Heterogeneity of Mantle Peridotites from the Polar Urals (Russia): Evidence from New LA-ICP-MS Data
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摘要
To discuss the nature of the compositional heterogeneity of the peridotite massifs of the Polar Urals(Russia), the geochemical study by LA-ICP-MS of pyroxenes and amphiboles from these mantle formations was performed. The trace element compositions in clinopyroxenes indicate the existence of the mantle protolith of two types. The first protolith type, represented by lherzolites and diopside harzburgites,was originated from the partial melting(5%–10%) under the spinel facies conditions, while the second one,represented by diopside harzburgites, was formed under the polybaric partial melting(17%–19%) under garnet and spinel facies conditions. Subsequently, the mantle peridotite protolith was subject to fluidinduced partial melting in the suprasubduction setting that was resulted in the formation of harzburgites.Being affected by penetrating melts and fluids peridotites experienced the refertilization(LREE enrichment of clinopyroxenes) and high-temperature hydratation with subsequent development of pargasite and Mg amphibole. The high-T fluid-induced metamorphism at the subduction zone was accompanied by the formation of metaperidotites with clinochlore and REE-depleted tremolite.
To discuss the nature of the compositional heterogeneity of the peridotite massifs of the Polar Urals(Russia), the geochemical study by LA-ICP-MS of pyroxenes and amphiboles from these mantle formations was performed. The trace element compositions in clinopyroxenes indicate the existence of the mantle protolith of two types. The first protolith type, represented by lherzolites and diopside harzburgites,was originated from the partial melting(5%–10%) under the spinel facies conditions, while the second one,represented by diopside harzburgites, was formed under the polybaric partial melting(17%–19%) under garnet and spinel facies conditions. Subsequently, the mantle peridotite protolith was subject to fluidinduced partial melting in the suprasubduction setting that was resulted in the formation of harzburgites.Being affected by penetrating melts and fluids peridotites experienced the refertilization(LREE enrichment of clinopyroxenes) and high-temperature hydratation with subsequent development of pargasite and Mg amphibole. The high-T fluid-induced metamorphism at the subduction zone was accompanied by the formation of metaperidotites with clinochlore and REE-depleted tremolite.
To discuss the nature of the compositional heterogeneity of the peridotite massifs of the Polar Urals(Russia), the geochemical study by LA-ICP-MS of pyroxenes and amphiboles from these mantle formations was performed. The trace element compositions in clinopyroxenes indicate the existence of the mantle protolith of two types. The first protolith type, represented by lherzolites and diopside harzburgites,was originated from the partial melting(5%–10%) under the spinel facies conditions, while the second one,represented by diopside harzburgites, was formed under the polybaric partial melting(17%–19%) under garnet and spinel facies conditions. Subsequently, the mantle peridotite protolith was subject to fluidinduced partial melting in the suprasubduction setting that was resulted in the formation of harzburgites.Being affected by penetrating melts and fluids peridotites experienced the refertilization(LREE enrichment of clinopyroxenes) and high-temperature hydratation with subsequent development of pargasite and Mg amphibole. The high-T fluid-induced metamorphism at the subduction zone was accompanied by the formation of metaperidotites with clinochlore and REE-depleted tremolite.
引文
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Arai,S.,Miura,M.,2016.Formation and Modification of Chromitites in the Mantle.Lithos,264:277-295.https://doi.org/10.1016/j.lithos.2016.08.039
