Rhenium-Osmium Isotope Constraints on the Age of Iron Meteorites
Author:
Affiliation:
1. U.S. Geological Survey, Mailstop 981, Reston, VA 22092
2. Isotope Geochemistry Laboratory, Department of Geology, University of Maryland, College Park, MD 20742
3. U.S. Geological Survey, Mailstop 990, Reston, VA 22092
Publisher
American Association for the Advancement of Science (AAAS)
Subject
Multidisciplinary
Reference24 articles.
1. BURNETT, D.S., EVIDENCE FOR FORMATION OF AN IRON METEORITE AT 3.8 BY 109 YEARS, EARTH AND PLANETARY SCIENCE LETTERS 2: 137 (1967).
2. BURNETT, D.S., 7RB-87SR AGES OF SILICATE INCLUSIONS IN IRON METEORITES, EARTH AND PLANETARY SCIENCE LETTERS 2: 397 (1967).
3. CHEN, J.H., THE ISOTOPIC COMPOSITION OF URANIUM AND LEAD IN ALLENDE INCLUSIONS AND METEORITIC PHOSPHATES, EARTH AND PLANETARY SCIENCE LETTERS 52: 1 (1981).
4. CHEN, J.H., THE ISOTOPIC COMPOSITION OF SILVER AND LEAD IN 2 IRON-METEORITES - CAPE-YORK AND GRANT, GEOCHIMICA ET COSMOCHIMICA ACTA 47: 1725 (1983).
5. CHEN, J.H., THE ISOTOPIC COMPOSITION OF AG IN METEORITES AND THE PRESENCE OF PD-107 IN PROTOPLANETS, GEOCHIMICA ET COSMOCHIMICA ACTA 54: 1729 (1990).
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