Compaction Phases and Pore Collapse in Lower Cretaceous Chalk: Insight from Biot’s Coefficient
Author:
Funder
Danish Offshore Technology Centre
Publisher
Springer Science and Business Media LLC
Link
https://link.springer.com/content/pdf/10.1007/s00603-024-03963-x.pdf
Reference67 articles.
1. Abdulraheem A, Roegiers JC, Zaman M (1992) Mechanisms of pore collapse in weak porous rocks. In: The 33rd U.S. Symposium on Rock Mechanics (USRMS) June 3–5, Santa Fe, New Mexico
2. Alam MM, Borre MK, Fabricius IL, Hedegaard K, Røgen B, Hossain Z, Krogsbøll AS (2010) Biot’s coefficient as an indicator of strength and porosity reduction: calcareous sediments from Kerguelen Plateau. J Petrol Sci Eng 70:282–297. https://doi.org/10.1016/j.petrol.2009.11.021
3. Alam MM, Fabricius IL, Christensen HF (2012) Static and dynamic effective stress coefficient of chalk. Geophysics 77:L1–L11. https://doi.org/10.1190/geo2010-0414.1
4. Amour F, Christensen HF, Hajiabadi MR, Nick HM (2021) Effects of porosity and water saturation on the yield surface of upper cretaceous reservoir chalks from the Danish North Sea. J Geophys Res Solid Earth 126:e2020JB020608. https://doi.org/10.1029/2020JB020608
5. Andreassen KA, Fabricius IL (2010) Biot critical frequency applied to description of failure and yield of highly porous chalk with different pore fluids. Geophysics 75:E205–E213. https://doi.org/10.1190/1.3504188
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