78th EAGE Conference and Exhibition 2016 2016
DOI: 10.3997/2214-4609.201600720
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Downhole Microseismic Data Processing - Consistency of Locations, Source Mechanisms and Stress State

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“…The second tested array configuration is a dual borehole monitoring array with 11 receivers in each well, similar to Jechumtálová et al (2016). The vertical wells are drilled 500 m from each other and the receivers are located at depths ranging from 1800 to 1920 m. In this case, we use as input both P-and Swave amplitudes, because they are commonly used for borehole receivers.…”
Section: Stability For Three Types Of Microseismic Monitoring Arraysmentioning
confidence: 99%
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“…The second tested array configuration is a dual borehole monitoring array with 11 receivers in each well, similar to Jechumtálová et al (2016). The vertical wells are drilled 500 m from each other and the receivers are located at depths ranging from 1800 to 1920 m. In this case, we use as input both P-and Swave amplitudes, because they are commonly used for borehole receivers.…”
Section: Stability For Three Types Of Microseismic Monitoring Arraysmentioning
confidence: 99%
“…This problem could be practically solved using arrays in slightly deviated wells (Vera Rodrigues et al, 2011) which improves focal sphere coverage in the problematic direction, or by using a constrained inversion (Jechumtálová and Šílený, 2005). Luckily, events located by Jechumtálová et al (2016) seems to be in a zone (cut by cross-sections in Fig. 2) where we get relatively components of M .…”
Section: Stability For Three Types Of Microseismic Monitoring Arraysmentioning
confidence: 99%
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