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Alderson Member

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Journal Article
Published: 01 March 2011
Bulletin of Canadian Petroleum Geology (2011) 59 (1): 27–53.
...Ryan Thomas Lemiski; Dr. Jussi Hovikoski; Dr. S. George Pemberton; Dr. Murray Gingras Abstract The Upper Cretaceous Alderson Member (Lea Park Formation) of Western Canada produces prolific amounts of biogenic gas from what is dominantly a fine-grained, low-permeability interval. This production has...
FIGURES | View All (14)
Journal Article
Published: 01 December 2008
Journal of Sedimentary Research (2008) 78 (12): 803–824.
... with rivers that supply abundant suspended sediments. Underestimating the role of grain-size segregation may lead to misinterpretations of energy levels and water depths, especially in some shale-dominated sedimentary units. The Upper Cretaceous Alderson Member (Lea Park Fm) is an up to 180-m-thick, gas...
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Journal Article
Published: 01 March 1981
Bulletin of Canadian Petroleum Geology (1981) 29 (1): 42–74.
... Alderson Member is proposed. The Alderson Member is of shallow-marine origin and is transitional between a sandy, nearshore, foreshore, shore and backshore facies (the Eagle and Milk River Formations) and a marine, offshore shale facies (the Lea Park Formation). The Milk River and Eagle Formations...
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Permeability to air (k a ) characteristics of <span class="search-highlight">Alderson</span> <span class="search-highlight">Member</span> facies (Hatto...
Published: 01 March 2011
Table 3. Permeability to air (k a ) characteristics of Alderson Member facies (Hatton gas field, southwest Saskatchewan). These data contains details regarding the testing method used (either a 5 or 10 mm spaced grid arrangement, or a fabric selected test format), permeability characteristics
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Permeability to air (k a ) characteristics of <span class="search-highlight">Alderson</span> <span class="search-highlight">Member</span> facies. Core ...
Published: 01 March 2011
Fig. 9. Permeability to air (k a ) characteristics of Alderson Member facies. Core photos have been annotated with spot-minipermeametry test locations and the corresponding permeability measurement in millidarcys. Core photos of facies comprising higher permeability have been contoured using
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Permeability to air (k a ) characteristics of <span class="search-highlight">Alderson</span> <span class="search-highlight">Member</span> facies. Core ...
Published: 01 March 2011
Fig. 9. Permeability to air (k a ) characteristics of Alderson Member facies. Core photos have been annotated with spot-minipermeametry test locations and the corresponding permeability measurement in millidarcys. Core photos of facies comprising higher permeability have been contoured using
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Results from high-pressure mercury injection porosimetry of <span class="search-highlight">Alderson</span> <span class="search-highlight">Member</span>...
Published: 01 March 2011
Table 4. Results from high-pressure mercury injection porosimetry of Alderson Member facies (Hatton gas field, southwest Saskatchewan).
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An example well log of the <span class="search-highlight">Alderson</span> <span class="search-highlight">Member</span> and adjacent units. 2 nd  WSS–2 ...
Published: 01 December 2008
Figure 2 An example well log of the Alderson Member and adjacent units. 2 nd WSS–2 nd White Speckled Shale.
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Stratigraphy of the <span class="search-highlight">Alderson</span> <span class="search-highlight">Member</span> in Hatton and Abbay–Lacadena areas. Mai...
Published: 01 December 2008
Figure 3 Stratigraphy of the Alderson Member in Hatton and Abbay–Lacadena areas. Main facies occurrences are shown. Well logs are gamma ray (GR), resistivity (Res) and neutron (N). Blue line–flooding surface, Red line–maximum flooding surface, Ca-calcium carbonate enrichment in matrix, Gl
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Core 17, Abbay–Lacadena, lower–middle <span class="search-highlight">Alderson</span> <span class="search-highlight">Member</span>. See  Figure 7  for e...
Published: 01 December 2008
Figure 5 Core 17, Abbay–Lacadena, lower–middle Alderson Member. See Figure 7 for explanation of sedimentological and ichnological symbols.
