Origin of earliest planetary crust: role of compositional convection
- 31 January 1987
- journal article
- Published by Elsevier in Earth and Planetary Science Letters
- Vol. 81 (2-3) , 118-126
- https://doi.org/10.1016/0012-821x(87)90150-6
Abstract
No abstract availableKeywords
This publication has 24 references indexed in Scilit:
- Thermal structure of crystallizing magma with two-phase ConvectionGeological Magazine, 1986
- On the interaction between convection and crystallization in cooling magma chambersEarth and Planetary Science Letters, 1986
- Nucleation, crystal growth and the thermal regime of cooling magmasJournal of Geophysical Research, 1984
- Adcumulus growth of anorthosite at the base of the lunar crustJournal of Geophysical Research, 1982
- Barrier to crystal nucleation in anorthiteJournal of Non-Crystalline Solids, 1981
- The fluid dynamics of a basaltic magma chamber replenished by influx of hot, dense ultrabasic magmaContributions to Mineralogy and Petrology, 1981
- Snowflake troctolite in the Hettasch intrusion, Labrador: Evidence for magma-mixing and supercooling in a plutonic environmentContributions to Mineralogy and Petrology, 1980
- The coupled turbulent transports of salt and and heat across a sharp density interfaceInternational Journal of Heat and Mass Transfer, 1965
- Types of Igneous CumulatesJournal of Petrology, 1960
- Two-Phase Convection in Igneous MagmasThe Journal of Geology, 1918