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Oak City Formation

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Image
—Breccia facies within breccia blocks of the Oak City Formation. (A) Classification of Yarnold and Lombard (1989). (B) Matrix-rich breccia of a carbonate breccia block (CS). Note the sharp contact with the underlying conglomerate of the Oak City Formation and the incorporation of quartzite clasts from the Oak City into this basal breccia facies (arrow). (C) Jigsaw breccia (carbonate block). Note the bands of matrix between separated and slightly rotated fragments. (D) Crackle breccia (quartzite block). Breccia fragments display very slight to no rotation in this facies (arrow).
Published: 01 July 1996
Fig. 5. —Breccia facies within breccia blocks of the Oak City Formation. (A) Classification of Yarnold and Lombard (1989) . (B) Matrix-rich breccia of a carbonate breccia block (CS). Note the sharp contact with the underlying conglomerate of the Oak City Formation and the incorporation
Journal Article
Journal: Geology
Published: 01 June 1995
Geology (1995) 23 (6): 547–550.
..., is a north-trending, west-dipping, low-angle (18 °–24 ° ) normal fault that juxtaposes syntectonic conglomerates and large-rock avalanches of the Miocene Oak City Formation against footwall rocks that have been ductilely, cataclastically, and brittlely deformed. The Oak City strata dip variably to the east...
Image
Map and cross section of Tertiary deposits in the western foothills of the Canyon Range, based on new mapping, on Hintze (1991d) and on Morris and Hebertson (1996). Bold lines are high-angle normal or strike-slip faults (dashed where inferred). Easternmost dashed fault and third fault from the east are inferred by Morris and Hebertson (1996) based on drainage patterns and distribution of springs; other faults were mapped in this study. pC and C, undifferentiated Precambrian and Cambrian rocks; Toc, Tertiary Oak City Formation conglomerates (stippled); Tqb, Tertiary quartzite slide breccia (medium gray); Tcb, Tertiary carbonate slide breccia (dark gray); QTt, TertiaryQuaternary travertine of Whisky Creek (Hintze 1991d). Gray letters (a–e) denote locations of outcrops discussed in text: a, gravel quarry exposing Oak City Formation member A; b, Lower Clay Spring section of Oak City Formation member A; c, exposures of Oak City Formation member B and carbonate slide block near communications tower; d, exposures of Oak City Formation member B and carbonate slide complex northeast of Upper Clay Spring; e, Oak City Formation member C.
Published: 01 November 1999
fault from the east are inferred by Morris and Hebertson ( 1996 ) based on drainage patterns and distribution of springs; other faults were mapped in this study. pC and C , undifferentiated Precambrian and Cambrian rocks; Toc , Tertiary Oak City Formation conglomerates ( stippled ); Tqb , Tertiary
Journal Article
Journal: AAPG Bulletin
Published: 01 July 1996
AAPG Bulletin (1996) 80 (7): 1135–1149.
...Fig. 5. —Breccia facies within breccia blocks of the Oak City Formation. (A) Classification of Yarnold and Lombard (1989) . (B) Matrix-rich breccia of a carbonate breccia block (CS). Note the sharp contact with the underlying conglomerate of the Oak City Formation and the incorporation...
FIGURES
First thumbnail for: Large-Rock Avalanche Deposits, Eastern Basin and R...
Second thumbnail for: Large-Rock Avalanche Deposits, Eastern Basin and R...
Third thumbnail for: Large-Rock Avalanche Deposits, Eastern Basin and R...
Image
—Distribution of carbonate cements within carbonate breccia blocks of the Oak City Formation. Note that the most distal block (Radio Tower) has all three cement types, whereas the most proximal block (block I) contains only cement 3 and vadose cements.
Published: 01 July 1996
Fig. 9. —Distribution of carbonate cements within carbonate breccia blocks of the Oak City Formation. Note that the most distal block (Radio Tower) has all three cement types, whereas the most proximal block (block I) contains only cement 3 and vadose cements.
Image
—Photograph of an undifferentiated Cambrian carbonate breccia block overlying conglomerate of the Oak City Formation. The block is located north of Upper Clay Spring (see Figure 1). At this location the entire vertical section is exposed and was measured at 34.6 m thick; however, to the east the block thickness is estimated at over 200 m. The block is approximately 3.5 km long and 1 km wide. Note the sharp basal contact (adjacent to shrubs, see arrow). View is to the north and block is dipping 8° back toward the Canyon Range to the east (right side of photo).
Published: 01 July 1996
Figure 3 —Photograph of an undifferentiated Cambrian carbonate breccia block overlying conglomerate of the Oak City Formation. The block is located north of Upper Clay Spring (see Figure 1 ). At this location the entire vertical section is exposed and was measured at 34.6 m thick; however
Image
—Conceptual model for the emplacement of large-rock avalanche deposits within the alluvial conglomerates of the Oak City Formation. The geology requires significant extension within the study area. (A) Large-rock avalanche deposits were triggered by seismic events occurring in the Sevier Desert basin and near the flanks of the Canyon Range during late Miocene extension. (B) As extension continues, large-rock avalanches are segmented by faults and the segments are differentially rotated. Basinward blocks were cemented initially by poorly oxygenated phreatic fluids (interpreted to be deeper burial conditions), and blocks proximal to the range were cemented by well-oxygenated vadose and phreatic fluids. (C) Present exposures after blocks have been exhumed.
