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Immiscibility |
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2003), and sulfur saturation is not related to the cooling of an enriched magma, but to the interaction between magma and crustal rocks to produce sulfide immiscibility. In the fifties, the condition of immiscibility in borate and silicate systems and its frequent occurrence had been noted by J. Senkler notes, for example, that a controlled degree of immiscibility serves as the key force to determine the size of rubber domains and their placement in the thermoplastic matrix. |
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