...Benjamin D. Herber; Paul Weimer; Renaud Bouroullec; Roger J. Barton; Daniel N. Behringer; William S. Hammon, III; William S. Gutterman ABSTRACT The Red Wing Creek field in the Williston Basin is one of a few well-known petroleum fields in the world to produce from a structure associated...

...L. W. Dan Bridges ABSTRACT During the early stages of development at Red Wing Creek field, meteoritic impact was the accepted explanation for structure. Spectacular structure that apparently did not persist below the Mississippian Madison Group and the presence of shatter cones, which were thought...

...Elmer S. Parson; Gordon W. Henderson; Louis J. Conti Abstract Red Wing Creek field is located near the center of the Williston basin in McKenzie County, North Dakota. The discovery well was drilled by True Oil Co. in August 1972. The primary trapping mechanism is structural. Seismic and subsurface...

...Elmer S. Parson, Jr. Abstract Red Wing Creek field is on the southwest flank of the Williston basin near the axis of the present basin. The field is centered in Sec. 27, T148N, R101W, McKenzie County, North Dakota. The discovery well was drilled by True Oil Company in August 1972. Seismic...

...Levie Donn, Jr. Abstract: The process of impact cratering results in the instantaneous formation of unique structures characterized by extensive fracturing and brecciation of the target rock. This process can be conducive to economic hydrocarbon accumulations (Red Wing Creek field with 130 million...

... in 1972, this structure was a seismic anomaly that fit no pattern for Williston basin structures. Exhibits presented to the North Dakota Industrial Commission during the spacing hearing for the Red Wing Creek field interpreted this structure as an astrobleme. Succeeding publications by Brennen et al (1975...

... fossils at Copperas Creek precluded a census collection. Specimens identified and tallied during these collection activities comprise the ‘field census’ (Online Supplemental File, Tables S1, S2). Representative samples of each morphotype, all unknown specimens, and well-preserved specimens that document...

... of a meteorite impact, Red Wing Creek Field, Williston Basin, western North Dakota : M.S. Thesis , University of Colorado at Boulder . Heritier F. E. Lossel P. Wathe E. , 1980 , Frigg Field: Large submarine-fan trap in Lower Eocene rocks of the Viking Graben, North Sea , in Halbouty M...

...− represents chron C25r, and zone D+ represents chron C25n. This section is 290 m thick and begins ∼3 km southwest of Basin, Wyoming, in a thick red paleosol that correlates lithostratigraphically to the top of the Sand Creek Divide section, and marks the P-E boundary in this region ( Figs. 1 and 8...

... thick amalgamated fluvial deposit (“boundary sandstone”) within the PETM interval, with gray to red-orange paleosols located both above and below the deposit. At Sand Creek Divide, a similar situation to that at PCB is reported whereby a change to drier, thicker, and more mature soils is observed during...

... increased for the first time in 4 years. The success rate, however, decreased in comparison to the past 2 years. Development drilling increased 47.1% and the success rate increased from 47.1 to 72.0%. One discovery, the Red Wing Creek field, appears to be unique to the Williston basin. Part...

... to vertical. Most thin sections show such intense crescentic fabric that individual burrows have been obscured. Some red beds show slickensides that, in the field, appear as shiny, clay-lined fractures that intersect to form concave-up, dish-shaped structures with amplitudes of ∼ 0.5 m and spacings of ∼ 1...

... the Sourdough 2 coal. The Sourdough 2 coal, 42 m above the Tipton Buttes faunal locality, appears to be of similar age to the 621 m level of the Elk Creek section in the Bighorn Basin, where a laterally extensive carbonaceous shale deposit occurs that is also rich in fossil plants (e.g., Davies-Vollum and Wing...

... Creek section because neither mammalian teeth nor paleosol nodules have been recovered from the base of the Willwood Formation in this section. Although direct evidence is lacking, we think the IETM is represented in this exposure, because the basal 30 m of the Willwood Formation has two very thick red...

..., occurrence of intercalary pseudo-veins; RP with 1/2 branches (left/right forewing); M simple; CuA with at least 7 branches. Left hind wing: length about 21 mm; vannus folded, no longer than the quarter of wing length. Occurrence .—Francis Creek Shale, Mazon Creek, Carbondale Fm., IL, USA; Westphalian D...

... or possibly Oligocene ( Mustard and Rouse 1994 ) and should not be confused with the Huntingdon Formation in Canada. Red circled areas in the Fraser River Valley denote the Kanaka Creek fossil plant site (right) in Kanaka Creek Regional Park and other para-contemporaneous fossil plant and palynological sites...

... and stratigraphically thickest paleosol δ 13 C org section in the southeastern Bighorn Basin. However, the same patterns were documented in three other trenched sections in the field area (CAB 10, Big Red Spit, and North Butte). Figure 1. (A) Map showing exposures of the Willwood Formation (shaded...

.... , Bouroullec , R. , Barton , R. , Behringer , D. , Hammon , W. , III , and Gutterman , W. , 2022 , Three-dimensional seismic interpretation of a meteorite impact feature, Red Wing Creek field, Williston Basin, western North Dakota : American Association of Petroleum Geologists Bulletin...