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Chungo Member

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Journal Article
Published: 01 November 1992
Journal of Sedimentary Research (1992) 62 (6): 933–945.
...Richard J. Cheel; Dale A. Leckie Abstract The Upper Cretaceous Chungo Member of the Wapiabi Formation at Mount Yamnuska, Alberta is composed of three cycles: two coarsening-upward progradational successions overlain by a fining-upward transgressive succession. The basal 3 m of the transgressive...
Journal Article
Published: 01 August 1992
Canadian Journal of Earth Sciences (1992) 29 (8): 1802–1805.
...R. W. C. Arnott Abstract Swaley cross-stratified sandstones are exposed in the Late Cretaceous Chungo Member of the Wapiabi Formation at Mount Yamnuska, Alberta. At this site, many of the individual flaggy-weathering, thin beds of sandstones that make up the swaley cross-stratified structure...
Journal Article
Published: 01 June 1991
Bulletin of Canadian Petroleum Geology (1991) 39 (2): 206.
...J. Bhattacharya The Campanian Chungo Member of the Wapiabi Formation in the Foothills and the equivalent Milk River Formation in the southern Alberta subsurface prograde to the southeast. New correlation of previously described Chungo Member outcrops indicates that it comprises a set of offlapping...
Journal Article
Published: 01 April 1987
Canadian Journal of Earth Sciences (1987) 24 (4): 771–783.
...Lorne R. P. Rosenthal; Roger G. Walker Abstract The Chungo Member of the Wapiabi Formation (Campanian) shales out northward and (or) eastward from Lundbreck to the Bow Valley, southern Alberta. At Lundbreck, basinal mudstones are overlain by turbidite and hummocky cross-stratified sandstones...
Journal Article
Published: 01 March 2009
Bulletin of Canadian Petroleum Geology (2009) 57 (1): 1–33.
... Campanian time and probably represent approximately 2.5 Ma. Only allomember L contains swaley-stratified sandstone bodies (correlative with the Chungo Member in outcrop) that represent at least 40 km of north-eastward shoreface progradation. The upper surface of allomember L is a major, pebble-veneered...
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Journal Article
Published: 01 June 1991
Bulletin of Canadian Petroleum Geology (1991) 39 (2): 206.
... lava provides an aquifer for irrigation water onshore and a potential unconventional hydrocarbon reservoir in the Bass Basin. SED2 BHATTACHARYA, J., Alberta Geological Survey, Edmonton, Alberta T6H 5X2 Parasequence architecture of the Upper Cretaceous Chungo Member and Milk River Formation in southern...
Journal Article
Published: 01 June 1991
Bulletin of Canadian Petroleum Geology (1991) 39 (2): 206.
... and jointed vesicular lava provides an aquifer for irrigation water onshore and a potential unconventional hydrocarbon reservoir in the Bass Basin. SED2 BHATTACHARYA, J., Alberta Geological Survey, Edmonton, Alberta T6H 5X2 Parasequence architecture of the Upper Cretaceous Chungo Member and Milk River...
Journal Article
Published: 01 June 1991
Bulletin of Canadian Petroleum Geology (1991) 39 (2): 206.
... Basin. SED2 BHATTACHARYA, J., Alberta Geological Survey, Edmonton, Alberta T6H 5X2 Parasequence architecture of the Upper Cretaceous Chungo Member and Milk River Formation in southern Alberta The Campanian Chungo Member of the Wapiabi Formation in the Foothills and the equivalent Milk River Formation...
Journal Article
Published: 01 June 1993
Bulletin of Canadian Petroleum Geology (1993) 41 (2): 186–217.
... Jerzykiewicz and McLean, 1980). Note location of the study area. Horizontal extent is approximately 420 km. by Stott (1963) of which the Chungo and Nomad are the most significant in the context of the present study. In the outcrop belt of the study area the Chungo Member sandstones are signi- ficant because...
Journal Article
Published: 01 June 1991
Bulletin of Canadian Petroleum Geology (1991) 39 (2): 205.
... and a potential unconventional hydrocarbon reservoir in the Bass Basin. SED2 BHATTACHARYA, J., Alberta Geological Survey, Edmonton, Alberta T6H 5X2 Parasequence architecture of the Upper Cretaceous Chungo Member and Milk River Formation in southern Alberta The Campanian Chungo Member of the Wapiabi Formation...
