Siderophile element constraints on the formation of metal in the metal-rich chondrites Bencubbin, Weatherford, and Gujba
Authors:
- Andrew J. CampbellACAndrew J. Campbell
- Munir HumayunMHMunir Humayun
- Michael K. WeisbergMWMichael K. Weisberg
- 1 February 2002
- journal article
- Published by Elsevier in Geochimica et Cosmochimica Acta
- Vol. 66 (4) , 647-660
Abstract
No abstract availableKeywords
Funding Information
- National Aeronautics and Space Administration (NAG 5-9800, NAG 5-4745)
This publication has 45 references indexed in Scilit:
- The Leonard Award Address: Presented 2000 August 30, Chicago, Illinois, USA: Early solar system events and timescalesMeteoritics & Planetary Science, 2001
- A New Astrophysical Setting for Chondrule FormationScience, 2001
- Origin of zoned metal grains in the QUE94411 chondriteGeochimica et Cosmochimica Acta, 2001
- The condensation origin of zoned metal grains in Queen Alexandra Range 94411: Implications for the formation of the Bencubbin‐like chondritesMeteoritics & Planetary Science, 2001
- Hf–W internal isochrons for ordinary chondrites and the initial 182Hf/180Hf of the solar systemChemical Geology, 2000
- Primitive FeNi metal grains in CH carbonaceous chondrites formed by condensation from a gas of solar compositionJournal of Geophysical Research, 1999
- High-Pressure and High-Temperature Experiments on Core-Mantle Segregation in the Accreting EarthScience, 1994
- A Striking Nitrogen Isotope Anomaly in the Bencubbin and Weatherford MeteoritesScience, 1985
- A metal particle from a Ca,Al-rich inclusion from the meteorite Allende, and the condensation of refractory siderophile elementsEarth and Planetary Science Letters, 1976
- Evidence for the formation of an iron meteorite at 3.8 × 109 yearsEarth and Planetary Science Letters, 1967