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Ozark Dome

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Series: AAPG Memoir
Published: 01 January 2019
DOI: 10.1306/13632141M116257
EISBN: 9781629812854
... Arkansas, and northeastern Oklahoma ( Figure 1 ) are the focus of this study. These rocks were deposited on the southern Burlington shelf along the southwestern edge of the Ozark dome ( Figure 1A ). This shelf was an expansive carbonate bank that extended for approximately 1000 mi (1600 km) across...
FIGURES | View All (19)
Series: GSA Field Guide
Published: 01 January 2010
DOI: 10.1130/2010.0017(06)
EISBN: 9780813756172
... basement. The latter is exposed as an uplift located about 40 mi southwest of the St. Francois Mountains and form the core of the Ozark dome. On day 1, participants will examine and explore major karst features developed in Paleozoic carbonate strata on the Current River; this will include Devil’s Well...
FIGURES | View All (50)
Journal Article
Journal: Geology
Published: 01 June 2000
Geology (2000) 28 (6): 511–514.
...Mark R. Hudson Abstract Structures that formed on the southern flank of the Ozark dome, in the foreland of the late Paleozoic Ouachita orogeny, have received little modern study. New mapping of the western Buffalo River region of northern Arkansas identifies diversely oriented faults and monoclinal...
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Image
Figure 4. Tectonic setting of foreland deformation in southern <b>Ozark</b> <b>dome</b> (...
Published: 01 June 2000
Figure 4. Tectonic setting of foreland deformation in southern Ozark dome (unpatterned). Foreland basins are indicated by dotted pattern.
Journal Article
Journal: GSA Bulletin
Published: 01 November 1962
GSA Bulletin (1962) 73 (11): 1365–1386.
... pebbles and frosted sand grains, both of which probably were derived from Cambrian or Ordovician formations that cropped out on the Pascola arch, an eastward-sloping extension of the Ozark dome. Quartz pebbles, heavy minerals, and some of the angular quartz sand present at the eastern edge...
Series: DNAG, Geology of North America
Published: 01 January 1991
DOI: 10.1130/DNAG-GNA-K2.503
EISBN: 9780813754611
... highland areas, the domed Ozark Plateaus and the tightly folded mountains of the Ouachita Province (Fig. 2). The Osage Plains and Interior Highlands have little in common, physiographically or stratigraphically, and are included in the same chapter for convenience because of their proximity to one another...
Journal Article
Journal: AAPG Bulletin
Published: 01 May 1982
AAPG Bulletin (1982) 66 (5): 638–639.
... with a few gypsym casts are characteristic of this unit. Regional dolomitization was a later diagenetic event related to the formation of a freshwater and seawater mixing zone beneath a landmass created by upwarping of the Cincinnati arch and Nashville and Ozark domes. Intensity of dolomitization...
Series: DNAG, Centennial Field Guides
Published: 01 January 1988
DOI: 10.1130/0-8137-5404-6.211
EISBN: 9780813754109
... Abstract U.S. 65 is a major north-south artery across Arkansas. In north-central Arkansas it traverses the Ozark Plateau Province, which represents a stable Paleozoic platform located on the southwest flank of the Ozark Dome and north of the Ouachita trough. In Searcy County the highway crosses...
Journal Article
Journal: Economic Geology
Published: 01 September 1999
Economic Geology (1999) 94 (6): 913–935.
... of the Arkoma basin and strong discharge over the crest of the Ozark dome. Ground-water temperature and velocity were found to increase with time during the early stages of uplift, before reaching a maximum and thereafter declining to somewhat lower values that remained steady over time. Continuous meteoric...
Journal Article
Journal: AAPG Bulletin
Published: 01 February 1956
AAPG Bulletin (1956) 40 (2): 423–424.
... foreland of the two above systems consisting of the Oklahoma lobe of the Ozark dome, the Central Oklahoma platform, and the Northern Oklahoma platform with the buried Nemaha ridge marking the western boundary of the Central Oklahoma platform. A small marginal part of the Gulf Coast geosyncline...
Journal Article
Published: 01 February 1994
Bulletin of the Seismological Society of America (1994) 84 (1): 105–118.
..., Missouri ( CCM ). This information is then used to study the nature of regional wave propagation from the New Madrid seismic zone to CCM across the Ozark Dome to interpret broadband seismograms written by small events. Receiver function inversion indicates a crust 40 km thick characterized by smooth...
Journal Article
Journal: Economic Geology
Published: 01 May 1987
Economic Geology (1987) 82 (3): 719–734.