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Sully Formation

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Journal Article
Published: 01 August 1983
Canadian Journal of Earth Sciences (1983) 20 (8): 1248–1259.
...C. R. Stelck; A. S. Hedinger Abstract An extensive microfauna of over 25 genera and 40 species of arenaceous foraminifera occurs in the lower Sully Formation on the Sikanni Chief River and consists of Bathysiphon spp., Hyperammina sp., Saccammina spp., Lituotuba ? sp., Glomospira sp., Ammodiscus sp...
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Outcrop in bank along Petitot River ( Fig. 15 ) showing Fish Scales marker ...
Published: 27 September 2022
Fig. 17. Outcrop in bank along Petitot River ( Fig. 15 ) showing Fish Scales marker unit in the Sully Formation. The Fish Scales unit marks the transition from east-derived sediment below to west-derived sediment above. The Sully Formation is a stratigraphic equivalent of the Shaftesbury
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( a ) Dunvegan <span class="search-highlight">Formation</span> marks the boundary of the sedimentary deposits wit...
Published: 14 July 2022
Formation and underlying Sully Formation based on data from Douglas and Norris (1976) , Stott (1982) and data from this study.
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Hayden’s exploring routes (1853 to 1866) in what was Nebraska (established ...
Published: 01 October 2021
route has not been verified. Hayden and Sully are associated with acquisition of a Lance [= Hell Creek] Formation hadrosaur Thespesius occidentalis named by Leidy ( 1859 [1860]); now considered nomen dubium) to be from the Grand River area (see Lull and Wright, 1942 , Locality 38). Fryxell’s (2010
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Eroded headland on the east side of <span class="search-highlight">Sully</span> Island, South Wales. Note the lac...
Published: 01 May 2007
Figure 7. Eroded headland on the east side of Sully Island, South Wales. Note the lack of debris on the raised platform surface, compared to surfaces lower down and more exposed to wave action. The bench at the top of the Carboniferous limestone lies above the limit of highest tides. We postulate
Journal Article
Published: 14 July 2022
Canadian Journal of Earth Sciences (2022) 59 (12): 984–1005.
... Formation and underlying Sully Formation based on data from Douglas and Norris (1976) , Stott (1982) and data from this study. ...
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—Measured sections (e.g., L19) of the Chinkeh <span class="search-highlight">Formation</span>. The type section o...
Published: 01 August 1991
Figure 9 —Measured sections (e.g., L19) of the Chinkeh Formation. The type section of the Liard Formation is Section L14 and the reference section is L19 a and b. Inset shows general locations of sections around the Liard basin. Detailed locations are shown in Figure 1 . Map sheet, geographic
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West–east correlation of lower member of the Domengine <span class="search-highlight">Formation</span> in the Gre...
Published: 01 October 2012
Fig 7 West–east correlation of lower member of the Domengine Formation in the Greathouse and Hazel Atlas adits at Somersville (see Fig. 4 for location). Only the upper 200 feet (60 meters) of the member was mined for glass sand in these two adits. The sections can be correlated using the Clark
Journal Article
Published: 01 September 2003
Bulletin of Canadian Petroleum Geology (2003) 51 (3): 234–252.
... and from the overlying Sikanni and lower Sully formations ( Stelck, 1975 ; Stelck and Hedinger, 1983 ). These reported a diverse foraminiferal assemblage from the upper interval of the Buckinghorse Formation, indicating the latest Albian Miliammina manitobensis Zone. Microflora of the same interval...
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Journal Article
Journal: AAPG Bulletin
Published: 01 December 1950
AAPG Bulletin (1950) 34 (12): 2337–2346.
... of the Stratigraphic Code. Three subdivisions of the Sully member, as used by the South Dakota Geological Survey, have been raised to member rank and the term Sully has been discarded. The Agency-Oacoma zone of Gries has been redefined and renamed the DeGrey member of the Pierre shale. Searight (1937 , p. 21...
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Journal Article
Journal: AAPG Bulletin
Published: 01 September 2005
AAPG Bulletin (2005) 89 (9): 1113–1137.
