Trace Element Mobility in Subducted Marble and Associated Eclogite: Constraints from UHP Rocks in the Shuanghe Area, Central-East China

Xingao Hou, Zhiqiang Yu, Shefa Chen, Lei Liu, Yilin Xiao

Journal of Earth Science ›› 2024, Vol. 35 ›› Issue (1) : 1-15. DOI: 10.1007/s12583-022-1692-3
Geochemistry and Mineral Deposits

Trace Element Mobility in Subducted Marble and Associated Eclogite: Constraints from UHP Rocks in the Shuanghe Area, Central-East China

Author information +
History +

Abstract

In order to decipher element mobility in UHP meta-sedimentary rocks in the continental subduction zone, major and trace element compositions are investigated for a continuous profile from a representative UHP region in the Dabie Mountains. Among the lithologic contact zone, contents of K, Ca, LREE, and LILE exhibit varying degrees of downward trends in both marble and eclogite toward the contact zone, indicating that marble and their associated eclogite can release a large amount of K, Ca, and a small number of LILEs and LREEs. Titanite is the main Ti phase in both marble and eclogite. Titanite rims around rutile can occasionally be seen in eclogite. Contents of Ti and HFSE exhibit a well-coupled relation among marble and eclogite, indicating that substantial Ti and HFSEs were migrated from eclogite to marble, in accord with the capacity of a melt medium. Rutiles and titanites in marble exhibit a relatively limited variation in Nb/Ta ratios (12.9–16.2), similar to those of titanites in eclogite (14.2–16.7), which demonstrates that rutiles and titanites in marble were sourced from eclogite because of short-distance migrations of Ti and HFSEs. According to the P-T path and the temperature and pressure conditions of the peak metamorphism reported by previous studies, the eclogite associated with marble may not form supercritical fluids in the subduction zone because of the addition of carbonate minerals.

Keywords

UHP metamorphism / eclogite / marble / element migration / fluid actions / geochemistry

Cite this article

Download citation ▾
Xingao Hou, Zhiqiang Yu, Shefa Chen, Lei Liu, Yilin Xiao. Trace Element Mobility in Subducted Marble and Associated Eclogite: Constraints from UHP Rocks in the Shuanghe Area, Central-East China. Journal of Earth Science, 2024, 35(1): 1‒15 https://doi.org/10.1007/s12583-022-1692-3

