1887

Abstract

Laboratory experiments with compacted specimens of brine saturated Kaolinite demonstrate effects similar to those seen in 4D seismics, when stress changes representative for those occurring in the overburden above a depleting reservoir are enforced. Incr

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/content/papers/10.3997/2214-4609.201400555
2009-06-08
2024-04-25
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201400555
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