Theoretical assessment of the full-moment-tensor resolvability for receiver arrays used in microseismic monitoring
Identifikátory výsledku
Kód výsledku v IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F67985891%3A_____%2F17%3A00479255" target="_blank" >RIV/67985891:_____/17:00479255 - isvavai.cz</a>
Nalezeny alternativní kódy
RIV/00216208:11320/17:10367222
Výsledek na webu
<a href="http://dx.doi.org/10.13168/AGG.2017.0006" target="_blank" >http://dx.doi.org/10.13168/AGG.2017.0006</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.13168/AGG.2017.0006" target="_blank" >10.13168/AGG.2017.0006</a>
Alternativní jazyky
Jazyk výsledku
angličtina
Název v původním jazyce
Theoretical assessment of the full-moment-tensor resolvability for receiver arrays used in microseismic monitoring
Popis výsledku v původním jazyce
An inversion of full moment tensors representing source mechanisms is becoming routinely used when interpreting microseismic monitoring. However, a stability of such inversion varies significantly for different receiver arrays. Unlike stability of location, which is hard to assess, the stability of inverted full moment tensor can be measured by a condition number. We tested three types of receiver arrays (dense surface array, dual borehole array and multi-borehole array) used in the microseismic monitoring and computed the theoretical stability of full moment tensor inversion from P-or P-and S-wave amplitudes at areas of interest. We analyzed a 3D distributions of the condition numbers and show that with surface and multi-borehole arrays of receivers we are capable of inverting stable source mechanisms for the events located at depths comparable to the maximum offset of receivers, but shallower events and the events at the depths of the borehole arrays are poorly constrained. This study provides a guidance for a quick prediction of source mechanism inversion quality. Computing condition numbers does not require any information about the data, it measures a theoretical quality of the moment tensor inversion. The computed condition numbers represent inversion for ideal dataset with the selected geometry.
Název v anglickém jazyce
Theoretical assessment of the full-moment-tensor resolvability for receiver arrays used in microseismic monitoring
Popis výsledku anglicky
An inversion of full moment tensors representing source mechanisms is becoming routinely used when interpreting microseismic monitoring. However, a stability of such inversion varies significantly for different receiver arrays. Unlike stability of location, which is hard to assess, the stability of inverted full moment tensor can be measured by a condition number. We tested three types of receiver arrays (dense surface array, dual borehole array and multi-borehole array) used in the microseismic monitoring and computed the theoretical stability of full moment tensor inversion from P-or P-and S-wave amplitudes at areas of interest. We analyzed a 3D distributions of the condition numbers and show that with surface and multi-borehole arrays of receivers we are capable of inverting stable source mechanisms for the events located at depths comparable to the maximum offset of receivers, but shallower events and the events at the depths of the borehole arrays are poorly constrained. This study provides a guidance for a quick prediction of source mechanism inversion quality. Computing condition numbers does not require any information about the data, it measures a theoretical quality of the moment tensor inversion. The computed condition numbers represent inversion for ideal dataset with the selected geometry.
Klasifikace
Druh
J<sub>imp</sub> - Článek v periodiku v databázi Web of Science
CEP obor
—
OECD FORD obor
10700 - Other natural sciences
Návaznosti výsledku
Projekt
—
Návaznosti
I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace
Ostatní
Rok uplatnění
2017
Kód důvěrnosti údajů
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Údaje specifické pro druh výsledku
Název periodika
Acta geodynamica et geomaterialia
ISSN
1214-9705
e-ISSN
—
Svazek periodika
14
Číslo periodika v rámci svazku
2
Stát vydavatele periodika
CZ - Česká republika
Počet stran výsledku
6
Strana od-do
235-240
Kód UT WoS článku
000405139400009
EID výsledku v databázi Scopus
2-s2.0-85020435938