Depletion‐Induced Seismicity at the Groningen Gas Field: Coulomb Rate‐and‐State Models Including Differential Compaction Effect

Author:

Candela Thibault1ORCID,Osinga Sander1,Ampuero Jean‐Paul2ORCID,Wassing Brecht1,Pluymaekers Maarten1,Fokker Peter A.13ORCID,Wees Jan‐Diederik13ORCID,Waal Hans A.4ORCID,Muntendam‐Bos Annemarie G.4ORCID

Affiliation:

1. TNO, Geological Survey of the Netherlands Utrecht The Netherlands

2. Université Côte d'Azur, IRD, CNRS, Observatoire de la Côte d'Azur, Géoazur Sophia Antipolis France

3. Department of GeosciencesUtrecht University Utrecht The Netherlands

4. State Supervision of Mines The Hague The Netherlands

Publisher

American Geophysical Union (AGU)

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics

Reference76 articles.

1. Response of rate-and-state seismogenic faults to harmonic shear-stress perturbations

2. Scale-free networks of earthquakes and aftershocks

3. A hierarchical O(N log N) force-calculation algorithm

4. Why earthquakes correlate weakly with the solid Earth tides: Effects of periodic stress on the rate and probability of earthquake occurrence

5. Bierman S. Kraaijeveld F. &Bourne S.(2015).Regularised direct inversion to compaction in the Groningen reservoir using measurements from optical leveling campaigns. Technical Report. Shell Global Solutions International. Amsterdam.

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