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Boninite primary magmas: Evidence from the Cape Vogel Peninsula, PNG

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Abstract

Boninites from Cape Vogel, PNG, are dominantly pyroxene-glass rocks, but many contain olivine, sometimes as refractory as Fo94. We derive a parental magma for this suite (in equilibrium with Fo94) which contains 20 wt.% MgO and is quartz-normative. This liquid is hydrous, and from petrographie evidence and whole rock H2O+ values, we estimate it to contain 2–3 wt.% H2O. These data suggest olivine fractionation and primary magmatic water are important in boninite genesis, but both are often obscured by later alteration. The derived parental magma has probably formed at 1,250–1,300° C and low pressures (< ?10kB) and is similar to those which gave rise to olivine-clinoenstatite phyric boninites from New Caledonia and from Howqua, Australia, and possibly to a proposed parental magma for the Bushveld Complex.

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References

  • Akella J, Williams RF, Mullins O (1976) Solubility of Cr, Ti and Al in coexisting olivine, spinel and liquid at 1 atm. Proc 7th Lunar Sci Conf, 1179–1194

  • Arculus RJ, Johnson RW, Chappell BW, McKee CO, Sakai H (1983) Ophiolite-contaminated andesites, trachybasalts, and cognate inclusions of Mount Lamington, Papua New Guinea: Anhydrite-amphibole-bearing lavas and the 1951 cumulodome. J Volcanol Geotherm Res (in press)

  • Bickle MJ, Ford CE, Nisbet EG (1977) The petrogenesis of peridotitic komatiites: evidence from high pressure melting experiments. Earth Planet Sci Lett 37:97–106

    Google Scholar 

  • Burnham CW (1975) Water and magmas: a mixing model. Geochim Cosmochim Acta 39:1077–1084

    Google Scholar 

  • Burnham CW (1979) The importance of volatile constituents. In: Yoder HS Jr (ed) The evolution of the igneous rocks, Princeton University Press, pp 439–482

  • Cameron WE, Nisbet EG, Dietrich VJ (1979) Boninites, komatiites and ophiolitie basalts. Nature 280:550–553

    Google Scholar 

  • Cameron WE, Nisbet EG (1982) Phanerozoic analogues of komatiitic basalts. In: Arndt NT, Nisbet EG (eds) Komatiites. Alien and Unwin, London pp 29–50

    Google Scholar 

  • Cameron WE, McCulloch MT, Walker DA (1983) Boninite petrogenesis: chemical and Nd-Sr isotopic constraints. Earth Planet Sci Lett (in press)

  • Crawford AJ (1980) A clinoenstatite-bearing cumulate olivine pyroxenite from Howqua, Victoria. Contrib Mineral Petrol 75:353–367

    Google Scholar 

  • Crawford AJ, Cameron WE, Keays RR (1983) The association boninite-low-Ti andesite-tholeiite in the Heathcote Greenstone Belt, Victoria. J Geol Soc Australia (in press)

  • Dallwitz WB (1968) Chemical composition and genesis of clinoenstatite-bearing volcanic rocks from Cape Vogel area, Papua: a discussion. Proc 23rd Int Geol Congr 2:229–242

    Google Scholar 

  • Dallwitz WB, Green DH, Thompson JE (1966) Clinoenstatite in a volcanic rock from the Cape Vogel area, Papua. J Petrol 7:375–403

    Google Scholar 

  • Davies G, Cawthorn RG, Barton JM Jr, Morton M (1980) Parental magma to the Bushveld complex. Nature 287:33–35

    Google Scholar 

  • Dietrich V, Gansser A, Sommerauer J, Cameron WE (1981) Paleogene komatiites from Gorgona Island, East Pacific — A primary magma for ocean floor basalts? Geochem J 15:141–161

    Google Scholar 

  • Drake MJ, Holloway JR (1981) Partitioning of Ni between olivine and silicate melt: the ‘Henry's Law problem’ re-examined. Geochim Cosmochim Acta 45:431–437

    Google Scholar 

  • Duke JM (1976) Distribution of the period four transition elements among olivine, calcic clinopyroxene and mafic silicate liquid: experimental results. J Petrol 17:499–521

    Google Scholar 

  • England RN, Davies HL (1973) Mineralogy of ultramafic cumulates and tectonites from Eastern Papua. Earth Planet Sci Lett 17:416–425

    Google Scholar 

  • Frey FA, Bryan WB, Thompson G (1974) Atlantic ocean floor: geochemistry and petrology of basalts from Legs 2 and 3 of the Deep Sea Drilling Project. J Geophys Res 79:5507–5527

    Google Scholar 

  • Gill JB (1981) Orogenic andesites and plate tectonics. Springer, New York

    Google Scholar 

  • Green DH (1976) Experimental testing of ‘equilibrium’ partial melting of peridotite under water-saturated, high-pressure conditions. Can Mineral 14:255–268

    Google Scholar 

  • Green DH, Nicholls IA, Viljoen MF, Viljoen RP (1975) Experimental demonstration of the existence of peridotitic liquids in earliest Archaean magmatism. Geology 3:11–14

    Google Scholar 

  • Green DH, Hibberson WD, Jaques AL (1979) Petrogenesis of midocean ridge basalts. In: McElhinney MH (ed) The earth: its origin, structure and evolution. Academic Press, London pp 265–299

    Google Scholar 

  • Hart SR, Davies KE (1978) Nickel partitioning between olivine and silicate melt. Earth Planet Sci Lett 40:203–219

