The Carlisle Lakes-type chondrites: A new grouplet with high Δ17O and evidence for nebular oxidation
- 1 September 1991
- journal article
- Published by Elsevier in Geochimica et Cosmochimica Acta
- Vol. 55 (9) , 2657-2669
- https://doi.org/10.1016/0016-7037(91)90380-n
Abstract
No abstract availableKeywords
This publication has 22 references indexed in Scilit:
- Petrology and mineralogy of Type II, FeO-rich chondrules in Semarkona (LL3.0): Origin by closed-system fractional crystallization, with evidence for supercoolingGeochimica et Cosmochimica Acta, 1990
- FeO‐rich rims and veins in Allende forsterite: Evidence for high temperature condensation at oxidizing conditionsMeteoritics, 1990
- Size‐frequency distributions of chondrules in CO3 chondritesMeteoritics, 1989
- Chondrules in the Murray CM2 meteorite and compositional differences between CM-CO and ordinary chondrite chondrulesGeochimica et Cosmochimica Acta, 1986
- Evidence for oxidizing conditions in the solar nebula from Mo and W depletions in refractory inclusions in carbonaceous chondritesEarth and Planetary Science Letters, 1985
- The oxygen isotope record in Murchison and other carbonaceous chondritesEarth and Planetary Science Letters, 1984
- Oxygen isotopes in eucrites, shergottites, nakhlites, and chassignitesEarth and Planetary Science Letters, 1983
- Cristobalite-pyroxene in an L6 chondrite: implications for metamorphismEarth and Planetary Science Letters, 1981
- The mineralogy and petrology of chondritic meteoritesEarth-Science Reviews, 1969
- A chemical-petrologic classification for the chondritic meteoritesGeochimica et Cosmochimica Acta, 1967