Microseismic monitoring and data from distributed acoustic sensing (DAS) can yield two independent measurements of the strain response to hydraulic stimulation of geologic formations. Microseismic monitoring provides a map of where, when and how the rock has catastrophically failed. DAS measurements from an optical fiber cable embedded in a horizontal well, adjacent to the stimulated well, can determine the relative strain response of the geologic formation that is in contact with the well bore. The strain response is not limited to rock failure and can respond to both dynamic and static deformation. However, DAS data are limited to the line defined by the spatial coordinates of the optical fiber cable and, in this configuration, cannot give a three-dimensional view of the strain response. By utilizing both DAS and microseismic data simultaneously and viewing both datasets in the same coordinate system, a more complete understanding of the rock response to hydraulic stimulation can be obtained.
Presentation Date: Wednesday, September 27, 2017
Start Time: 3:05 PM
Presentation Type: ORAL
Number of Pages
Boone,K., andA.Ridge,2016,Cross-well Communication Report OFS-16-0066:OptaSense Ltd.
Cooke,M. L., andC. A.Underwood,2001,Fracture termination and step-over at bedding interfaces due to frictional slip and interface opening:Journal of Structural Geology,23,223–238,10.1016/S0191-8141(00)00092-4.
Zobak,M. D.,2010;Reservoir Geomechanics:Cambridge University Press.
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