Locating Magnetic Contacts: a Comparison of the Horizontal Gradient, Analytic Signal, And Local Wavenumber Methods
By J. Phillips. 2000
152 citations recorded by the source corpus.
Subfields: Geophysics, Ocean Engineering
View Paper: https://www.semanticscholar.org/paper/13086f41bb56926566867b8c9c3c3e5c41970e56
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- R. Hansen
- R. Blakely
- J. Phillips
Citations in the corpus
- The use of curvature in potential-field interpretation (2006, background): “…√( ∂P ∂x )2 + ( ∂P ∂y )2 ∂2P ∂h∂z = ∂ 2P ∂x∂z ∂P ∂x√( ∂P ∂x )2 + ( ∂P ∂y )2 + ∂ 2P ∂y∂z ∂P ∂y√( ∂P ∂x )2 + ( ∂P ∂y )2 = ∂2P ∂x∂z ∂P ∂x + ∂ 2P ∂y∂z ∂P ∂y√( ∂P ∂x )2 + ( ∂P ∂y )2 (12) Therefore, in terms of x and y, equation (11) becomes (Phillips, 2000; Pilkington and Keating, 2004): LW(x,…”