| Titre | Seismic stratigraphic inferences regarding late-phase volcanism and subsidence history along southern Alpha Ridge |
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| Auteur | Shimeld, J W; Jackson, H R; Chian, D; Mosher, D C ; Hutchinson, D; Lebedeva-Ivanova, N N |
| Source | L'Association géologique du Canada-L'Association minéralogique du Canada, Réunion annuelle conjointe, Recueil des résumés vol. 35, 2012 p. 127 |
| Liens | Online - En ligne
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| Année | 2012 |
| Séries alt. | Secteur des sciences de la Terre, Contribution externe 20110353 |
| Réunion | Joint Annual Meeting, Geological Association of Canada and Mineralogical Association of Canada; St. John's; CA; mai 27-29, 2012 |
| Document | publication en série |
| Lang. | anglais |
| Media | papier |
| Province | Région extracotière du nord |
| Région | Alpha-Mendeleev ridge; Océan Arctique; Arctic Ocean Basin |
| Sujets | dorsales sous-marines; levés sismiques; profils sismiques; levés de reflexion sismiques; roches ignées; géophysique; stratigraphie; géologie marine |
| Programme | Délimitation du plateau continental du Canada en vertu de la Convention des Nations Unies sur le droit de la mer (UNCLOS) |
| Diffusé | 2012 01 01 |
| Résumé | (disponible en anglais seulement)
The Alpha-Mendeleev ridge complex is a submarine mountain system extending in an arcuate trend across the Arctic Ocean Basin from the Canadian margin, northwest
of Ellesmere Island, to the Siberian margin north of Wrangel Island. Ranging in elevation from about 3500 to 250 m below sea level, and covering an area of 7.5E5 sq km, the ridge complex exhibits highly variable morphologies. It is generally
interpreted to be a large igneous province that possibly includes domains of continental crust. However, the nature and origin of the Alpha-Mendeleev complex are actively debated because of the sparseness of geological and geophysical data and the
complexity of the tectonic framework. Modern 16-channel seismic reflection data collected from icebreakers over the southernmost flanks of the ridge complex reveal a distinctive unit deposited immediately on top of presumed igneous crust (inferred
from acoustic basement). The unit comprises high amplitude, continuous, parallel to sub-parallel internal reflections. Its base forms a angular unconformity that extends southward into Canada Basin until it is eventually obscured by deep burial. The
top of the unit is an onlap surface that also exhibits pronounced truncation along regions of Nautilus Spur. Modelling of wide-angle reflection and refraction sonobuoy data demonstrates a range of seismic velocities within the unit. For burial depths
of less than 1.0 km, velocities range from 2.0 to 3.3 km/s. At deeper burial depths velocities are between 4.1 and 4.6 km/s. High impedance contrasts indicate the presence of indurated lithologies such as calcareous or siliceous sediments, or
possibly volcanics. Ranging up to about 600 m in thickness, the unit appears to be concordant with basement topography. Faulting is generally minor, but normal offsets at several locations indicate that deposition of the unit predates the most recent
phase of significant extension in Canada Basin. The distinct onlap of the overlying sedimentary succession indicates that the extension was associated with rapid subsidence followed by tectonic quiescence. Throughout the northern reaches of Canada
Basin, the unit onlaps the flanks of several large basement structures interpreted to be volcanic edifices, suggesting a temporal and possibly genetic linkage to late-phase volcanism. Samples have not yet been obtained, but a working hypothesis is
that the unit consists of high-velocity siliceous oozes interbedded with hemipelagic and pelagic sedimentation. |
| GEOSCAN ID | 289867 |
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