References

[]
Adam J, Green T. Experimentally Determined Partition Coefficients for Minor and Trace Elements in Peridotite Minerals and Carbonatitic Melt, and Their Relevance to Natural Carbonatites. European Journal of Mineralogy, 2001, 13(5): 815-827.
CrossRef Google scholar
[]
Arculus R J, Lapierre H, Jaillard. Geochemical Window into Subduction and Accretion Processes: Raspas Metamorphic Complex, Ecuador. Geology, 1999, 27(6): 547-550.
CrossRef Google scholar
[]
Auzanneau E, Vielzeuf D, Schmidt M W. Experimental Evidence of Decompression Melting during Exhumation of Subducted Continental Crust. Contributions to Mineralogy and Petrology, 2006, 152(2): 125-148.
CrossRef Google scholar
[]
Barth M G, Foley S F, Horn I. Partial Melting in Archean Subduction Zones: Constraints from Experimentally Determined Trace Element Partition Coefficients between Eclogitic Minerals and Tonalitic Melts under Upper Mantle Conditions. Precambrian Research, 2002, 113(3/4): 323-340.
CrossRef Google scholar
[]
Becker H, Jochum K P, Carlson R W. Trace Element Fractionation during Dehydration of Eclogites from High-Pressure Terranes and the Implications for Element Fluxes in Subduction Zones. Chemical Geology, 2000, 163(1/2/3/4): 65-99.
CrossRef Google scholar
[]
Beinlich A, Klemd R, John T, et al. Trace-Element Mobilization during Ca-Metasomatism along a Major Fluid Conduit: Eclogitization of Blueschist as a Consequence of Fluid-Rock Interaction. Geochimica et Cosmochimica Acta, 2010, 74(6): 1892-1922.
CrossRef Google scholar
[]
Brenan J M, Shaw H F, Ryerson F J. Experimental Evidence for the Origin of Lead Enrichment in Convergent-Margin Magmas. Nature, 1995, 378(6552): 54-56.
CrossRef Google scholar
[]
Buob A. Experiments on CaCO3-MgCO3 Solid Solutions at High Pressure and Temperature. American Mineralogist, 2006, 91(2/3): 435-440.
CrossRef Google scholar
[]
Bureau H, Keppler H. Complete Miscibility between Silicate Melts and Hydrous Fluids in the Upper Mantle: Experimental Evidence and Geochemical Implications. Earth and Planetary Science Letters, 1999, 165(2): 187-196.
CrossRef Google scholar
[]
Byrnes A P, Wyllie P J. Subsolidus and Melting Relations for the Join CaCO3-MgCO3 at 10 Kbar. Geochimica et Cosmochimica Acta, 1981, 45(3): 321-328.
CrossRef Google scholar
[]
Carswell D A, Wilson R N, Zhai M. Ultra-High Pressure Aluminous Titanites in Carbonate-Bearing Eclogites at Shuanghe in Dabieshan, Central China. Mineralogical Magazine, 1996, 60(400): 461-471.
CrossRef Google scholar
[]
Chen R X, Yin Z Z, Xia C P. Crustal Metasomatism of Mantle Wedge during Collisional Orogeny: Insights from Orogenic Peridotites in the Dabie-Sulu Orogenic Belt. Bulletin of Mineralogy, Petrology and Geochemistry, 2019, 38(3): 459 484 438
[]
Chen R X, Zheng Y F, Gong B, et al. Origin of Retrograde Fluid in Ultrahigh-Pressure Metamorphic Rocks: Constraints from Mineral Hydrogen Isotope and Water Content Changes in Eclogite-Gneiss Transitions in the Sulu Orogen. Geochimica et Cosmochimica Acta, 2007, 71(9): 2299-2325.
CrossRef Google scholar
[]
Chen R X, Zheng Y F, Gong B, et al. Oxygen Isotope Geochemistry of Ultrahigh-Pressure Metamorphic Rocks from 200–4 000 m Core Samples of the Chinese Continental Scientific Drilling. Chemical Geology, 2007, 242(1/2): 51-75.
CrossRef Google scholar
[]
Chen Y X, Tang J, Zheng Y F, et al. Geochemical Constraints on Petrogenesis of Marble-Hosted Eclogites from the Sulu Orogen in China. Chemical Geology, 2016, 436: 35-53.
CrossRef Google scholar
[]
Chen Y X, Zheng Y F, Hu Z. Petrological and Zircon Evidence for Anatexis of UHP Quartzite during Continental Collision in the Sulu Orogen. Journal of Metamorphic Geology, 2013, 31(4): 389-413.
