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Magmatic underplating and crustal intrusions accommodate extension during Red Sea continental rifting. [PDF]
Nat CommunSanfilippo A +10 more
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Reviews in Mineralogy and Geochemistry, 2004
Epidote was first recognized as a magmatic mineral in the alpine Bergell tonalite by Cornelius (1915). Field observations and microscopic textures let Cornelius to conclude "... the only possibility is, that epidote is a primary mineral in our tonalite, crystallizing early from the magma, i.e., before (in part also contemporaneous with) biotite ...
M. W. Schmidt, S. Poli
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Epidote was first recognized as a magmatic mineral in the alpine Bergell tonalite by Cornelius (1915). Field observations and microscopic textures let Cornelius to conclude "... the only possibility is, that epidote is a primary mineral in our tonalite, crystallizing early from the magma, i.e., before (in part also contemporaneous with) biotite ...
M. W. Schmidt, S. Poli
openaire +5 more sources
Geological Society, London, Memoirs, 1993
AbstractDuring the past 150 years, a wide range of processes have been invoked to explain the mechanism by which magmas differentiate.These may be divided into those which operate essentially in the liquid state, such as liquid immiscibility and thermogravitational diffusion, and those which involve some form of crystal-liquid fractionation.
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AbstractDuring the past 150 years, a wide range of processes have been invoked to explain the mechanism by which magmas differentiate.These may be divided into those which operate essentially in the liquid state, such as liquid immiscibility and thermogravitational diffusion, and those which involve some form of crystal-liquid fractionation.
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Passive magmatism on Earth and Earth-like planets
Geosystems and Geoenvironment, 2022San-Zhong Li, Yanhui Suo
exaly