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Kimberlitic chromian pocroilmenities with intergrowths of titanian chromite and rutile

Bruce A. Wyatt

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Abstract

A suite of chromian picroilmenite macrocrysts (up to 13 wt% Cr203 %) from kimberlite which contain lameliar intergrowths of titanian chromites (23–42 wt% TiO2, 7–16 wt% Cr2O3) and rutile are described. Using the mineral chemistry of coexisting phases in the natural assemblages as well as the preliminary results of an ongoing study on the system, ilmenite-spinel, it has been possible to construct a phase compatibility diagram for systems containing ilmenite-spinel-Cr2O3-rutile relevant to upper mantle conditions. A model is developed whereby the spinel and rutile lamellae intergrowths may be formed by an initial step involving reduction “exsolution” followed by isochemical breakdown during cooling.

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A suite of chromian picroilmenite macrocrysts (up to 13 wt% Cr203 %) from kimberlite which contain lameliar intergrowths of titanian chromites (23–42 wt% TiO2, 7–16 wt% Cr2O3) and rutile are described. Using the mineral chemistry of coexisting phases in the natural assemblages as well as the preliminary results of an ongoing study on the system, ilmenite-spinel, it has been possible to construct a phase compatibility diagram for systems containing ilmenite-spinel-Cr2O3-rutile relevant to upper mantle conditions. A model is developed whereby the spinel and rutile lamellae intergrowths may be formed by an initial step involving reduction “exsolution” followed by isochemical breakdown during cooling.

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Available abstract

A suite of chromian picroilmenite macrocrysts (up to 13 wt% Cr203 %) from kimberlite which contain lameliar intergrowths of titanian chromites (23–42 wt% TiO2, 7–16 wt% Cr2O3) and rutile are described. Using the mineral chemistry of coexisting phases in the natural assemblages as well as the preliminary results of an ongoing study on the system, ilmenite-spinel, it has been possible to construct a phase compatibility diagram for systems containing ilmenite-spinel-Cr2O3-rutile relevant to upper mantle conditions. A model is developed whereby the spinel and rutile lamellae intergrowths may be formed by an initial step involving reduction “exsolution” followed by isochemical breakdown during cooling.

Key concepts: Ilmenite, Rutile, Spinel, Kimberlite, Chromite, Geochemistry, Geology, Mineralogy

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