Evidence for Komatiite‐type lavas on Mars from Phobos ISM data and other observations
- 15 May 1994
- journal article
- Published by American Geophysical Union (AGU) in Geophysical Research Letters
- Vol. 21 (10) , 887-890
- https://doi.org/10.1029/94gl01002
Abstract
No abstract availableKeywords
This publication has 16 references indexed in Scilit:
- Results from the ISM experimentNature, 1989
- Komatiites II: Experimental and Theoretical Investigations of Post-emplacement Cooling and CrystallizationJournal of Petrology, 1986
- SNC meteorites: Clues to Martian petrologic evolution?Reviews of Geophysics, 1985
- Komatiites I: Eruption and FlowJournal of Petrology, 1985
- Petrogenesis of the Elephant Moraine A79001 meteorite: Multiple magma pulses on the shergottite parent bodyGeochimica et Cosmochimica Acta, 1983
- A review of lava flow processes related to the formation of lunar sinuous rillesSurveys in Geophysics, 1982
- Pyroxene accumulation in spinifex-textured rocksGeological Magazine, 1982
- On the original igneous source of Martian finesIcarus, 1981
- Internal structure and properties of MarsIcarus, 1977
- Komatiitic and Iron-rich Tholeiitic Lavas of Munro Township, Northeast OntarioJournal of Petrology, 1977