Re-Os Isotope Evidence for a Mid-Archaean Age of Diamondiferous Eclogite Xenoliths from the Udachnaya Kimberlite, Siberia: Constraints on Eclogite Petrogenesis. and Archaean Tectonics

D. G. Pearson, S. B. Shirey, N. V. Sobolev, G. A. Snyder and L. A. Taylor
Department of Earth Sciences, The Open University, Milton Keynes, MK7 6AA, UK
Department of Terrestrial Magnetism, 5241 Broad Branch Rd, N.W. Washington, D.C. 20015, USA
Institute of Mineralogy and Petrography, Siberian Branch, Russian Academy of Sciences, Novosibirsk, Russia
Department of Geological Sciences, University of Tennessee, Knoxville, TN 37996, USA

Mineralogical Magazine; August–September 1994 v. 58A; no. 2; p. 705-706; DOI: 10.1180/minmag.1994.58A.2.105
© 1994, The Mineralogical Society
Mineralogical Society (www.minersoc.org)