Seismik s.r.o. - Passive Seismic Services

Seismik s.r.o. - Passive Seismic Services

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        Seismik s.r.o.

        A privately held company established in 2010 in Prague, Czech Republic.  Providing seismic services for the oil and gas industry with an orientation on passive seismic.

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        08 February 2021
        New peer reviewed publication

        Seismik is proud to announce a new peer reviewed publication result from collaboration with the CPG of KFUPM, FDammam, Saudi Arabia. Our latest publication is on 'Microseismic Location Error Due to Eikonal Traveltime Calculation' and a free access pdf version can be downloaded at https://www.mdpi.com/2076-3417/11/3/982

         

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  • StressInversion

StressInversion ‑ geomechanical analysis

StressInversion is a proprietary effective, autonomous tool that specifies the stress state that accounts the best for a set of microearthquake focal mechanisms.

The orientations of the principal stress axes σ1, σ2 and σ3 (σ1 > σ2 > σ3) are determined from passive seismic datasets, adding a new value to the existing microseismic data. Using the orientation of the stresses, one can optimally place wellbores optimizing the recovery from a reservoir.

StressInversion recovers four parameters of the stress tensor: three angles defining the directions of the three principal stresses, σ1, σ2 and σ3, and the ratio between their differences, Φ = (σ2 - σ3) / (σ1 - σ3). StressInversion calculates the effective stress corresponding to a homogeneous tectonic stress in the source region. The uncertainties of the retrieved stress directions are calculated by the jack-knife method.

       

 

Left picture: Variability of the input source mechanisms of events recorded during the Soultz injection experiment in 2003. Stacked principal axes: T-axes - triangle apex up, P-axes - triangle apex right. Right picture: The results of StressInversion. Stress is inverted using the 45 focal mechanisms from input. The optimum position of the directions of the principal stresses σ1, σ2 and σ3 are marked by darker colour symbols. Clusters of same coloured symbols denote the confidence zones of maximum σ1 (red), medium σ2 (grey) and minimum σ3 (blue) stress axes derived from the jack-knife uncertainty test.

 

REFERENCES

  • Staněk F., Jechumtálová Z., Eisner L. (2015), Reservoir stress from microseismic source mechanisms, The Leading Edge, 34(8), 890–893, 895
Seismik s.r.o. - Passive Seismic Services

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