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This document compares traditional core compaction correction methods with an iterative procedure aimed at improving the accuracy of effective stress calculations in clastic reservoirs. The iterative method utilizes a modest data set to derive a mean effective stress based on the Biot alpha parameter, leading to more reliable corrections for petrophysical core data. The authors emphasize the importance of understanding the stress regime in situ to enhance the quality assurance in geoscience applications.
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- used5940
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- EN