2010
DOI: 10.1111/j.1365-246x.2010.04724.x
|View full text |Cite
|
Sign up to set email alerts
|

Abstract: S U M M A R YIn recent years, there has been an increase in the deployment of relatively dense arrays of seismic stations. The availability of spatially densely sampled global and regional seismic data has stimulated the adoption of industry-style imaging algorithms applied to converted-and scattered-wave energy from distant earthquakes, leading to relatively high-resolution images of the lower crust and upper mantle. We use seismic interferometry to extract reflection responses from the coda of transmitted en… Show more

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
3
1
1

Citation Types

0
62
0
2

Year Published

2011
2011
2016
2016

Publication Types

Select...
10

Relationship

3
7

Authors

Journals

citations
Cited by 74 publications
(64 citation statements)
references
References 35 publications
0
62
0
2
Order By: Relevance
“…This would mean that one might need to sum parts of the retrieved positive and negative times to obtain a more complete retrieved reflection (for different cases of summation see, e.g., Draganov et al, 2009;Ruigrok et al, 2010). The presence of many scatterers in the subsurface helps to prevent such a situation, because the scatterers serve as secondary sources that help to illuminate the receiver array from below from many directions.…”
Section: Description Of the Modeling Studiesmentioning
confidence: 99%
“…This would mean that one might need to sum parts of the retrieved positive and negative times to obtain a more complete retrieved reflection (for different cases of summation see, e.g., Draganov et al, 2009;Ruigrok et al, 2010). The presence of many scatterers in the subsurface helps to prevent such a situation, because the scatterers serve as secondary sources that help to illuminate the receiver array from below from many directions.…”
Section: Description Of the Modeling Studiesmentioning
confidence: 99%
“…The theory can be applied to natural earthquake records (Ruigrok et al, 2010) as well as exploration seismology, for example, in conjunction with the virtual source (VS) method (Bakulin and Calvert, 2006).…”
Section: Introductionmentioning
confidence: 99%
“…This technique has been applied to earthquake data in various ways, such as measuring shear-wave velocity [e.g., Snieder and ƞafak, 2006;Sawazaki et al, 2009] and estimating deep subsurface structure [e.g., Tonegawa et al, 2009;Ruigrok et al, 2010].…”
Section: Introductionmentioning
confidence: 99%