Zobrazeno 1 - 10
of 18
pro vyhledávání: '"Robert G. Keys"'
Publikováno v:
GEOPHYSICS. 86:MR67-MR79
Hydrocarbon generation in a source rock is a complex, irreversible phase change that occurs when a source rock is heated during burial to change the phase to a fluid. The fluid density is less than the kerogen density; therefore, in a closed or parti
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::873743a1443ae8b3254a191792786e5c
https://doi.org/10.1190/geo2020-0205.1
https://doi.org/10.1190/geo2020-0205.1
Publikováno v:
GEOPHYSICS. 82:S247-S258
The effectiveness of basin simulators for deriving subsalt velocity models has been previously shown through the use of a correlation to relate effective stress to velocity. We build on this and others’ work by using physical models to relate poros
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c94870e0a11b147bfa70b139ffabca5f
https://doi.org/10.1190/geo2016-0316.1
https://doi.org/10.1190/geo2016-0316.1
Publikováno v:
The Leading Edge. 35:240-245
Basin simulators have been used previously for deriving subsalt velocity models with the use of a correlation to relate effective stress to velocity. We build on this, and the work of others, to use physical models to relate porosity to velocity for
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c77fbcbc57b90fa2c9763310c8739d56
https://doi.org/10.1190/tle35030240.1
https://doi.org/10.1190/tle35030240.1
Publikováno v:
The Leading Edge. 26:1424-1428
A key factor for imaging geology below complex salt bodies is identifying and defining the shape of the salt geometry. In recent years, a combination of improved imaging algorithms, increased computational speed, and integrated interpretation platfor
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ae01cf465d1193da6c20b999c52e170e
https://doi.org/10.1190/1.2805763
https://doi.org/10.1190/1.2805763
Publikováno v:
Beijing 2014 International Geophysical Conference & Exposition, Beijing, China, 21-24 April 2014.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::0c89071bb8ea424375622809bbd63408
https://doi.org/10.1190/igcbeijing2014-313
https://doi.org/10.1190/igcbeijing2014-313
Publikováno v:
All Days.
Description of the material The study area is situated SB311 block of Malaysia. The tectonic evolution of the area is linked to the rifting of South China Sea. The image of the target in this study is affected by the shallow gas-obscured zone in the
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::3066259a173a29761edd8b8187c6c685
https://doi.org/10.4043/24745-ms
https://doi.org/10.4043/24745-ms
Publikováno v:
The Leading Edge. 16:1233-1239
“Principles of AVO crossplotting” by Castagna and Swan (TLE, April 1997) raises some very interesting points and we would like to add to the discussion. Crossplotting the AVO attributes is useful for interpreting anomalies in the context of litho
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d842d7c466d8253e8b1d8e75cebf4f35
https://doi.org/10.1190/1.1437768
https://doi.org/10.1190/1.1437768
Autor:
Sanjay Sood, Peter M. Eick, Frank D. Janiszewski, Chengbo Li, Charles C. Mosher, Erik Keskula, Elias Ata, Robert G. Keys, Larry Morley, Sam T. Kaplan, Joel D. Brewer, Robert Olson
Publikováno v:
SEG Technical Program Expanded Abstracts 2012.
Summary Ideas from the field of compressive sensing are rapidly making their way into the geophysical realm. We believe that these concepts will motivate major changes in the way that our industry acquires, processes, and images seismic data. In prep
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::56ec226e261b00cf0579bb32b2009b39
https://doi.org/10.1190/segam2012-1460.1
https://doi.org/10.1190/segam2012-1460.1
Publikováno v:
SEG Technical Program Expanded Abstracts 2007.
Forward modeling using Britannia data shows a characteristic set of subtle reservoir AVO signatures due to the significant Vp:Vs contrast that exists between sands and shales (Figure 1). The same responses can be seen, to a certain degree, in an AVO
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::39f4170223b1452d15d28c40c89696e9
https://doi.org/10.1190/1.2792411
https://doi.org/10.1190/1.2792411