Zobrazeno 1 - 10
of 15
pro vyhledávání: '"Peter M. Manning"'
Autor:
Don C. Lawton, Gary F. Margrave, Malcolm B. Bertram, Eric V. Gallant, Kevin W. Hall, Joe Wong, Kristopher A. Innanen, Kevin L. Bertram, Peter M. Manning
Publikováno v:
SEG Technical Program Expanded Abstracts 2015.
Two new geophysical test holes were drilled and completed at the University of Calgary's Priddis Geophysical Observatory (PGO), south of Calgary, Alberta, Canada in 2013. The test holes were drilled to a depth of 146 m and were cased with schedule 80
Autor:
Henry C. Bland, Robert R. Stewart, Peter M. Manning, Brian H. Hoffe, Darren S. Foltinek, Gary F. Margrave
Publikováno v:
GEOPHYSICS. 67:1853-1868
This paper uses an experimental seismic line recorded with three‐component (3C) receivers to develop a case history demonstrating very little benefit from receiver arrays as compared to point receivers. Two common array designs are tested; they are
Autor:
Gary F. Margrave, Peter M. Manning
Publikováno v:
SEG Technical Program Expanded Abstracts 2004.
The theory of correction filters for one and two dimensional finite-difference modelling has been presented by the authors in earlier papers (Manning and Margrave 2000, 2001). In those papers we showed how a correction filter could compensate for fin
Autor:
Peter M. Manning, Gary F. Margrave
Publikováno v:
SEG Technical Program Expanded Abstracts 2003.
A technique is described to generate an optimum set of points beyond the boundary of a finite-difference model; points which can be used for finitedifference operations, and which eliminate reflections from that boundary. The rationale is explained,
Autor:
Gary F. Margrave, Peter M. Manning
Publikováno v:
SEG Technical Program Expanded Abstracts 2002.
Autor:
Peter M. Manning, Gary F. Margrave
Publikováno v:
SEG Technical Program Expanded Abstracts 2001.
Autor:
Gary F. Margrave, Peter M. Manning
Publikováno v:
SEG Technical Program Expanded Abstracts 2000.
Fourier analysis is used to present conclusions about stability and dispersion in finite-difference modelling. The most elementary finite-difference model is presented, one dimension in space with second-order differencing in space and time. For this
Autor:
Peter M. Manning, Gary F. Margrave
Publikováno v:
SEG Technical Program Expanded Abstracts 1999.
Finite difference modelling of elastic wave fields is a practical method for elucidating features of records obtained for exploration seismic purposes, including surface waves. This has become possible because of the major increase in computing power
Publikováno v:
SEG Technical Program Expanded Abstracts 1999.
During November 1997 the CREWES Project at the University of Calgary recorded a 3C-2D seismic survey at the Blackfoot field east of Calgary. This survey consisted of recording dynamite shots into a combination of conventional 20 m and high-resolution
Publikováno v:
SEG Technical Program Expanded Abstracts 1993.
A four-source multioffset three-component (3-C) VSP experiment was carried out in a 3-D prospect area. The data were processed with a view to studying coal anisotropy and comparing the resolution of multioffset-VSP and 3-D surface data. Converted-wav