Seismic interferometry applied to walkaway VSP data in the seismic monitoring of CO2 storage security - A synthetic study
Access Status
Authors
Date
2011Type
Metadata
Show full item recordCitation
Source Title
ISBN
School
Collection
Abstract
The CO2SINK project is the first EU onshore CO2 storage project and officially started in April 2004 at the Ketzin anticline near Berlin, Germany. One of the seismic methods that has been applied there is vertical seismic profiling (VSP). VSP data may allow faults to be detected that cannot be imaged with surface seismic data. These faults may be a security risk for CO2 storage. However, the imaging range of traditional VSP methods is limited, therefore, we decided to test the potential of seismic interferometry to redatum walkaway VSP (or moving source profiling, MSP) data sets to SWP (single well profile) data sets. The redatumed data sets may provide better image resolution because the redatumed geometry is closer to the target fault. We generated both acoustic and elastic walkaway VSP synthetic data sets based on the geological structure at Ketzin, and then applied seismic interferometry to redatum the data sets to SWP data sets to enhance the imaging of a fault.
Related items
Showing items related by title, author, creator and subject.
-
Feitz, A.; Pevzner, R.; Harris, Brett; Schaa, R.; Tertyshnikov, K.; Ziramov, S.; Gunning, M.; Ransley, T.; Lai, E.; Bailey, A.; Schacht, U.; Fomin, T.; Urosevic, M. (2017)The CO2CRC is undertaking a feasibility study for a planned controlled release and monitoring experiment at a shallow fault at the CO2CRC Otway Project site in 2018. Interpretation of pre-2016 seismic data could trace the ...
-
Ahmadi, O.; Juhlin, Christopher; Ask, M.; Lund, B. (2015)© 2015 Author(s). A new seismic reflection survey for imaging deeper levels of the end-glacial Pärvie fault system in northern Sweden was acquired in June 2014. The Pärvie fault system hosts the largest fault scarp so far ...
-
Abdi, A.; Heinonen, S.; Juhlin, Christopher; Karinen, T. (2015)Unloading of the ice during the last glacial period in northern Fennoscandia is believed to have generated major faulting. These faults, often referred to as post-glacial faults, typically have clear surface exposures, ...