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Cross section through the Milk River Formation and the <span class="search-highlight">Alderson</span> <span class="search-highlight">Member</span> of t...
Published: 01 November 2002
Figure 9 Cross section through the Milk River Formation and the Alderson Member of the Lea Park Formation, in the area of the southeast Alberta gas field. (A) Schematic relationship between coastal facies of the Dead Horse Coulee Member and shoreface sandstone of the Virgelle Member of the Milk
Journal Article
Published: 01 June 2003
Bulletin of Canadian Petroleum Geology (2003) 51 (2): 155–176.
... Mountains area. All Virgelle allomembers commonly test wet, probably due to a large amount of interconnectivity among the coastal sandstones of the allomembers, which enabled the migration of hydrocarbons up structural dip. Unconventional reservoirs such as the Alderson Member of the southern Alberta Milk...
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Journal Article
Published: 06 January 2015
Canadian Journal of Earth Sciences (2015) 52 (2): 96–111.
.... The Medicine Hat gas field hosted by the Alderson Member (Alberta), which is separated from the other members by a regional unconformity, and the Tiger Ridge gas field near the Bears Paw Mountains (Montana) limit the extent of the aquifer. The unified 3D geological model forms the necessary basis...
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Journal Article
Published: 29 October 2002
Canadian Journal of Earth Sciences (2002) 39 (10): 1553–1577.
...- or facies-equivalent rocks around Writing-On-Stone Provincial Park, but is time equivalent to the Alderson Member of the Lea Park Formation in southeastern Alberta. A hiatus of ∼2.5 Ma is present between the top of the Milk River Formation in the outcrop area and the basal beds of the Pakowki Formation...
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Journal Article
Published: 01 December 2017
Bulletin of Canadian Petroleum Geology (2017) 65 (4): 425–435.
... facilitate robust age correlation between important hydrocarbon bearing units in southern Alberta, including the prolific Alderson Member. Several short normal polarity intervals within C33r, a zone usually associated with exclusively reversed polarity, are observed. Résumé Nous présentons les nouvelles...
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Journal Article
Published: 22 February 2007
Canadian Journal of Earth Sciences (2006) 43 (12): 1859–1875.
... to the Alderson Member of southern Saskatchewan. Strong seismic reflections within the complex could be due to gas-filled porosity. Where undermined by salt removal in the Colonsay Collapse, the clinoform structures now form drape antiforms. Corresponding author (e-mail: don.gendzwill@usask.ca ). 4 8...
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Unified elevation contours of the top of several geological units (left) an...
Published: 06 January 2015
Collection section. ( a ) Elevation and thickness of the Milk River Formation (including Telegraph Creek, Virgelle, Deadhorse Coulee, and Alderson members). ( b ) Elevation and thickness of the Virgelle Member. ( c ) Elevation and thickness of the Alderson Member. ( d ) Elevation and thickness of the Pakowki
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Seismic line T34-2.00 ( a ) and geological interpretation ( b ) (see Fig.  ...
Published: 22 February 2007
Fig. 7. Seismic line T34-2.00 ( a ) and geological interpretation ( b ) (see Fig.  3 b for location). BD, base of drift – top of Lea Park Formation; C1, C2, and C3, Alderson Member clinoforms 1, 2, and 3; LPM1 and LPM2, Lea Park markers 1 and 2, or top of Alderson Member; Mud, mudbank; MV
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Facies descriptions derived from the sedimentological and ichnological logg...
Published: 01 March 2011
Table 1. Facies descriptions derived from the sedimentological and ichnological logging of Alderson Member strata (Hatton gas field area, southwest Saskatchewan). Abbreviations and symbology are defined in Table 2 .
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Facies descriptions derived from the sedimentological and ichnological logg...
Published: 01 March 2011
Table 1. Facies descriptions derived from the sedimentological and ichnological logging of Alderson Member strata (Hatton gas field area, southwest Saskatchewan). Abbreviations and symbology are defined in Table 2 .