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intrusive magma GEOL

magma chamber GEOL

Monolingual examples (not verified by PONS Editors)

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Phlogopite and/or potassic amphibole probably are typical in the sources from which many such magmas have been derived.
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Nepheline benmoreite magmas derived from mantle sources containing lherzolite xenoliths display similarities to some plutonic nepheline syenites.
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These results have been used to provide indication of the conditions prevailing during the progressive crystallization of magmas.
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These pyroxenite layers have come to be inferred as a yield of the reaction between rising magmas and peridotite of the upper mantle.
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Primary melts derived from the mantle are especially important, and are known as "primitive melts" or primitive magmas.
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The high water contents of back-arc basin basalt magmas is derived from water carried down the subduction zone and released into the overlying mantle wedge.
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Many explanations focus on water content and oxidation states of the magmas.
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In the western portion of the field the buttes consist of the feeder diatremes of monchiquite and nepheline syenite magmas.
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