Joint location and source mechanism inversion of microseismic events: benchmarking on seismicity induced by hydraulic fracturing
Identifikátory výsledku
Kód výsledku v IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F67985891%3A_____%2F14%3A00434520" target="_blank" >RIV/67985891:_____/14:00434520 - isvavai.cz</a>
Výsledek na webu
<a href="http://dx.doi.org/10.1093/gji/ggu126" target="_blank" >http://dx.doi.org/10.1093/gji/ggu126</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.1093/gji/ggu126" target="_blank" >10.1093/gji/ggu126</a>
Alternativní jazyky
Jazyk výsledku
angličtina
Název v původním jazyce
Joint location and source mechanism inversion of microseismic events: benchmarking on seismicity induced by hydraulic fracturing
Popis výsledku v původním jazyce
Seismic monitoring can greatly benefit from imaging events with a low signal-to-noise ratio (SNR) as the number of the events with a low signal grows exponentially. One way to detect weaker events is improvement of a SNR by migration-type stacking of waveforms from multiple stations. We have developed a new method of location of seismic events that involves stacking of seismic phases and amplitudes along diffraction traveltime curves to suppress noise and detect seismic events with a SNR lower than thaton individual receivers. The stacking includes polarity correction based on a simultaneous seismic moment tensor inversion and detection algorithm on the stack function. We applied this method to locate microseismicity induced by hydraulic fracturing. First we calibrated the velocity model by locating perforation shots at known locations. Then we processed 3 d of data from microseismic monitoring of shale stimulation and benchmarked migration-type locations of the largest events that we
Název v anglickém jazyce
Joint location and source mechanism inversion of microseismic events: benchmarking on seismicity induced by hydraulic fracturing
Popis výsledku anglicky
Seismic monitoring can greatly benefit from imaging events with a low signal-to-noise ratio (SNR) as the number of the events with a low signal grows exponentially. One way to detect weaker events is improvement of a SNR by migration-type stacking of waveforms from multiple stations. We have developed a new method of location of seismic events that involves stacking of seismic phases and amplitudes along diffraction traveltime curves to suppress noise and detect seismic events with a SNR lower than thaton individual receivers. The stacking includes polarity correction based on a simultaneous seismic moment tensor inversion and detection algorithm on the stack function. We applied this method to locate microseismicity induced by hydraulic fracturing. First we calibrated the velocity model by locating perforation shots at known locations. Then we processed 3 d of data from microseismic monitoring of shale stimulation and benchmarked migration-type locations of the largest events that we
Klasifikace
Druh
J<sub>x</sub> - Nezařazeno - Článek v odborném periodiku (Jimp, Jsc a Jost)
CEP obor
DB - Geologie a mineralogie
OECD FORD obor
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Návaznosti výsledku
Projekt
<a href="/cs/project/GAP210%2F12%2F2451" target="_blank" >GAP210/12/2451: Seismicita v důsledku injektáže kapalin</a><br>
Návaznosti
I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace
Ostatní
Rok uplatnění
2014
Kód důvěrnosti údajů
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Údaje specifické pro druh výsledku
Název periodika
Geophysical Journal International
ISSN
0956-540X
e-ISSN
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Svazek periodika
198
Číslo periodika v rámci svazku
1
Stát vydavatele periodika
GB - Spojené království Velké Británie a Severního Irska
Počet stran výsledku
10
Strana od-do
249-258
Kód UT WoS článku
000339717200018
EID výsledku v databázi Scopus
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