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Wed, 20 May 1998 12:08:05 -0800 |
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Dear Isogeochemists,
Can anybody tell if pressure-solution along cleavage in a limestone
or a marble may shift the carbonate C- and O-isotope compositions, not only
because of the infiltration of an exotic fluid, but especially because of a
dissolution mechanism similar to decarbonatation reactions (those often
modelled by a Rayleigh fractionation model) ?
Any personal statement or bibliographic reference is welcome.
Cheers,
Eric
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Eric Pili
Center for Isotope Geochemistry
University of California - Berkeley
Lawrence Berkeley National Laboratory - Earth Sciences Division
MS: 70A-3363 - 1 Cyclotron road , Berkeley, CA 94720, USA
Phone: 510-495-2443 (office) or 510-486-4975 (lab) - Fax: 510-486-5496
email : [log in to unmask]
web pages : http://www.ens-lyon.fr/~pili
Formerly and occasionally at :
Laboratoire de Sciences de la Terre - Ecole Normale Superieure de Lyon
46, Allee d'Italie - F 69364 Lyon Cedex 07 - France
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