par Wollast, Roland ;Pytkowicz, Ricardo MARCOS
Référence Geochemical Journal, 12, 3, page (199-200)
Publication Publié, 1978
Article révisé par les pairs
Résumé : In this work the conditions required for the presence of two solid phases in equilibrium with a solution are discussed with special reference to the co-existence of magnesium calcites and dolomite in seawater. The criterion is determined in terms of the phase rule and of the solid-seawater ratio. © 1978, GEOCHEMICAL SOCIETY OF JAPAN. All rights reserved.