Coronas around Olivine in the Miaowan Olivine Norite, Yangtze Craton, South China
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摘要
Coronitic microstructures have been used to interpret the late-stage solidification history of igneous rocks and to constrain the corresponding chemical and/or physical changes. Coronas with three shells were also recognized in the Miaowan olivine norite, Yangtze Craton, South China. In our study, orthopyroxene intergrowth with vermicular magnetite in the inner shell is in optical continuity with magnetite-free orthopyroxene in the middle shell. In the outer shell of brown amphibole remaining magnetite-free orthopyroxene inclusions sporadically occur. Meanwhile Mg# values of orthopyroxene(76–80) in the inner and middle shells are basically consistent with olivine(78–81). In this paper, we propose a multi-stage genetic model for the formation of coronas in the Miaowan olivine norite. In the first stage, the magnetite-free orthopyroxene shell formed through reaction between primocrystal olivine with the residual Si-rich melt at 990–1 053 ℃ and 6.2–6.5 kbar. In the second stage, the orthopyroxene-magnetite symplectite shell formed when primocrystal olivine reacted with the late-stage residual Fe-rich melt promoted by high oxygen fugacity condition at 927–1 035 ℃ and 6.0–6.5 kbar. In the third stage, the brown amphibole shell formed as the presence of residual hydrous melt and replaced the middle shell at 821–900 ℃ and 5.5–6.0 kbar.
Coronitic microstructures have been used to interpret the late-stage solidification history of igneous rocks and to constrain the corresponding chemical and/or physical changes. Coronas with three shells were also recognized in the Miaowan olivine norite, Yangtze Craton, South China. In our study, orthopyroxene intergrowth with vermicular magnetite in the inner shell is in optical continuity with magnetite-free orthopyroxene in the middle shell. In the outer shell of brown amphibole remaining magnetite-free orthopyroxene inclusions sporadically occur. Meanwhile Mg# values of orthopyroxene(76–80) in the inner and middle shells are basically consistent with olivine(78–81). In this paper, we propose a multi-stage genetic model for the formation of coronas in the Miaowan olivine norite. In the first stage, the magnetite-free orthopyroxene shell formed through reaction between primocrystal olivine with the residual Si-rich melt at 990–1 053 ℃ and 6.2–6.5 kbar. In the second stage, the orthopyroxene-magnetite symplectite shell formed when primocrystal olivine reacted with the late-stage residual Fe-rich melt promoted by high oxygen fugacity condition at 927–1 035 ℃ and 6.0–6.5 kbar. In the third stage, the brown amphibole shell formed as the presence of residual hydrous melt and replaced the middle shell at 821–900 ℃ and 5.5–6.0 kbar.
Coronitic microstructures have been used to interpret the late-stage solidification history of igneous rocks and to constrain the corresponding chemical and/or physical changes. Coronas with three shells were also recognized in the Miaowan olivine norite, Yangtze Craton, South China. In our study, orthopyroxene intergrowth with vermicular magnetite in the inner shell is in optical continuity with magnetite-free orthopyroxene in the middle shell. In the outer shell of brown amphibole remaining magnetite-free orthopyroxene inclusions sporadically occur. Meanwhile Mg# values of orthopyroxene(76–80) in the inner and middle shells are basically consistent with olivine(78–81). In this paper, we propose a multi-stage genetic model for the formation of coronas in the Miaowan olivine norite. In the first stage, the magnetite-free orthopyroxene shell formed through reaction between primocrystal olivine with the residual Si-rich melt at 990–1 053 ℃ and 6.2–6.5 kbar. In the second stage, the orthopyroxene-magnetite symplectite shell formed when primocrystal olivine reacted with the late-stage residual Fe-rich melt promoted by high oxygen fugacity condition at 927–1 035 ℃ and 6.0–6.5 kbar. In the third stage, the brown amphibole shell formed as the presence of residual hydrous melt and replaced the middle shell at 821–900 ℃ and 5.5–6.0 kbar.
