1-20 OF 75 RESULTS FOR

Big Coulee Fault

Results shown limited to content with bounding coordinates.
Follow your search
Access your saved searches in your account

Would you like to receive an alert when new items match your search?
Close Modal
Sort by
Journal Article
Published: 01 March 1996
Bulletin of Canadian Petroleum Geology (1996) 44 (1): 1–13.
...-verging allochthonous wedge of Mesozoic rocks, overlain by west-verging thrust sheets of Upper Cretaceous and Tertiary rocks, and underlain by undeformed Paleozoic strata. The Big Coulee Fault, which rides within the Bearpaw Formation, represents the boundary between east- and west-verging structures...
Journal Article
Published: 01 June 1996
Bulletin of Canadian Petroleum Geology (1996) 44 (2): 202–214.
... (the Big Coulee Fault). RÉSUMÉ Les nouvelles cartes structurelles et interprétations sismiques indiquent que la zone triangulaire et les structures connexes exposées le long et adjacent à Oldman River, au sud des Foothills de l’Alberta, englobent une structure compliquée impliquant une déformation...
Journal Article
Journal: AAPG Bulletin
Published: 15 April 2020
AAPG Bulletin (2020) 104 (4): 767–793.
... basement. This strike-slip system may be secondary to the regional left-lateral Brockton-Froid fault zone, which lies to the north of the study area. The fracture network in the Elm Coulee field is likely to be enhanced around such antiformal structures, providing a plausible explanation for the locations...
FIGURES | View All (18)
Series: GSA Field Guides, GSA Field Guides
Published: 01 January 2017
DOI: 10.1130/2017.0049(08)
EISBN: 9780813756493
... of the several dozen gigantic late Wisconsin floods (and doubtless pre-Wisconsin ones) that did most of the erosional work. Collectively they excavated more of the coulee, finishing carving of scabland about the coulee’s head. Within upper and lower Grand Coulee, the late Wisconsin floods left sporadic big...
FIGURES | View All (27)
Journal Article
Published: 01 June 2015
Bulletin of Canadian Petroleum Geology (2015) 63 (2): 192–223.
... Three Forks-Bakken petroleum reservoirs are related to basement fault systems and/or dissolution of older evaporite beds overlying the basement faults and occurring simultaneously with fault movements ( Wright et al. 1994 ; Sonnenberg and Pramudito, 2009 ). The lower Big Valley shoal deposits...
FIGURES | View All (27)
Journal Article
Journal: Geosphere
Published: 01 June 2015
Geosphere (2015) 11 (3): 542–562.
...William Hutchison; Tamsin A. Mather; David M. Pyle; Juliet Biggs; Gezahegn Yirgu Abstract In volcanically and seismically active rift systems, preexisting faults may control the rise and eruption of magma, and direct the flow of hydrothermal fluids and gas in the subsurface. Using high-resolution...
FIGURES | View All (12)
Journal Article
Journal: AAPG Bulletin
Published: 01 October 1966
AAPG Bulletin (1966) 50 (10): 2245–2259.
... in the Lower member of the Tyler Formation. Reconstruction of the pre-Amsden structure and the Tyler-Heath paleogeology shows that oil accumulations at Sumatra, Stensvad, Ivanhoe, Keg Coulee, Bascom, Melstone, and Big Wall fields occur where the paleostructural position of the lower Tyler sandstone beds...
FIGURES | View All (20)
Journal Article
Journal: GSA Bulletin
Published: 06 May 2020
GSA Bulletin (2021) 133 (1-2): 115–133.
... of the Yakima or to the SE beyond Badger Coulee ( Fig. 3 ). Well-log data obtained from the City of Richland, Washington, show that the frontal fault zone on the Yakima Bluffs dips ∼30° to the SW at the Duportail Bridge site ( Figs. 3 and 5 ). The frontal fault forms an emergent fault that extends from...
FIGURES | View All (17)
Journal Article
Journal: AAPG Bulletin
Published: 01 November 1965
AAPG Bulletin (1965) 49 (11): 1824–1832.
... Belt Mountains on the west to Porcupine dome on the east. The regional structural features are ( Fig. 2 ) the Central Montana uplift and the Lake Basin-Huntley fault zone. Some of the more prominent local features here discussed are Judith basin, Little Belt Mountains, Shawmut anticlinal trend, Big...
FIGURES | View All (19)
Journal Article
Published: 29 November 2000
