Zobrazeno 1 - 10
of 39
pro vyhledávání: '"Raymon L. Brown"'
Publikováno v:
Geophysical Journal International. 178:1625-1648
SUMMARY The estimation of illite-rich shale anisotropy to account for the alignment of clays and gas- or brine-filled cracks is presented via mathematical modelling. Such estimation requires analysis to interpret the dominance of one effect over anot
Autor:
Raymon L. Brown
Publikováno v:
The Leading Edge. 28:420-425
When P- and S-waves travel through porous sandstone saturated with hydrocarbons, a bit of magic happens to make the velocities of these waves more frequency-dependent (dispersive) than when the formation is saturated with brine. This article explores
Publikováno v:
GEOPHYSICS. 70:C1-C5
A theoretical comparison is made of PP and PS angle–dependent reflection coefficients at the top of two fractured-reservoir models using exact, general, anisotropic reflection coefficients. The two vertical-fracture models are taken to have the sam
Publikováno v:
GEOPHYSICS. 66:90-96
We create a log of intrinsic dispersion and attenuation for the Antelope Shale formation of the Buena Vista Hills field, San Joaquin Valley, California. High dispersion (or low Q) values correlate with thin sand and carbonate beds within the Antelope
Publikováno v:
GEOPHYSICS. 63:1190-1199
We can use guided seismic waves to map properties of reservoirs between wells, with the low‐velocity layers acting as waveguides. When guided waves are detected, they are an indication of the continuity of the bed examined. Guided waveforms are cha
Autor:
Raymon L. Brown, Dirk Seifert
Publikováno v:
GEOPHYSICS. 62:477-486
Apparent discrepancies between velocity measurements made with different frequencies in a formation at the Gypsy test site are explained in terms of elastic scattering and intrinsic attenuation. The elastic scattering component of the dispersion (38%
Autor:
Raymon L. Brown
Publikováno v:
The Leading Edge. 15:125-129
This article is on the subject of estimating the relative distances over which different types of waves might be detected. While emphasis is on the transmission and detection of waves between boreholes, the basic philosophy can be applied to any prob
Autor:
Raymon L. Brown
Publikováno v:
SEG Technical Program Expanded Abstracts 2009.
Autor:
Raymon L. Brown
Publikováno v:
SEG Technical Program Expanded Abstracts 2009.
Pore space, pore fluid and the solid minerals control both the seismic behavior and permeability of a rock. Ignoring changes in the mineral matrix, the pore space is used to explain many issues associated with stress, pore pressure, permeability and
Autor:
Raymon L. Brown, J. R. Everett
Publikováno v:
The Leading Edge. 10:29-34
Continental breakup and collision are exciting topics of academic discussion, but their presence in an exploration environment nearly always complicates the situation. The recent flurry of exploration in the Arkoma basin of southeastern Oklahoma/sout