Published: 01 July 1996
Fig. 7. —Conceptual model for the emplacement of large-rock avalanche deposits within the alluvial conglomerates of the Oak City Formation. The geology requires significant extension within the study area. (A) Large-rock avalanche deposits were triggered by seismic events occurring in the Sevier
Image
a, Fault juxtaposing Neoproterozoic rocks (left) against Cambrian Tintic Quartzite. Note apparent drag folding in the rocks. View is north toward Mahagony Hollow (fig. 2, MH). b, Cross section across central Canyon Range showing about 1.25 km of minimum offset for the range-bounding fault. The cross section is highly simplified; more detailed sections appear in Mitra and Sussman (1997). pCc, Caddy Canyon Quartzite and equivalents; pCi, Inkom Formation; pCm, Mutual Formation; Ct, Tintic Quartzite; Co, Ophir Formation; Cu, undifferentiated Cambrian carbonates; O, S, D, Ordovician, Silurian, and Devonian strata, respectively; TKc, Canyon Range Formation; Toc, Oak City Formation. (Following Christie-Blick [1982], Christie-Blick and Levy [1989], and Levy and Christie-Blick [1991], we avoid the potentially misleading SE Idaho stratigraphic nomenclature sometimes applied to the Canyon Range Neoproterozoic rocks. We thus classify all rocks stratigraphically below the Inkom Formation as Caddy Canyon Quartzite and equivalents, including the units mapped by Millard [1983], Holladay [1984], and Hintze [1991a, 1991b, 1991c, 1991d, 1991e] as Pocatello Formation and Blackrock Canyon Limestone.)
Published: 01 November 1999
, S , D , Ordovician, Silurian, and Devonian strata, respectively; TKc , Canyon Range Formation; Toc , Oak City Formation. (Following Christie-Blick [ 1982 ], Christie-Blick and Levy [ 1989 ], and Levy and Christie-Blick [ 1991 ], we avoid the potentially misleading SE Idaho stratigraphic
Journal Article
Published: 01 November 1999
The Journal of Geology (1999) 107 (6): 659–681.
... fault from the east are inferred by Morris and Hebertson ( 1996 ) based on drainage patterns and distribution of springs; other faults were mapped in this study. pC and C , undifferentiated Precambrian and Cambrian rocks; Toc , Tertiary Oak City Formation conglomerates ( stippled ); Tqb , Tertiary...
FIGURES
First thumbnail for: Tertiary Normal Faulting in the Canyon Range, East...
Second thumbnail for: Tertiary Normal Faulting in the Canyon Range, East...
Third thumbnail for: Tertiary Normal Faulting in the Canyon Range, East...
Journal Article
Journal: AAPG Bulletin
Published: 01 May 1975
AAPG Bulletin (1975) 59 (5): 766–779.
... is produced from three uranium-mining areas—Karnes, Live Oak, and Duval—named for the counties in which they principally lie. In each area the host rock is different. Marine-beach sandstone of the Whitsett Formation is the primary host rock in the Karnes area, but some ore has been taken from crosscutting...
FIGURES
First thumbnail for: South Texas Uranium Deposits
Second thumbnail for: South Texas Uranium Deposits
Third thumbnail for: South Texas Uranium Deposits
Journal Article
Journal: GSA Bulletin
Published: 01 February 1991
GSA Bulletin (1991) 103 (2): 157–170.
... of reworking by eolian activity, with late Pleistocene formation of sand dunes continuing until 11,600 yr B.P. within the Western Lowlands. The sedimentological sequence indicates a progressive, stepwise loss of glacial meltwater and coarse sediment supply during the late-glacial interval, resulting...
Journal Article
Journal: AAPG Bulletin
Published: 01 August 1953
AAPG Bulletin (1953) 37 (8): 2046–2050.
... of shales and sandstones between the Belle City and Vamoosa formations in central Seminole County (T. 9 N.). Fig. 1. Index map showing location of Seminole County, Oklahoma. Oakes (1951) and Ries (1951) redefined the Vamoosa formation, excluding the lowermost beds which are below...
FIGURES
First thumbnail for: Hilltop <span class="search-highlight">Formation</...
Second thumbnail for: Hilltop <span class="search-highlight">Formation</...
Third thumbnail for: Hilltop <span class="search-highlight">Formation</...
Journal Article
Journal: AAPG Bulletin
Published: 01 July 1946
AAPG Bulletin (1946) 30 (7): 1140–1191.
