Igneous rock associations 10. Komatiites
J Dostal - Geoscience Canada, 2008 - erudit.org
Komatiites are ultramafic volcanic rocks that occur mainly in Archean and Paleoproterozoic
greenstone belts. These olivine-rich rocks are assumed to have crystallized from magmas …
greenstone belts. These olivine-rich rocks are assumed to have crystallized from magmas …
Hydrous komatiites from Commondale, South Africa: an experimental study
This study examines the emplacement conditions of komatiites in the 3.33 Ga Commondale
Ultramafic Suite in South Africa. The komatiites of Commondale are unlike any other …
Ultramafic Suite in South Africa. The komatiites of Commondale are unlike any other …
[HTML][HTML] Department of Geology Saint Mary's University Halifax, NS, Canada, B3H 3C3 jdostal@ smu. ca Submitted March 2008. Accepted as revised, June 2008
J Dostal - journals.lib.unb.ca
Komatiites are ultramafic volcanic rocks that occur mainly in Archean and Paleoproterozoic
greenstone belts. These olivine-rich rocks are assumed to have crystallized from magmas …
greenstone belts. These olivine-rich rocks are assumed to have crystallized from magmas …