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Meeteetse Formation

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Hand-contoured depth structure map on the top of <b>Meeteetse</b> <b>Formation</b>. Note ...
Published: 01 March 2001
Figure 10. Hand-contoured depth structure map on the top of Meeteetse Formation. Note Cave Gulch 4 on the north side of a large east-west fault system that bisects the shallow Cave Gulch Field. Arbitrary seismic lines D-D′, E-E′, and F-F′ are shown in Figures 11 –13. The area of best shallow
Image
Hand-contoured depth structure map on the top of <b>Meeteetse</b> <b>Formation</b>. Note ...
Published: 01 December 2000
Figure 10. Hand-contoured depth structure map on the top of Meeteetse Formation. Note Cave Gulch 4 on the north side of a large east-west fault system that bisects the shallow Cave Gulch Field. Arbitrary seismic lines D-D′, E-E′, and F-F′ are shown in Figures 11 –13. The area of best shallow
Image
—Thickness map of Cody, Mesaverde, Lewis, and <b>Meeteetse</b> <b>Formations</b> in Wind ...
Published: 01 November 1965
FIG. 17. —Thickness map of Cody, Mesaverde, Lewis, and Meeteetse Formations in Wind River basin.
Series: GSA Special Papers
Published: 01 January 1986
DOI: 10.1130/SPE210-p123
... as a prograding delta shoreline complex of sand bodies on which coastal swamps were established. Peat accumulation in the Mesaverde was terminated by deposition of the widespread marine transgressive white sandstone member of Troyer and Keefer (1955). During deposition of the overlying Meeteetse Formation, local...
Journal Article
Journal: AAPG Bulletin
Published: 01 January 1965
AAPG Bulletin (1965) 49 (1): 116–117.
... are readily distinguishable; they are, in ascending order, the Eagle Sandstone, Claggett Shale, Judith River Formation, and Bearpaw Shale. In the western part of the basin the equivalent stratigraphic section includes the Mesaverde (Gebo Formation of Hewitt), and the Meeteetse Formation. Non-marine deposits...
Journal Article
Journal: AAPG Bulletin
Published: 01 March 1965
AAPG Bulletin (1965) 49 (3): 277–285.
... section includes the Mesaverde Formation (Gebo Formation of Hewitt), Meeteetse Formation, and Lance Formation. In the eastern part of the basin four formations are readily distinguishable; they are, in ascending order, the Eagle Sandstone, Claggett Shale, Judith River Formation, and Bearpaw Shale. Major...
FIGURES | View All (6)
Journal Article
Journal: AAPG Bulletin
Published: 01 October 1958
AAPG Bulletin (1958) 42 (10): 2424–2443.
... shale of northern Wyoming and Montana, was found to intertongue with the Meeteetse formation in the Wind River and Big Horn basins. 1 Manuscript received, March 13, 1958. Publication authorized by the director of the United States Geological Survey. 2 Geologist, United States...
FIGURES | View All (6)
Journal Article
Published: 01 December 2019
Rocky Mountain Geology (2019) 54 (2): 47–95.
... of strongly overturned outcrops of the Eocene Willwood Formation. The Upper Cretaceous Meeteetse Formation is the stratigraphic horizon at which the dips attain vertical or slightly overturned orientations. All consequential faults within the newly mapped area are thrusts, and they show generally westward...
FIGURES | View All (41)
Series: Memoir - AAPG, Memoir - AAPG
Published: 01 January 1968
DOI: 10.1306/M9363C53
EISBN: 9781629812311
... Abstract Latest Cretaceous and Tertiary beds constitute almost two-thirds of the maximum of 33,000 ft of sedimentary rocks in the Wind River basin. The marine Upper Cretaceous Cody Shale is overlain, with intertonguing, by the Mesaverde Formation. The next-overlying Lewis Shale and Meeteetse...
Series: AAPG Studies in Geology, AAPG Studies in Geology
Published: 01 January 1984
DOI: 10.1306/St17437C12
EISBN: 9781629811635
...) coal field; Beaver Creek coal field; Big Sand Draw coal field; Alkali Butte coal field; and Arminto (Powder River) coal field. Their major coal deposits are found in the Mesaverde and Meeteetse Formations, along the basin perimeter. The Alkali Butte coal field contains three coalbeds greater than 4 ft...
