At Seriphos, Cyclades, Greece, the shallow intrusion of a granodiorite pluton produced a contact metamorphic aureole and extensive contact metasomatic skarn and Fe-ore deposits. Based on geological evidence a simplified, one-dimensional, two-stage mathematical model is developed describing the coupled transfer of heat and mass during the thermal evolution of the intrusive system.-from Authors
CITATION STYLE
Salemink, J., & Schuiling, R. D. (1987). A two-stage, transient heat and mass transfer model for tht granodiorite intrusion at Seriphos, Greece, and the associated formation of contact metasomatic skarn and Fe- ore deposits. Chemical Transport in Metasomatic Processes, 547–575. https://doi.org/10.1007/978-94-009-4013-0_20
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