CORDIS Project
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This project develops models that integrate magmatism into the dynamics of continental rifts and mid-ocean ridges. By applying a two-phase flow theory, it seeks to enhance our understanding of plate tectonics and the role of magma in geological processes.
There is widespread recognition of the central role of magma at divergent plate boundaries.
However in almost all models, magmatism is treated as a by-product and is excluded from the dynamics. A thorough understanding of continental rifts and mid-ocean ridges, which are fundamental to plate tectonics, requires consistent models of magma intrusion into the lithosphere and crust.
This is a proposal to develop models in which magmatism is an integral thermal, chemical, and mechanical component, an…
THE CHANCELLOR, MASTERS AND SCHOLARS OF THE UNIVERSITY OF OXFORD
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