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Bug Creek valley

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Journal Article
Journal: Geology
Published: 01 April 1986
Geology (1986) 14 (4): 279–282.
...David E. Fastovsky; Robert H Dott, Jr. Abstract Bug Creek Valley, the source of an unusual and controversial Cretaceous-Paleogene coincidence of mammals, dinosaurs, pollen, and indium, exemplifies the importance of depositional process in the reconstruction of evolutionary events. Five sedimentary...
Series: GSA Special Papers
Published: 01 January 2014
DOI: 10.1130/2014.2503(02)
... In 1907, Barnum Brown named the Hell Creek beds (Formation) for the strata exposed in the Hell Creek Valley and other downstream tributaries of the Missouri River. In the absence of a stratotype section, a lectostratotype is herein proposed for the Hell Creek Formation based on 84.2-m-thick...
Journal Article
Journal: AAPG Bulletin
Published: 01 October 1981
AAPG Bulletin (1981) 65 (10): 1840–1842.
... and 681 bbl condensate/d from commingled Mississippian, Pennsylvanian, and Permian reservoirs. In southeastern Utah, Wexpro Company opened the Bug field with the 1 Bug well that flowed 608 bbl/d and 1,128 mcf gas/d from the Middle Pennsylvanian Desert Creek pay (Paradox). By year’s end, Bug field had five...
FIGURES
Journal Article
Journal: GSA Bulletin
Published: 01 March 2015
GSA Bulletin (2015) 127 (3-4): 393–409.
.... In the eastern part of our field area, primarily in McCone County, the base of the Tullock Member is exposed in the area between the valley of Bug Creek and, to the south, the valley of McGuire Creek. For over a century, the valley of Bug Creek has been a focus of paleontological, and later, beginning...
FIGURES | View All (7)
Journal Article
Journal: GSA Bulletin
Published: 02 August 2021
GSA Bulletin (2021)
... downstream at Kennedy Table, Bug Table (BT), Squaw Leap (SL), McKenzie Table (MT), Table Mountain (TM), Perkins West Table (PWT), and as a chain of remnants near Little Dry Creek (LDC); see Figures 2 5. Elevations: Mammoth Crest 3100 3500 m; Takt vent (top) 2805 m; Fish Creek confluence 1630 m; South Fork...
Journal Article
Journal: GSA Bulletin
Published: 01 January 2009
GSA Bulletin (2009) 121 (1-2): 65–79.
... the Ludlow Member of the Fort Union Formation. K hc —Hell Creek Formation, T lm —Ludlow Member, T tr —Tongue River Member, T sb —Sentinel Butte Member, T gv —Golden Valley Formation. (C) Generalized stratigraphy of Paleocene and Eocene section of the Williston Basin in southwestern North Dakota. BB—Bighorn...
FIGURES | View All (12)
Journal Article
Journal: AAPG Bulletin
Published: 01 June 1992
AAPG Bulletin (1992) 76 (6): 851–863.
.... Production at Bug field is from a stratigraphic trap in the Pennsylvanian Honaker Trail Formation and the Desert Creek member of the Paradox Formation. Patterson Canyon production is from an algal mound in the Ismay member of the Paradox Formation. Production at Cave Canyon is from a depth of 4000-6000 ft...
FIGURES | View All (16)
Journal Article
Published: 07 December 2020
Canadian Journal of Earth Sciences (2021) 58 (9): 936–967.
... localities (3–5) are denoted by solid black circles (including the temporally mixed Bug Creek Anthills locality); Paleocene localities (1–2) are denoted by open circles; the Eocene locality (6) is denoted by a solid black square. Map created using Photoshop 6, base map data © Google 2020. Specimens...
FIGURES | View All (20)
Journal Article
Journal: GSA Bulletin
Published: 02 May 2018
GSA Bulletin (2018) 130 (9-10): 1615–1644.
...—Biscuit Butte, PL—Pearl Lake, HC—Hell Creek Marina Road (Lerbekmo), HX—Haxby Road, IS—Isaac Ranch, TR—Thomas Ranch, SC—Sandy Chicken, BC—Bug Creek, PH—Purgatory Hill, MC—McGuire Creek (Lofgren [LG] in Table 1 ), ZL—Z-Line, JC—Jack’s Channel. Figure is modified from Sprain et al. (2016) . Within...
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Journal Article
Published: 08 February 2008
Canadian Journal of Earth Sciences (2008) 45 (1): 83–98.
... (Fig.  3 ). East of the present terminus of Todd Glacier is west-facing Sage glacier (unofficial name) with a steep bedrock slope at its terminus. East-facing Two glacier (unofficial name) is located within the headwaters of Two glacier valley (unofficial name) and is the source of a small creek...
