Zobrazeno 1 - 10
of 10
pro vyhledávání: '"Anthony P. Hamblin"'
Autor:
Peter S. Giles, Nicolas Pinet, Peter Hannigan, James R. Dietrich, Denis Lavoie, Sébastien Castonguay, Anthony P. Hamblin
Publikováno v:
Bulletin of Canadian Petroleum Geology. 59:54-84
The Paleozoic sedimentary successions in eastern Canada occur in four major tectonostratigraphic domains: the Lower–Middle Paleozoic autochthonous St. Lawrence Platform, extending from southern Quebec to western Newfoundland; the deformed Lower Pal
Autor:
Erick R. Burns, Paul R. J. Wozniak, Derald G. Smith, Stephen E. Grasby, Masaki Hayashi, Laurence R. Bentley, Anthony P. Hamblin
Publikováno v:
Hydrogeology Journal. 18:1375-1390
Fluvial systems tend to deposit sediment in well-defined relational geometries and in vertically and laterally repeating patterns. These sedimentary deposits are preserved to varying degrees depending on how much the fluvial system reworks the deposi
Autor:
Paul R.J. WozniakP.R.J. Wozniak, Anthony P. Hamblin, Zhuoheng ChenZ. Chen, Stephen E. Grasby, Arthur R. Sweet
Publikováno v:
Canadian Journal of Earth Sciences. 45:1501-1516
The Paskapoo Formation of southern Alberta supports more groundwater wells than any other aquifer system in the Canadian Prairies. Located in a region of rapid population growth and straddling watersheds where no new surface water licenses are availa
Autor:
R.G. Walker, Anthony P. Hamblin
Publikováno v:
Bulletin of Canadian Petroleum Geology. 48:84-89
Recently Cant and Stockmal (1999) published new structural observations and interpretations, and a revision of sedimentological interpretations of Hamblin and Walker (1979) on the Trans-Canada Highway outcrop section at Banff, formerly known as the B
Autor:
David A. Eberth, Anthony P. Hamblin
Publikováno v:
Canadian Journal of Earth Sciences. 30:174-200
The lithostratigraphic interval between the Taber and Lethbridge coal zones in the upper portion of the nonmarine Judith River Group of southeastern Alberta is divisible into two lithostratigraphic units separated by a regionally extensive and diachr
Autor:
Anthony P. Hamblin
Publikováno v:
Sedimentology. 39:263-284
The Strathlorne Formation is the middle formation of a three-part Horton Group stratigraphy present throughout the post-Acadian Orogeny Maritimes Basin in Atlantic Canada. It is up to 600 m in thickness and is of Tournaisian age. The formation was de
Autor:
John Utting, Anthony P. Hamblin
Publikováno v:
International Journal of Coal Geology. 19:439-456
The Thermal Alteration Index (TAI) obtained from spore colouration is a useful maturity indicator that may be obtained from palynological preparations. Thermal maturity is an important parameter in determining the hydrocarbon potential of the Lower C
Autor:
Brian R. Rust, Anthony P. Hamblin
Publikováno v:
Basin Research. 2:239-255
The Devono-Carboniferous Horton Group of Cape Breton Island WE; mostly deposited in two fault-bounded asymmetric sub-basins which were part of a large intracontinental rift system. This system lay at a palaeolatitude of about 10-15° S-a warm, semi-a
Autor:
Anthony P. Hamblin, Roger G. Walker
Publikováno v:
Canadian Journal of Earth Sciences. 16:1673-1690
The transition from the Passage Beds of the Fernie into the lowermost part of the Kootenay Formation is exposed in 11 sections in the Crowsnest Pass to Banff area. Six distinct facies can be defined. Facies A (thin bedded turbidites) and facies B (th
Autor:
Anthony P. Hamblin, Roger G. Walker
Publikováno v:
Canadian Journal of Earth Sciences. 18:667-668