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Deer Creek formation

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Journal Article
Published: 25 January 2019
Canadian Journal of Earth Sciences (2019) 56 (10): 1041–1051.
...–ID–TIMS age of 66.936 ± 0.047/0.060/0.140 Ma for the Battle bentonite, an altered vitric ash in the upper portion of the BFm at Knudsen’s Farm in the Red Deer River valley of Alberta. This age supersedes those previously reported, confirms that rates of sediment accumulation for the formation were...
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—Diagrammatic cross section of Deer Creek formation north of Huerfano River, Sec. 23–24, T. 27 S., R. 72 W.
Published: 01 August 1959
Fig. 7. —Diagrammatic cross section of Deer Creek formation north of Huerfano River, Sec. 23–24, T. 27 S., R. 72 W.
Journal Article
Journal: AAPG Bulletin
Published: 01 August 1959
AAPG Bulletin (1959) 43 (8): 1896–1939.
...Fig. 7. —Diagrammatic cross section of Deer Creek formation north of Huerfano River, Sec. 23–24, T. 27 S., R. 72 W. ...
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Published: 01 September 2003
Appendix II: Reference to outcrop locations of the Carlile Formation along Deer Creek on the east side of East Butte of Sweetgrass Hills in northern Montana.
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Thrust on north side of Deer Creek Peak. King Lear formation (Kkl) overlies andesite (pK) and is overlain by Pansy Lee conglomerate (TKp). Andesitic flows, flow-breccias, and agglomerates (pK) are exposed on upper plate of thrust. Half mile from Deer Creek Peak to Kkl-pK contact.
Published: 01 October 1958
Fig. 10. Thrust on north side of Deer Creek Peak. King Lear formation (Kkl) overlies andesite (pK) and is overlain by Pansy Lee conglomerate (TKp). Andesitic flows, flow-breccias, and agglomerates (pK) are exposed on upper plate of thrust. Half mile from Deer Creek Peak to Kkl-pK contact.
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A. Van Krevelen diagrams of sediments from the Carlile and Niobrara formations sampled at Deer Creek, Montana and from the well 13-20-17-7W4. B. Van Krevelen diagram of the three informal units of the Carlile Formation from the Deer Creek outcrop.
Published: 01 September 2003
Fig. 10. A. Van Krevelen diagrams of sediments from the Carlile and Niobrara formations sampled at Deer Creek, Montana and from the well 13-20-17-7W4. B. Van Krevelen diagram of the three informal units of the Carlile Formation from the Deer Creek outcrop.
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Scanning electron photomicrographs: (A) authigenic pore-lining smectite; (sample Kn-5, lower Scollard Formation, Kneehills Creek locality); (B) vermicular authigenic kaolinite (sample Kn-3, lower Scollard Formation, Kneehills Creek locality); (C) late diagenetic chlorite (sample 7, upper Coalspur Formation, Red Deer River locality); (D) authigenic chlorite/smectite clay (sample 8, upper Coalspur Formation, Red Deer River locality); (E) dickite formation during deep burial (sample C-2, lower Willow Creek Formation, Crowsnest River locality); (F) authigenic illite formed as a late diagenetic clay (sample 7, upper Willow Creek Formation, Oldman Dam Reservoir locality).
Published: 01 September 2009
, upper Coalspur Formation, Red Deer River locality); (D) authigenic chlorite/smectite clay (sample 8, upper Coalspur Formation, Red Deer River locality); (E) dickite formation during deep burial (sample C-2, lower Willow Creek Formation, Crowsnest River locality); (F) authigenic illite formed as a late
Journal Article
Journal: Geosphere
Published: 01 October 2021
Geosphere (2021) 17 (6): 1715–1744.
... landslides are subsequent slides that consist of debris from the primary slides; these also partially blocked and diverted the Colorado River as well as the Deer Creek and Tapeats Creek tributaries into new bedrock gorges over the past 1 m.y. The sequence of landslides is reconstructed from inset...