CrossRef Google scholar
[]
Chu X L, Guo J H, Fan H R, et al. Oxygen Isotope Compositions of Eclogites in Rongcheng, Eastern China. Chinese Science Bulletin, 2003, 48(4): 372-378.
[]
Cong B L, Zhai M G, Carswell D A C, et al. Petrogenesis of Ultrahigh-Pressure Rocks and Their Country Rocks at Shuanghe in Dabieshan, Central China. European Journal of Mineralogy, 1995, 7(1): 119-138.
CrossRef Google scholar
[]
Dasgupta R, Hirschmann M M, Withers A C. Deep Global Cycling of Carbon Constrained by the Solidus of Anhydrous, Carbonated Eclogite under Upper Mantle Conditions. Earth and Planetary Science Letters, 2004, 227(1/2): 73-85.
CrossRef Google scholar
[]
Frost B R, Chamberlain K R, Schumacher J C. Sphene (Titanite): Phase Relations and Role as a Geochronometer. Chemical Geology, 2001, 172(1/2): 131-148.
CrossRef Google scholar
[]
Fu B, Zheng Y F, Wang Z R, et al. Oxygen and Hydrogen Isotope Geochemistry of Gneisses Associated with Ultrahigh Pressure Eclogites at Shuanghe in the Dabie Mountains. Contributions to Mineralogy and Petrology, 1999, 134(1): 52-66.
CrossRef Google scholar
[]
Gao J, John T, Klemd R, et al. Mobilization of Ti-Nb-Ta during Subduction: Evidence from Rutile-Bearing Dehydration Segregations and Veins Hosted in Eclogite, Tianshan, NW China. Geochimica et Cosmochimica Acta, 2007, 71(20): 4974-4996.
CrossRef Google scholar
[]
Gao X Y, Zheng Y F, Chen Y X. U-Pb Ages and Trace Elements in Metamorphic Zircon and Titanite from UHP Eclogite in the Dabie Orogen: Constraints on P-T-t Path. Journal of Metamorphic Geology, 2011, 29(7): 721-740.
CrossRef Google scholar
[]
Grassi D, Schmidt M W. The Melting of Carbonated Pelites from 70 to 700 km Depth. Journal of Petrology, 2011, 52(4): 765-789.
CrossRef Google scholar
[]
Green T H, Pearson N J. Ti-Rich Accessory Phase Saturation in Hydrous Mafic-Felsic Compositions at High P, T. Chemical Geology, 1986, 54(3/4): 185-201.
CrossRef Google scholar
[]
Guo S, Su B, John T, et al. Boron Release and Transfer Induced by Phengite Breakdown in Subducted Impure Metacarbonates. Lithos, 2022, 408/409: 106548.
CrossRef Google scholar
[]
Guo S, Zhao K D, John T, et al. Metasomatic Flow of Metacarbonate-Derived Fluids Carrying Isotopically Heavy Boron in Continental Subduction Zones: Insights from Tourmaline-Bearing Ultra-High Pressure Eclogites and Veins (Dabie Terrane, Eastern China). Geochimica et Cosmochimica Acta, 2019, 253: 159-200.
CrossRef Google scholar
[]
Hammouda T, Moine B N, Devidal J L, et al. Trace Element Partitioning during Partial Melting of Carbonated Eclogites. Physics of the Earth and Planetary Interiors, 2009, 174(1/2/3/4): 60-69.
CrossRef Google scholar
[]
Hawkesworth C J, Hergt J M, Ellam R M, et al. Element Fluxes Associated with Subduction Related Magmatism. Philosophical Transactions of the Royal Society of London Series A: Physical and Engineering Sciences, 1991, 335(1638): 393-405.
CrossRef Google scholar
[]
Hellman P L, Green T H. The Role of Sphene as an Accessory Phase in the High-Pressure Partial Melting of Hydrous Mafic Compositions. Earth and Planetary Science Letters, 1979, 42(2): 191-201.
CrossRef Google scholar
[]
Hermann J. Allanite: Thorium and Light Rare Earth Element Carrier in Subducted Crust. Chemical Geology, 2002, 192(3/4): 289-306.
CrossRef Google scholar
[]
Hermann J, Spandler C J. Sediment Melts at Sub-Arc Depths: An Experimental Study. Journal of Petrology, 2008, 49(4): 717-740.
CrossRef Google scholar
[]
Hermann J, Spandler C, Hack A, et al. Aqueous Fluids and Hydrous Melts in High-Pressure and Ultra-High Pressure Rocks: Implications for Element Transfer in Subduction Zones. Lithos, 2006, 92(3/4): 399-417.
