Page 244 - Fundamentals of Gas Shale Reservoirs
P. 244

224   PASSIVE SEISMIC METHODS FOR UNCONVENTIONAL RESOURCE DEVELOPMENT


                                            REC_CNTR (receiver index counter)
                                            1        59      114      164     224      274      332      384
                                       18400                                                                18400
                                       18600                                                                18600
                                       18800                                                                18800
                            3          19000                                                                19000
                   2                   19200                                                                19200
                                      Time (milliseconds)  19600                                            19600 Time (milliseconds)
                                       19400
                                                                                                            19400
                      1                19800                                                                19800
                                       20000
                                                                                                            20200
                                       20200                                                                20000
                                       20400                                                                20400
                                       20600                                                                20600
                                       20800                                                                20800
                                       21000                                                                21000


                                          REC_CNTR (receiver index counter)
                                          1134          658           62            667          430
                                      18400                                                                 18400
              1      2          3     18600                                                                 18600
                                      18800                                                                 18800
                                      19000                                                                 19000
                                      19200                                                                 19200
                                      Time (milliseconds)  19600                                            19600 Time (milliseconds)
                                      19400
                                                                                                            19400
                                      19800
                                                                                                            19800
                                      20000
                                      20200                                                                 20000
                                                                                                            20200
                                      20400                                                                 20400
                                      20600                                                                 20600
                                      20800                                                                 20800
                                      21000                                                                 21000
            FIGURE 10.12  Focusing of the trace data using travel times from ray tracing. The microearthquake (MEQ) occurs in a specific voxel of
            the volume. The traces for the MEQ are flattened when the travel times for the voxel in which it occurred are used to time‐shift the traces.
            After flattening, the traces are ready for the imaging step.


            total energy than the relatively rare, large earthquakes. SET   may be caught in addition to fish. Even with effective
            captures  all  seismic  activity  above  the  noise floor, which   removal of coherent noise at the trace‐processing stage,
            consists mainly of instrumental sensitivity and the ability of   random noise will produce some low‐level false structure
            the rock column to transmit signal.                  because random processes exhibit clustering and anticluster­
              MEQs alone represent only a small fraction of the total   ing. Although low‐level signal may be part of this structure,
            seismic energy produced by hydraulic fracture treatments.   the low end of the cumulative activity distribution must be
            SET also captures energy from other types of seismic phe­  clipped from stacked volumes to further minimize the effect
            nomena. These types of phenomena include LPLD activity,   of noise.
            long‐duration P‐wave emissions (EDS), and perhaps other,   10.5.2.2  Parameters and Data Required for Set  The
            as‐yet‐undiscovered types of seismic emissions. LPLD and   quality of the results of the SET method depends on several
            long‐duration P‐wave emissions do not have distinct first   factors:
            arrivals and may persist from many seconds to tens of min­  1.  Velocity model and statics
            utes or even hours. For these reasons, such phenomena are
            ignored by conventional seismological methods. If we use   2.  Design of geophone grid layout
            fishing as an analogy, SET is like fishing with a net (you   3.  Noise in the area of the grid, especially coherent
            catch everything), whereas conventional earthquake seis­    surface wave noise
            mology is like fishing with a lure (you only catch big fish of   4.  Lithology‐dependent variation of the amount of signal
            a few particular species). The downside is that trash (noise)   generated in the rocks being fractured
   239   240   241   242   243   244   245   246   247   248   249