Numerical model of crustal accretion and cooling rates of fast-spreading mid-ocean ridges

We designed a thermo-mechanical numerical model for fast-spreading mid-ocean ridge with variable viscosity, hydrothermal cooling, latent heat release, sheeted dyke layer, and variable melt intrusion possibilities. The model allows for modulating several accretion possibilities such as the "gabb...

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Bibliographic Details
Main Authors: P. Machetel, C. J. Garrido
Format: Article
Language:English
Published: Copernicus Publications 2013-10-01
Series:Geoscientific Model Development
Online Access:http://www.geosci-model-dev.net/6/1659/2013/gmd-6-1659-2013.pdf