This research demonstrates thermal reactions of basite magma influencing rock transformation, suggesting important geological processes.
Thermal reaction of basite magma with the enclosing rocks manifests itself in recrystallization of the cover rocks, their partial melting or dissociation of dolomites in a scale of fluidization of “carbonate salt” deposits. As basite magma reacts with these rocks, the immiscibility evolves to form 2 or 3 liquids: aluminosilicate, “ore-silicate”, and ferritic.
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Sharapov et al. (1992) studied this question.
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