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• W2600763846 abstract "Ilmenite is a near-liquidus mineral in picrite near t}te base of the Mount Ayliff Intrusion, Transkei. The ilmenite contains up to l l wt.%o MgO and over l9o Cr2O3, and is texturally and chemically anomalous with respect to all other tholeiitic suites. In a single sample ilmenite compositions are similar, regardless of enclosing silicate phases, which precludes extensive subsolidus re-equilibration, The overlying gabbro contains ilmenite that is low in magnesium and chromium, and that is texturally comparable to typi cal ilmenite in tholeiitic rocks where it usually forms as a near-solidus mineral. These differences in the two types of ilmenite are attributed to the emplacement of two distinct magma types, one tloleiitic, tle other more magnesian. The nickel content of olivine has been studied in samples from two profiles through the picrite and gabbro, and provides evidence for the timing and extent of formation of an immiscible sulfide liquid. In one profile (Ingeli) these data suggest continuous separation of olivine and very minor sulfide liquid in the picrite. In contrast, the data for the second profile (Ionti) suggest he separation oflarger quantities of sulfide near the base and top of the picrite, which may result from mixing between distinct magma pulses." @default.
• W2600763846 created "2017-04-07" @default.
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• W2600763846 date "1988-03-01" @default.
• W2600763846 modified "2023-09-24" @default.
• W2600763846 title "Contrasting magma-types in the Mount Ayliff Intrusion (Insizwa Complex), Transkei; evidence from ilmenite compositions" @default.
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• W2600763846 hasPublicationYear "1988" @default.
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