On the isotopic composition in dD and d18O of water and ice during freezing.

Results indicate that evolution takes place, in a dD-d18O diagram, along a straight line with a characteristic slope. This slope, different from that due to the precipitation effect gives a finger-print of the occurrence of a freezing or of a melting-refreezing process in the studied reservoir.-from...

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Bibliographic Details
Main Authors: Souchez, Roland, Jouzel, Jean
Format: Article in Journal/Newspaper
Language:English
Published: 1984
Subjects:
Géologie et minéralogie
Glaciologie
Journal of Glaciology
Online Access:http://hdl.handle.net/2013/ULB-DIPOT:oai:dipot.ulb.ac.be:2013/202942
Description
Summary:Results indicate that evolution takes place, in a dD-d18O diagram, along a straight line with a characteristic slope. This slope, different from that due to the precipitation effect gives a finger-print of the occurrence of a freezing or of a melting-refreezing process in the studied reservoir.-from Authors SCOPUS: NotDefined.j info:eu-repo/semantics/published

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