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Pequop Formation

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Journal Article
Published: 01 November 1974
Journal of Paleontology (1974) 48 (6): 1170–1173.
Journal Article
Journal: AAPG Bulletin
Published: 01 September 1963
AAPG Bulletin (1963) 47 (9): 1776.
... comprises Reipe Spring limestone, Reipetown sandstone, Pequop formation, and Loray formation. In the Confusion Range, Butte Mountains, and Ely area, Pequop and Loray formations are generally recognizable, but no distinctive boundary for mapping purposes can be recognized. In these areas, the Arcturus...
Journal Article
Journal: AAPG Bulletin
Published: 01 May 1959
AAPG Bulletin (1959) 43 (5): 1105.
... named the Pequop formation. The Pequop formation is 1,525 feet thick at its type section in Sec. 3, T. 33 N., R. 65 E., Elko County, Nevada. Composed of purplish gray, irregularly bedded, platy, silty limestones with interbedded fusuline coquinas, the lower contact is placed at the red silt member which...
Journal Article
Journal: AAPG Bulletin
Published: 01 May 1964
AAPG Bulletin (1964) 48 (5): 565–636.
... area, but considerable confusion attends its present concept; it is herein proposed to raise it to group rank to include, in ascending order, these formations: Riepe Spring Limestone (Early to Medial Wolfcampian age), Riepetown Formation (Medial to Late Wolfcampian age), Pequop Formation (Leonardian...
FIGURES
First thumbnail for: Ely, Arcturus, and Park City Groups (Pennsylvanian...
Second thumbnail for: Ely, Arcturus, and Park City Groups (Pennsylvanian...
Third thumbnail for: Ely, Arcturus, and Park City Groups (Pennsylvanian...
Journal Article
Journal: AAPG Bulletin
Published: 01 February 1963
AAPG Bulletin (1963) 47 (2): 350–351.
..., and Leppy Range of western Utah, and in the Cherry Creek Mountains, Butte Mountains, Pequop Mountains, Diamond Range, and Pancake Range of Nevada. Ferguson Mountain Formation (Wolfcampian) of northeastern Nevada and part of adjacent Utah is approximately 2,000 feet of alternating reefoid, bioclastic matrix...
Journal Article
Journal: GSA Bulletin
Published: 01 September 1962
GSA Bulletin (1962) 73 (9): 1083–1110.
... type locality in eastern Elko County, Nevada, contains one of the most prolific Wolfcampian fusulinid faunas in the eastern Great Basin. It is conformably overlain by the Pequop Formation, Leonardian in age, also rich in fusulinids. The Pequop is unconformably overlain by the Loray Formation...
Image
 Figure1—Location map showing Pequop Mountains area. 1 = Reference section of Pequop Formation; 2 = Ninemile Canyon section
Published: 01 November 2008
Figure 1 —Location map showing Pequop Mountains area. 1 = Reference section of Pequop Formation; 2 = Ninemile Canyon section
Journal Article
Published: 01 May 2010
Journal of Paleontology (2010) 84 (3): 529–537.
... and the Darwin Canyon Formation in California, Paraheritschioides fergusonensis n. sp. from the Ferguson Mountain and Bird Spring formations in Nevada, and Wendoverella arca n. gen. and n. sp., Permastraea nevadensis n. sp., and Pararachnastraea moormanensis n. sp. from the Pequop Formation in eastern Nevada...
FIGURES
First thumbnail for: NEW EARLY PERMIAN COLONIAL RUGOSE CORALS FROM THE ...
Second thumbnail for: NEW EARLY PERMIAN COLONIAL RUGOSE CORALS FROM THE ...
Third thumbnail for: NEW EARLY PERMIAN COLONIAL RUGOSE CORALS FROM THE ...
Journal Article
Published: 01 May 1963
Journal of Paleontology (1963) 37 (3): 723–724.
... are described. The collecting localities listed in 1960 for White Pine County are now referable to the Pequop Formation [Permian], Arcturus Formation [Pennsylvanian], Reipetown sandstone [Permian], Riepe Spring Limestone [Permian], and the Hogan Formation [Pennsylvanian]. GeoRef, Copyright 2004, American...
Journal Article
Published: 01 July 1969
Journal of Paleontology (1969) 43 (4): 936–940.
...Taylor V. Mayou Abstract Twenty-three nearly complete specimens and many broken parts of Archaeophiomusium bispinosum n.sp., and two specimens of A. burrisi (Miller), were collected from the Leonardian Pequop Formation in the Maverick Springs Range, eastern Nevada. Preservation is exceptional...