Image
View to the north. Strata near the K me  symbol (<b>Meeteetse</b> Fm.) are just no...
Published: 01 December 2019
strata dominating this photograph is the immediately recognizable form of bedding characteristic of the type Meeteetse Formation that surrounds the Bighorn Basin’s town of Meeteetse (for its location, see the present paper’s Fig. 4 and its excerpted fig. 32 from Lillegraven [2009] ).
Journal Article
Journal: AAPG Bulletin
Published: 01 September 1983
AAPG Bulletin (1983) 67 (9): 1457.
..., designated as Meeteetse Trail and Burgess Lignite occur in typical Fort Union sediments. The Meeteetse Trail locality is less than 0.25 mi (0.4 m) from vertical Madison Limestone with a westerly dip “under” the Madison. The other, the Burgess Lignite locality, is composed of alternating papery fusinitic...
Journal Article
Journal: AAPG Bulletin
Published: 01 May 1979
AAPG Bulletin (1979) 63 (5): 825.
...William H. Curry Abstract Electrical accessory curves have been used to map the Mesaverde, Lance-Meeteetse, Fort Union, and Willwood Formations in the Bighorn basin of Wyoming. These subsurface mapping units have been correlated to mapped outcrops on the flank of the basin. Recent authors have...
Journal Article
Published: 01 May 1997
Rocky Mountain Geology (1997) 31 (2): 1–26.
...Edward S. Belt; Jason F. Hicks; David A. Murphy Abstract A regional unconformity lies beneath Harebell-Lance-Hell Creek nonmarine facies and above much older Meeteetse and Fox Hills marginal marine facies. This pre-Lancian unconformity (U 1 ) extends eastward from the Sevier overthrust belt...
Image
Detrital zircon age-probability distributions for Paleogene TSA4 composite ...
Published: 01 September 2013
Figure 16. Detrital zircon age-probability distributions for Paleogene TSA4 composite ( n = 285), and for the Maastrichtian composite (Lance and Meeteetse Formations, n = 198).
Journal Article
Journal: AAPG Bulletin
Published: 01 August 1956
AAPG Bulletin (1956) 40 (8): 1899–1914.
... formation was deposited. North of Spread Creek about 675 feet of the Meeteetse formation is locally present, overlying the Mesaverde formation, but in no place was the Harebell found in contact with the Meeteetse. It is presumed that the Meeteetse, because the weak character of the bentonitic shale...
FIGURES
Journal Article
Journal: AAPG Bulletin
Published: 01 October 2009
AAPG Bulletin (2009) 93 (10): 1379–1401.
... and Almond formations (Green River Basin), Farrer and Neslen formations (Uinta Basin), Meeteetse Formation (Wind River Basin), Eagle Sandstone (Crazy Mountain Basin), Hell Creek Formation (Williston Basin), Menefee Formation (San Juan Basin), and formations in the Bohai Basin of China, offshore Thailand...
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Journal Article
Journal: AAPG Bulletin
Published: 01 August 1956
AAPG Bulletin (1956) 40 (8): 1863–1898.
..., Appendix), and hexagonal flakes of biotite, a few grains of augite, and a grain of pleochroic apatite are present in a magnetic separate of a sample collected near the top of the Willwood formation (note 15, Appendix). The Willwood formation southeast of Meeteetse has been reported to contain leaf-bearing...
FIGURES | View All (11)
Image
Abundant metamorphic pebbles shown in this photograph are in the basal Meet...
Published: 01 December 2019
Figure 33. Abundant metamorphic pebbles shown in this photograph are in the basal Meeteetse Formation (K me ), conformably deposited upon sands of the uppermost Mesaverde Formation (K mv ) as it exists directly below the summit on the eastern slope of the prominent hilltop shown in Figures 30
Image
View to the northeast. The red star, which marks the faulted contact betwee...
Published: 01 December 2019
Figure 35. View to the northeast. The red star, which marks the faulted contact between the Meeteetse Formation (K me ) and overlying Lance Formation (K l ), is placed just south of the northeastern corner of NW1/4 of NE1/4 of SE1/4 of section 21, T. 56 N., R. 103 W. This photograph, perhaps