2005
DOI: 10.1016/j.wavemoti.2004.05.006
|View full text |Cite
|
Sign up to set email alerts
|

A review of shear-wave splitting in the compliant crack-critical anisotropic Earth

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
4
1

Citation Types

1
121
0

Year Published

2007
2007
2018
2018

Publication Types

Select...
10

Relationship

0
10

Authors

Journals

citations
Cited by 162 publications
(122 citation statements)
references
References 70 publications
1
121
0
Order By: Relevance
“…The key assumption for application of this approach to hydraulic fracture-induced microseismic data is that the tectonic stress in the subsurface is close to the critical stress needed for brittle failure (e.g., [13]). As such, increasing fluid pressure (i.e., injecting fluid) within the reservoir results in a transient increase of the reservoir pore-pressure and a decrease in effective stress.…”
Section: Pore-pressure Triggeringmentioning
confidence: 99%
“…The key assumption for application of this approach to hydraulic fracture-induced microseismic data is that the tectonic stress in the subsurface is close to the critical stress needed for brittle failure (e.g., [13]). As such, increasing fluid pressure (i.e., injecting fluid) within the reservoir results in a transient increase of the reservoir pore-pressure and a decrease in effective stress.…”
Section: Pore-pressure Triggeringmentioning
confidence: 99%
“…It has an extremely important role on the ultrasonic non-destructive measurement of stresses (Crecraft, 1967;Lu and Roy, 1996) and has wide application in the fields of geotechnical engineering, petroleum geophysics for the estimation of crustal stress (Crampin and Peacock, 2005;Tian and Wang, 2006;Winkler and McGowan, 2004).…”
Section: Introductionmentioning
confidence: 99%
“…SWS occurs during S wave propagation through an anisotropic medium as S waves are splitted into two components with perpendicular polarization directions and different propagation velocities (Crampin and Chastin, 2003;Crampin and Peacock, 2005). The two splitting parameters that can be measured through shear wave data processing defining the anisotropy are the polarization direction φ of the fast shear wave component and the time-delay dt between the two components.…”
Section: Introductionmentioning
confidence: 99%