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Willesden Green Field

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Journal Article
Journal: AAPG Bulletin
Published: 01 December 1988
AAPG Bulletin (1988) 72 (12): 1469–1494.
...Roger G. Walker; Carolyn H. Eyles ABSTRACT Willesden Green field is a long narrow sandstone body completely encased in marine mudstones. The field is Late Cretaceous (Turonian) in age, and contains as many as seven stacked, sandier upward sequences. The sequences are as much as 12 m (39.3 ft) thick...
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Graphic lithological log of the Viking Formation in the <b>Willesden</b> <b>Green</b> Fie...
Published: 01 March 2004
Fig. 10. Graphic lithological log of the Viking Formation in the Willesden Green Field, showing stacked conglomeratic tidal inlet deposits associated with the estuary mouth. Well 05-06-41-06W5. Refer to Figure 2 for legend of symbols.
Image
Graphic lithological log of the Viking Formation in the <b>Willesden</b> <b>Green</b> Fie...
Published: 01 March 2004
Fig. 9. Graphic lithological log of the Viking Formation in the Willesden Green Field, showing conglomeratic estuary-mouth and pebble- and granule-bearing sandy bay deposits. Well 10-35-40-07W5. Refer to Figure 2 for legend of symbols.
Series: SEPM Short Course Notes
Published: 01 January 2007
DOI: 10.2110/pec.07.52.0273
EISBN: 9781565761407
... the discovery of these deposits in the Crystal Field in 1978 (cf. Reinson et al., 1985; 1988 ). The productive Crystal estuarine deposits occur in the Albian-aged (Lower Cretaceous) Viking Formation (Fig. 1 ). Subsequent IVF successions were recognized from the Willesden Green (Boreen 1989; Boreen and Walker...
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Characteristic ichnogenera associated with the  Glossifungites  ichnofacies...
Published: 01 November 2005
, and Zoophycos . Albian Viking Formation, Willesden Green field, Alberta, 10-35-40-7W5, 2327 m (7634 ft). (B) A proximal expression of a regionally extensive transgressive surface of erosion in the Viking Formation with a pebble lag passively infilling firm-ground Diplocraterion (D) and Skolithos
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—Map showing location of <b>Willesden</b> <b>Green</b> (WG) and Ferrier <b>fields</b>; adjacent ...
Published: 01 December 1988
Figure 1 —Map showing location of Willesden Green (WG) and Ferrier fields; adjacent fields shown in inset at lower left (thrust symbol marks edge of deformed belt). Also shows location of topographic crest and low between Willesden Green and Ferrier, and locations of cross sections 1-8 ( Figures
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FIGURE 5 —Cretaceous ichnofaunas in estuarine deposits of the Western Inter...
Published: 01 August 2005
- and combined-flow- rippled sandstones and burrowed sandy mudstones deposited in proximity to estuary-mouth complex. Bioturbation index is 3. Suite includes Rosselia (Ro), Thalassinoides (Th), Planolites (P), Teichichnus (Te), and Palaeophycus (Pa). Viking Formation, Willesden Green Field, Well 06-36
Image
—Isopach map of interval from datum to E5. Note dip of E5 surface toward li...
Published: 01 December 1988
Figure 14 —Isopach map of interval from datum to E5. Note dip of E5 surface toward line of deepest erosion between Willesden Green and Ferrier, and undulating topography of top of field. Letters H along the northeastern side of field designate a “high,” northeast of which is a deep trough. Note
Series: SEPM Special Publication
Published: 01 January 1999
DOI: 10.2110/pec.99.64.0179
EISBN: 9781565761865
...Abstract Abstract Whether from the foreshore, shoreface, shelf, or incised esruarine valleys, sedimentary deposits along the western edge of the Western Interior seaway quite uniformly record southerly directed paleoflows. Cardium Formation shoreface gravels at Willesden Green, Alberta...
Series: SEPM Special Publication
Published: 01 January 1994
DOI: 10.2110/pec.94.12.0129
EISBN: 9781565760905
...Abstract Abstract The Upper Albian Viking Formation produces hydrocarbons from anomalous deposits in the Crystal, Willesden Green, Cyn-Pem, Sundance, and Edson fields of west-central Alberta. These anomalous deposits are interpreted to represent lowstand incised-valley systems...
Journal Article
Journal: AAPG Bulletin
Published: 01 May 2014
AAPG Bulletin (2014) 98 (5): 881–892.
