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Magma
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Hot semifluid material found beneath the surface of Earth
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Subject of 6
Time scales of crystal mixing in magma mushes
scholarly article by Jillian M. Schleicher et al published 24 February 2016 in Geophysical Research Letters
Time Scales of Crystal Fractionation in Magma Chambers—Integrating Physical, Isotopic and Geochemical Perspectives
Trends in rhyolite geochemistry, mineralogy, and magma storage during the last 50 kyr at Okataina and Taupo volcanic centres, Taupo Volcanic Zone, New Zealand
scholarly article by Victoria C. Smith et al published December 2005 in Journal of Volcanology and Geothermal Research
Martian magmas contained abundant chlorine, but little water
scholarly article by Justin Filiberto & Allan Treiman published 1 December 2009 in Geology
Experimental evidence for the origin of lead enrichment in convergent-margin magmas
scientific article published in Nature
Seismic anisotropy from compositional banding in granulites from the deep magmatic arc of Fiordland, New Zealand
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Wikipedia

Magma (from Ancient Greek μάγμα (mágma) 'thick unguent') is the molten or semi-molten natural material from which all igneous rocks are formed. Magma (sometimes colloquially but incorrectly referred to as lava) is found beneath the surface of the Earth, and evidence of magmatism has also been discovered on other terrestrial planets and some...

Subclass of
Stone
References
Wikidata