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Mass transfers and volume changes related to pressure solution–fracturing interactions in carbonate rocks: Example of the Oligocene deformation of the Coniacian chalk from the Omey area (Paris Basin, France)

✍ Scribed by J. Richard


Book ID
113756848
Publisher
Elsevier Science
Year
2008
Tongue
English
Weight
988 KB
Volume
30
Category
Article
ISSN
0191-8141

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