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TitreCrustal suture preserved in the Paleoproterozoic Trans-Hudson orogen, Canada
AuteurWhite, D J; Zwanzig, H V; Hajnal, Z
SourceGeology v. 28, no. 6, 2000 p. 527-530, https://doi.org/10.1130/0091-7613(2000)28<527:cspitp>2.0.co;2
Année2000
Séries alt.Commission géologique du Canada, Contributions aux publications extérieures 1999190
ÉditeurGeological Society of America
Documentpublication en série
Lang.anglais
DOIhttps://doi.org/10.1130/0091-7613(2000)28<527:cspitp>2.0.co;2
Mediapapier; en ligne; numérique
Formatspdf
ProvinceManitoba; Saskatchewan
SNRC63K; 63L; 63M; 63N; 64C; 64D; 64E; 64F; 73I; 73P; 74A; 74H
Lat/Long OENS-106.0000 -100.0000 58.0000 54.0000
Sujetslevés de reflexion sismiques; levés sismiques, sol; gravité; lignes de suture; croûte océanique; croûte continentale; subduction; obduction; Orogène Trans-Hudsonien; Complexe de Flin Flon - Glennie ; Domaine de Kisseynew ; Ceinture de Lynn Lake ; Ceinture de la Ronge ; Domaine de Rottenstone ; Domaine de South Indian ; Province de Superior ; Batholite de Wathaman - Chipewyan ; Ceinture de Wollaston Fold ; Ceinture de Rusty Lake ; Ceinture de South Indian ; Zone de Granville Lake Structural ; géophysique; géologie régional; tectonique; Protérozoïque
Illustrationssketch maps; seismic profiles; profiles; density models
Résumé(disponible en anglais seulement)
LITHOPROBE seismic reflection data acquired in 1994 within the Trans-Hudson orogen include a 180 km profile that crosses the boundary between a collapsed marginal basin (Kisseynew domain) and an older volcanic-plutonic arc terrane (Lynn Lake belt). The seismic data image a prominent band of northeast-dipping anastomosing reflections that extend to 10 s two-way traveltime from the surface location of a geological boundary where interpreted oceanic crust is preserved, and separate thick crust (16 s) of the Kisseynew domain from the abruptly thinner crust (12 s) of the Lynn Lake belt. Highly reflective lower crust (10-16 s) of the Kisseynew domain dips gently northward and extends laterally for at least 40 km beneath the adjacent Lynn Lake belt in a manner reminiscent of the western Alps. Complementary gravity modeling shows that the thickness of metasedimentary rocks within the Kisseynew domain is 20 ± 3 km. The seismic image is interpreted as portraying a crustal-scale collisional suture that formed as the end result of northward subduction of backarc basin crust (ancestral Kisseynew basin floor), and subsequent contraction and thrusting of the remnant Kisseynew basin fill under the margin of the Lynn Lake belt.
GEOSCAN ID211020