Phyllosilicate‐poor palagonitic dust from Mauna Kea Volcano (Hawaii): A mineralogical analogue for magnetic Martian dust?
- 25 March 2001
- journal article
- Published by American Geophysical Union (AGU) in Journal of Geophysical Research
- Vol. 106 (E3) , 5057-5083
- https://doi.org/10.1029/2000je001328
Abstract
No abstract availableKeywords
This publication has 79 references indexed in Scilit:
- Controls on palagonitization versus pedogenic weathering of basaltic tephra: Evidence from the consolidation and geochemistry of the Keanakako'i Ash Member, Kilauea VolcanoGeochemistry, Geophysics, Geosystems, 2000
- Mineralogy, composition, and alteration of Mars Pathfinder rocks and soils: Evidence from multispectral, elemental, and magnetic data on terrestrial analogue, SNC meteorite, and Pathfinder samplesJournal of Geophysical Research, 2000
- Magnetic enhancement on the surface of Mars?Journal of Geophysical Research, 2000
- Mineralogic and compositional properties of Martian soil and dust: Results from Mars PathfinderJournal of Geophysical Research, 2000
- Martian soil simulant available for scientific, educational studyEos, 1998
- Hisingerite: A Ferric Kaolin Mineral with Curved MorphologyClays and Clay Minerals, 1998
- In situ compositions of Martian volcanics: Implications for the mantleJournal of Geophysical Research, 1997
- Low‐temperature reflectivity spectra of red hematite and the color of MarsJournal of Geophysical Research, 1997
- Spatial Variations in the Spectral Properties of Bright Regions on MarsIcarus, 1993
- Ferrihydrite and allophane in four Andepts from Hawaii and implications for their classificationGeoderma, 1988