CrossRef Google scholar
[]
Huang J A, Xiao Y L. Element Mobility in Mafic and Felsic Ultrahigh-Pressure Metamorphic Rocks from the Dabie UHP Orogen, China: Insights into Supercritical Liquids in Continental Subduction Zones. International Geology Review, 2014, 57(9/10): 1103-1129.
[]
Huang J, Xiao Y, Gao Y, et al. Nb-Ta Fractionation Induced by Fluid-Rock Interaction in Subduction-Zones: Constraints from UHP Eclogite- and Vein-Hosted Rutile from the Dabie Orogen, Central-Eastern China. Journal of Metamorphic Geology, 2012, 30(8): 821-842.
CrossRef Google scholar
[]
Irving A J, Wyllie P J. Subsolidus and Melting Relationships for Calcite, Magnesite and the Join CaCO3-MgCO3 36 Kb. Geochimica et Cosmochimica Acta, 1975, 39(1): 35-53.
CrossRef Google scholar
[]
Jahn B M. Hacker B R, Liou J G. Geochemical and Isotopic Characteristics of UHP Eclogites and Ultramafic Rocks of the Dabie Orogen: Implications for Continental Subduction and Collisional Tectonics. When Continents Collide: Geodynamics and Geochemistry of Ultrahigh-Pressure Rocks, 1998 Dordrecht Springer 203-239.
CrossRef Google scholar
[]
Jahn, B. M., Rumble, D. Liou, J., 2003. Geochemistry and Isotope Tracer Study of UHP Metamorphic Rocks. In: Caeswell, D. A., Compagnoni, R., Rolfo, F., eds., Ultrahigh Pressure Metamorphism. Mineralogical Society of Great Britain and Ireland. 365–414. https://doi.org/10.1180/emu-notes.5.12
[]
Jochum K P, Stoll B, Herwig K, et al. MPI-DING Reference Glasses for in Situ Microanalysis: New Reference Values for Element Concentrations and Isotope Ratios. Geochemistry, Geophysics, Geosystems, 2006, 7(2): Q02008.
CrossRef Google scholar
[]
John T, Klemd R, Klemme S, et al. Nb-Ta Fractionation by Partial Melting at the Titanite-Rutile Transition. Contributions to Mineralogy and Petrology, 2011, 161(1): 35-45.
CrossRef Google scholar
[]
John T, Scherer E E, Haase K, et al. Trace Element Fractionation during Fluid-Induced Eclogitization in a Subducting Slab: Trace Element and Lu-Hf-Sm-Nd Isotope Systematics. Earth and Planetary Science Letters, 2004, 227(3/4): 441-456.
CrossRef Google scholar
[]
Kessel R, Schmidt M W, Ulmer P, et al. Trace Element Signature of Subduction-Zone Fluids, Melts and Supercritical Liquids at 120–180 km Depth. Nature, 2005, 437(7059): 724-727.
CrossRef Google scholar
[]
Klemme S, Blundy J D, Wood B J. Experimental Constraints on Major and Trace Element Partitioning during Partial Melting of Eclogite. Geochimica et Cosmochimica Acta, 2002, 66(17): 3109-3123.
CrossRef Google scholar
[]
Kogiso T, Tatsumi Y, Nakano S. Trace Element Transport during Dehydration Processes in the Subducted Oceanic Crust: 1. Experiments and Implications for the Origin of Ocean Island Basalts. Earth and Planetary Science Letters, 1997, 148(1/2): 193-205.
CrossRef Google scholar
[]
Li S G, Jagoutz E, Chen Y Z, et al. Sm-Nd and Rb-Sr Isotopic Chronology and Cooling History of Ultrahigh Pressure Metamorphic Rocks and Their Country Rocks at Shuanghe in the Dabie Mountains, Central China. Geochimica et Cosmochimica Acta, 2000, 64(6): 1077-1093.
CrossRef Google scholar
[]
Li X P, Zheng Y F, Wu Y B, et al. Low-T Eclogite in the Dabie Terrane of China: Petrological and Isotopic Constraints on Fluid Activity and Radiometric Dating. Contributions to Mineralogy and Petrology, 2004, 148(4): 443-470.
CrossRef Google scholar
[]
Li Y L, Zheng Y F, Fu B, et al. Oxygen Isotope Composition of Quartz-Vein in Ultrahigh-Pressure Eclogite from Dabieshan and Implications for Transport of High-Pressure Metamorphic Fluid. Physics and Chemistry of the Earth, Part A: Solid Earth and Geodesy, 2001, 26(9/10): 695-704.
CrossRef Google scholar
[]
