| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 4734761 | Proceedings of the Geologists' Association | 2011 | 6 Pages |
Abstract
Onshore, the low gradient magnetic field, with little significant shallow magnetic structure within a thick succession of sedimentary rocks, is subjected to a range of filtering techniques that permit a preliminary interpretation of lineaments within the succession. This line work is considered in conjunction with the regional fault mapping undertaken as part of a seismic re-interpretation.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Geology
Authors
James C. White, David Beamish,