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TitleSeismic velocities and composition of the Canadian crust
AuthorPostlethwaite, B; Bostock, M G; Christensen, N I; Snyder, D B
SourceTectonophysics 2014 p. 1-12, https://doi.org/10.1016/j.tecto.2014.07.024
Year2014
Alt SeriesEarth Sciences Sector, Contribution Series 20140182
PublisherElsevier
Documentserial
Lang.English
Mediapaper; on-line; digital
File formatpdf
ProvinceBritish Columbia; Alberta; Saskatchewan; Manitoba; Ontario; Quebec; New Brunswick; Nova Scotia; Prince Edward Island; Newfoundland and Labrador; Northwest Territories; Yukon; Nunavut
NTS1; 2; 3; 10; 11; 12; 13; 14; 15; 16; 20; 21; 22; 23; 24; 25; 26; 27; 28; 29; 30; 31; 32; 33; 34; 35; 36; 37; 38; 39; 40; 41; 42; 43; 44; 45; 46; 47; 48; 49; 52; 53; 54; 55; 56; 57; 58; 59; 62; 63; 64; 65; 66; 67; 68; 69; 72; 73; 74; 75; 76; 77; 78; 79; 82; 83; 84; 85; 86; 87; 88; 89; 92; 93; 94; 95; 96; 97; 98; 99; 102; 103; 104; 105; 106; 107; 114O; 114P; 115; 116; 117; 120; 340; 560
Subjectsgeophysics; seismic interpretations; seismic velocities; seismic surveys; continental crust; teleseismic surveys
Illustrationslocation maps; plots; profiles
ProgramRae Province Project Management, GEM2: Geo-mapping for Energy and Minerals
AbstractTo investigate variations in crustal structure and composition, we analyze approximately 80,000 teleseismic P wave seismograms recorded at 343 broadband stations distributed about the Canadian landmass. These data are binned by horizontal slowness and simultaneously deconvolved into receiver functions. We apply stacking methods to retrieve estimates of the bulk crustal velocity ratio VP/VS and thickness H from this receiver function dataset under the assumption of locally 1D structure. These crustal parameters are analyzed together with a compilation of velocity and thickness estimates from previous active source experiments and global crustal thickness models to investigate competing models of crustal composition and evolution. Crustal thicknesses vary between ~ 25 km and ~ 48 km with an area-weighted average of 37 km for all stations. VP/VS estimates range from 1.65 to 1.95 and display a systematic increasing trend from NW to SE across the Churchill, Superior and Grenville provinces. Analysis of intra-crustal conversions indicates little evidence for a well-defined, widespread Conrad discontinuity, although the lower crust appears to be more transparent to teleseismic converted waves than the upper crust. This observation runs contrary to that of P-reflectivity in many active source studies, and may be reconciled through a dominant scale-length of heterogeneity that is less than ~ 800 m. The VP/VS observations and VP constraints from active source studies are compared with laboratory measurements for common crustal rocktypes and found to be consistent with bulk compositions falling between granite gneiss and diorite. Previously reported systematic variations in crustal thickness and VP/VS with age in a global data set are not supported by our data set.
Summary(Plain Language Summary, not published)
Understanding where diamonds and economically important metals originate deep in the Earth requires mapping these depths with geophysical methods using observed seismic wave speed variations or density variations inferred from small changes in the observed gravity field. This paper estimates the thickness of the relatively low wave speed, low density Earth's crust in order to remove its effect and thus reveal variations in the deeper mantle. This compilation estimates both the thickness and average wave speed of the crust at 343 locations across Canada, compares them with previous study results, and extrapolates them across the main geologic provinces of Canada. Ongoing follow-up studies of the mantle using seismic waves and gravity variations will build upon these results.
GEOSCAN ID295137