How hydrofractures become arrested

Terra Nova

Volumn 13, Issue 6, 2001, Pages 456-462

  Gudmundsson, Agust ^a   Brenner, Sonja L ^a  

^a UNIVERSITY OF BERGEN   (Norway)

Author keywords

[No Author keywords available]

Indexed keywords

BUOYANCY; CRUSTAL STRUCTURE; FLUID PRESSURE; FRACTURE; FRACTURE MECHANICS;

EID: 0035713187     PISSN: 09544879     EISSN: None     Source Type: Journal    
DOI: 10.1046/j.1365-3121.2001.00380.x     Document Type: Article

References (27)

1. Consequences of fluid lag in three-dimensional hydraulic fractures
2. Nearfield modifications of stress induced by dyke injection at shallow depth
3. Displacement and gravity-anomaly produced by a shallow vertical dyke in a cohesionless medium
4. On tensile cracks close to and across the interface between two welded elastic half-spaces
5. Numerical simulations of the propagation path and the arrest of fluid-filled fractures in the Earth
6. The tip region of a fluid-driven fracture in an elastic medium
7. Effect of tensile stress concentration around magma chambers on intrusion and extrusion frequencies
8. Emplacement of dikes, sills and crustal magma chambers at divergent plate boundaries
9. Dynamics of volcanic systems in Iceland
10. Injection and arrest of dykes: Implications for volcanic hazards
11. Fracture networks and fluid transport in active fault zones
12. Hydrofracturing stress measurements in the Iceland research drilling project drill hole at Reydarfjordur, Iceland
13. Role of fluids in faulting inferred from stress field signatures
14. Dykes, faults and palaeostresses in the Teno and Anaga massifs of Tenerife (Canary Islands)
15. Limits on strength and deformation properties of jointed basaltic rock masses
16. Containment of massive hydraulic fractures
17. Basics of hydraulic fracturing
18. Measurement of width and pressure in a propagating hydraulic fracture