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Journal ArticleDOI

Magnetic upward continuation from an uneven track

Robert L. Parker, +1 more
- 01 Aug 1972 - 
- Vol. 37, Iss: 4, pp 662-668
TLDR
In this paper, a new method for continuing two-dimensional potential data upward from an uneven track is developed with special emphasis on solving a particular practical problem, that of magnetic data taken near the bottom of the ocean.
Abstract
A new method for continuing two‐dimensional potential data upward from an uneven track is developed with special emphasis on solving a particular practical problem, that of magnetic data taken near the bottom of the ocean. The method is based on the use of the Schwarz‐Christoffel transformation, which maps the original, irregular track into a horizontal straight line. It has been found to be very fast computationally and to suffer none of the restrictions found in some earlier two‐dimensional algorithms.

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Journal ArticleDOI

The historical development of the magnetic method in exploration

TL;DR: The magnetic method is the primary exploration tool in the search for minerals, oil and gas, geothermal resources, and groundwater, and for a variety of other purposes such as natural hazards assessment, mapping impact structures, and engineering and environmental studies as discussed by the authors.
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The inversion of magnetic anomalies in the presence of topography

TL;DR: In this paper, the inversion of magnetic anomalies in terms of an irregular layer of magnetized material is studied, and an efficient procedure for constructing solutions is developed, but the solution is not unique because of the existence of a magnetization (called the magnetic annihilator) that produces no observable magnetic field.
Journal ArticleDOI

Historical development of the gravity method in exploration

TL;DR: The gravity method was the first geophysical technique to be used in oil and gas exploration and has continued to be an important and sometimes crucial constraint in a number of exploration areas as discussed by the authors.
Journal ArticleDOI

Detailed near-bottom geophysical study of the Gorda Rise

TL;DR: A deeply towed instrument package was used to survey the fine details of topography, sediment distribution, and magnetization of the Gorda rise, an active spreading center off northern California as discussed by the authors.
Journal ArticleDOI

The Galapagos Spreading Centre: A Near-Bottom Geophysical Survey

TL;DR: The bathymetric relief is dominated by small blocks which tilt slightly away from the spreading center and which are bounded by inward-facing scarps as mentioned in this paper, which is similar to that found on slow-spreading ridges, but on a smaller scale.
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