1. New geophysical models for subsurface velocity structure in the Nechako-Chilcotin plateau from 2.5-d waveform tomography
- Author
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Smithyman, B.R., Clowes, R.M., and Bordet, E.
- Subjects
Geophysics -- Research ,Geological research ,Waveforms -- Research ,Tomography -- Methods ,Earth sciences - Abstract
Seismic inversion is applied to generate physical property models (P-wave velocity and numerical attenuation) for four profiles in the Nechako-Chilcotin plateau region of south-central British Columbia, Canada. A newly developed method that combines three-dimensional (3-D) travel-time inversion and 2.5-dimensional (2.5-D) visco-acoustic full-waveform inversion was applied to generate the geophysical models from vibroseis data acquired along the preexisting crooked roads. These models are useful for the characterization of rock types in terms of their positions and thicknesses, which may be used in conjunction with geological ground truth to infer the extent of lithostratigraphic units in the subsurface. The velocity structures also may be used for future reprocessing of the seismic reflection data to derive improved images based on the better near-surface velocity models. The subsurface geology of the Nechako-Chilcotin plateau region is complex, resulting from multiple stages of tectonic compression and extension, contemporaneous with the deposition of sediments and volcanic material. Several basin structures are identified from the joint interpretation of the waveform tomography velocity models and post-stack time migration images. The combination of these results enables the extrapolation and characterization of geological structures to ~3 km depth, particularly within the Cenozoic volcanic units that dominate near-surface stratigraphy. Based on the seismic profiles, a fence-diagram geological interpretation that extends to ~3 km depth illustrates the complex structure of the Jurassic to Neogene stratigraphic sequence. Des modeles de proprietes physiques (vitesse des ondes P et attenuation numerique) sont generes par inversion sismique le long de quatre profiles dans la region du plateau de Nechako-Chilcotin au sud-est de la Colombie Britannique. Une methode recemment developpee combine l'inversion tridimensionnelle (3-D) des temps de trajet et une inversion 2.5dimensionnelle (2.5-D) des formes d'ondes viscoacoustiques. Cette methode est utilisee pour generer les modeles geophysiques a partir de donnees sismiques acquises a partir d'une source vibroseis le long de routes curvilignes. De tels modeles sont utiles afin de caracteriser la position et l'epaisseur des successions rocheuses; ainsi, combines a des donnees geologiques de surfaces, ces modeles permettent de deduire l'etendue des unites lithostratigraphiques en sous-surface. Les structures imagees par les modeles de vitesse peuvent aussi etre utilisees pour le retraitement de donnees de sismique reflexion: elles permettent d'obtenir des profils ameliores fondes sur des meilleurs modeles de vitesse en proche surface. La geologie du plateau de Nechako-Chilcotin est complexe, et resulte d'evenements tectoniques successifs de compression et extension durant le depot de materiel sedimentaire et volcanique. Plusieurs bassins sont identifies a partir de l'interpretation conjointe de modeles tomographiques et d'images de migration en temps. La combinaison de ces resultats permet d'extrapoler et de caracteriser les structures geologiques jusqu'a 3 km de profondeur, particulierement au sein des unites volcaniques d'age Cenozoique qui dominent la stratigraphie de proche surface. Une section geologique interpretative entre 0 et 3 km de profondeur est construite a partir des profils sismiques et illustre la complexite structurale de la succession d'age Jurassique a Neogene., Introduction Interest in the Mesozoic (mainly Cretaceous) sedimentary units of the Nechako-Chilcotin plateau has been economically motivated by the potential for hydrocarbon development (Hannigan et al. 1994; Hayes et al. [...]
- Published
- 2014
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