The cooling history of the Lewis Cliff 86010 angrite as inferred from kirschsteinite lamellae in olivine
- 1 September 1998
- journal article
- Published by Wiley in Meteoritics & Planetary Science
- Vol. 33 (5) , 977-983
- https://doi.org/10.1111/j.1945-5100.1998.tb01704.x
Abstract
No abstract availableKeywords
This publication has 17 references indexed in Scilit:
- Exsolution lamellae of kirschsteinite in magnesium-iron olivine from an angrite meteoriteAmerican Mineralogist: Journal of Earth and Planetary Materials, 1995
- Neodymium, strontium and chromium isotopic studies of the LEW86010 and Angra dos Reis meteorites and the chronology of the angrite parent bodyMeteoritics, 1994
- Age and isotopic relationships among the angrites Lewis Cliff 86010 and Angra dos ReisGeochimica et Cosmochimica Acta, 1992
- Rare earth elements in Angra dos Reis and Lewis Cliff 86010, two meteorites with similar but distinct magma evolutionsEarth and Planetary Science Letters, 1990
- Cations in olivine, Part 2: Diffusion in olivine xenocrysts, with applications to petrology and mineral physicsContributions to Mineralogy and Petrology, 1988
- Ca-Fe-Mg olivines: phase relations and a solution modelContributions to Mineralogy and Petrology, 1984
- Preface: The Angra dos Reis consortiumEarth and Planetary Science Letters, 1977
- Fe-Mg lattice diffusion in olivineJournal of Geophysical Research, 1973
- Xenon from the Angra dos Reis meteoriteGeochimica et Cosmochimica Acta, 1970
- Cooling rates of 27 iron and stony-iron meteoritesGeochimica et Cosmochimica Acta, 1967