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...
Main Authors: | , |
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Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
1984
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Subjects: | |
Online Access: | http://hdl.handle.net/2013/ULB-DIPOT:oai:dipot.ulb.ac.be:2013/202942 |
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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