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Microearthquake Studies at the Salton Sea Geothermal Field

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The objective of this project is to detect and locate microearthquakes to aid in the characterization of reservoir fracture networks. Accurate identification and mapping of the large numbers of microearthquakes induced in EGS is one technique that provides diagnostic information when determining the location, orientation and length of underground crack systems for use in reservoir development and management applications. Conventional earthquake location techniques often are employed to locate microearthquakes. However, these techniques require labor-intensive picking of individual seismic phase onsets across a network of sensors. For this project we adapt the Matched Field Processing (MFP) technique to the elastic propagation problem in geothermal reservoirs to identify more and smaller events than traditional methods alone.

Citation Formats

Lawrence Livermore National Laboratory. (2013). Microearthquake Studies at the Salton Sea Geothermal Field [data set]. Retrieved from https://dx.doi.org/10.15121/1148809.
Export Citation to RIS
Templeton, Dennise. Microearthquake Studies at the Salton Sea Geothermal Field. United States: N.p., 01 Oct, 2013. Web. doi: 10.15121/1148809.
Templeton, Dennise. Microearthquake Studies at the Salton Sea Geothermal Field. United States. https://dx.doi.org/10.15121/1148809
Templeton, Dennise. 2013. "Microearthquake Studies at the Salton Sea Geothermal Field". United States. https://dx.doi.org/10.15121/1148809. https://gdr.openei.org/submissions/250.
@div{oedi_3095, title = {Microearthquake Studies at the Salton Sea Geothermal Field}, author = {Templeton, Dennise.}, abstractNote = {The objective of this project is to detect and locate microearthquakes to aid in the characterization of reservoir fracture networks. Accurate identification and mapping of the large numbers of microearthquakes induced in EGS is one technique that provides diagnostic information when determining the location, orientation and length of underground crack systems for use in reservoir development and management applications. Conventional earthquake location techniques often are employed to locate microearthquakes. However, these techniques require labor-intensive picking of individual seismic phase onsets across a network of sensors. For this project we adapt the Matched Field Processing (MFP) technique to the elastic propagation problem in geothermal reservoirs to identify more and smaller events than traditional methods alone.}, doi = {10.15121/1148809}, url = {https://gdr.openei.org/submissions/250}, journal = {}, number = , volume = , place = {United States}, year = {2013}, month = {10}}
https://dx.doi.org/10.15121/1148809

Details

Data from Oct 1, 2013

Last updated May 26, 2017

Submitted Oct 1, 2013

Organization

Lawrence Livermore National Laboratory

Contact

Dennise Templeton

925.422.2021

Authors

Dennise Templeton

Lawrence Livermore National Laboratory

Research Areas

DOE Project Details

Project Lead Lauren Boyd

Project Number AID 19981

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