..., as was initially identified in the Ferrier and Willesden Green fields by Keith (1985) , (1991) and subsequently in the Pembina field by Joiner (1991) . The unconventional drilling targets currently being developed are the tighter and shalier sandstones found below and adjacent to the conventional reservoir...
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(a) Structure contour map (contour interval = 100 m) and the locations of m...
Published: 01 January 2002
= Eureka; 9 = Kerrobert; 10 = Plato; 11 = Chigwell; 12 = Harmattan; 13 = Garrington; 14 = Willesden Green; 15 = Caroline. (b) Organic maturity of the Second White Specks Formation (modified from Creaney and Allan, 1990 ). Contours of the reconstructed Eocene surface topography are superimposed (contour
Journal Article
Published: 01 June 1991
Bulletin of Canadian Petroleum Geology (1991) 39 (2): 123–144.
...Tom Boreen; Roger G. Walker ABSTRACT Over 500 well logs and 153 cores have been used to map three erosion surfaces in the Viking Formation in the area of Garrington, Ferrier, Willesden Green, Crystal, Gilby and Joffre. These erosion surfaces (Viking erosion surfaces VE2, VE3 and VE4), or bounding...
Journal Article
Published: 01 September 1987
Bulletin of Canadian Petroleum Geology (1987) 35 (3): 362–374.
... Creek, either part way through the Raven River Member or at the base of the Carrot Creek Member; at Willesden Green, part way through the Raven River Member; at Caroline, Garrington and Crossfield, at the base of the Burnstick Member; and at Ricinus, at the base of the Ricinus Member. Although...
Journal Article
Published: 01 March 2004
Bulletin of Canadian Petroleum Geology (2004) 52 (1): 77–104.
...Fig. 10. Graphic lithological log of the Viking Formation in the Willesden Green Field, showing stacked conglomeratic tidal inlet deposits associated with the estuary mouth. Well 05-06-41-06W5. Refer to Figure 2 for legend of symbols. ...
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Journal Article
Published: 01 June 1986
Bulletin of Canadian Petroleum Geology (1986) 34 (2): 213–225.
... Edmonton I " I " , I ' t % ICARROT CREEK I I WILLESDEN B.C. h ALBERTA ~I~,WIGREE N I I ~L~[LBERTA- -~ , ] =1 ( \ 'llmV x \ i \~FERRIER ~/ II' Cleo r we ter R. ) 4i GARR iNGTON ~ l I ' / k " .~ / \ ~CROSSFIELD q LOCHEND X ~. Calgary 0 KM 50 IO0 15TH Fig. 1. Location of main Cardium fields...
Journal Article
Published: 01 June 1973
Bulletin of Canadian Petroleum Geology (1973) 21 (2): 236–246.
... and the reserve estimates of the Willesden Green Cardium A pool is wea k and even negative . The data are shown in Figure 3 . As can be seen , there is little relation between wells drilled and reserves estimated . The last two figures suggest that pools of both types are capable o f further appreciation...
Journal Article
Published: 01 March 2013
Bulletin of Canadian Petroleum Geology (2013) 61 (1): 1–40.
... become progressively muddier upward and form a retrogradational stacking pattern, indicative of long-term transgression. Ammonites and bivalves locate the Turonian-Coniacian boundary just above the E5.5 surface. The E6.5 surface, originally recognized in the Willesden Green area, has been traced over...
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Journal Article
Journal: AAPG Bulletin
Published: 01 August 1990
AAPG Bulletin (1990) 74 (8): 1165–1182.
... the single surface now known as E5. The geometry of the E5 surface has been described at Carrot Creek by Bergman and Walker (1987 , 1988 ) and at Willesden Green by Walker and Eyles (1988 ); in this paper, we map the erosion surface from Carrot Creek into the largest of the Cardium fields—Pembina ( Figure...
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Journal Article
Published: 01 March 1998
Bulletin of Canadian Petroleum Geology (1998) 46 (1): 89–105.
... a pause in an overall transgression, asat Joffre (Downing and Walker, 1988), Gilby (Raddysh, 1988), Willesden Green (Boreen and Walker, 1991), Caroline and Garrington (Davies and Walker, 1993), and Joarcam (Posamentier and Chamberlain, 1993; Walker and Wiseman, 1995). Other sandbodies have a more north...