Liou J G, Zhang R Y, Jahn B M. Petrology, Geochemistry and Isotope Data on a Ultrahigh-Pressure Jadeite Quartzite from Shuanghe, Dabie Mountains, East-Central China. Lithos, 1997, 41(1/2/3): 59-78.
CrossRef Google scholar
[]
Liu F L, Gerdes A, Liou J G, et al. SHRIMP U-Pb Zircon Dating from Sulu-Dabie Dolomitic Marble, Eastern China: Constraints on Prograde, Ultrahigh-Pressure and Retrograde Metamorphic Ages. Journal of Metamorphic Geology, 2006, 24(7): 569-589.
CrossRef Google scholar
[]
Liu L, Xiao Y L, Wörner G, et al. Detrital Rutile Geochemistry and Thermometry from the Dabie Orogen: Implications for Source-Sediment Links in a UHPM Terrane. Journal of Asian Earth Sciences, 2014, 89: 123-140.
CrossRef Google scholar
[]
Liu Q, Hermann J, Zhang J F. Polyphase Inclusions in the Shuanghe UHP Eclogites Formed by Subsolidus Transformation and Incipient Melting during Exhumation of Deeply Subducted Crust. Lithos, 2013, 177: 91-109.
CrossRef Google scholar
[]
Liu X C, Hu K, Li X X, et al. The Diversity and Origion of Eclogites from the Dabie: Sulu High: Pressure Metamorphic Belt. Geological Review, 1994, 40(6): 494 501 (in Chinese with English Abstract)
[]
Lucassen F, Dulski P, Abart R, et al. Redistribution of HFSE Elements during Rutile Replacement by Titanite. Contributions to Mineralogy and Petrology, 2010, 160(2): 279-295.
CrossRef Google scholar
[]
Malaspina N, Hermann J, Scambelluri M, et al. Multistage Metasomatism in Ultrahigh-Pressure Mafic Rocks from the North Dabie Complex (China). Lithos, 2006, 90(1/2): 19-42.
CrossRef Google scholar
[]
Manning C E. The Chemistry of Subduction-Zone Fluids. Earth and Planetary Science Letters, 2004, 223(1/2): 1-16.
CrossRef Google scholar
[]
Massonne H J, Fockenberg T. Melting of Phengite-Bearing Eclogite at Pressures of 4 and 9 GPa Relevant to Deep Regions of a Subduction Zone. Earth and Planetary Science Letters, 2022, 584: 117475.
CrossRef Google scholar
[]
McDonough W F, Sun S S. The Composition of the Earth. Chemical Geology, 1995, 120(3/4): 223-253.
CrossRef Google scholar
[]
Meinhold G. Rutile and Its Applications in Earth Sciences. Earth-Science Reviews, 2010, 102(1/2): 1-28.
CrossRef Google scholar
[]
Mibe K, Kawamoto T, Matsukage K N, et al. Slab Melting Versus Slab Dehydration in Subduction-Zone Magmatism. Proceedings of the National Academy of Sciences of the United States of America, 2011, 108(20): 8177-8182.
CrossRef Google scholar
[]
Nichols G T, Wyllie P J, Stern C R. Subduction Zone Melting of Pelagic Sediments Constrained by Melting Experiments. Nature, 1994, 371(6500): 785-788.
CrossRef Google scholar
[]
Okay A I. Petrology of a Diamond and Coesite-Bearingc Metamorphic Terrain: Dabie Shan, China. European Journal of Mineralogy, 1993, 5(4): 659-676.
CrossRef Google scholar
[]
Plank T, Langmuir C H. Tracing Trace Element from Sediment Input to Volcanic Output at Subduction Zones. Nature, 1993, 362: 739-742.
CrossRef Google scholar
[]
Plank T, Langmuir C H. The Chemical Composition of Subducting Sediment and Its Consequences for the Crust and Mantle. Chemical Geology, 1998, 145(3/4): 325-394.
CrossRef Google scholar
[]
Polat A, Hofmann A W, Rosing M T. Boninite-Like Volcanic Rocks in the 3.7–3.8 Ga Isua Greenstone Belt, West Greenland: Geochemical Evidence for Intra-Oceanic Subduction Zone Processes in the Early Earth. Chemical Geology, 2002, 184(3/4): 231-254.
CrossRef Google scholar
[]
Rubatto D, Hermann J. Zircon Formation during Fluid Circulation in Eclogites (Monviso, Western Alps): Implications for Zr and Hf Budget in Subduction Zones. Geochimica et Cosmochimica Acta, 2003, 67(12): 2173-2187.
CrossRef Google scholar
[]
