Zobrazeno 1 - 10
of 34
pro vyhledávání: '"Mark E. Odegard"'
Publikováno v:
Geofísica Internacional, Vol 14, Iss 1, Pp 65-66 (1974)
Se presenta una interpretación detallada de la estructura de la corteza y del manto superior para la Placa de Nazca oriental, la trinchera Peruana-Chilena, y la plataforma continental peruana entre las latitudes de 8 a 12° sur. Se. utilizan método
Externí odkaz:
https://doaj.org/article/ed8bf8bdc0be47d2a15d64ce33280a7a
Publikováno v:
Second International Meeting for Applied Geoscience & Energy.
Autor:
Mark E. Odegard
Publikováno v:
First International Meeting for Applied Geoscience & Energy Expanded Abstracts.
Publikováno v:
Interpretation. 7:SH133-SH152
Is there a petroleum system here? How extensive and effective is it? How is it defined? Although we had presented a 2005 AAPG poster to address these questions, we now have performed an exploration look-back or case study demonstrating basin-wide pre
Publikováno v:
Geological Society, London, Special Publications. 431:219-233
Autor:
Mark E. Odegard
Publikováno v:
SEG Technical Program Expanded Abstracts 2016.
Autor:
Mark E. Odegard
Publikováno v:
14th International Congress of the Brazilian Geophysical Society & EXPOGEF, Rio de Janeiro, Brazil, 3-6 August 2015.
Publikováno v:
Marine and Petroleum Geology. 20:309-322
Evaluation of tertiary sequences of West Africa and Brazil typically requires large budgets and staffs to identify drilling targets. Since these tertiary sedimentary systems extend for hundreds of kilometers (Proc. Petrol. Geol. Deepwater Depositiona
Publikováno v:
The Leading Edge. 20:873-876
Converting sea-surface height variations, derived from satellite altimetry, to free air gravity is not new. In the early 1980s William Haxby (Lamont Doherty Geological Observatory) produced the first global marine gravity map from SeaSat satellite al
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