Walte, N., Li, J.H., 2005.The Petrology of Two Distinct Granulite Types in the Hengshan Mts, China, and Tectonic Implications.Journal of Asian Earth Sciences, 24(5):615-627. https://doi.org/10.1016/j.jseaes.2004.01.002

Oh, C.W., Liou, J.G., 1998.A Petrogenetic Grid for Eclogite and Related Facies under High-Pressure Metamorphism.The Island Arc, 7(1-2):36-51. https://doi.org/10.1046/j.1440-1738.1998.00180.x

Pang, E.C., Xu, Y.J., Shi, G.H., et al., 2010.Geochemistry and Chronology of Hongtang Ore-Bearing Rocks in the Daixian Rutile Deposit, Shanxi Province.Acta Petrologica et Mineralogica, 29(5):497-506 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-YSKW201005005.htm

Peng, P., Guo, J.H., Zhai, M.G., et al., 2012.Genesis of the Hengling Magmatic Belt in the North China Craton:Implications for Paleoproterozoic Tectonics.Lithos, 148(3):27-44. https://doi.org/10.1016/j.lithos.2012.05.021

Peng, P., Zhai, M., Zhang, H., et al., 2005.Geochronological Constraints on the Paleoproterozoic Evolution of the North China Craton:SHRIMP Zircon Ages of Different Types of Mafic Dikes.International Geology Review, 47(5):492-508. https://doi.org/10.2747/0020-6814.47.5.492

Peng, P., Wang, X.P., Windley, B.F., et al., 2014.Spatial Distribution of~1 950-1 800 Ma Metamorphic Events in the North China Craton:Implications for Tectonic Subdivision of the Craton.Lithos, 202-203:250-266. https://doi.org/10.1016/j.lithos.2014.05.033

Qian, J.H., Wei, C.J., 2016.P-T-t Evolution of Garnet Amphibolites in the Wutai-Hengshan Area, North China Craton:Insights from Phase Equilibria and Geochronology.Journal of Metamorphic Geology, 34(5):423-446. https://doi.org/10.1111/jmg.12186

Qian, J.H., Wei, C.J., Clarke, G.L., et al., 2015.Metamorphic Evolution and Zircon Ages of Garnet-Orthoamphibole Rocks in Southern Hengshan, North China Craton:Insights into the Regional Paleoproterozoic P-T-t History.Precambrian Research, 256:223-240. https://doi.org/10.1016/j.precamres.2014.11.013

Qian, J.H., Wei, C.J., Yin, C.Q., 2017.Paleoproterozoic P-T-t Evolution in the Hengshan-Wutai-Fuping Area, North China Craton:Evidence from Petrological and Geochronological Data.Precambrian Research, (in Press). http://www.sciencedirect.com/science/article/pii/S0301926816305186

Qian, J.H., Wei, C.J., Zhou, X.W., et al., 2012.Genesis of the Megacryst Orthoamphibole Rock from Hengshan Mts, Shanxi Province:Evidence from Geochemistry and Sm-Nd Isotopic Data.Acta Petrologica Sinica, 28(9):2819-2830 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-YSXB201209013.htm

Qian, J.H., Wei, C.J., Zhou, X.W., et al., 2013.Metamorphic P-T Paths and New Zircon U-Pb Age Data for Garnet-Mica Schist from the Wutai Group, North China Craton.Precambrian Research, 233:282-296. https://doi.org/10.1016/j.precamres.2013.05.012

Roberts, M.P., Finger, F., 1997.Do U-Pb Zircon Ages from Granulites Reflect Peak Metamorphic Conditions? Geology, 25(4):319-322.https://doi.org/10.1130/0091-7613(1997)025<0319:dupzaf>2.3.co;2 doi: 10.1130/0091-7613(1997)025<0319:dupzaf>2.3.co;2

Rubatto, D., 2002.Zircon Trace Element Geochemistry:Partitioning with Garnet and the Link between U-Pb Ages and Metamorphism.Chemical Geology, 184(1-2):123-138. https://doi.org/10.1016/s0009-2541(01)00355-2

Schmidt, M.W., Poli, S., 1998.Experimentally Based Water Budgets for Dehydrating Slabs and Consequences for Arc Magma Generation.Earth and Planetary Science Letters, 163(1-4):361-379. https://doi.org/10.1016/s0012-821x(98)00142-3

