Cooling and contamination of mafic and ultramafic magmas during ascent through continental crust
- 1 August 1985
- journal article
- Published by Elsevier BV in Earth and Planetary Science Letters
- Vol. 74 (4), 371-386
- https://doi.org/10.1016/s0012-821x(85)80009-1
Abstract
No abstract availableKeywords
This publication has 33 references indexed in Scilit:
- Contaminated komatiites (reply)Nature, 1985
- Contaminated komatiitesNature, 1985
- Emplacement and cooling of komatiite lavasNature, 1984
- Relative roles of source composition, fractional crystallization and crustal contamination in the petrogenesis of Andean volcanic rocksPhilosophical Transactions of the Royal Society of London. Series A, Mathematical and Physical Sciences, 1984
- Geochemical and isotopic evidence for the origin of continental flood basalts with particular reference to the Snake River Plain Idaho, U. S. APhilosophical Transactions of the Royal Society of London. Series A, Mathematical and Physical Sciences, 1984
- Relative contribution of crust and mantle to flood basalt magmatism, Mahabaleshwar area, Deccan TrapsPhilosophical Transactions of the Royal Society of London. Series A, Mathematical and Physical Sciences, 1984
- Elemental fingerprints of isotopic contamination of hebridean Palaeocene mantle-derived magmas by archaean sialBeiträge zur Mineralogie und Petrographie, 1982
- Thermal effects of basalt on continental crust and crustal contamination of magmasNature, 1980
- Boninites, komatiites and ophiolitic basaltsNature, 1979
- The petrogenesis of peridotitic komatiites: Evidence from high-pressure melting experimentsEarth and Planetary Science Letters, 1977