Fluid compositions in equilibrium with silica-undersaturated magmas in the system Na<SUB>2</SUB>O-Al<SUB>2</SUB>O<SUB>3</SUB>-SiO<SUB>2</SUB>-H<SUB>2</SUB>O: Clues to the composition of fenitizing fluids

Abstract

NatuurwetenskappeAardwetenskappePlease help us populate SUNScholar with the post print version of this article. It can be e-mailed to: [email protected]

    Similar works