Batanova,V.G.,Belousov,I.A.,Savelieva,G.N.,et al.,2011.Consequences of Channelized and Diffuse Melt Transport in Supra-Subduction Zone Mantle:Evidence from the Voykar Ophiolite(Polar Urals).Journal of Petrology,52(12):2483-2521.https://doi.org/10.1093/petrology/egr053
Belousov,I.A.,Batanova,V.G.,Savelieva,G.N.,et al.,2009.Evidence for the Suprasubduction Origin of Mantle Section Rocks of Voykar Ophiolite,Polar Urals.Doklady Earth Sciences,429(1):1394-1398.https://doi.org/10.1134/s1028334x09080340
Bizimis,M.,Salters,V.J.M.,Bonatti,E.,2000.Trace and REE Content of Clinopyroxenes from Supra-Subduction Zone Peridotites.Implications for Melting and Enrichment Processes in Island Arcs.Chemical Geology,165(1/2):67-85.https://doi.org/10.1016/s0009-2541(99)00164-3
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Hellebrand,E.,Snow,J.E.,Hoppe,P.,et al.,2002.Garnet-Field Melting and Late-Stage Refertilization in“Residual”Abyssal Peridotites from the Central Indian Ridge.Journal of Petrology,43(12):2305-2338.https://doi.org/10.1093/petrology/43.12.2305
Ishida,Y.,Morishita,T.,Arai,S.,et al.,2004.Simultaneous in-situ Multi-Element Analysis of Minerals on Thin Section Using LA-ICP-MS.The Science Reports of Kanazawa University,48:31-42
Ishii,T.,Robinson,P.T.,Maekawa,H.,et al.,1992.Petrological Studies of Peridotites from Diapiric Serpentinite Seamounts in the Izu-Ogazawara-Mariana Forearc,LEG 125.Proceeding of the Ocean Drilling Program,Scientific Results,125:445-485.https://doi.org/10.2973/odp.proc.sr.125.129.1992
Jean,M.M.,Shervais,J.W.,Choi,S.H.,et al.,2010.Melt Extraction and Melt Refertilization in Mantle Peridotite of the Coast Range Ophiolite:An LA-ICP-MS Study.Contributions to Mineralogy and Petrology,159(1):113-136.https://doi.org/10.1007/s00410-009-0419-0
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Johnson,K.T.M.,Dick,H.J.B.,1992.Open System Melting and Temporal and Spatial Variation of Peridotite and Basalt at the Atlantis II Fracture Zone.Journal of Geophysical Research,97(B6):9219-9241.https://doi.org/10.1029/92jb00701
Kelemen,P.B.,Shimizu,N.,Dunn,T.,1993.Relative Depletion of Niobium in some Arc Magmas and the Continental Crust:Partitioning of K,Nb,La and Ce during Melt/rock Reaction in the Upper Mantle.Earth and Planetary Science Letters,120(3/4):111-134.https://doi.org/10.1016/0012-821x(93)90234-z
Kelemen,P.B.,Hirth,G.,Shimizu,N.,et al.,1997.A Review of Melt Migration Processes in the Adiabatically Upwelling Mantle beneath Oceanic Spreading Ridges.Philosophical Transactions of the Royal Society of London Series A:Mathematical,Physical and Engineering Sciences,355(1723):283-318.https://doi.org/10.1098/rsta.1997.0010
Khedr,M.Z.,Arai,S.,Tamura,A.,et al.,2010.Clinopyroxenes in High-PMetaperidotites from Happo-O'ne,Central Japan:Implications for Wedge-Transversal Chemical Change of Slab-Derived Fluids.Lithos,119(3/4):439-456.https://doi.org/10.1016/j.lithos.2010.07.021
Leake,B.E.,Woolley,A.R.,Arps,C.E.S.,et al.,1997.Nomenclature of Amphiboles:Report of the Subcommittee on Amphiboles of the International Mineralogical Association Commission on New Minerals and Mineral Names.Mineralogical Magazine,61(405):295-310.https://doi.org/10.1180/minmag.1997.061.405.13
Longerich,H.P.,Jackson,S.E.,Günther,D.,1996.Inter-Laboratory Note.Laser Ablation Inductively Coupled Plasma Mass Spectrometric Transient Signal Data Acquisition and Analyte Concentration Calculation.Journal of Analutical Atomic Spectrometry,11(9):899-904.https://doi.org/10.1039/ja9961100899
Makeev,A.B.,Perevozchikov,B.V.,Afanasiev,A.K.,1985.Chromite Potential of the Polar Urals.Komi Fil.USSR Acad.Sci.,Siktivkar.152(in Russian)
Morishita,T.,Ishida,Y.,Arai,S.,et al.,2005.Determination of Multiple Trace Element Compositions in Thin(>30μm)Layers of NIST SRM 614 and 616Using Laser Ablation-Inductively Coupled Plasma-Mass Spectrometry(LA-ICP-MS).Geostandards and Geoanalytical Research,29(1):107-122.https://doi.org/10.1111/j.1751-908x.2005.tb00659.x