FIGURES | View All (13)
Journal Article
Published: 20 June 2018
Journal of Paleontology (2018) 92 (5): 896–910.
... surfaces of successive cusps are flat, and there is no overlap at the bases of successive cusps. Figure 4 Comparison of upper and lower first molars of Valenopsalis joyneri (Bug Creek Anthills locality, Hell Creek Formation, northeastern Montana, earliest Paleocene), Catopsalis kakwa n. sp...
FIGURES
Journal Article
Published: 01 July 2006
Journal of Paleontology (2006) 80 (4): 672–683.
..., 1982 : 127). This description agrees with that of Estes and Berberian (1970 : 32), who described the Lance Formation as representing “a wooded swamp habitat, with small to medium sized watercourses and some ponding.” Estes and Berberian (1970 : 32) noted that the Bug Creek Anthills locality...
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Journal Article
Journal: AAPG Bulletin
Published: 01 November 1982
AAPG Bulletin (1982) 66 (11): 1779–1783.
... of the Paradox basin, J. M. Huber completed the Squaw Creek field opener 3-43-1 Griffith (Sec. 3, T39N, R20W), flowing 208 BOPD and 750 MCFGD from the Desert Creek. The new field is located 3 mi northeast of Bug field (discovered in 1980 by Wexpro Co.), which also produces from the Desert Creek. Exploratory...
FIGURES
Journal Article
Journal: AAPG Bulletin
Published: 01 September 1980
AAPG Bulletin (1980) 64 (9): 1340–1344.
... in the United States. Drilling activity has remained relatively high in the Basin and Flange province, with 18 exploratory wells drilled in 1979. Almost all of these were located in the graben valleys where valley fill sediments and volcanic rocks were the objectives. With the discovery in Nevada...
FIGURES
Journal Article
Published: 22 December 2020
Geochemistry: Exploration, Environment, Analysis (2021) 21 (1): geochem2020-048.
... Hill and Ironclad pits Burnett (1995) Te Positive correlation Grassy Valley Rosdeutscher (1999) Ag, As, K, Sb, V, Cu, Mo, Si, Hg, Te Na Mn, Ba, Sr Au mineralization halo determined by factor analysis Negative correlation with Au Alteration halo determined by factor analysis Gold Bug...
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Journal Article
Journal: Economic Geology
Published: 01 December 2000
Economic Geology (2000) 95 (8): 1635–1656.
... mineralization relative to their neighboring greenstone-granite subprovinces. One notable exception is the Werner-Gordon-Rex-Bug Lake area in the Umfreville-Conifer Lake granulite zone of the western English River subprovince ( Fig. 1 ), where numerous occurrences of polymetallic mineralization (Co, Ni, Cu, Au...
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Journal Article
Published: 20 February 2001
Canadian Journal of Earth Sciences (2002) 39 (2): 207–221.
... ). To the northeast, along Swift Current Creek, the Frenchman–Battle is up to 55 m thick and also directly overlies the Bearpaw Formation, apparently representing continuation of this erosional valley ( Kupsch 1957 ). Consistent with this interpretation, the Frenchman–Battle thins to the west and to the east, rests...
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Journal Article
Published: 18 April 2013
Canadian Journal of Earth Sciences (2013) 50 (3): 341–354.
... designated the MCZ Coal, exposed in the valley of McGuire Creek, McCone County. This probably is the Z coal of Collier and Knechtel (1939) , which overlies a locality yielding a Pu1 local fauna ( Archibald and Lofgren 1990 ). Fm., Formation; HFZ, Hauso Flats Z Coal; IrZ, Iridium Z Coal; NALMA, North...
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Journal Article
Journal: GSA Bulletin
Published: 01 September 2011
GSA Bulletin (2011) 123 (9-10): 2083–2111.
... in the Cougar Creek complex record left-lateral mylonitic fabric development from 260 to 220 Ma, synchronous with igneous activity ( Kurz et al., 2009 ). Lower Permian to Upper Triassic volcanic rocks consist of keratophyre and spilite interbedded within volcaniclastic rocks (Seven Devils Group; Vallier, 1977...
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Journal Article
Journal: AAPG Bulletin
Published: 01 November 1946
AAPG Bulletin (1946) 30 (11): 1797–1829.
... shale of the Enid group of lower Permian age crops out in the entire area of the West Edmond field. With the exception of the valley of Deer Creek which runs from southwest to northeast across T. 14 N., R 4 W., the Hennessey shale forms unwooded, flat to gently rolling pasture lands. Subsurface...
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