Canadian Journal of Earth Sciences (2001) 38 (1): 1–19.
... Coulée Formation, which are unconformably overlain by the Bonaventure Formation, have also been recognized underlying, with a similar type of contact, the Lower Member of the Cannes-de-Roches Formation. From this and from facies similarities, the Lower and Middle members of the Cannes-de-Roches Formation...
FIGURES | View All (17)
Series: AAPG Memoir
Published: 01 January 2017
DOI: 10.1306/13572002M113508
EISBN: 9781629812762
... in large parts of the central basin and the Parshall area in the east, where gradients exceed 0.7 psi/ft. Elm Coulee has a pressure gradient around 0.55 psi/ft. Parshall is reported to have a gradient of 0.74 psi/ft. The area west of the Nesson anticline has pressure gradients of 0.6 to 0.7 psi/ft...
FIGURES | View All (51)
Journal Article
Journal: AAPG Bulletin
Published: 01 July 1974
AAPG Bulletin (1974) 58 (7): 1305–1322.
... boundary of the Cat Creek block, etc . Other major features also terminate against major lineaments. Kevin-Sunburst dome, Poplar dome, Wibaux nose, Rough Rider ridge, Porcupine dome, Big Coulee dome, the Bighorn Mountains, and the Reed Point syncline all start or stop against the lineaments...
FIGURES | View All (13)
Image
Line drawing of a composite seismic line acquired along Willow Creek across...
Published: 01 December 2001
and merges to the east with the triangle zone upper detachment, the Big Coulee Fault (BCF).
Journal Article
Journal: Geosphere
Published: 01 December 2012
Geosphere (2012) 8 (6): 1527–1567.
... in the 11th hour of the 60-h-long eruption and continued fitfully for 3.5 days. Several big landslides and pumiceous debris flows shaken loose by the collapse-related seismicity are bracketed in time by their levels of intercalation within the Novarupta pumice-fall sequence. An intracaldera lake was ∼10 m...
FIGURES | View All (42)
Image
Reinterpretation of seismic reflection data originally interpreted by  Lawt...
Published: 01 December 2001
Formation, M = Mississippian, BCF = Big Coulee Fault, CF = Co-op Fault, WF = Waldron Fault, CCF = Callum Creek Fault. Seismic line location indicated in Figures 5 and 8 . Top: migrated uninterpreted section. Bottom: interpreted section. See text for discussion.
Journal Article
Journal: AAPG Bulletin
Published: 01 January 1953
AAPG Bulletin (1953) 37 (1): 1–113.
.... North of the Emeq is Galilee, a highland area of ridges, mountains, and narrow valleys, with the Upper Jordan Valley on the east and the coastal plain on the west. Structural differences divide the country into eight geologic provinces: (1) the Dead Sea-Wadi Araba graben, with faulted anticlines...
FIGURES | View All (64)
Journal Article
Journal: Geosphere
Published: 01 August 2012
Geosphere (2012) 8 (4): 740–751.
... ). The anomalous volume and frequency of magmatism in the Long Valley area compared to other late Quaternary (e.g., Big Pine, Coso) volcanic fields along the eastern Sierra Nevada ( Fig. 1 ) suggest that some tectonic process results in localized magmatic intensification. The Sierra Nevada frontal fault system...
FIGURES | View All (7)
Series: GSA Field Guide
Published: 01 January 2009
DOI: 10.1130/2009.fld015(21)
EISBN: 9780813756158
... of silicic eruptive centers. The rhyolitic rocks generally are successively younger to the northwest, describing a mirror image to the basalt plateau and rhyolite age progression of the Snake River Plain. The High Lava Plains is associated with a zone of numerous, small northwest-striking faults and lies...
Journal Article
Published: 01 December 2001
Bulletin of Canadian Petroleum Geology (2001) 49 (4): 472–496.
... and merges to the east with the triangle zone upper detachment, the Big Coulee Fault (BCF). ...
FIGURES | View All (32)
Journal Article
Journal: Geosphere
Published: 01 December 2014
Geosphere (2014) 10 (6): 1315–1365.
... prebatholith wall rocks. All of the many mafic and silicic vents of the Mammoth system are west or southwest of the structural boundary of Long Valley caldera; none is inboard of the caldera’s buried ring-fault zone, and only one Mammoth-related vent is within the zone. Mammoth Mountain has sometimes been...
FIGURES | View All (36)