Shi, G.H., Li, X.H., Li, Q.L., et al., 2012.Ion Microprobe U-Pb Age and Zr-in-Rutile Thermometry of Rutiles from the Daixian Rutile Deposit in the Hengshan Mountains, Shanxi Province, China.Economic Geology, 107(3):525-535. https://doi.org/10.2113/econgeo.107.3.525

Thompson, A.B., England, P.C., 1984.Pressure-Temperature-Time Paths of Regional Metamorphism 2.Their Inference and Interpretation Using Mineral Assemblages in Metamorphic Rocks.Journal of Petrology, 25(4):929-955. doi: 10.1093/petrology/25.4.929

Tian, Y.Q., 1991.Geology and Gold Mineralization of Wutai-Hengshan Greenstone Belt.Shanxi Science and Technology Press, Taiyuan (in Chinese).

Trap, P., Faure, M., Lin, W., et al., 2007.Late Paleoproterozoic (1 900-1 800 Ma) Nappe Stacking and Polyphase Deformation in the Hengshan-Wutaishan Area:Implications for the Understanding of the Trans-North-China Belt, North China Craton.Precambrian Research, 156(1-2):85-106. https://doi.org/10.1016/j.precamres.2007.03.001

Trap, P., Faure, M., Lin, W., et al., 2009.The Lüliang Massif:A Key Area for the Understanding of the Palaeoproterozoic Trans-North China Belt, North China Craton.Geological Society, London, Special Publications, 323(1):99-125. https://doi.org/10.1144/sp323.5

Trap, P., Faure, M., Lin, W., et al., 2012.Paleoproterozoic Tectonic Evolution of the Trans-North China Orogen:Toward a Comprehensive Model.Precambrian Research, 222-223:191-211. https://doi.org/10.1016/j.precamres.2011.09.008

Wan, Y.S., Miao, P.S., Liu, D.Y., et al., 2010.Formation Ages and Source Regions of the Palaeoproterozoic Gaofan, Hutuo and Dongjiao Groups in the Wutai and Dongjiao Areas of the North China Craton from SHRIMP U-Pb Dating of Detrital Zircons:Resolution of Debates over Their Stratigraphic Relationships.Chinese Science Bulletin, 55(13):1278-1284. https://doi.org/10.1007/s11434-009-0615-3

Wang, K.Y., Hao, J., Wilde, S.A., et al., 2000.Reconsideration of Some Key Geological Problems of Late Archean-Early Proterozoic in the Wutaishan-Hengshan Area:Constraints from SHRIMP U-Pb Zircon Data.Scientia Geologica Sinica, 35(2):175-184 (in Chinese with English abstract). doi: 10.1360/03yd0265

Wang, K.Y., Zhou, S.P., Hao, J., 1996.The Metamorphism and Significance of Kyanite-Bearing Assemblages from the Original Jingangku Formation of Wutaishan Area.Acta Petrologica Sinica, 12(1):88-97 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-YSXB601.007.htm

Wang, Z.H., Wilde, S.A., Wan, J.L., 2010.Tectonic Setting and Significance of 2.3-2.1 Ga Magmatic Events in the Trans-North China Orogen:New Constraints from the Yanmenguan Mafic-Ultramafic Intrusion in the Hengshan-Wutai-Fuping Area.Precambrian Research, 178(1-4):27-42. https://doi.org/10.1016/j.precamres.2010.01.005

Wang, Z.H., Wilde, S.A., Wang, K.Y., et al., 2004.A MORB-Arc Basalt-Adakite Association in the 2.5 Ga Wutai Greenstone Belt:Late Archean Magmatism and Crustal Growth in the North China Craton.Precambrian Research, 131(3-4):323-343. https://doi.org/10.1016/j.precamres.2003.12.014

Watson, E.B., Harrison, T.M., 1984.Accessory Minerals and the Geochemical Evolution of Crustal Magmatic Systems:A Summary and Prospectus of Experimental Approaches.Physics of the Earth and Planetary Interiors, 35(1-3):19-30. https://doi.org/10.1016/0031-9201(84)90031-1

Wei, C.J., 2016.Granulite Facies Metamorphism and Petrogenesis of Granite (Ⅱ):Quantitative Modeling of the HT-UHT Phase Equilibria for Metapelites and the Petrogenesis of S-Type Granite.Acta Petrologica Sinica, 32(6):1625-1643 (in Chinese with English abstract). doi: 10.1007/s11430-016-9029-7

Wei, C.J., Guan, X., Dong, J., 2017.HT-UHT Metamorphism of Metabasites and the Petrogenesis of TTGs.Acta Petrologica Sinica, 33(5):1381-1404 (in Chinese with English abstract). http://www.ysxb.ac.cn/ysxb/ch/reader/view_news.aspx?id=20170926060627381