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Reflected-light images of fossils from the Fernie Formation at Ya Ha Tinda Ranch. A) Pavement of the scallop bivalve Ochotochlamys (TMP2015.050.0005; Pliensbachian, 2 m in section, Red Deer Member, East Tributary). B) The scallop bivalve Camptonectes (TMP2015.051.0076; 1.2–1.6 m in section, Scalp Creek). C) The true oyster bivalve Liostrea (part, TMP2015.051.0098a; Toarcian, Poker Chip Shale Member, Scalp Creek). D) Ammonite (TMP2015.051.0050; 1.2–1.6 m in section, Scalp Creek). E) Inoceramid bivalve (TMP2015.050.0256; Toarcian, 10.5 m in section, Red Deer Member, East Tributary). F) Wood (TMP2015.051.0061; Scalp Creek). G) A mussel bivalve of the Order Mytilida (TMP2015.051.0077; 1.2–1.6 m in section, Scalp Creek). H) The scallop bivalve Meleagrinella (counterpart TMP2015.051.0108b; 1.2–1.6 m in section, Scalp Creek). I) Rhynchonellid brachiopod (TMP2015.050.0007; Pliensbachian, Red Deer Member, East Tributary). J) The linguliformean (inarticulate) brachiopod Discinisca (TMP2015.050.0254; Toarcian, 14.6 m in section, Poker Chip Shale, East Tributary). K) Ammonite (TMP2015.050.0067; Pliensbachian, Red Deer Member, East Tributary). L) Belemnites left in outcrop (Red Deer Member, East Tributary). M) Coleoid gladii with ink sac (TMP2015.050.0257; 10.26 m in section, Red Deer Member, East Tributary). N) Two decapod crustacean arms (TMP2015.050.0258; Toarcian, 10.50 m in section, Red Deer Member, East Tributary). O) Claw of the decapod crustacean Uncina pacifica (TMP2018.024.0003; Red Deer Member, East Tributary). P) Tail of a decapod crustacean (TMP2018.024.0001; Red Deer Member, East Tributary). Q) U-shaped burrow trace fossil Arenicolites left in outcrop (9 m, Red Deer Member, East Tributary). R) Fish (Actinopterygii) vertebrae, ribs, and tail (TMP2015.051.0118; Toarcian, 1.2–1.6 m in section, Poker Chip Shale Member, Scalp Creek). S) Fish (Actinopterygii) ribs and fins (TMP2015.050.0065; Pliensbachian, Red Deer Member, East Tributary). T) Articulated fish (Actinopterygii, likely Leptolepis sp.) with skull, vertebrae, ribs, fins, and gill arches (part, TMP2014.021.0043a; Toarcian, 16 m, Poker Chip Shale Member, East Tributary).
Published: 04 November 2019
Fig. 3.— Reflected-light images of fossils from the Fernie Formation at Ya Ha Tinda Ranch. A ) Pavement of the scallop bivalve Ochotochlamys (TMP2015.050.0005; Pliensbachian, 2 m in section, Red Deer Member, East Tributary). B ) The scallop bivalve Camptonectes (TMP2015.051.0076; 1.2–1.6 m
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Scanning electron photomicrographs: (A) euhedral growth of authigenic albite (sample D-1, lower Willow Creek Formation, Crowsnest River locality); (B) euhedral growth of authigenic quartz (sample 14, upper Scollard Formation, Red Deer River section 1); (C) intercalation of dickite crystals between stacks of partly dissolved kaolin plates which suggests that the sandstones underwent 3 to 4 km of burial (Lanson et al., 2002); (sample A-3, lower Willow Creek Formation, Oldman Reservoir Dam locality); (D) fibrous authigenic illite on corroded feldspar grains (sample F-3, upper Willow Creek Formation, Oldman Dam Reservoir locality); (E) authigenic illite. Note the fibrous nature of the authigenic illite (sample G-2, Willow Creek Formation, Crowsnest River locality); (F) complete conversion of authigenic smectite to chlorite, and euhedral quartz overgrowth (sample 10, upper Coalspur Formation, Red Deer River locality).
Published: 01 September 2009
Fig. 23. Scanning electron photomicrographs: (A) euhedral growth of authigenic albite (sample D-1, lower Willow Creek Formation, Crowsnest River locality); (B) euhedral growth of authigenic quartz (sample 14, upper Scollard Formation, Red Deer River section 1); (C) intercalation of dickite
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Map of Bighorn Basin showing the distribution of the basin and surrounding mountains as well as the location of Upper Deer Creek section (redrawn after Smith et al., 2008; Neasham and Vondra, 1972). The Willwood Formation in the center of the Bighorn Basin is shown in light gray with paleocurrent direction marked. The studied Upper Deer Creek section is located north of Bighorn Basin. Inset: The localities of studied Paleocene-Eocene Thermal Maximum (PETM) sections in Utah (UT) and North Dakota (ND) are indicated.
Published: 01 July 2017
Figure 1. Map of Bighorn Basin showing the distribution of the basin and surrounding mountains as well as the location of Upper Deer Creek section (redrawn after Smith et al., 2008 ; Neasham and Vondra, 1972 ). The Willwood Formation in the center of the Bighorn Basin is shown in light gray
Journal Article
Journal: AAPG Bulletin
Published: 01 November 1936
AAPG Bulletin (1936) 20 (11): 1454–1475.
