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of many gases and melted mantle rocks.[2(passive) is composedAndesitic magma
fractional crystallization and(passive) triggered bymagma differentiation
pegmatitesoriginatedfrom differentiated granitic magma
Styles of eruption are controlled more by the physical structure and stress environment of the lithosphere through which magmas ascendinfluencesthe extent of magma differentiation
a factorcausingfurther differentiation of the magma
degassing - induced crystallization during magma ascent ... and that the pressure sensor can also be regarded as a degassing sensor , with more hydrous melts beginning to degas at greater depths(passive) is triggered bymagma ponding
This fractionated melt was mixed with the overlying main magmacausingdifferentiation of the Kutsugata magma
the carbonatitic complexesoriginatedthrough the differentiation of a nephelinitic magma
BlackOpsNewsShow 0(passive) created byMagma , Encor
in the division of rocksresultsin the division of rocks
hematite to be There are in addition manyknown methods of separating magnetic iron from iron orescauseshematite to be There are in addition manyknown methods of separating magnetic iron from iron ores
successively in a pegmatitic rest - magma containing small amounts of metals and hydrothermal solutions containing abundant metalsresultedsuccessively in a pegmatitic rest - magma containing small amounts of metals and hydrothermal solutions containing abundant metals
in different magma its propertiesresultingin different magma its properties
to the Plinian eruptionsleadingto the Plinian eruptions
to variations of Zr / Hf but not those of Nb / Ta , suggesting major Nb / Ta fractionations during plate subductionmight have contributedto variations of Zr / Hf but not those of Nb / Ta , suggesting major Nb / Ta fractionations during plate subduction
in the heavier crystals settling in magma chamberresultsin the heavier crystals settling in magma chamber
cracks(passive) caused bycracks
alsomay ... causealso
in iron enrichment and is unlikely to be affected by variations in oxygen partial pressure or in the initial composition of the magmaresultsin iron enrichment and is unlikely to be affected by variations in oxygen partial pressure or in the initial composition of the magma