Wei, C.J., Qian, J.H., Zhou, X.W., 2014.Paleoproterozoic Crustal Evolution of the Hengshan-Wutai-Fuping Region, North China Craton.Geoscience Fronteris, 5(4):485-497. https://doi.org/10.1016/j.gsf.2014.02.008

Wei, C.J., Zhang, J.S., 2007.H₂O Behaviour in Subsolidus Metamorphic Processes.Geological Journal of China Universities, 13(3):507-514 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-GXDX200703014.htm

White, R.W., Powell, R., Holland, T.J.B., 2001.Calculation of Partial Melting Equilibria in the System Na₂O-CaO-K₂O-FeO-MgO-Al₂O₃-SiO₂-H₂O (NCKFMASH).Journal of Metamorphic Geology, 19(2):139-153. https://doi.org/10.1046/j.0263-4929.2000.00303.x

Wilde, S.A., Cawood, P., Wang, K.Y., 1997.The Relationship and Timing of Granitoid Evolution with Respect to Felsic Volcanism in the Wutai Complex, North China Craton.Proceedings of the 30th IGC, Beijing.

Wilde, S.A., Cawood, P.A., Wang, K.Y., et al., 2005.Granitoid Evolution in the Late Archean Wutai Complex, North China Craton.Journal of Asian Earth Sciences, 24(5):597-613. https://doi.org/10.1016/j.jseaes.2003.11.006

Wilde, S.A., Cawood, P.A., Wang, K.Y., et al., 2004a.Determining Precambrian Crustal Evolution in China:A Case-Study from Wutaishan, Shanxi Province, Demonstrating the Application of Precise SHRIMP U-Pb Geochronology.Geological Society, London, Special Publications, 226(1):5-25. https://doi.org/10.1144/gsl.sp.2004.226.01.02

Wilde, S.A., Zhao, G.C., Wang, K.Y., et al., 2004b.First SHRIMP Zircon U-Pb Ages for Hutuo Group in Wutaishan:Further Evidence for Palaeoproterozoic Amalgamation of North China Craton.Chinese Science Bulletin, 49(1):83-90. https://doi.org/10.1007/bf02901747

Xu, S., K., Deng, X.L., Liu, L.S., et al., 2008.Geochemical Characteristics of Nianzigou Rutile Deposit in Daixian County, Shanxi Province.Mineral Deposits, 27(4):503-519 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-KCDZ200804007.htm

Xu, S.K., Liu, L.S., Yun, L.T., 2002.Metamorphic Process of Nianzigou Rutile Deposit and Its Relation to Rutile Miner.Geology of Chemical Minerals, 24 (1):48-56 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-HGKC201003003.htm

Zhai, M.G., 2009.Two Kinds of Granulites (HT-HP and HT-UHT) in North China Craton:Their Genetic Relation and Geotectonic Implications.Acta Petrologica Sinica, 25(8):1753-1771 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-YSXB200908005.htm

Zhai, M.G., 2011.Cratonization and the Ancient North China Continent:A Summary and Review.Science China Earth Sciences, 54(8):1110-1120. https://doi.org/10.1007/s11430-011-4250-x

Zhai, M.G., Bian, A.G., Zhao, T.P., 2000.The Amalgamation of the Supercontinent of North China Craton at the End of Neo-Archaean and Its Breakup during Late Palaeoproterozoic and Meso-Proterozoic.Science China Earth Sciences, 43(S1):219-232. https://doi.org/10.1007/bf02911947

Zhai, M.G., Guo, J.H., Liu, W.J., 2005.Neoarchean to Paleoproterozoic Continental Evolution and Tectonic History of the North China Craton:A Review.Journal of Asian Earth Sciences, 24(5):547-561. https://doi.org/10.1016/j.jseaes.2004.01.018

Zhai, M.G., Santosh, M., 2011.The Early Precambrian Odyssey of the North China Craton:A Synoptic Overview.Gondwana Research, 20(1):6-25. https://doi.org/10.1016/j.gr.2011.02.005

Zhang, J., Zhao, G.C., Li, S.Z., et al., 2007.Deformation History of the Hengshan Complex:Implications for the Tectonic Evolution of the Trans-North China Orogen.Journal of Structural Geology, 29(6):933-949. https://doi.org/10.1016/j.jsg.2007.02.013

Zhang, R.Y., Liou, J.G., 1997.Partial Transformation of Gabbro to Coesite-Bearing Eclogite from Yangkou, the Sulu Terrane, Eastern China.Journal of Metamorphic Geology, 15(2):183-202. https://doi.org/10.1111/j.1525-1314.1997.00012.x

Zhang, Y.H., 2013.Phase Equilibria Modelling for Metamorphic Evolution of High-Pressure Granulites and Anatexis of Gneisses in the Hengshan Complex, Shanxi Province (Dissertation).Peking University, Beijing (in Chinese with English abstract).

