Origin of Granulite Terranes and the Formation of the Lowermost Continental Crust
Author:
Affiliation:
1. U.S. Geological Survey, Mail Stop 910, 345 Middlefield Road, Menlo Park, CA 94025.
2. Department of Earth and Space Sciences, State University of New York, Stony Brook, NY 11794.
Publisher
American Association for the Advancement of Science (AAAS)
Subject
Multidisciplinary
Reference38 articles.
1. BERGER, G.W., GEOTHERMOMETRY FROM AR-40-AR-39 DATING EXPERIMENTS, GEOCHIMICA ET COSMOCHIMICA ACTA 45: 795 (1981).
2. BOHLEN, S.R., EXPERIMENTAL INVESTIGATIONS AND GEOLOGICAL APPLICATIONS OF EQUILIBRIA IN THE SYSTEM FEO-TIO2-AL2O3-SIO2-H2O, AMERICAN MINERALOGIST 68: 1049 (1983).
3. BOHLEN, S.R., EXPERIMENTAL INVESTIGATION AND APPLICATION OF GARNET GRANULITE EQUILIBRIA, CONTRIBUTIONS TO MINERALOGY AND PETROLOGY 83: 52 (1983).
4. BOHLEN, S.R., PRESSURE-TEMPERATURE-TIME PATHS AND A TECTONIC MODEL FOR THE EVOLUTION OF GRANULITES, JOURNAL OF GEOLOGY 95: 617 (1987).
5. BOHLEN, S.R., A BAROMETER FOR GARNET AMPHIBOLITES AND GARNET GRANULITES, JOURNAL OF PETROLOGY 27: 1025 (1986).
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