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Mineralogy of New Caledonian metamorphic rocks

III. Pyroxenes, and major element partitioning between coexisting pyroxenes, amphiboles and garnets from the Ouégoa district

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Abstract

The compositions of metamorphic pyroxenes from blueschists in northern New Caledonia are investigated. Aegerine-augite occurs in siliceous metasediments and aegerine in some low-grade sodic basic schists. Calcic metamorphic pyroxene (omphacite and chloromelanite) appears first in metabasalts in higher grades of the lawsonite zone and is widespread in metamorphosed igneous rocks and quartzofeldspathic gneisses of the epidote zone. Omphacites in basic rocks have higher Mg∶Fe ratios and are less jadeitic than omphacites from adjacent interbedded quartzofeldspathic gneisses. With increasing metamorphic grade pyroxenes become more jadeitic and diopsidic at the expense of their acmite component. Elemental partitioning between coexisting pyroxenes, garnets and amphiboles from in situ regional metamorphic rocks is generally regular, suggesting equilibrium crystallization. Omphacite appears to be a stable phase within blueschist facies over a temperature range of at least 350° to 550° C. The “eclogitic” assemblage almandine-omphacite is stable within the earth's crust in metamorphosed sediments and igneous rocks over a temperature range of 400° to at least 550° C. No estimate of absolute pressures involved in metamorphism in the Ouégoa district can yet be made.

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  1. Department of Geology, University of Auckland, Auckland, New Zealand

    Philippa M. Black

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  1. Philippa M. Black
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Black, P.M. Mineralogy of New Caledonian metamorphic rocks. Contr. Mineral. and Petrol. 45, 281–288 (1974). https://doi.org/10.1007/BF00371748

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  • DOI: https://doi.org/10.1007/BF00371748

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