Zobrazeno 1 - 10
of 12
pro vyhledávání: '"Martin F. Mushayandebvu"'
Publikováno v:
GEOPHYSICS. 66:814-823
The Euler homogeneity relation expresses how a homogeneous function transforms under scaling. When implemented, it helps to determine source location for particular potential field anomalies. In this paper, we introduce an additional relation that ex
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::6a37ce22e92066758cc6f26354327e4d
https://doi.org/10.1190/1.1444971
https://doi.org/10.1190/1.1444971
Publikováno v:
GEOPHYSICS. 65:512-520
Tensor Euler deconvolution has been developed to help interpret gravity tensor gradient data in terms of 3-D subsurface geological structure. Two forms of Euler deconvolution have been used in this study: conventional Euler deconvolution using three
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::1c6584d649423a2961285f77f4f2a41e
https://doi.org/10.1190/1.1444745
https://doi.org/10.1190/1.1444745
Publikováno v:
Journal of Geophysical Research: Solid Earth. 101:11291-11303
We have estimated the effective elastic thickness of the continental lithosphere beneath South Africa using the coherence technique. This involves (1) estimating the coherence between Bouguer gravity anomalies and topography in the spectral domain an
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::9ba3948135102f326090cf4d785d2e38
https://doi.org/10.1029/95jb03718
https://doi.org/10.1029/95jb03718
Publikováno v:
Journal of African Earth Sciences. 19:27-34
The 2-D spectral analysis of gravity and topography data has been used to identify structural trends of recognized geological entities within the tectonic provinces of South Africa. The mean amplitude of the spectra within very thin rings, taken to h
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::98c5a4e14d45d58c93e1ee8f43295066
https://doi.org/10.1016/0899-5362(94)90034-5
https://doi.org/10.1016/0899-5362(94)90034-5
Publikováno v:
SEG Technical Program Expanded Abstracts 2004.
Summary Tertiary fluvial and Quaternary glacial paleo-channels with no current topographic expression are common phenomena in the Western Canadian Sedimentary Basin (WCSB). These channels are infilled by fluvial sediment of Cordilleran and local orig
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e8edb40e6da79ff8bed044153b32904c
https://doi.org/10.1190/1.1842418
https://doi.org/10.1190/1.1842418
Publikováno v:
SEG Technical Program Expanded Abstracts 2002.
Summary We present a new method for interpretation of potentialfield anomaly data. A linear equation, involving the anomaly and its horizontal gradient, is derived to provide both the depth and nature of the buried sources. The proposed method is sim
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::91dfcb806c20f332ea57b1a7d0c0e613
https://doi.org/10.1190/1.1817358
https://doi.org/10.1190/1.1817358
Publikováno v:
SEG Technical Program Expanded Abstracts 2000.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::0f97d42af8c1a24a70dcc0b7b00d0928
https://doi.org/10.1190/1.1816077
https://doi.org/10.1190/1.1816077
Publikováno v:
SEG Technical Program Expanded Abstracts 1999.
The Euler homogeneity relation expresses how a homogeneous function transforms under scaling. When implemented it helps to determine source location for particular potential field anomalies. In this paper we introduce an additional relation that expr
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::393bdea1ea41ed602bfe9b14e3ea4cb0
https://doi.org/10.1190/1.1821035
https://doi.org/10.1190/1.1821035
Publikováno v:
Journal of Geophysical Research. 95:17371
We report 26 new heat flow and 13 radiogenic heat production measurements from Zimbabwe, Zambia and Tanzania, together with details and some revisions of 18 previous heat flow measurements by other investigators from Kenya and Tanzania. These measure
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c2a7b718687927bc2600e9211d3c2e0b
https://doi.org/10.1029/jb095ib11p17371
https://doi.org/10.1029/jb095ib11p17371
Publikováno v:
Journal of Geophysical Research. Solid Earth; 1996, Vol. 101 Issue B5, p11291-11303, 13p