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- W1994371552 abstract "Summary Igneous layering resulting from variations in intercumulus mineralogy has been observed in the Kalka Intrusion in central Australia. The layering is parallel to cumulus layering, and is outlined by a mottled heteradcumulus ‘clump’ texture in leucogabbros, which occur in a generally adcumulate anorthositic sequence. Such intercumulus layering is thought to originate in slow cooling intrusions at times of slow crystal accumulation and/or relatively high rates of intercumulus crystallization when a zone of melt supersaturation (the cumulus nucleation zone) rises above the intrusion floor leaving the intercumulus melt undersaturated with respect to the settled cumulus phases. Adcumulates are produced when the supersaturated zone is coincident with the top of the crystal pile. The morphological elongation of clump plates parallel to the gross layering is probably controlled by the cumulus plagioclase fabric which tends to be planar laminate." @default.
- W1994371552 created "2016-06-24" @default.
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- W1994371552 date "1977-05-01" @default.
- W1994371552 modified "2023-09-23" @default.
- W1994371552 title "Intercumulus igneous layering in the Kalka Layered Intrusion, central Australia" @default.
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- W1994371552 doi "https://doi.org/10.1017/s0016756800044794" @default.
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