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Seismic velocity structure at a gas hydrate reflector, offshore western Colombia, from full waveform inversion

Author
MINSHULL, T. A1 ; SINGH, S. C; WESTBROOK, G. K
[1] Univ. Cambridge, Bullard Laboratories, dep. earth sci., United Kingdom
Source

Journal of geophysical research. 1994, Vol 99, Num B3, pp 4715-4734 ; Illustration , Table ; ref : 1 p. 3/4

ISSN
0148-0227
Scientific domain
Astronomy earth cosmic environment; Geology; Geophysics; Climatology, meteorology; Oceanography
Publisher
American Geophysical Union, Washington, DC
Publication country
United States
Document type
Article
Language
English
Keyword (fr)
Amplitude Forme onde Hydrate gaz Impédance acoustique Marge continentale Méthane Profil sismique vertical Réflecteur Simulation numérique Sismique réflexion Sismogramme Stabilité Structure vitesse Sédiment marin Colombie Amérique du Sud
Keyword (en)
amplitude waveforms gas hydrates acoustic impedance continental margin methane vertical seismic profiles reflectors digital simulation reflection methods seismograms stability velocity structure marine sediments Colombia South America
Keyword (es)
Amplitud Hidrato gas Margen continental Metano Perfil sísmico vertical Simulación numérica Método reflexión sísmica Sismograma Estabilidad Estructura velocidad Sedimento marino Colombia America del sur
Classification
Pascal
001 Exact sciences and technology / 001E Earth, ocean, space / 001E01 Earth sciences / 001E01H Marine geology

Pascal
001 Exact sciences and technology / 001E Earth, ocean, space / 001E01 Earth sciences / 001E01M Internal geophysics / 001E01M04 Applied geophysics

Discipline
Earth sciences
Origin
Inist-CNRS
Database
PASCAL
INIST identifier
3986471

Sauf mention contraire ci-dessus, le contenu de cette notice bibliographique peut être utilisé dans le cadre d’une licence CC BY 4.0 Inist-CNRS / Unless otherwise stated above, the content of this bibliographic record may be used under a CC BY 4.0 licence by Inist-CNRS / A menos que se haya señalado antes, el contenido de este registro bibliográfico puede ser utilizado al amparo de una licencia CC BY 4.0 Inist-CNRS

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