Výsledky vyhledávání - "Derald G. Smith"

Seismic geomorphology and sedimentology of a tidally influenced river deposit, Lower Cretaceous Athabasca oil sands, Alberta, Canada

Autor: Stephen M. Hubbard, Haley Nielsen, Dale A. Leckie, Lorraine Bloom, Milovan Fustic, Derald G. Smith, Ronald J. Spencer

Publikováno v: AAPG Bulletin. 95:1123-1145

The bitumen of the Lower Cretaceous McMurray Formation in Alberta arguably represents one of the most important hydrocarbon accumulations in the world. In-situ development relies on heat transfer through the reservoir via horizontal steam injection w

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::fcfaaecf0672d53a6c04f6ffb402d83d
https://doi.org/10.1306/12131010111

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Hydrogeological implications of paleo-fluvial architecture for the Paskapoo Formation, SW Alberta, Canada: a stochastic analysis

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

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::dd53db7937d548c34fd4e9b321f3d638
https://doi.org/10.1007/s10040-010-0608-y

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Counter point bar deposits: lithofacies and reservoir significance in the meandering modern Peace River and ancient McMurray Formation, Alberta, Canada

Autor: Milovan Fustic, Dale A. Leckie, Stephen M. Hubbard, Derald G. Smith

Publikováno v: Sedimentology. 56:1655-1669

Counter point bar deposits in the meandering Peace River, North-centralAlberta, Wood Buffalo National Park, are distinct from point bar deposits interms of morphology, lithofacies and reservoir potential for ﬂuids.Previously referred to as the dist

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::5b0bc4c014097d3e74f666b86c2b1ad4
https://doi.org/10.1111/j.1365-3091.2009.01050.x

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Floodplain stratigraphy of the ice jam dominated middle Yukon River: a new approach to long-term flood frequency

Autor: Joanne M. Livingston, Duane G. Froese, Derald G. Smith, Chris H. Hugenholtz

Publikováno v: Hydrological Processes. 23:357-371

Floodplain stratigraphy is used as a new method for reconstructing ice jam flood histories of northern rivers. The method, based on reconstruction of the sedimentary record of vertically-accreting floodplains, relies on stratigraphic logging and inte

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::5e153ddcafafdafffb57d37a3bc951f9
https://doi.org/10.1002/hyp.7106

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Application of Floodplain Stratigraphy to Determine the Recurrence of Ice-Jam Flooding Along the Lower Peace and Athabasca Rivers, Alberta

Autor: Derald G. Smith, Joanne M. Livingston, Chris H. Hugenholtz

Publikováno v: Canadian Water Resources Journal. 34:79-94

Multi-proxy reconstructions of ice-jam flooding have increased significantly in the last several decades, providing important estimates of changes in ice-jam activity over time. Here, the floodplain sedimentary archive is investigated as a stratigrap

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::93d22a5db087675d6c643c9c8593e14e
https://doi.org/10.4296/cwrj3401079

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Invasive Saltcedar (Tamarix): Its Spread from the American Southwest to the Northern Great Plains

Autor: Derald G. Smith, Cheryl M. Pearce

Publikováno v: Physical Geography. 28:507-530

The advance of saltcedar from the American southwest to Montana between the mid-19th and mid-20th centuries crossed the Continental Divide—a major topographic and climatic barrier to natural dispersal by southern plants. Interviews, archival inform

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::5da4ece2639d5f28e7e8e89d8fe0c550
https://doi.org/10.2747/0272-3646.28.6.507

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