Rumble D, Wang Q C, Zhang R Y. Stable Isotope Geochemistry of Marbles from the Coesite UHP Terrains of Dabieshan and Sulu, China. Lithos, 2000, 52(1/2/3/4): 79-95.
CrossRef Google scholar
[]
Rüpke L H, Morgan J P, Hort M, et al. Are the Regional Variations in Central American Arc Lavas Due to Differing Basaltic Versus Peridotitic Slab Sources of Fluids?. Geology, 2002, 30(11): 1035-1038.
CrossRef Google scholar
[]
Scambelluri M, Bottazzi P, Trommsdorff V, et al. Incompatible Element-Rich Fluids Released by Antigorite Breakdown in Deeply Subducted Mantle. Earth and Planetary Science Letters, 2001, 192(3): 457-470.
CrossRef Google scholar
[]
Schertl H P, Okay A I. A Coesite Inclusion in Dolomite in Dabie Shan, China: Petrological and Rheological Significance. European Journal of Mineralogy, 1994, 6(6): 995-1000.
CrossRef Google scholar
[]
Schmidt M W. Experimental Constraints on Recycling of Potassium from Subducted Oceanic Crust. Science, 1996, 272(5270): 1927-1930.
CrossRef Google scholar
[]
Schmidt M W, Vielzeuf D, Auzanneau E. Melting and Dissolution of Subducting Crust at High Pressures: The Key Role of White Mica. Earth and Planetary Science Letters, 2004, 228(1/2): 65-84.
CrossRef Google scholar
[]
Shen A H, Keppler H. Direct Observation of Complete Miscibility in the Albite-H2O System. Nature, 1997, 385(6618): 710-712.
CrossRef Google scholar
[]
Sheng Y M, Xia Q K, Dallai L, et al. H2O Contents and D/H Ratios of Nominally Anhydrous Minerals from Ultrahigh-Pressure Eclogites of the Dabie Orogen, Eastern China. Geochimica et Cosmochimica Acta, 2007, 71(8): 2079-2103.
CrossRef Google scholar
[]
Sindern S. Analysis of Rare Earth Elements in Rock and Mineral Samples by ICP-MS and LA-ICP-MS. Physical Sciences Reviews, 2017, 2(2): 20160066.
CrossRef Google scholar
[]
Spandler C, Hermann J, Arculus R, et al. Redistribution of Trace Elements during Prograde Metamorphism from Lawsonite Blueschist to Eclogite Facies; Implications for Deep Subduction-Zone Processes. Contributions to Mineralogy and Petrology, 2003, 146(2): 205-222.
CrossRef Google scholar
[]
Spandler C, Mavrogenes J, Hermann J. Experimental Constraints on Element Mobility from Subducted Sediments Using High-P Synthetic Fluid/Melt Inclusions. Chemical Geology, 2007, 239(3/4): 228-249.
CrossRef Google scholar
[]
Storkey A C, Hermann J, Hand M, et al. Using in situ Trace-Element Determinations to Monitor Partial-Melting Processes in Metabasites. Journal of Petrology, 2005, 46(6): 1283-1308.
CrossRef Google scholar
[]
Suito K, Namba J, Horikawa T, et al. Phase Relations of CaCO3 at High Pressure and High Temperature. American Mineralogist, 2001, 86(9): 997-1002.
CrossRef Google scholar
[]
Suo S T, Zhong Z Q, Zhou H W, et al. Multi-Stage Tectonic Exhumation Processes of Ultrahigh-Pressure (UHP) Metamorphic Rocks in the Dabie-Sulu Area, East-Central China. Earth Science, 2012, 37(1): 1 17 (in Chinese with English Abstract)
[]
Tatsumi Y, Eggins S. Subduction Zone Magmatism, 1995 Cambridge Blackwell Science
[]
Tenthorey E, Hermann J. Composition of Fluids during Serpentinite Breakdown in Subduction Zones: Evidence for Limited Boron Mobility. Geology, 2004, 32(10): 865-868.
CrossRef Google scholar
[]
Tropper P, Manning C E. The Current Status of Titanite-Rutile Thermobarometry in Ultrahigh-Pressure Metamorphic Rocks: The Influence of Titanite Activity Models on Phase Equilibrium Calculations. Chemical Geology, 2008, 254(3/4): 123-132.
CrossRef Google scholar
[]
Tsuno K, Dasgupta R. The Effect of Carbonates on Near-Solidus Melting of Pelite at 3 GPa: Relative Efficiency of H2O and CO2 Subduction. Earth and Planetary Science Letters, 2012, 319/320: 185-196.
CrossRef Google scholar
[]