Zhang, Y.H., Wei, C.J., Tian, W., et al., 2013.Reinterpretation of Metamorphic Age of the Hengshan Complex, North China Craton.Chinese Science Bulletin, 58(34):4300-4307. https://doi.org/10.1007/s11434-013-5993-x

Zhao, G.C., Cawood, P.A., Li, S.Z., et al., 2012.Amalgamation of the North China Craton:Key Issues and Discussion.Precambrian Research, 222-223:55-76. https://doi.org/10.1016/j.precamres.2012.09.016

Zhao, G.C., Cawood, P.A., Lu, L.Z., 1999.Petrology and P-T History of the Wutai Amphibolites:Implications for Tectonic Evolution of the Wutai Complex, China.Precambrian Research, 93(2-3):181-199. https://doi.org/10.1016/s0301-9268(98)00090-4

Zhao, G.C., Kröner, A., Wilde, S.A., et al., 2007.Lithotectonic Elements and Geological Events in the Hengshan-Wutai-Fuping Belt:A Synthesis and Implications for the Evolution of the Trans-North China Orogen.Geological Magazine, 144 (5):753-775. https://doi.org/10.1017/s0016756807003561

Zhao, G.C., Sun, M., Wilde, S.A., et al., 2005.Late Archean to Paleoproterozoic Evolution of the North China Craton:Key Issues Revisited.Precambrian Research, 136(2):177-202. https://doi.org/10.1016/j.precamres.2004.10.002

Zhao, G.C., Wilde, S.A., Cawood, P.A., et al., 2001.Archean Blocks and Their Boundaries in the North China Craton:Lithological, Geochemical, Structural and P-T Path Constraints and Tectonic Evolution.Precambrian Research, 107(1-2):45-73. https://doi.org/10.1016/s0301-9268(00)00154-6

Zhao, R.F., Guo, J.H., Peng, P., et al., 2011.2.1 Ga Crustal Remelting Event in Hengshan Complex:Evidence from Zircon U-Pb Dating and Hf-Nd Isotopic Study on Potassic Granites.Acta Petrologica Sinica, 27(6):1607-1623 (in Chinese with English abstract). doi: 10.1007/s11434-012-5315-8

Zhou, L.G., Zhai, M.G., Lu, J.S., et al., 2017.Paleoproterozoic Metamorphism of High-Grade Granulite Facies Rocks in the North China Craton:Study Advances, Questions and New Issues.Precambrian Research, 303:520-547. https://doi.org/10.1016/j.precamres.2017.06.025

Zhou, X.W., Zhao, G.C., Geng, Y.S., 2010.Helanshan High Pressure Pelitic Granulite:Petrologic Evidence for Collision Event in the Western Block of the North China Craton.Acta Petrologica Sinica, 26(7):2113-2121 (in Chinese with English abstract). http://www.oalib.com/paper/1475792

白瑾, 1986.五台山早前寒武纪地质.天津:天津科学技术出版社.

杜利林, 杨崇辉, 郭敬辉, 等, 2010.五台地区滹沱群底界时代:玄武安山岩SHRIMP锆石U-Pb定年.科学通报, 55(3):246-254. http://www.oalib.com/paper/4152179

杜利林, 杨崇辉, 任留东, 等, 2009.山西五台山区滹沱群变质玄武岩岩石学、地球化学特征及其成因意义.地质通报, 28(7):867-876. http://www.oalib.com/paper/4152179

杜利林, 杨崇辉, 王伟, 等, 2011.五台地区滹沱群时代与地层划分新认识:地质学与锆石年代学证据.岩石学报, 27(4):1037-1055. http://www.doc88.com/p-7137673371198.html

郭敬辉, 翟明国, 李永刚, 等, 1999.恒山西段石榴石角闪岩和麻粒岩的变质作用、PT轨迹及构造意义.地质科学, 34(3):311-325. http://www.cnki.com.cn/Article/CJFDTOTAL-DZLP200302005.htm

贾琇明, 2007. 山西代县碾子沟金红石矿床矿物学及年代学研究(博士学位论文). 北京: 中国地质大学.