Image
Generalized section of Brazeau structure south of <span class="search-highlight">Chungo</span> Creek. Formation c...
Published: 01 November 1951
FIG. 4. Generalized section of Brazeau structure south of Chungo Creek. Formation contacts, light solid lines; members shown by dashed lines. Faults, heavy solid lines; arrows in direction of movement.
Journal Article
Published: 01 June 2004
Bulletin of Canadian Petroleum Geology (2004) 52 (2): 139–155.
... Formation, in the Foothills south of the Bow River, Stott (1963) recognized the Chungo and Nomad members, which he interpreted as equivalent respectively to the Milk River and Pakowki formations in the Plains to the east. Working along and south of the Bow River, Rosenthal and Walker (1987) recognized...
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Journal Article
Journal: AAPG Bulletin
Published: 01 November 1951
AAPG Bulletin (1951) 35 (11): 2316–2347.
...FIG. 4. Generalized section of Brazeau structure south of Chungo Creek. Formation contacts, light solid lines; members shown by dashed lines. Faults, heavy solid lines; arrows in direction of movement. ...
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Journal Article
Published: 01 March 1990
Bulletin of Canadian Petroleum Geology (1990) 38 (1): 78–88.
... of the type area in the Plains. South of Smoky River Stott, 1963 North of Smoky River Stott, 1967 WAPITI Frnn. Nomad Mbr. z Nomad Mbr. 0 l- Chungo Mbr. ~ Chungo Mbr. 0 z Hanson Mbt Hanson Mbr. 0 ~ ~ Thistle Mbr. Thistle Mbr. D Dowling Mbr. ~ Dowling Mbr. a. a_ 0 ~ ~i , ¢: E oi ~ Marshybank a: Bad Heart Member...
Image
Looking north across Canyon Creek in the fault complex of the northeast fla...
Published: 01 November 1951
FIG. 7. Looking north across Canyon Creek in the fault complex of the northeast flank of Chungo anticline. The three prominent light-colored sandstone bands are repetitions of the basal member of the Cardium formation in the three upper thrust plates of Figure 5 . The two at the right were
Journal Article
Published: 01 September 1981
Bulletin of Canadian Petroleum Geology (1981) 29 (3): 334–377.
...-grey mudstone beds below the contact are strongly calcareous, whereas above they are weakly calcareous or noncalcareous. However, in sections at Ruby Creek, Chungo Creek, Gap Lake and Fall Creek (Fig. 2), strongly calcare- ous mudstone beds were observed within the Moosebar Member as well, although...
Journal Article
Published: 01 August 1977
Bulletin of Canadian Petroleum Geology (1977) 25 (4): 842–867.
..., Highwood and Sheep Rivers, as will 'be shown below. The type section of the Nomad Member is on a tributary of the Cardinal River in the central Foothills and consists of shales and siltstones lying between the fine-grained sands or siltstones of the Chungo Member of the Wapiabi and the coarse-grained...
Journal Article
Published: 01 June 1996
Bulletin of Canadian Petroleum Geology (1996) 44 (2): 282–298.
...). It dips about 20 ° to the NE and appears to be rooted below the Chungo Member in the Wapiabi Fornnation. The hanging walt cut off of the top of the Wapiabi Formation is not exposed at surface, and the corresponding footwalt cut- off is situated at about l km depth. This limits the amount of displacement...
Journal Article
Published: 01 January 2014
Journal of Paleontology (2014) 88 (1): 187–194.
... Formation is currently divided in five members, in ascending order: Dowling, Thistle, Hanson, Chungo, and Nomad ( Hu and Plint, 2009 ) ( Fig. 2 ). Relevant to this study, the sandy Chungo Member and the overlying, mudstone and siltstone-dominated Nomad Member have been assigned an early Campanian age based...
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Journal Article
Journal: Geology
Published: 01 December 2006
Geology (2006) 34 (12): 1073–1076.
... stratification : Journal of Sedimentary Petrology , v. 60 p. 211 – 219 . Arnott , R.W.C. , 1992 , Ripple cross-stratification in swaley cross-stratified sandstones of the Chungo Member, Mount Yamnuska, Alberta : Canadian Journal of Earth Sciences , v. 29 p. 1802 – 1805 . Cheel , R.J...
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