... MIDDLE ORDOVICIAN NEAR LENOIR CITY, TENNESSEE Description Thickness in Feet Moccasin limestone   Maroon, thin-bedded, argillaceous limestone, sandstone and claystone 1,110–1,300 Witten limestone   Bluish gray, limestone; estimated thickness 50 Bowen formation   Maroon...
FIGURES
First thumbnail for: Lower Middle Ordovician of Southwest Virginia and ...
Second thumbnail for: Lower Middle Ordovician of Southwest Virginia and ...
Third thumbnail for: Lower Middle Ordovician of Southwest Virginia and ...
Journal Article
Journal: AAPG Bulletin
Published: 01 February 1949
AAPG Bulletin (1949) 33 (2): 131–152.
... are thought to be due to a development of calcareous beds within the zone (undifferentiated on the cross section) from the Wildhorse limestone down to and including the Wann formation. This is similar to the conditions found by Oakes 25 on the surface in southern Osage County. This conclusion has not been...
FIGURES
First thumbnail for: Subsurface Cross Sections from Marion County Kansa...
Second thumbnail for: Subsurface Cross Sections from Marion County Kansa...
Third thumbnail for: Subsurface Cross Sections from Marion County Kansa...
Journal Article
Journal: AAPG Bulletin
Published: 01 November 1959
AAPG Bulletin (1959) 43 (11): 2623–2635.
..., and Stones Switch sandstone members, consists chiefly of bentonitic clays and tuff near the top and sandstones near the base. The McElroy formation consists of the Conquista clay (a new name substituted for the pre-empted name Falls City shale of Ellisor, 1933 ), the Dilworth sandstone, and the Manning clay...
FIGURES
First thumbnail for: Stratigraphy of Jackson Group (Eocene), South-Cent...
Journal Article
Published: 01 February 2012
Environmental & Engineering Geoscience (2012) 18 (1): 51–64.
... space of White Oak Farm ( Figure 2 ). Ahmanson Ranch and White Oak Farm are now state park properties used for outdoor recreation. Along the first part of this stream reach, Las Virgenes Creek flows across the Modelo Formation and its eroded alluvial valley fill products ( Figure 4 ). The Modelo...
FIGURES
First thumbnail for: Origin of Stream Flows at the Wildlands-Urban Inte...
Second thumbnail for: Origin of Stream Flows at the Wildlands-Urban Inte...
Third thumbnail for: Origin of Stream Flows at the Wildlands-Urban Inte...
Journal Article
Published: 01 November 2024
Earth Sciences History (2024) 43 (2): 303–326.
... accurately depicted the geological and environmental characteristics of the Adriatic port city of Ancona and the nearby Monte Cònero mountain. In this research, besides a meticulous study of architectural, geomorphologic, faunal, and floral details, we focused on the representation of a large outcrop...
FIGURES
First thumbnail for: THE PINK ROCKS OF CARLO CRIVELLI (CIRCA 1489)
Second thumbnail for: THE PINK ROCKS OF CARLO CRIVELLI (CIRCA 1489)
Third thumbnail for: THE PINK ROCKS OF CARLO CRIVELLI (CIRCA 1489)
Journal Article
Journal: AAPG Bulletin
Published: 01 March 1943
AAPG Bulletin (1943) 27 (3): 306–312.
... sandstones and shales, may be recognized. The upper sandstones of Oak Run Valley, 2,500–3,000 feet above the base of the section, are the probable correlatives of the base of the Cretaceous section at Chico Creek 70 miles south. 1 Read before the Pacific Section of the Association at Los Angeles...
FIGURES
First thumbnail for: Cretaceous: East Side Sacramento Valley, Shasta an...
Second thumbnail for: Cretaceous: East Side Sacramento Valley, Shasta an...
Journal Article
Published: 05 July 2018
Canadian Journal of Earth Sciences (2018) 55 (7): 730–767.
...-central Ontario (modified from Sharpe et al. 2011 ). ( a ) Age, lithostratigraphy, and chronostratigraphy; note that a regional (channel) unconformity (long sloping red line) is present beneath both Oak Ridges Moraine (ORM) and upper Thorncliffe Formation (TF) sediments; Lower sediment (blue sequence...
FIGURES
First thumbnail for: Conceptual hydrogeological model of the Yonge Stre...
Second thumbnail for: Conceptual hydrogeological model of the Yonge Stre...
Third thumbnail for: Conceptual hydrogeological model of the Yonge Stre...
Journal Article
Journal: AAPG Bulletin
Published: 01 August 1923
AAPG Bulletin (1923) 7 (5): 532–545.
... in Starr, Jim Hogg, Duval, McMullen, and Live Oak counties is also at present the object of much interest. Webb, Zapata, and Starr counties border the Rio Grande, the Mexican state of Tamaulipas lying across the river. Jim Hogg, Duval, McMullen, and Live Oak counties are north and east of the three...
FIGURES
First thumbnail for: The Relation of the Reynosa Escarpment to the Oil ...