Image
Field photographs of variable deformation in the Pequop Mountains. (A) Boudinaged meta-chert in OꞒnp showing SE stretching, with the right photo showing top-SE shear; (B) dark calcite marble (lm) flowing around more rigid dolomite (dol) marble boudin; (C) southeast-directed thrust faulting (f) within the Cambrian–Ordovician rocks; (D) variable expressions of pervasive top-southeast shear observed across the range; and (E) isoclinal folds with variable shallowly plunging fold axes (FA). Locations: (A) −114.636513W, 40.914893N; (B) 114.61808W, 40.938775N; (C) 114.600652W, 40.975283N; (D) (left to right) 114.59328W, 40.97021N; 114.61262W, 40.994288N; 114.576177W, 40.94675N. (E) (left to right) 114.640088W, 40.932855N; 114.615102W, 40.967954N; 114.602142W, 40.932022N; (F) 114.59252W, 41.07429N; (G) 114.58844W, 41.13150N; (H) ∼114.560056W, 41.074889N. (F–H) Other structural complexities within the range include (F) west-directed reverse faulting in the Devonian Guilmette Formation north of Interstate 80 (red arrows point to fault; white dashed lines are offset marker beds; 0.5–1.0 m tall sagebrush for scale); (G) bedding-parallel fault in the Permian Pequop Formation that omitted section (note bed pinchout marked by two rock hammers); and (H) complex high-angle normal faulting that is missed without fortuitous road cuts (photo from 1961; view no longer exists due to modern highway construction). Mtp—Mississippian Tripon Pass; Mc—Mississippian Chainman Shale.
Published: 27 October 2021
complexities within the range include (F) west-directed reverse faulting in the Devonian Guilmette Formation north of Interstate 80 (red arrows point to fault; white dashed lines are offset marker beds; 0.5–1.0 m tall sagebrush for scale); (G) bedding-parallel fault in the Permian Pequop Formation that omitted
Image
Field photographs of variable deformation in the Pequop Mountains. (A) Boudinaged meta-chert in OꞒnp showing SE stretching, with the right photo showing top-SE shear; (B) dark calcite marble (lm) flowing around more rigid dolomite (dol) marble boudin; (C) southeast-directed thrust faulting (f) within the Cambrian–Ordovician rocks; (D) variable expressions of pervasive top-southeast shear observed across the range; and (E) isoclinal folds with variable shallowly plunging fold axes (FA). Locations: (A) −114.636513W, 40.914893N; (B) 114.61808W, 40.938775N; (C) 114.600652W, 40.975283N; (D) (left to right) 114.59328W, 40.97021N; 114.61262W, 40.994288N; 114.576177W, 40.94675N. (E) (left to right) 114.640088W, 40.932855N; 114.615102W, 40.967954N; 114.602142W, 40.932022N; (F) 114.59252W, 41.07429N; (G) 114.58844W, 41.13150N; (H) ∼114.560056W, 41.074889N. (F–H) Other structural complexities within the range include (F) west-directed reverse faulting in the Devonian Guilmette Formation north of Interstate 80 (red arrows point to fault; white dashed lines are offset marker beds; 0.5–1.0 m tall sagebrush for scale); (G) bedding-parallel fault in the Permian Pequop Formation that omitted section (note bed pinchout marked by two rock hammers); and (H) complex high-angle normal faulting that is missed without fortuitous road cuts (photo from 1961; view no longer exists due to modern highway construction). Mtp—Mississippian Tripon Pass; Mc—Mississippian Chainman Shale.
Published: 27 October 2021
complexities within the range include (F) west-directed reverse faulting in the Devonian Guilmette Formation north of Interstate 80 (red arrows point to fault; white dashed lines are offset marker beds; 0.5–1.0 m tall sagebrush for scale); (G) bedding-parallel fault in the Permian Pequop Formation that omitted
Journal Article
Journal: AAPG Bulletin
Published: 01 November 1975
AAPG Bulletin (1975) 59 (11): 2079–2098.
... the Ely Limestone ranges from 0 to 2,500 ft (762 m) in thickness. Hogan Formation — Robinson (1961, p. 103-104) proposed this formation name for a 250-ft (76 m) sequence of silty-sandy limestone and calcareous siltstone in the central Pequop Mountains. At the type locality Hogan Formation...
FIGURES
First thumbnail for: Late Pennsylvanian and Early Permian Sedimentation...
Second thumbnail for: Late Pennsylvanian and Early Permian Sedimentation...
Third thumbnail for: Late Pennsylvanian and Early Permian Sedimentation...
