dc.contributor.author |
Durrheim, RJ
|
en_US |
dc.contributor.author |
Cooper, GRJ
|
en_US |
dc.date.accessioned |
2007-01-12T13:27:04Z |
en_US |
dc.date.accessioned |
2007-06-07T10:02:58Z |
|
dc.date.available |
2007-01-12T13:27:04Z |
en_US |
dc.date.available |
2007-06-07T10:02:58Z |
|
dc.date.copyright |
|
en_US |
dc.date.issued |
1998-07 |
en_US |
dc.identifier.citation |
Durrheim, RJ and Cooper GRJ. 1998. Euldep: A program for the Euler deconvolution of magnetic and gravity data. Computers and Geosciences, vol 24 (6), pp 545-550 |
en_US |
dc.identifier.issn |
0098-3004 |
en_US |
dc.identifier.uri |
http://hdl.handle.net/10204/1409
|
en_US |
dc.identifier.uri |
http://hdl.handle.net/10204/1409
|
|
dc.description.abstract |
Measurements of the geomagnetic field can be used to help determine the structure of the Earth, since rocks often contain magnetic minerals. Measurements of the strength of the Earth's gravitational field can also be used, since the more dense the rocks, the stronger the field. The interpretation of large amounts of data can be aided by "automatic" interpretation techniques such as Euler deconvolution. This considers the anomalies to be caused by many relatively simple sources (such as dipoles or lines of dipoles) and produces the positions and depths of these sources. This data can then be used as a basis for a more detailed interpretation. |
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dc.format.extent |
479948 bytes |
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dc.format.mimetype |
application/pdf |
en_US |
dc.language.iso |
en |
en_US |
dc.publisher |
Pergamon-Elsevier Science Ltd |
en_US |
dc.rights |
Copyright: 1998 Pergamon-Elsevier Science Ltd |
en_US |
dc.source |
|
en_US |
dc.subject |
Geomagnetic fields |
en_US |
dc.subject |
Gravitational fields |
en_US |
dc.subject |
Solid minerals |
en_US |
dc.subject |
Technology |
en_US |
dc.subject |
Computer Sciences |
en_US |
dc.subject |
Geosciences |
en_US |
dc.title |
Euldep: A program for the Euler deconvolution of magnetic and gravity data |
en_US |
dc.type |
Article |
en_US |
dc.identifier.apacitation |
Durrheim, R., & Cooper, G. (1998). Euldep: A program for the Euler deconvolution of magnetic and gravity data. http://hdl.handle.net/10204/1409 |
en_ZA |
dc.identifier.chicagocitation |
Durrheim, RJ, and GRJ Cooper "Euldep: A program for the Euler deconvolution of magnetic and gravity data." (1998) http://hdl.handle.net/10204/1409 |
en_ZA |
dc.identifier.vancouvercitation |
Durrheim R, Cooper G. Euldep: A program for the Euler deconvolution of magnetic and gravity data. 1998; http://hdl.handle.net/10204/1409. |
en_ZA |
dc.identifier.ris |
TY - Article
AU - Durrheim, RJ
AU - Cooper, GRJ
AB - Measurements of the geomagnetic field can be used to help determine the structure of the Earth, since rocks often contain magnetic minerals. Measurements of the strength of the Earth's gravitational field can also be used, since the more dense the rocks, the stronger the field. The interpretation of large amounts of data can be aided by "automatic" interpretation techniques such as Euler deconvolution. This considers the anomalies to be caused by many relatively simple sources (such as dipoles or lines of dipoles) and produces the positions and depths of these sources. This data can then be used as a basis for a more detailed interpretation.
DA - 1998-07
DB - ResearchSpace
DP - CSIR
KW - Geomagnetic fields
KW - Gravitational fields
KW - Solid minerals
KW - Technology
KW - Computer Sciences
KW - Geosciences
LK - https://researchspace.csir.co.za
PY - 1998
SM - 0098-3004
T1 - Euldep: A program for the Euler deconvolution of magnetic and gravity data
TI - Euldep: A program for the Euler deconvolution of magnetic and gravity data
UR - http://hdl.handle.net/10204/1409
ER -
|
en_ZA |