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TitreScaling behavior and the effects of heterogeneity on shallow seismic imaging of mineral deposits: a case study from Brunswick No. 6 mining area, Canada
AuteurCheraghi, S; Malehmir, A; Bellefleur, G; Bongajum, E; Bastani, M
SourceJournal of Applied Geophysics vol. 90, 2013 p. 1-18, https://doi.org/10.1016/j.jappgeo.2012.12.003
Année2013
Séries alt.Secteur des sciences de la Terre, Contribution externe 20120174
ÉditeurElsevier
Documentpublication en série
Lang.anglais
DOIhttps://doi.org/10.1016/j.jappgeo.2012.12.003
Mediapapier; en ligne; numérique
Formatspdf
ProvinceNouveau-Brunswick
SNRC21P/05
Lat/Long OENS-65.9056 -65.7956 47.4567 47.3872
Sujetsméthodes analytiques; gisements minéraux; méthodes sismiques; méthodes statistiques; levés de reflexion sismiques; vitesse des ondes sismiques; diagraphie de densité compensée; Mine Brunswick No. 6 ; géophysique
Illustrationsgeological sketch maps
ProgrammeDeveloppements methodologie, Initiative géoscientifique ciblée (IGC-4)
ProgrammeÉtude des gîtes de sulfures massifs volcaniques, Initiative géoscientifique ciblée (IGC-4)
Résumé(disponible en anglais seulement)
We have studied the scaling behavior of compressional-wave velocity and density logs from an exploration borehole that extends down to about 700 m depth in the Brunswick No. 6 mining area, Bathurst Mining Camp, Canada. Using statistical methods, vertical and horizontal scale lengths of heterogeneity were estimated. Vertical scale length estimates from the velocity, density and calculated acoustic impedance are 14 m, 33 m,
and about 20 m, respectively. Although the estimated scale length for the acoustic impedance implies a weak scattering environment, elastic finite difference modeling of seismic wave propagation in 2D heterogeneous media demonstrates that even this weak scattering medium can mask seismic signals from small, but yet economically feasible, massive sulfide deposits. Further analysis of the synthetic seismic data suggests that in the presence of heterogeneity, lenticular-shaped targets may only exhibit incomplete diffraction signals whereby the down-dip tails of these diffractions are mainly visible on the stacked sections. Therefore, identification of orebody generated diffractions is much easier on the unmigrated stacked sections than on migrated stacked sections. The numerical seismic modeling in 2D heterogeneous media indicates that in the presence of large horizontal, but small vertical scale lengths (structural anisotropy), identification of massive sulfide deposits is possible, but their delineation at depth requires detailed velocity modeling and processing algorithms which can handle the anisotropy.
GEOSCAN ID291720