... to avoid lengthy descriptions, detailed columnar sections have been arranged to show the gradations and relative positions of the sediments below the Marlow overlap. The Vamoosa formation overlaps southward. The continuous limestone which separates the Vamoosa from the Pontotoc terrane is the Deer Creek...
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Journal Article
Journal: GSA Bulletin
Published: 01 January 1914
GSA Bulletin (1914) 25 (1): 355–380.
... Pierre (upper), Belly River (intercalation). Fort Pierre (upper) of Red Deer River, Alberta 1909–1913 Ojo Alamo formation of northern New Mexico 1904 Lance Creek formation of Converse County, Wyoming 1900–1901 I have determined the geologic sequence in each of these formations and the succession...
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Location maps of the reference section for the Carlile Formation. A. Overview of the Sweetgrass Hills with location of the type section of the Ferdig Member, Carlile Formation reference section, Wireline logs at 10-7-1-8W4 and 13-20-17-7W4. B. Detailed map of the location of the Deer Creek outcrop.
Published: 01 September 2003
Fig. 9. Location maps of the reference section for the Carlile Formation. A. Overview of the Sweetgrass Hills with location of the type section of the Ferdig Member, Carlile Formation reference section, Wireline logs at 10-7-1-8W4 and 13-20-17-7W4. B. Detailed map of the location of the Deer
Journal Article
Journal: AAPG Bulletin
Published: 01 July 1984
AAPG Bulletin (1984) 68 (7): 939.
...John S. Isby; M. Dane Picard ABSTRACT The Currant Creek Formation is composed of conglomerate, sandstone, and fine-grained clastic rocks that crop out along the northwestern margin of the Uinta basin in north-central Utah. Lateral gradations in grain size define proximal, medial, and distal parts...
Journal Article
Journal: AAPG Bulletin
Published: 01 May 1974
AAPG Bulletin (1974) 58 (5): 914–915.
...L. T. MacMillan Abstract Previous workers have delineated deltaic sedimentation from a western source within the South Platte Formation. Outcrop studies in the Morrison-Deer Creek area provide a model for sedimentation within the region of maximum channel development of the South Platte Formation...
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(a) Geologic map of the Cypress Hills area of southeastern Alberta, showing formational boundaries and locations of subsections studied. A, Elkwater core hole; B1 and B2, Medicine Lodge Coulee sections; C, Thelma Creek section; D, Thelma core hole; E, Manyberries section; 6, Dinosaur Park Formation; 7, Bearpaw Formation; 8, Eastend Formation; 9, Whitemud and Battle formations; 10, Frenchman Formation; 11, Ravenscrag Formation; 12, Cypress Hills Formation. Geology from Irish (1967) with small Whitemud and Battle formation areas omitted. (b) Red Deer Valley area east of Drumheller, showing location of sections studied in the Bearpaw Formation. D, Dorothy section; EC, East Coulee section; WC, Willow Creek section.
Published: 15 April 2002
Fig. 1. ( a ) Geologic map of the Cypress Hills area of southeastern Alberta, showing formational boundaries and locations of subsections studied. A, Elkwater core hole; B1 and B2, Medicine Lodge Coulee sections; C, Thelma Creek section; D, Thelma core hole; E, Manyberries section; 6, Dinosaur
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Outcrop along Deer Creek on the eastern side of the Sweetgrass Hills, Montana (Outcrop 7, see Appendix II and Fig. 9 for location). The outcrop shows the upper unit of Carlile Formation and the boundary to the Niobrara Formation. The unit is dominated by shale and siltstone, but two upward-coarsening intervals are observed. The boundary to the Niobrara Formation is placed just below the thick (up to 50 cm) concretions seen in the top of the photo.
Published: 01 September 2003
Fig. 13. Outcrop along Deer Creek on the eastern side of the Sweetgrass Hills, Montana (Outcrop 7, see Appendix II and Fig. 9 for location). The outcrop shows the upper unit of Carlile Formation and the boundary to the Niobrara Formation. The unit is dominated by shale and siltstone, but two
Journal Article
Published: 01 August 1987
Canadian Journal of Earth Sciences (1987) 24 (8): 1688–1704.
...Russell L. Hall Abstract New ammonite faunas are described from sections along Bighorn and Scalp creeks in central-western Alberta where Lower Jurassic parts of the Fernie Formation are exposed. The first record of the upper Sinemurian Obtusum Zone from the Fernie is based on the occurrence...
Journal Article
Published: 01 September 2003
Bulletin of Canadian Petroleum Geology (2003) 51 (3): 304–346.
...Appendix II: Reference to outcrop locations of the Carlile Formation along Deer Creek on the east side of East Butte of Sweetgrass Hills in northern Montana. ...
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