High temperature rims around chondrules in primitive chondrites: evidence for fluctuating conditions in the solar nebula
- 31 July 1991
- journal article
- Published by Elsevier BV in Earth and Planetary Science Letters
- Vol. 105 (1-3), 65-80
- https://doi.org/10.1016/0012-821x(91)90121-w
Abstract
No abstract availableKeywords
This publication has 18 references indexed in Scilit:
- The origin and history of the metal and sulfide components of chondrulesGeochimica et Cosmochimica Acta, 1985
- Cathodoluminescence zoning and minor elements in forsterites from the Murchison (C2) and Allende (C3V) carbonaceous chondritesNature, 1985
- On the formation of meteoritic chondrules by aerodynamic drag heating in the solar nebulaEarth and Planetary Science Letters, 1984
- Coarse-grained chondrule rims in type 3 chondritesGeochimica et Cosmochimica Acta, 1984
- Ca-Fe-Mg olivines: phase relations and a solution modelBeiträge zur Mineralogie und Petrographie, 1984
- Relict grains in chondrulesNature, 1981
- Evidence for secondary origin of chondrulesNature, 1981
- Chondrules in H3 chondrites: textures, compositions and originsGeochimica et Cosmochimica Acta, 1981
- RELATIVE ABUNDANCES OF CHONDRULE PRIMARY TEXTURAL TYPES IN ORDINARY CHONDRITES AND THEIR BEARING ON CONDITIONS OF CHONDRULE FORMATIONMeteoritics, 1981
- Chemical and petrographic constraints on the origin of chondrules and inclusions in carbonaceous chondritesGeochimica et Cosmochimica Acta, 1977