Oxygen Isotope Composition of Subglacially Precipitated Calcite: Possible Paleoclimatic Implications

Author:

Hanshaw Bruce B.1,Hallet Bernard2

Affiliation:

1. U.S. Geological Survey, National Center, Mail Stop 431, Reston, Virginia 22092

2. Department of Geology, Stanford University, Stanford, California 94305

Publisher

American Association for the Advancement of Science (AAAS)

Subject

Multidisciplinary

Reference27 articles.

1. BAUER, V.F., ZEITSCHRIFT FUR GLETSCHERKUNDE UND GLAZIALGEOLOGIE 4: 215 (1961).

2. BJAERKE, T, QUATERNARY STROMATOLITIC LIMESTONE OF SUB-GLACIAL ORIGIN FROM SCANDINAVIA, JOURNAL OF SEDIMENTARY PETROLOGY 47: 1321 (1977).

3. CLAYTON, R.N., ISOTOPE STUDIES OF DOLOMITE FORMATION UNDER SEDIMENTARY CONDITIONS, GEOCHIMICA ET COSMOCHIMICA ACTA 32: 415 (1968).

4. Glacier Oxygen-18 Content and Pleistocene Ocean Temperatures

5. EMILIANI, C, PLEISTOCENE TEMPERATURES, JOURNAL OF GEOLOGY 63: 538 (1955).

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