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The gradient tensor of potential field anomalies: some implications on data collection and data processing of maps
Uppsala Universitet, Department of Earth Sciences.
Uppsala Universitet, Department of Earth Sciences.ORCID iD: 0000-0002-1629-2920
1990 (English)In: Geophysics, ISSN 0016-8033, E-ISSN 1942-2156, Vol. 55, no 12, p. 1558-1566Article in journal (Refereed) Published
Abstract [en]

The full gradient tensor is presently not measured routinely onboard airplanes or on land. This paper describes some improvements that can be made in strategies of data collection and in processing of potential field maps if such tensor measurements were available. We suggest that, in addition to producing for example standard total field anomaly maps, the invariants of the tensor be mapped

Place, publisher, year, edition, pages
1990. Vol. 55, no 12, p. 1558-1566
National Category
Geophysics
Research subject
Exploration Geophysics
Identifiers
URN: urn:nbn:se:ltu:diva-68847DOI: 10.1190/1.1442807OAI: oai:DiVA.org:ltu-68847DiVA, id: diva2:1209272
Available from: 2018-05-22 Created: 2018-05-22 Last updated: 2018-05-22Bibliographically approved

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