引文
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Baltatzis,E.,Skounakis,S.,1990.Coronas in Olivine-Gabbros from Lavanovo Village,Northern Pindos,Greece.Chemie der Erde-Geochemistry,50:297-302
Barton,M.,Gaans,C.V.,1988.Formation of Orthopyroxene-Fe-Ti Oxide Symplectites in Precambrian Intrusives,Rogaland,Southwestern Norway.American Mineralogist,73(9/10):1046-1059
Bucher,K.,Grapes,R.,2009.The Eclogite-Facies Allalin Gabbro of the Zermatt-Saas Ophiolite,Western Alps:A Record of Subduction Zone Hydration.Journal of Petrology,50(8):1405-1442.https://doi.org/10.1093/petrology/egp035
Chen,C.,Yuan,J.L.,Kong,L.Y.,et al.,2018.Documentation of Early Paleozoic Mafic Dykes in the Dahongshan Region,Northern Yangze Block and Its Geological Significance.Earth Science,43(7):2370-2388(in Chinese with English Abstract)
Chen,S.,Li,X.P.,Kong,F.M.,et al.,2018.Metamorphic Evolution and Zircon U-Pb Ages of the Nanshankou Mafic High Pressure Granulites from the Jiaobei Terrane,North China Craton.Journal of Earth Science,29(5):1219-1235.https://doi.org/10.1007/s12583-017-0956-9
Cheng,C.,Xia,B.,Zheng,H.,et al.,2018.Chronology,Geochemistry and Tectonic Significance of Daba Ophiolites in Western Segment of Yarlung Zangbo Suture Zone,Tibet.Earth Science,43(4):975-990(in Chinese with English Abstract)
Claeson,D.T.,1998.Coronas,Reaction Rims,Symplectites and Emplacement Depth of the Rymmen Gabbro,Transscandinavian Igneous Belt,Southern Sweden.Mineralogical Magazine,62(6):743-757.https://doi.org/10.1180/002646198548133
Coombs,M.L.,Gardner,J.E.,2004.Reaction Rim Growth on Olivine in Silicic Melts:Implications for Magma Mixing.American Mineralogist,89(5/6):748-758.https://doi.org/10.2138/am-2004-5-608
Cruciani,G.,Franceschelli,M.,Groppo,C.,et al.,2008.Formation of Clinopyroxene+Spinel and Amphibole+Spinel Symplectites in Coronitic Gabbros from the Sierra de San Luis(Argentina):A Key to Post-Magmatic Evolution.Journal of Metamorphic Geology,26(7):759-774.https://doi.org/10.1111/j.1525-1314.2008.00786.x
de Haas,G.J.L.,Nijland,T.G.,Valbracht,P.J.,et al.,2002.Magmatic versus Metamorphic Origin of Olivine-Plagioclase Coronas.Contributions to Mineralogy and Petrology,143(5):537-550.https://doi.org/10.1007/s00410-002-0362-9
Deng,H.,Peng,S.B.,Polat,A.,et al.,2017.Neoproterozoic IAT Intrusion into Mesoproterozoic MOR Miaowan Ophiolite,Yangtze Craton:Evidence for Evolving Tectonic Settings.Precambrian Research,289:75-94.https://doi.org/10.1016/j.precamres.2016.12.003
Dirksen,O.,Humphreys,M.C.S.,Pletchov,P.,et al.,2006.The2001-2004 Dome-Forming Eruption of Shiveluch Volcano,Kamchatka:Observation,Petrological Investigation and Numerical Modelling.Journal of Volcanology and Geothermal Research,155(3/4):201-226.https://doi.org/10.1016/j.jvolgeores.2006.03.029
Efimov,A.A.,Malitch,K.N.,2012.Magnetite-Orthopyroxene Symplectites in Gabbros of the Urals:A Structural Track of Olivine Oxidation.Geology of Ore Deposits,54(7):531-539.https://doi.org/10.1134/s1075701511070075
England,R.N.,1974.Corona Structures Formed by Near-Isochemical Reaction between Olivine and Plagioclase in a Metamorphosed Dolerite.Mineralogical Magazine,39(307):816-818.https://doi.org/10.1180/minmag.1974.039.307.11
Faryad,S.W.,Kachlík,V.,Sláma,J.,et al.,2015.Implication of Corona Formation in a Metatroctolite to the Granulite Facies Overprint of HP-UHP Rocks in the Moldanubian Zone(Bohemian Massif).Journal of Metamorphic Geology,33(3):295-310.https://doi.org/10.1111/jmg.12121
Gao,S.,Yang,J.,Zhou,L.,et al.,2011.Age and Growth of the Archean Kongling Terrain,South China,with Emphasis on 3.3 Ga Granitoid Gneisses.American Journal of Science,311(2):153-182.https://doi.org/10.2475/02.2011.03
Gardner,P.M.,Robins,B.,1974.The Olivine-Plagioclase Reaction:Geological Evidence from the Seiland Petrographic Province,Northern Norway.Contributions to Mineralogy and Petrology,44(2):149-156.https://doi.org/10.1007/bf00385787
Goode,A.D.T.,1974.Oxidation of Natural Olivines.Nature,248(5448):500-501.https://doi.org/10.1038/248500a0
Grant,S.M.,1988.Diffusion Models for Corona Formation in Metagabbros from the Western Grenville Province,Canada.Contributions to Mineralogy and Petrology,98(1):49-63.https://doi.org/10.1007/bf00371909
Hammarstrom,J.M.,Zen,E.,1986.Aluminum in Hornblende:An Empirical Igneous Geobarometer.American Mineralogist,71(11):1297-1313.https://doi.org/10.1180/minmag.1986.050.358.28
Han,Q.S.,Peng,S.B.,Kusky,T.,et al.,2017.A Paleoproterozoic Ophiolitic Mélange,Yangtze Craton,South China:Evidence for Paleoproterozoic Suturing and Microcontinent Amalgamation.Precambrian Research,293:13-38.https://doi.org/10.1016/j.precamres.2017.03.004
Haselton,J.D.,Nash,W.P.,1975.Ilmenite-Orthopyroxene Intergrowths from the Moon and the Skaergaard Intrusion.Earth and Planetary Science Letters,26(3):287-291.https://doi.org/10.1016/0012-821x(75)90003-5
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