Muntener,O.,Manatschal,G.,Desmurs,L.,et al.,2010.Plagioclase Peridotites in Ocean-Continent Transitions:Refertilized Mantle Domains Generated by Melt Stagnation in the Shallow Mantle Lithosphere.Journal of Petrology,51(1/2):255-294.https://doi.org/10.1093/petrology/egp087
Mc Donough,W.F.,Sun,S.S.,1995.The Composition of the Earth.Chemical Geology,120(3/4):223-253.https://doi.org/10.1016/0009-2541(94)00140-4
Niu,Y.L.,2004.Bulk-Rock Major and Trace Element Compositions of Abyssal Peridotites:Implications for Mantle Melting,Melt Extraction and Post-Melting Processes beneath Mid-Ocean Ridges.Journal of Petrology,45(12):2423-2458.https://doi.org/10.1093/petrology/egh068
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Peacock,S.M.,Wang,K.,1999.Seismic Consequences of Warm Versus Cool Subduction Metamorphism:Examples from Southwest and Northeast Japan.Science,286(5441):937-939.https://doi.org/10.1126/science.286.5441.937
Pearce,N.J.G.,Perkins,W.T.,Westgate,J.A.,et al.,1997.A Compilation of New and Published Major and Trace Element Data for NIST SRM 610 and NIST SRM 612 Glass Reference Materials.Geostandards and Geoanalytical Research,21(1):115-144.https://doi.org/10.1111/j.1751-908x.1997.tb00538.x
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Arai,S.,1994.Characterization of Spinel Peridotites by Olivine-Spinel Compositional Relationships:Review and Interpretation.Chemical Geology,113(3/4):191-204.https://doi.org/10.1016/0009-2541(94)90066-3
Arai,S.,Miura,M.,2016.Formation and Modification of Chromitites in the Mantle.Lithos,264:277-295.https://doi.org/10.1016/j.lithos.2016.08.039
Batanova,V.G.,Belousov,I.A.,Savelieva,G.N.,et al.,2011.Consequences of Channelized and Diffuse Melt Transport in Supra-Subduction Zone Mantle:Evidence from the Voykar Ophiolite(Polar Urals).Journal of Petrology,52(12):2483-2521.https://doi.org/10.1093/petrology/egr053
Belousov,I.A.,Batanova,V.G.,Savelieva,G.N.,et al.,2009.Evidence for the Suprasubduction Origin of Mantle Section Rocks of Voykar Ophiolite,Polar Urals.Doklady Earth Sciences,429(1):1394-1398.https://doi.org/10.1134/s1028334x09080340
Bizimis,M.,Salters,V.J.M.,Bonatti,E.,2000.Trace and REE Content of Clinopyroxenes from Supra-Subduction Zone Peridotites.Implications for Melting and Enrichment Processes in Island Arcs.Chemical Geology,165(1/2):67-85.https://doi.org/10.1016/s0009-2541(99)00164-3
Chashchukhin,I.S.,Votyakov,S.L.,Shchapova,Y.V.,2007.Crystal Chemistry of Spinel and Oxythermobarometry of Ultramafic Rocks from Fold Areas.IGG UrO RAN,Yekaterinburg.310(in Russian)
Coltorti,M.,Bonadiman,C.,Faccini,B.,et al.,2007.Amphiboles from Suprasubduction and Intraplate Lithospheric Mantle.Lithos,99(1/2):68-84.https://doi.org/10.1016/j.lithos.2007.05.009
Dick,H.J.B.,Bullen,T.,1984.Chromian Spinel as a Petrogenetic Indicator in Abyssal and Alpine-Type Peridotites and Spatially Associated Lavas.Contributions to Mineralogy and Petrology,86(1):54-76.https://doi.org/10.1007/bf00373711
Dobretsov,N.L.,Moldavantsev,J.E.,Kazak,A.P.,et al.,1977.Petrology and Metamorphism of Ancient Pphiolites:Evidence from the Polar Urals and Western Sayan.Novosibirsk,Nauka.217(in Russian)
Hellebrand,E.,Snow,J.E.,Dick,H.J.B.,et al.,2001.Coupled Major and Trace Elements as Indicators of the Extent of Melting in Mid-Ocean-Ridge Peridotites.Nature,410(6829):677-681.https://doi.org/10.1038/35070546
Hellebrand,E.,Snow,J.E.,Hoppe,P.,et al.,2002.Garnet-Field Melting and Late-Stage Refertilization in“Residual”Abyssal Peridotites from the Central Indian Ridge.Journal of Petrology,43(12):2305-2338.https://doi.org/10.1093/petrology/43.12.2305
Ishida,Y.,Morishita,T.,Arai,S.,et al.,2004.Simultaneous in-situ Multi-Element Analysis of Minerals on Thin Section Using LA-ICP-MS.The Science Reports of Kanazawa University,48:31-42
