Melt production by viscous dissipation: Role of heat advection by magma transport
- 1 February 1980
- journal article
- Published by American Geophysical Union (AGU) in Geophysical Research Letters
- Vol. 7 (2), 145-148
- https://doi.org/10.1029/gl007i002p00145
Abstract
No abstract availableThis publication has 14 references indexed in Scilit:
- Asthenospheric shear flow: Thermally stable or unstable?Geophysical Research Letters, 1977
- Textures and Fabrics of Upper-Mantle Peridotites as Illustrated by Xenoliths from BasaltsJournal of Petrology, 1975
- Viscous heat production in a slabJournal of Geophysical Research, 1973
- Possible Temperatures in the Oceanic Upper Mantle and the Formation of MagmaGSA Bulletin, 1973
- High temperature rhelogy of westerly graniteJournal of Geophysical Research, 1971
- Earth Tides, Global Heat Flow, and TectonicsScience, 1970
- Rheology of Basalt in the Melting RangeJournal of Petrology, 1969
- Two-component Flow Model for Convection in the Earth's Upper MantleNature, 1968
- The viscosity of basaltic magma; an analysis of field measurements in Makaopuhi lava lake, HawaiiAmerican Journal of Science, 1968
- Petrological evidence on temperature distribution in the mantle of the EarthEOS, Transactions American Geophysical Union, 1954