Wang S J, Teng F Z, Li S G. Tracing Carbonate-Silicate Interaction during Subduction Using Magnesium and Oxygen Isotopes. Nature Communications, 2014, 5: 5328.
CrossRef Google scholar
[]
Wu Y B, Zheng Y F, Zhao Z F, et al. U-Pb, Hf and O Isotope Evidence for Two Episodes of Fluid-Assisted Zircon Growth in Marble-Hosted Eclogites from the Dabie Orogen. Geochimica et Cosmochimica Acta, 2006, 70(14): 3743-3761.
CrossRef Google scholar
[]
Wyllie P J, Ryabchikov I D. Volatile Components, Magmas, and Critical Fluids in Upwelling Mantle. Journal of Petrology, 2000, 41(7): 1195-1206.
CrossRef Google scholar
[]
Xia Q K, Sheng Y M, Yang X Z, et al. Heterogeneity of Water in Garnets from UHP Eclogites, Eastern Dabieshan, China. Chemical Geology, 2005, 224(4): 237-246.
CrossRef Google scholar
[]
Xia Q X, Zheng Y F, Chen Y X. Protolith Control on Fluid Availability for Zircon Growth during Continental Subduction-Zone Metamorphism in the Dabie Orogen. Journal of Asian Earth Sciences, 2013, 67/68: 93-113.
CrossRef Google scholar
[]
Xia Q X, Zheng Y F, Zhou L G. Dehydration and Melting during Continental Collision: Constraints from Element and Isotope Geochemistry of Low-T/UHP Granitic Gneiss in the Dabie Orogen. Chemical Geology, 2008, 247(1/2): 36-65.
CrossRef Google scholar
[]
Xiao Y L, Sun H, Gu H O, et al. Fluid/Melt in Continental Deep Subduction Zones: Compositions and Related Geochemical Fractionations. Science China Earth Sciences, 2015, 58(9): 1457-1476.
CrossRef Google scholar
[]
Xiao Y L, Sun W D, Hoefs J, et al. Making Continental Crust through Slab Melting: Constraints from Niobium-Tantalum Fractionation in UHP Metamorphic Rutile. Geochimica et Cosmochimica Acta, 2006, 70(18): 4770-4782.
CrossRef Google scholar
[]
Xie Z J, Liu X W, Jin Z M, et al. Microstructures and Phase Transition in Omphacite: Constraints on the P-T Path of Shuanghe Eclogite (Dabie Orogen). Journal of Earth Science, 2020, 31(2): 254-261.
CrossRef Google scholar
[]
Xiong X L, Adam J, Green T H. Rutile Stability and Rutile/Melt HFSE Partitioning during Partial Melting of Hydrous Basalt: Implications for TTG Genesis. Chemical Geology, 2005, 218(3/4): 339-359.
CrossRef Google scholar
[]
Xiong X L, Keppler H, Audétat A, et al. Partitioning of Nb and Ta between Rutile and Felsic Melt and the Fractionation of Nb/Ta during Partial Melting of Hydrous Metabasalt. Geochimica et Cosmochimica Acta, 2011, 75(7): 1673-1692.
CrossRef Google scholar
[]
Xiong X, Keppler H, Audétat A, et al. Experimental Constraints on Rutile Saturation during Partial Melting of Metabasalt at the Amphibolite to Eclogite Transition, with Applications to TTG Genesis. American Mineralogist, 2009, 94(8/9): 1175-1186.
CrossRef Google scholar
[]
Yan W H, Wang Q, Li W Q. Behavior of Mg-Fe-C-O Isotopes at the Contact Zone between Marble and Eclogite in Subduction Zones. Acta Geologica Sinica, 2022, 96(2): 500 516 (in Chinese with English Abstract)
[]
Ye K, Liu J B, Cong B L, et al. Ultrahigh-Pressure (UHP) Low-Al Titanites from Carbonate-Bearing Rocks in Dabieshan-Sulu UHP Terrane, Eastern China. American Mineralogist, 2002, 87(7): 875-881.
CrossRef Google scholar
[]
Zack T, Kronz A, Foley S F, et al. Trace Element Abundances in Rutiles from Eclogites and Associated Garnet Mica Schists. Chemical Geology, 2002, 184(1/2): 97-122.
CrossRef Google scholar
[]
Zack T, Rivers T, Foley S. Cs-Rb-Ba Systematics in Phengite and Amphibole: An Assessment of Fluid Mobility at 2.0 GPa in Eclogites from Trescolmen, Central Alps. Contributions to Mineralogy and Petrology, 2001, 140(6): 651-669.
CrossRef Google scholar
[]
Zhai M G, Cong B L, Zhao Z, et al. High Pressure Jadeitic Quartzite from Dabie Eclogite Belt and Its Geological Implication. Chinese Science Bulletin, 1992, 37:1013-1015.
