Zobrazeno 1 - 9
of 9
pro vyhledávání: '"Chinaemerem Kanu"'
Autor:
H. Jin, Chinaemerem Kanu, Esteban Díaz, D. Ni, Andrew Brenders, K. Fu, Q. Li, Scott Michell, T. Manning, J.R. Sandschaper, Robert Pool, Joe Dellinger, S. LaDart, T. Yang, Mariana Gherasim
Publikováno v:
81st EAGE Conference and Exhibition 2019.
To realize the vision of automatic velocity model building with full-waveform inversion, a paradigm shift in the way seismic data are acquired is necessary. In December 2017 – January 2018 BP acquired 1000km of source lines over the deepwater sub-s
Autor:
Chinaemerem Kanu, Mariana Gherasim, Linda Hodgson, Qie Zhang, Aoife Toomey, Bosen Du, Elizabeth L'Heureux
Publikováno v:
The Leading Edge. 35:888-893
Imaging and characterizing time-lapse changes in reservoir properties rely on accurate estimation of the corresponding time shifts and amplitude changes. We evaluated the accuracy of competing time-shift extraction algorithms — cross correlation, n
Autor:
Xukai Shen, Kareem Vincent, Bertram Nolte, Pedro Paramo, Chinaemerem Kanu, Hu Jin, James Mika, Imtiaz Ahmed
Publikováno v:
SEG Technical Program Expanded Abstracts 2018.
Publikováno v:
SEG Technical Program Expanded Abstracts 2018.
Publikováno v:
SEG Technical Program Expanded Abstracts 2018.
Autor:
Roel Snieder, Chinaemerem Kanu
Publikováno v:
Geophysical Journal International. 203:1923-1936
Autor:
Roel Snieder, Chinaemerem Kanu
Publikováno v:
Journal of Geophysical Research: Solid Earth. 120:5595-5605
Multiply scattered seismic waves, due to their long path length within a finite volume, provide information that can be used to detect and image weak time-lapse changes within a medium. Such weak changes are usually not resolved with singly scattered
Publikováno v:
SEG Technical Program Expanded Abstracts 2014.
Multiply scattered seismic waves, due to their long path length in a limited volume, provide information that can be used to detect and image weak timelapse changes within a medium. Such weak changes are usually not resolved with singly scattered wav
Autor:
Chinaemerem Kanu, Kaj M. Johnson
Publikováno v:
Journal of Geophysical Research. 116
[1] Theodolite measurements across the right-lateral Hayward fault, San Francisco Bay, California, show a dramatic reduction in surface creep rate from 5 to 10 mm/yr before the 1989 Loma Prieta earthquake to nearly zero creep rate after the earthquak