    Google Scholar 

  • Henderson P (1975) Reaction trends shown by chrome spinels of the Rhum layered intrusion. Geochim Cosmochim Acta 39:1035–1044

    Google Scholar 

  • Hickey R, Frey FA (1982) Geochemical characteristics of boninite series volcanics: implications for their source. Geochim Cosmochim Acta 46:2099–2115

    Google Scholar 

  • Irvine TN (1979) Rocks whose composition is determined by crystal accumulation and sorting. In: Yoder HS Jr (ed) The evolution of the igneous rocks. Princeton University Press, pp 245–306

  • Irving AJ (1978) A review of experimental studies of crystal/liquid trace element partitioning. Geochim Cosmochim Acta 42:743–770

    Google Scholar 

  • Ishii T (1975) The relations between temperature and composition of pigeonite in some lavas and their application to geothermometry. Mineral J 8:48–57

    Google Scholar 

  • Jaques AL, Chappell BW (1980) Petrology and trace element geochemistry of the Papuan Ultramafic Belt. Contrib Mineral Petrol 75:55–70

    Google Scholar 

  • Jenner GA (1981) Geochemistry of high-Mg andesites from Cape Vogel, PNG. Chem Geology 33:307–332

    Google Scholar 

  • Kushiro I (1972) Effect of H2O on the composition of magmas formed at high pressures. J Petrol 13:311–334

    Google Scholar 

  • Mysen BO (1976) Nickel partitioning between upper mantle crystals and partial melts as a function of pressure, temperature, and nickel concentration. Carnegie Inst Wash Yearb 75:662–668

    Google Scholar 

  • Nabalek PI (1980) Nickel partitioning between olivine and liquid in natural basalts: Henry's Law behaviour. Earth Planet Sci Lett 48:293–302

    Google Scholar 

  • Natland J (1981) Crystal morphologies and pyroxene compositions in boninites and tholeiitic basalts from the Deep Sea Drilling Project, Holes 458 and 459 in the Mariana fore-arc region. In: Hussong DM, Uyeda S (eds) Initial reports of the deep sea drilling project. US Gov Printing Office, Washington 60:681–707

    Google Scholar 

  • Perfit MR, Gust DA, Bence AE, Arculus RJ, Taylor SR (1980) Chemical characteristics of island-arc basalts: implications for mantle sources. Chem Geology 30:227–256

    Google Scholar 

  • Ritchey JL, Eggler DH (1978) Amphibole stability in a differentiated calc-alkaline magma chamber: an experimental investigation. Carnegie Inst Wash Yearb 77:790–793

    Google Scholar 

  • Roeder PL, Emslie RF (1970) Olivine-liquid equilibrium. Contrib Mineral Petrol 29:275–289

    Google Scholar 

  • Roeder PL, Campbell IA, Jamieson HE (1979) A re-evaluation of the olivine-spinel geothermometer. Contrib Mineral Petrol 68:325–334

    Google Scholar 

  • Schreiber HD, Haskin LA (1976) Chromium in basalts: experimental determination of redox states and partitioning among synthetic silicate phases. Proc 7th Lunar Sci Conf:1221–1260

  • Sharaskin AYa, Dobretsov NL, Sobolev NV (1980) Marianites: the clinoenstatite bearing pillow-lavas associated with the ophiolite assemblage of Mariana trench. In: Panayiotou A (ed) Ophiolites. Cyprus Geol Survey, Nicosia pp 473–479

    Google Scholar 

  • Smith IE, Davies HL (1976) Geology of the southeast Papuan mainland. Bull Aust Bur Mineral Res 165

  • Sun S-S, Nesbitt RW (1978) Geochemical regularities and genetic significance of ophiolitic basalts. Geology 6:689–693

    Google Scholar 

  • Tatsumi Y (1981) Melting experiments on a high-magnesian andesite. Earth Planet Sci Lett 54:357–365

    Google Scholar 

  • Tilley CE, Yoder HS Jr, Schairer JF (1964) New relations on melting of basalts. Carnegie Inst Washington Yearb 63:92–97

    Google Scholar 

  • Varne R, Brown AV (1978) The geology and petrology of the Adamsfield ultramafic complex, Tasmania. Contrib Mineral Petrol 67:195–207

    Google Scholar 

  • Walker DA, McDougall I (1982) 40Ar/39Ar and K-Ar dating of altered glassy volcanic rocks: the Dabi Volcanics PNG. Geochim Cosmochim Acta 46:2181–2190

    Google Scholar 

  • Warner RD (1973) Liquidus relations in the system CaO-MgO-SiO2-H2O at 10 kb \(P_{H_2 O} \) and their petrologic significance. Am J Sci 273:925–946

    Google Scholar 

  • Wilson AH (1982) The geology of the Great ‘Dyke’, Zimbabwe: the ultramafic rocks. J Petrol 23:240–292

    Google Scholar 

  • Wyllie PJ (1979) Petrogenesis and physics of the Earth. In: Yoder HS Jr (ed) The evolution of the igneous rocks. Princeton University Press, pp 483–520

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Walker, D.A., Cameron, W.E. Boninite primary magmas: Evidence from the Cape Vogel Peninsula, PNG. Contr. Mineral. and Petrol. 83, 150–158 (1983). https://doi.org/10.1007/BF00373088

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  • DOI: https://doi.org/10.1007/BF00373088

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