[]
Zhang R Y, Liou J G. Coesite Inclusions in Dolomite from Eclogite in the Southern Dabie Mountains, China; The Significance of Carbonate Minerals in UHPM Rocks. American Mineralogist, 1996, 81(1/2): 181-186.
CrossRef Google scholar
[]
Zhang R Y, Liou J G, Cong B L. Talc-, Magnesite- and Ti-Clinohumite-Bearing Ultrahigh-Pressure Meta-Mafic and Ultramafic Complex in the Dabie Mountains, China. Journal of Petrology, 1995, 36: 1011-1037.
CrossRef Google scholar
[]
Zhang Z M, Xiao Y L, Xu Z Q, et al. UHP Metamorphic Rocks from the Chinese Continental Scientific Drilling Project: I. Petrology and Geochemistry of the Main Hole (0-2, 050 m). Contributions to Mineralogy and Petrology, 2013, 166(1): 1.
CrossRef Google scholar
[]
Zhao Z F, Chen B, Zheng Y F, et al. Mineral Oxygen Isotope and Hydroxyl Content Changes in Ultrahigh-Pressure Eclogite-Gneiss Contacts from Chinese Continental Scientific Drilling Project Cores. Journal of Metamorphic Geology, 2007, 25(2): 165-186.
CrossRef Google scholar
[]
Zhao Z F, Zheng Y F, Chen R X, et al. Element Mobility in Mafic and Felsic Ultrahigh-Pressure Metamorphic Rocks during Continental Collision. Geochimica et Cosmochimica Acta, 2007, 71(21): 5244-5266.
CrossRef Google scholar
[]
Zheng Y F, Fu B, Gong B, et al. U-Pb Dating of Marble Associated with Eclogite from the Dabie Mountains, East China. Chinese Journal of Geochemistry, 1997, 16(3): 193-201.
CrossRef Google scholar
[]
Zheng Y F, Fu B, Gong B, et al. Carbon Isotope Anomaly in Marbles Associated with Eclogites from the Dabie Mountains. Chinese Science Bulletin, 1998, 43(2): 155-160.
CrossRef Google scholar
[]
Zheng Y F, Fu B, Gong B, et al. Stable Isotope Geochemistry of Ultrahigh Pressure Metamorphic Rocks from the Dabie-Sulu Orogen in China: Implications for Geodynamics and Fluid Regime. Earth-Science Reviews, 2003, 62(1/2): 105-161.
CrossRef Google scholar
[]
Zheng Y F, Fu B, Li Y L, et al. Oxygen and Hydrogen Isotope Geochemistry of Ultrahigh-Pressure Eclogites from the Dabie Mountains and the Sulu Terrane. Earth and Planetary Science Letters, 1998, 155(1/2): 113-129.
CrossRef Google scholar
[]
Zheng Y F, Fu B, Xiao Y L, et al. Hydrogen and Oxygen Isotope Evidence for Fluid-Rock Interactions in the Stages of Pre- and Post-UHP Metamorphism in the Dabie Mountains. Lithos, 1999, 46(4): 677-693.
CrossRef Google scholar
[]
Zheng Y F, Gao X Y, Chen R X, et al. Zr-in-Rutile Thermometry of Eclogite in the Dabie Orogen: Constraints on Rutile Growth during Continental Subduction-Zone Metamorphism. Journal of Asian Earth Sciences, 2011, 40(2): 427-451.
CrossRef Google scholar
[]
Zheng Y F, Gong B, Zhao Z F, et al. Two Types of Gneisses Associated with Eclogite at Shuanghe in the Dabie Terrane: Carbon Isotope, Zircon U-Pb Dating and Oxygen Isotope. Lithos, 2003, 70(3/4): 321-343.
CrossRef Google scholar
[]
Zheng Y F, Wu Y B, Zhao Z F, et al. Metamorphic Effect on Zircon Lu-Hf and U-Pb Isotope Systems in Ultrahigh-Pressure Eclogite-Facies Metagranite and Metabasite. Earth and Planetary Science Letters, 2005, 240(2): 378-400.
CrossRef Google scholar
[]
Zheng Y F, Xia Q X, Chen R X, et al. Partial Melting, Fluid Supercriticality and Element Mobility in Ultrahigh-Pressure Metamorphic Rocks during Continental Collision. Earth-Science Reviews, 2011, 107(3/4): 342-374.
CrossRef Google scholar
[]
Zheng Y F, Zhang S B, Zhao Z F, et al. Contrasting Zircon Hf and O Isotopes in the Two Episodes of Neoproterozoic Granitoids in South China: Implications for Growth and Reworking of Continental Crust. Lithos, 2007, 96(1/2): 127-150.
CrossRef Google scholar

Accesses

Citations

Detail

Sections
Recommended

/