--> The Use of Passive Seismic Monitoring for the Exploration and Production of Hydrocarbon Reservoirs
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The Use of Passive Previous HitSeismicNext Hit Previous HitMonitoringNext Hit for the Exploration and Production of Hydrocarbon Reservoirs

Peter M. Duncan, James Lakings, and Christopher Neale. MicroSeismic, Inc, 800 Tully Rd, Suite 175, Houston, TX 77079, phone: 7137254806, [email protected]

The use of passive Previous HitseismicNext Hit energy to help understand the static and dynamic nature of the subsurface is rapidly gaining industry interest. These naturally occurring sources can provide a wealth of information regarding larger scale structural features, as well as Previous HitreservoirNext Hit scale production or injection induced changes in fluid and rock properties.

Two applications are being progressed that exploit passive Previous HitseismicNext Hit on differing scales. Transmission Tomography utilizes local micro-earthquakes as Previous HitseismicNext Hit source to create three-dimensional P and S wave velocity volumes, from which structure, faulting and lithology can be inferred. The environmentally benign acquisition methods make Transmission Tomography ideally suited for many exploration applications in the Rocky Mountains due to the negligible permitting requirements and low overall cost.

Previous HitMonitoringNext Hit the release of micro-Previous HitseismicNext Hit energy associated with Previous HitreservoirNext Hit level production activities is becoming a well established technique for understanding several dynamic Previous HitreservoirNext Hit processes. Two different methods are being commercially progressed, downhole and surface Previous HitmonitoringNext Hit. Downhole observation utilizes a linear array of geophones placed in a wellbore to detect and locate the hypo-centers of discrete micro-Previous HitseismicNext Hit events. Surface Previous HitmonitoringNext Hit ‘beam-steers' the output from a relatively dense surface array to identify the location of both continuous and transient acoustic sources without requiring the detection of discrete events. Both methods allow the operator to relate micro-Previous HitseismicNext Hit events to the progression of dynamic Previous HitreservoirNext Hit processes such as hydraulically stimulated fracture growth, injected fluid movement, Previous HitreservoirTop compaction, reactivated fault movement and compartmentalization.