Gordon Cooper

Dr. Gordon Cooper

School of Geosciences, University of the Witwatersrand, Private Bag X3, Johannesburg P.O. Box Wits 2050, South Africa
orcid

Research Focus & Metrics

Academic Career Length

30Years (1997-Present)

(Calculated once Scilit publication data is synced: current year − year of first publication + 1)

Representative Publications

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1 December 2006 in Computers & Geosciences
Verified
Journal Article
Closed access
GCGordon Cooper
Gordon Cooper
DCD.R. Cowan
D.R. Cowan

1 November 2003 in Quaternary Science Reviews
Verified
Journal Article
Closed access
KHKarin Holmgren
Karin Holmgren
JLJulia A. Lee-Thorp
Julia A. Lee-Thorp
GCGordon Cooper
Gordon Cooper
KLKatarina Lundblad
Katarina Lundblad
TPTimothy C. Partridge
Timothy C. Partridge
PTPeter D. Tyson
Peter D. Tyson

1 January 2008 in Geophysics
Verified
Journal Article
Closed access
GCGordon Cooper
Gordon Cooper
DCDuncan R. Cowan
Duncan R. Cowan
Edge enhancement in potential-field data helps geologic interpretation. There are many methods for enhancing edges, most of which are high-pass filters based on the horizontal or vertical derivatives of the field. Normalized standard deviation (NSTD), a new edge-detection filter, is based on ratios of the windowed standard deviation of derivatives of the field. NSTD is demonstrated using aeromagnetic data from Australia and gravity data from South Africa. Compared with other filters, the NSTD filter produces more detailed results.

1 February 2008 in Computers & Geosciences
Verified
Journal Article
Closed access
GCGordon Cooper
Gordon Cooper
DCD.R. Cowan
D.R. Cowan

1 June 2004 in Computers & Geosciences
Verified
Journal Article
Closed access
GCGordon Cooper
Gordon Cooper
DCD.R Cowan
D.R Cowan

1 January 2009 in Geophysics
Verified
Journal Article
Closed access
GCGordon Cooper
Gordon Cooper
Horizontal and vertical gradients, and filters based on them (such as the analytic signal), are used routinely to enhance detail in aeromagnetic data. However, when the data contain anomalies with a large range of amplitudes, the filtered data also will contain large and small amplitude responses, making the latter hard to see. This study suggests balancing the analytic signal amplitude (sometimes called the total gradient) by the use of its orthogonal Hilbert transforms, and shows that the balanced profile curvature can be an effective method of enhancing potential-field data. Source code is available from the author on request.