Zobrazeno 1 - 10
of 14
pro vyhledávání: '"T. K. Kan"'
Autor:
Herbert W. Swan, T. K. Kan
Publikováno v:
GEOPHYSICS. 66:1937-1946
The phenomenon of geopressure is essentially stratigraphic in nature. In most cases, its occurrence correlates strikingly well with some mappable geologic characteristics, such as lithology changes, sediment deformation, and faulting. High‐precisio
Autor:
T. K. Kan, C. Sicking
Publikováno v:
4th International Congress of the Brazilian Geophysical Society.
Autor:
John P. Castagna, R. S. Spratt, N. R. Goins, T. J. Fitch, Samir K. Dey-Sarkar, Steve V. Svatek, Herbert W. Swan, T. K. Kan, C. Y. Young, Leon Thomsen
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::2b10034774020a2c61df8ae38845d308
https://doi.org/10.1190/1.9781560802624.ch1
https://doi.org/10.1190/1.9781560802624.ch1
Autor:
T. K. Kan, C. J. Sicking
Publikováno v:
EAGE/SEG Research Workshop 1990.
Interval velocity is often computed from Normal Moveout (NMO) or migration velocities. Examples of using interval velocity from these sources are shown for lithology discrimination and geopressure prediction.
Publikováno v:
Journal of Geophysical Research. 79:483-488
An underice survey was carried out in a pack ice field near Fletcher's Ice Island (T-3) by means of a 48-kHz Kelvin Hughes transit sonar. The transducer was lowered through a hole, and discrete underice scans were made through 360°. Five sets of dat
Mantle reflections beneath the crestal zone of the East Pacific Rise from multi-channel seismic data
Publikováno v:
Marine Geology. 35:83-97
Two 24-fold, stacked multi-channel seismic-reflection profiles show the position of the M-discontinuity nearly continuously across the East Pacific Rise near 9°N. In the past, the position of this important boundary in the oceans has been determined
Publikováno v:
GEOPHYSICS. 39:683-691
An electromagnetic transient signal is distorted as it travels in the conducting earth. At vertical incidence, the signal is stretched by a time that is proportional to the magnetic permeability, conductivity, and depth squared. The stretch is a func
Publikováno v:
The Journal of the Acoustical Society of America. 53:777-781
A narrow‐beam scanning sonar was used to measure the relative backscattering strengths at 48 kHz of the undersurface of arctic sea ice. The graphic records displaying the range and relative scattering levels were assembled into a sonar map that dis
Publikováno v:
SEG Technical Program Expanded Abstracts 1983.