Podrobnosti záznamu

Jméno
   Eisner, L.
Autor článku
   Automated P- and S-wave picking of microearthquakes recorded by a vertical array
   Back azimuth relocation of monitoring arrays
   Computation of additional components of the first-order ray approximation in isotropic media
   Computation of additional components of the first-order ray approximation in isotropic media
   Detection of repeated hydraulic fracturing (out-of-zone growth) by microseismic monitoring
   Determination of S-wave backazimuth from a linear array of borehole receivers
   Determination of S-wave slowness from a linear array of borehole receivers
   Determination of S-wave slowness from a linear array of borehole receivers
   Importance of borehole deviation surveys for monitoring of hydraulic fracturing treatments
   Microseismic signatures of hydraulic fracture growth in sediment formations: Observations and modeling
   Microseismic signatures of hydraulic fracture propagation in sedimentary formations
   Moment tensors of events induced in Cotton Valley gas field from waveform inversion
   New analytical techniques to help improve our understanding of hydraulically induced microseismicity and fracture propagation. SPE 110813
   Non-double-couple mechanisms of microearthquakes induced by hydraulic fracturing
   Non-double-couple mechanisms of microearthquakes induced by hydraulic fracturing
   Non-double-couple seismic events induced by hydraulic fracturing observed from a linear array of receivers
   Seismic source mechanism inversion from a linear array of receivers reveals non-double-couple seismic events induced by hydraulic fracturing in sedimentary formation
   Seismic wave modeling by the ray method with the first order additional terms
   Seismic wave modeling by the ray method with the first order additional terms