All Stories

  1. Clustering characteristics of gas-extraction induced seismicity in the Groningen gas field
  2. Depletion‐Induced Seismicity at the Groningen Gas Field: Coulomb Rate‐and‐State Models Including Differential Compaction Effect
  3. Traffic Light Systems: To What Extent Can Induced Seismicity Be Controlled?
  4. Categorizing seismic risk for the onshore gas fields in the Netherlands
  5. The effect of imposed production measures on gas extraction induced seismic risk
  6. From checking deterministic predictions to probabilities, scenarios and control loops for regulatory supervision
  7. Production induced subsidence and seismicity in the Groningen gas field – can it be managed?
  8. A guideline for assessing seismic risk induced by gas extraction in the Netherlands
  9. The effective subsidence capacity concept: How to assure that subsidence in the Wadden Sea remains within defined limits?
  10. Inversion of surface subsidence data to quantify reservoir compartmentalization: A field study
  11. Seismic Risk Analysis of Small Earthquakes Induced by Hydrocarbon Production in The Netherlands
  12. Inversion of Surface Subsidence Data to Quantify Reservoir Compartmentalization: A Field Study
  13. Subsidence in the Netherlands – Measuring, Matching, Monitoring, Modelling
  14. Unraveling shallow causes of subsidence
  15. Detecting Remaining Gas Reserves Based on Coupled Modelling of Subsidence and Reservoir Depletion Processes
  16. Disentangling Shallow and Deep Processes Causing Surface Movement
  17. Unraveling reservoir compaction parameters through the inversion of surface subsidence observations
  18. Time-dependent Inversion of Surface Subsidence due to Dynamic Reservoir Compaction
  19. Kinematics of the southwestern U.S. deformation zone inferred from GPS motion data
  20. A joint analysis of GPS motions and InSAR to infer the coseismic surface deformation of the Izmit, Turkey earthquake
  21. Surface deformation and tectonic setting of Taiwan inferred from a GPS velocity field
  22. The resolving power of coseismic surface displacement data for fault slip distribution at depth
  23. Duration of deep earthquakes determined by stacking of Global Seismograph Network seismograms