Origin of the Sudbury Complex by Meteoritic Impact: Neodymium Isotopic Evidence
Author:
Affiliation:
1. Department of Geological Sciences, University of Rochester, Rochester, New York 14627
2. U.S. Geological Survey, Denver, Colorado 80225
Publisher
American Association for the Advancement of Science (AAAS)
Subject
Multidisciplinary
Reference25 articles.
1. ALLEGRE, C.J., THE GROWTH OF THE CONTINENT THROUGH GEOLOGICAL TIME STUDIED BY ND ISOTOPE ANALYSIS OF SHALES, EARTH AND PLANETARY SCIENCE LETTERS 67: 19 (1984).
2. ALLEGRE, C.J., ND-SR ISOTOPIC RELATIONSHIP IN GRANITOID ROCKS AND CONTINENTAL-CRUST DEVELOPMENT - A CHEMICAL APPROACH TO OROGENESIS, NATURE 286: 335 (1980).
3. DePaolo, D. J., Geophysical Research Letters 3: 249 (1976).
4. DIETZ, R.S., SUDBURY STRUCTURE AS AN ASTROBLEME, JOURNAL OF GEOLOGY 72: 412 (1964).
5. DING, T.P., OXYGEN ISOTOPIC AND CHEMICAL-COMPOSITIONS OF ROCKS OF THE SUDBURY BASIN, ONTARIO, CANADIAN JOURNAL OF EARTH SCIENCES 21: 305 (1984).
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