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pro vyhledávání: '"Grant W. Lowey"'
Autor:
Grant W Lowey
Publikováno v:
AIMS Geosciences, Vol 7, Iss 3, Pp 355-389 (2021)
Mesozoic convergence of the Wrangellia composite terrane with the western margin of North America resulted in the collapse of intervening flysch basins. One of these basins, the Jurassic-Cretaceous Gravina-Nuzotin belt, comprises from south to north,
Externí odkaz:
https://doaj.org/article/6fa68674a4e748318c49c269c4877f5a
Autor:
Grant W. Lowey
Publikováno v:
GSA Bulletin.
The debate concerning eastward versus westward subduction along the western margin of Mesozoic North America involves three main arguments: The tomography argument (westward) claims subducted slabs are observed by tomographic processing of seismic wa
Autor:
Grant W. Lowey
Supplemental Material S1: A Logic Cheat Sheet.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::44a2a3c45b06164963fc7112ed42d602
https://doi.org/10.1130/gsab.s.21676703.v1
https://doi.org/10.1130/gsab.s.21676703.v1
Publikováno v:
AIMS Geosciences, Vol 7, Iss 3, Pp 355-389 (2021)
Mesozoic convergence of the Wrangellia composite terrane with the western margin of North America resulted in the collapse of intervening flysch basins. One of these basins, the Jurassic-Cretaceous Gravina-Nuzotin belt, comprises from south to north,
Autor:
Grant W. Lowey
Publikováno v:
Canadian Journal of Earth Sciences. 56:77-100
The Mesozoic convergence of the allochthonous Wrangellia composite terrane (WCT) with the western margin of Laurasia coincided with the construction of the Chitina magmatic arc on the WCT, and the dispersal of volcanic flows and sediment gravity flow
Autor:
Grant W. Lowey
Publikováno v:
Tectonics. 36:2736-2740
Autor:
Darrel G.F. Long, Grant W. Lowey
Publikováno v:
Geoscience Frontiers, Vol 2, Iss 3, Pp 277-288 (2011)
Mid-Cretaceous strata within the Tintina Trench, 3 km west of the community of Ross River, contain evidence of deposition in two distinct, alternating, fluvial settings. Coal-bearing, mud-dominated strata are commonly associated with high-constructiv
Autor:
Grant W. Lowey
Publikováno v:
Lithos. 125:86-100
The Chitina arc in the northern Cordillera of North America evolved during the accretion of the Wrangellia composite terrane to the western margin of North America in the Jurassic and Cretaceous. The Dezadeash Formation, a 3000 m thick sequence of de
Publikováno v:
Bulletin of Canadian Petroleum Geology. 57:350-386
Whitehorse trough is a frontier basin in south-central Yukon that is thought to contain gas and possibly oil. It consists of up to 7000 m of sedimentary and volcanic rocks referred to as the Lewes River Group (Triassic), Laberge Group (Jurassic), and
Autor:
Grant W. Lowey
Publikováno v:
Sedimentary Geology. 198:273-291
The Dezadeash Formation is a northwest trending belt of predominantly Jura–Cretaceous deep-marine siliciclastic rocks in southwestern Yukon, Canada. It is truncated to the southwest by the Denali Fault System, a major transcurrent fault along which