.... (2003) , offsets a sandstone-shale sequence that is part of the 230–260-m (754–853-ft)-thick Domengine Formation of middle Eocene age ( Sullivan et al., 1994 , 2003 ). The 185-m (606-ft)-thick lower member of this formation is composed of cross-bedded estuarine subtidal sandstone that is interbedded...
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Journal Article
Published: 01 June 1977
Bulletin of Canadian Petroleum Geology (1977) 25 (3): 631–634.
... equivalent. At the Sully Creek locality the palynologic assemblage was similar although in situ forms were more abundant. Regional studies of the Mattson indicate that it has eroded to the east and north and that it thickens and is overlain by the Fantasque Formation (Permian) to the southwest and south...
Journal Article
Published: 01 July 2015
Bulletin de la Société Géologique de France (2015) 186 (4-5): 273–290.
...Maurizio Gasparo Morticelli; Vera Valenti; Raimondo Catalano; Attilio Sulli; Mauro Agate; Giuseppe Avellone; Cinzia Albanese; Luca Basilone; Calogero Gugliotta Abstract Neogene-Quaternary wedge-top-basins arose during the Sicilian fold and thrust belt (FTB) build-up. The infilling sedimentary...
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Journal Article
Journal: AAPG Bulletin
Published: 01 July 1948
AAPG Bulletin (1948) 32 (7): 1265–1274.
...Roland W. Brown ABSTRACT New stratigraphic and paleontologic evidence indicates that the Sentinel Butte shale, lately considered by some geologists to be of Wasatch (Eocene) age, is, as originally described and assigned, a dark sequence of strata in the upper part of the Fort Union formation...
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Journal Article
Published: 01 June 1997
Bulletin of Canadian Petroleum Geology (1997) 45 (2): 178–193.
... Slave Plain but only west of about 119°W, just west of the Cameron Hills. In the type area of northeast British Columbia, Fort St. John strata consist of the following formations (bottom to top): Chinkeh (sandstone), Garbutt (shale), Scatter (sandstone), Lepine (shale), Sikanni (sandstone) and Sully...
Journal Article
Published: 01 May 2007
The Journal of Geology (2007) 115 (3): 253–269.
...Figure 7. Eroded headland on the east side of Sully Island, South Wales. Note the lack of debris on the raised platform surface, compared to surfaces lower down and more exposed to wave action. The bench at the top of the Carboniferous limestone lies above the limit of highest tides. We postulate...
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Journal Article
Published: 01 February 2020
Italian Journal of Geosciences (2020) 139 (1): 54–75.
... sedimentary sequences results in the formation of submarine topographical highs, capped by iron-manganese oxide crusts and condensed pelagic sequences, and adjacent slope-to-basinal areas with pelagic succession associated to igneous activity (pillow lavas and diabase dykes, M ascle , 1979 ; B ellia et...
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Journal Article
Journal: PALAIOS
Published: 01 August 2000
PALAIOS (2000) 15 (4): 356–362.
... to 13 beds in the newly studied section of Bretteville (Fig. 1) . The boundary of the OFB with the overlying formation (“Calcaires à Spongiaires”) may be transitional similar to that seen at Sully, or sharp where it corresponds to another omission surface as at Bretteville (Fig. 2) . The great...
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Journal Article
Journal: AAPG Bulletin
Published: 01 September 1948
AAPG Bulletin (1948) 32 (9): 1823–1824.
... reduced to an horizon at the top of a prominent “Marker bed” labelled “SS21” which is a distinctive silicified tree-bearing zone. Dr. Brown takes particular issue with the writer’s correlation of this bed from Sentinel Butte (Point 1 on Profile, Fig. 1) to Sully Springs Railroad station (Point 3...
Journal Article
Published: 30 January 2014
Journal of the Geological Society (2014) 171 (2): 211–226.
... . Gugliotta C. Agate M. Sulli A. 2013 . Sedimentology and sequence stratigraphy of wedge-top clastic successions: Insights and open questions from the upper Tortonian Terravecchia Formation of the Scillato Basin (central–northern Sicily, Italy) . Marine and Petroleum Geology , 43 , 239...
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