Cumulate rock
igneous rocks formed by the accumulation of crystals from a magma either by settling or floating.
Cumulate rocks are igneous rocks formed by the accumulation of crystals from a magma either by settling or floating. Cumulate rocks are named according to their texture; cumulate texture is diagnostic of the conditions of formation of this group of igneous rocks. Cumulates can be deposited on top of other older cumulates of different composition and colour, typically giving the cumulate rock a layered or banded appearance.
Formation
Cumulate rocks are the typical product of precipitation of solid crystals from a fractionating magma chamber. These accumulations typically occur on the floor of the magma chamber, although they are possible on the roofs if anorthite plagioclase is able to float free of a denser mafic melt.
Cumulates are typically found in ultramafic intrusions, in the base of large ultramafic lava tubes in komatiite and magnesium rich basalt flows and also in some granitic intrusions.
Terminology
Cumulates are named according to their dominant mineralogy and the percentage of crystals to their groundmass (Hall, 1996).
Adcumulates are rocks containing ~100–93% accumulated magmatic crystals in a fine-grained groundmass.
Mesocumulates are rocks with between 93 and 85% accumulated minerals in a groundmass.
Orthocumulates are rocks containing between 85 and 75% accumulated minerals in groundmass.
“Cumulate rock” enters the record as igneous rocks formed by the accumulation of crystals from a magma either by settling or floating. Crown Archives preserves that source wording while asking what Cumulate, rock and igneous can confirm, complicate or overturn.
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