Ishii,T.,Robinson,P.T.,Maekawa,H.,et al.,1992.Petrological Studies of Peridotites from Diapiric Serpentinite Seamounts in the Izu-Ogazawara-Mariana Forearc,LEG 125.Proceeding of the Ocean Drilling Program,Scientific Results,125:445-485.https://doi.org/10.2973/odp.proc.sr.125.129.1992
Jean,M.M.,Shervais,J.W.,Choi,S.H.,et al.,2010.Melt Extraction and Melt Refertilization in Mantle Peridotite of the Coast Range Ophiolite:An LA-ICP-MS Study.Contributions to Mineralogy and Petrology,159(1):113-136.https://doi.org/10.1007/s00410-009-0419-0
Johnson,K.T.M.,Dick,H.J.B.,Shimizu,N.,1990.Melting in the Oceanic Upper Mantle:An Ion Microprobe Study of Diopsides in Abyssal Peridotites.Journal of Geophysical Research,95(B3):2661-2678.https://doi.org/10.1029/jb095ib03p02661
Johnson,K.T.M.,Dick,H.J.B.,1992.Open System Melting and Temporal and Spatial Variation of Peridotite and Basalt at the Atlantis II Fracture Zone.Journal of Geophysical Research,97(B6):9219-9241.https://doi.org/10.1029/92jb00701
Kelemen,P.B.,Shimizu,N.,Dunn,T.,1993.Relative Depletion of Niobium in some Arc Magmas and the Continental Crust:Partitioning of K,Nb,La and Ce during Melt/rock Reaction in the Upper Mantle.Earth and Planetary Science Letters,120(3/4):111-134.https://doi.org/10.1016/0012-821x(93)90234-z
Kelemen,P.B.,Hirth,G.,Shimizu,N.,et al.,1997.A Review of Melt Migration Processes in the Adiabatically Upwelling Mantle beneath Oceanic Spreading Ridges.Philosophical Transactions of the Royal Society of London Series A:Mathematical,Physical and Engineering Sciences,355(1723):283-318.https://doi.org/10.1098/rsta.1997.0010
Khedr,M.Z.,Arai,S.,Tamura,A.,et al.,2010.Clinopyroxenes in High-PMetaperidotites from Happo-O'ne,Central Japan:Implications for Wedge-Transversal Chemical Change of Slab-Derived Fluids.Lithos,119(3/4):439-456.https://doi.org/10.1016/j.lithos.2010.07.021
Leake,B.E.,Woolley,A.R.,Arps,C.E.S.,et al.,1997.Nomenclature of Amphiboles:Report of the Subcommittee on Amphiboles of the International Mineralogical Association Commission on New Minerals and Mineral Names.Mineralogical Magazine,61(405):295-310.https://doi.org/10.1180/minmag.1997.061.405.13
Longerich,H.P.,Jackson,S.E.,Günther,D.,1996.Inter-Laboratory Note.Laser Ablation Inductively Coupled Plasma Mass Spectrometric Transient Signal Data Acquisition and Analyte Concentration Calculation.Journal of Analutical Atomic Spectrometry,11(9):899-904.https://doi.org/10.1039/ja9961100899
Makeev,A.B.,Perevozchikov,B.V.,Afanasiev,A.K.,1985.Chromite Potential of the Polar Urals.Komi Fil.USSR Acad.Sci.,Siktivkar.152(in Russian)
Morishita,T.,Ishida,Y.,Arai,S.,et al.,2005.Determination of Multiple Trace Element Compositions in Thin(>30μm)Layers of NIST SRM 614 and 616Using Laser Ablation-Inductively Coupled Plasma-Mass Spectrometry(LA-ICP-MS).Geostandards and Geoanalytical Research,29(1):107-122.https://doi.org/10.1111/j.1751-908x.2005.tb00659.x
Muntener,O.,Manatschal,G.,Desmurs,L.,et al.,2010.Plagioclase Peridotites in Ocean-Continent Transitions:Refertilized Mantle Domains Generated by Melt Stagnation in the Shallow Mantle Lithosphere.Journal of Petrology,51(1/2):255-294.https://doi.org/10.1093/petrology/egp087
Mc Donough,W.F.,Sun,S.S.,1995.The Composition of the Earth.Chemical Geology,120(3/4):223-253.https://doi.org/10.1016/0009-2541(94)00140-4
Niu,Y.L.,2004.Bulk-Rock Major and Trace Element Compositions of Abyssal Peridotites:Implications for Mantle Melting,Melt Extraction and Post-Melting Processes beneath Mid-Ocean Ridges.Journal of Petrology,45(12):2423-2458.https://doi.org/10.1093/petrology/egh068
Parkinson,I.J.,Pearce,J.A.,Thirwall,M.F.,et al.,1992.Trace Element Geochemistry of Peridotites from the Izu-Bonin-Mariana Forearc,Leg125.In:Fryer,P.,Pearce,J.A.,Stokking,L.B.,eds.,Proceedings of the Ocean Drilling Program:Scientific Results.487-506.https://doi.org/10.2973/odp.proc.sr.125.183.1992
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