陆松年, 李怀坤, 田永清, 2003.恒山雁门关巨晶石榴子石直闪石岩的初步研究.地质调查与研究, 26(1):15-20, 26. doi: 10.3969/j.issn.1672-4135.2003.01.004

苗培森, 张振福, 张建中, 等, 1999.五台山区早元古代地层层序探讨.中国区域地质, 18(4):405-413. doi: 10.1360/zd-2013-43-10-1583

庞尔成, 徐永婧, 施光海, 等, 2010.山西代县金红石矿床洪塘矿区含矿岩石的地球化学及年代学.岩石矿物学杂志, 29(5):497-506. http://www.cnki.com.cn/Article/CJFDTOTAL-JXTW201334016.htm

钱加慧, 魏春景, 周喜文, 等, 2012.山西恒山巨晶状直闪岩的成因:来自地球化学和Sm-Nd同位素的证据, 岩石学报, 28(9):2819-2830. https://www.wenkuxiazai.com/doc/d1b5b7f5f705cc175527096b.html

田永清, 1991.五台山-恒山绿岩带地质及金的成矿作用.太原:山西科学技术出版社.

王凯怡, 郝杰, Wilde, S.A., 等, 2000.山西五台山-恒山地区晚太古-早元古代若干关键地质问题的再认识:单颗粒锆石离子探针质谱年龄提出的地质制约.地质科学, 35(2):175-184. http://industry.wanfangdata.com.cn/dl/Detail/Periodical?id=Periodical_dzkx200002006

王凯怡, 周少平, 郝杰, 1996.五台山地区原金刚库组中含蓝晶石组合的变质作用及其意义.岩石学报, 12(1):88-97. https://mall.cnki.net/qikan-QHWJ200301003.html

魏春景, 2016.麻粒岩相变质作用与花岗岩成因-Ⅱ:变质泥质岩高温-超高温变质相平衡与S型花岗岩成因的定量模拟, 岩石学报, 32(6):1625-1643. http://www.cnki.com.cn/Article/CJFDTotal-YSXB201606004.htm

魏春景, 关晓, 董杰, 2017.基性岩高温-超高温变质作用与TTG质岩成因.岩石学报, 33(5):1381-1404. https://mall.cnki.net/qikan-YSXB201705002.html

魏春景, 张景森, 2007.固相线以下变质过程中水的行为, 高校地质学报, 13(3):507-514. doi: 10.3969/j.issn.1006-7493.2007.03.019

徐少康, 邓小林, 刘力生, 等, 2008.山西代县碾子沟金红石矿床地球化学特征.矿床地质, 27(4):503-519. http://www.cnki.com.cn/Article/CJFDTOTAL-HGKC603.013.htm

徐少康, 刘力生, 云连涛, 2002.碾子沟金红石矿床变质作用特征及其与成矿的关系.化工矿产地质, 24(1):48-56. https://www.wenkuxiazai.com/doc/eb9c0a1dff00bed5b9f31d4b.html

翟明国, 2009.华北克拉通两类早前寒武纪麻粒岩(HT-HP和HT-UHT)及其相关问题.岩石学报, 25(8):1753-1771. doi: 10.1360/csb2014-59-7-593

张颖慧, 2013. 山西恒山高压麻粒岩变质演化与片麻岩深熔作用的相平衡研究(博士学位论文). 北京: 北京大学.

赵瑞幅, 郭敬辉, 彭澎, 等, 2011.恒山地区古元古代2.1 Ga地壳重熔事件:钾质花岗岩锆石U-Pb定年及Hf-Nd同位素研究.岩石学报, 27(6):1607-1623. http://www.cnki.com.cn/Article/CJFDTotal-JDXK201509004.htm

周喜文, 赵国春, 耿元生, 2010.贺兰山高压泥质麻粒岩-华北克拉通西部陆块拼合的岩石学证据, 岩石学报, 26(7):2113-2121. http://www.oalib.com/paper/1475792

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(10)

Get Citation

PDF

XML

Article views (6704) PDF downloads(200)

Paleoproterozoic Metamorphism and Tectonic Evolution in Wutai-Hengshan Region, Trans-North China Orogen

doi: 10.3799/dqkx.2018.002

Abstract

References

Proportional views

Catalog

通讯作者: 陈斌, bchen63@163.com

Proportional views

Export File

Citation

Format

Content