Image
Figure5—Arcochiton richardsoni n. sp. 1–3, tail plate, dorsal, right lateral, and ventral views, Ft. Apache Limestone, UCMP 154090; 4–7, holotype, tail plate, dorsal, ventral, right lateral views, and left lateral view showing trace of color pattern (×7), Bird Spring Formation, UCMP 154091; 8–12, intermediate plate, dorsal, right lateral, posterior, ventral views, and left lateral view showing trace of color pattern (×7), Bird Spring Formation (D-5252), UI x8896; 13–15, intermediate plate, right lateral and ventral views, and right lateral view showing trace of color pattern (×7), Bird Spring Formation (D-5252), UCMP 154093; 16–18, intermediate plate, right lateral, posterior, and ventral views, Bird Spring Formation (D-5252), UI x8897; 19, 20, intermediate plate, ventral and right lateral views, Bird Spring Formation, UCMP 154092; 21, 22, head plate, dorsal and ventral views, Bird Spring Formation, UCMP 154094; 23, 24, head plate, anterior and ventral views, Pequop Formation UCMP 154095; 25, 26, head plate, dorsal and right lateral views, Bird Spring Formation (D-5252), UI x8898; 27–29, head plate, dorsal, posterior, and right lateral views, Bird Spring Formation (D-5252), UI x8899. All figures ×10 except as noted
Published: 01 March 2002
and ventral views, Bird Spring Formation, UCMP 154094; 23, 24, head plate, anterior and ventral views, Pequop Formation UCMP 154095; 25, 26, head plate, dorsal and right lateral views, Bird Spring Formation (D-5252), UI x8898; 27 – 29, head plate, dorsal, posterior, and right lateral views, Bird Spring
Journal Article
Published: 01 November 2008
Journal of Paleontology (2008) 82 (6): 1190–1200.
...Figure 1 —Location map showing Pequop Mountains area. 1 = Reference section of Pequop Formation; 2 = Ninemile Canyon section ...
FIGURES
First thumbnail for: Fasciculate Rugose Corals from Gzhelian and Lower ...
Second thumbnail for: Fasciculate Rugose Corals from Gzhelian and Lower ...
Third thumbnail for: Fasciculate Rugose Corals from Gzhelian and Lower ...
Journal Article
Journal: AAPG Bulletin
Published: 01 May 1967
AAPG Bulletin (1967) 51 (5): 791–802.
...; the Missourian and Virgilian are absent; and the Permian consists, in ascending order of Wolfcampian Ferguson Mountain Formation (north end of the range) and lateral equivalents, Riepe Spring Limestone and Riepetown Formation (south end of range), Leonardian Pequop Formation, Loray Formation (late Leonardian...
FIGURES
First thumbnail for: Pennsylvanian and Permian Basins in Northwestern U...
Second thumbnail for: Pennsylvanian and Permian Basins in Northwestern U...
Journal Article
Journal: AAPG Bulletin
Published: 01 February 1970
AAPG Bulletin (1970) 54 (2): 285–312.
... and skeletal limestone of the Oquirrh Formation. The Kirkman Limestone is not known to be present, but the uppermost few hundreds of feet of the Oquirrh resemble some units of the Kirkman. The units of the Permian System in the Pequop-Diamond Creek and Montello-Sublett basins are, in ascending order...
FIGURES
First thumbnail for: Realms of Permian Tectonism and Sedimentation in W...
Second thumbnail for: Realms of Permian Tectonism and Sedimentation in W...
Third thumbnail for: Realms of Permian Tectonism and Sedimentation in W...
Journal Article
Published: 01 March 2002
Journal of Paleontology (2002) 76 (2): 256–264.
... and ventral views, Bird Spring Formation, UCMP 154094; 23, 24, head plate, anterior and ventral views, Pequop Formation UCMP 154095; 25, 26, head plate, dorsal and right lateral views, Bird Spring Formation (D-5252), UI x8898; 27 – 29, head plate, dorsal, posterior, and right lateral views, Bird Spring...
FIGURES
First thumbnail for: PERMIAN POLYPLACOPHORA (MOLLUSCA) FROM NEVADA, UTA...
Second thumbnail for: PERMIAN POLYPLACOPHORA (MOLLUSCA) FROM NEVADA, UTA...
Third thumbnail for: PERMIAN POLYPLACOPHORA (MOLLUSCA) FROM NEVADA, UTA...
Journal Article
Journal: GSA Bulletin
Published: 01 August 1970
GSA Bulletin (1970) 81 (8): 2417–2448.
...CHARLES H THORMAN Abstract The Wood Hills and Pequop Mountains of northeastern Nevada are located within the Cordilleran miogeosyncline of Paleozoic age and in the Basin and Range province of Cenozoic age. Two structural units or plates, designated Plates I and II, are juxtaposed along the Wood...
Journal Article
Journal: AAPG Bulletin
Published: 01 February 1965
AAPG Bulletin (1965) 49 (2): 139–156.
..., is considered preferable to retention of the name Butte-Deep Creek trough. The names of lithologic units used here are: Riepe Spring Limestone and Rib Hill, Pequop, Loray, Arcturus, and Dry Mountain lithosomes ( Fig. 5 ). The first four lithosomes are named for formations and they include all or the most...
FIGURES
First thumbnail for: Pre-Kaibab Permian Stratigraphy and History of But...
Second thumbnail for: Pre-Kaibab Permian Stratigraphy and History of But...
Third thumbnail for: Pre-Kaibab Permian Stratigraphy and History of But...