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...dome, regional dome, local nose, regional nose, local anticline, regional anticline, and [[syncline]]. The following outline shows the classes, some of the sub ...l.aspx?id=1022 AAPG Memoir 60], p. 219-235.</ref> || rowspan = 2 | ''Local anticline'' || ''Fault bounded or cross faulted'' || ''Relief, symmetry, internal fau

...Hoversten /> acquired MT data over both the Angore anticline and the Hides anticline. The interpreted models from these two data sets provide depth estimates of

...ger, H., R., Hamill, M., 1976, Petrofabric analysis of the Dry Creek Ridge anticline, Montana: Geological Society of America Bulletin, vol. 87, p. 555–566, DO ...een stresses inferred from calcite twin lamellae and macrofractures, Teton anticline, Montana: Geological Society of America Bulletin, vol. 82, p. 3151–3162,

...er|1}}Vectors and equipotential lines for a hydrocarbon accumulation in an anticline in a hydrodynamic environment. Modified. Copyright: North;<ref name=North19 ...ors and the equipotential lines for a hydrocarbon [[accumulation]] in an [[anticline]] in a hydrodynamic environment.

...d of the Top Keuper horizon extending roughly parallel to the trend of the anticline. The Top Zechstein and Top Keuper are approximately conformable in this vol

...tional geometries are draped over the east–west down-to-the-north rollover anticline, resulting in a seismic reflection amplitude pattern that shows north-to-so ...l [[dip]]-oriented gravity-flow sandstone draped over the postdepositional anticline is likely to have two-way structural termination of a petroleum-associated

...aps into the East Breaks 160-161 [[''Glob alt'']] through [[''Trim A'']] [[Anticline|anticlinal]] traps. Periodic vertical migration of oil probably took place

...[[Stratigraphic trap|stratigraphic]]/ structural trap, [[Fold trap regime|anticline]]/[[Fault trap regime|fault]] trap, and tilted fault-block/[[Erosional trap

...or faulting, among others, a fold should have its crown or crest as the [[anticline]] and the trough of its structures as the syncline. The anticlinal and sync

...4.jpg|thumb|200px|Miocene rocks in the northeastern limb of the Youshashan anticline and sculptured by fluvial incision and wind erosion. Courtesy AAPG Bulletin

...rata. Surface elevations rise up to 850 m (2788 ft) on the Qara Chauq Dagh anticline ([[:file:M106Ch12Fig01.jpg|Figure 1]]). There are many towns and cities in ...e Zagros foldbelt is topographically lower and is characterized by large [[anticline]]s trending to the northwest. In the southwestern part of the foldbelt, syn

...of Pinedale field ([[:File:M107FG1.jpg|Figure 1]]), were brought onto the anticline that commercial production was established. These techniques finally allowe ...development patterns exist. This ensures that at any one time, 92% of the anticline has no development activity. It also benefits wildlife in that it reduces h

...duced laterally continuous sheetlike reservoirs subsequently draped over [[Anticline|anticlinal]] structure.

...was made by William Logan in 1844 when he noted the occurrence of oil on [[anticline]]s. I.C. White took Logan's anticlinal trap concept and applied it to searc

...nd the second set is extended to different layers. The study of the Oliana anticline (south-central Spanish Pyrenees) (Fig.8) explains joint networks extended t ...21-Alibrahim-Figure8.png|thumbnail|Figure 8: A geologic map for the Oliana anticline location. (Shackleton, 2005)]]

...ic [[Petroleum generation|generation]] (such as those along the Aylesworth anticline in the Anadarko basin) were probably once filled to the spill point and hav

file:dipmeters_fig6.png|{{figure number|6}}Model of a tilted plunging anticline as it would appear on an arrow plot. ...signature of a tilted plunging anticline. A cross-sectional sketch of the anticline can be produced using the rule of interchangability of perspectives in whic

...1997/07jul/1110/1110.htm Quantitative evaluation of fractures on Monkshood anticline, a detachment fold in the foothills of western Canada]: AAPG Bulletin, vol.

...mation has expanded north and south along the main structure of the Nesson anticline, along with expansion into the central Williston Basin (North Dakota) and e | Discovery Well || Stanolind Oil and Gas Co. #1 Woodrow Starr (Antelope anticline)

...an “elongate, symmetric, northeast-trending, fault-propagation/fault-bend anticline with nearly 800 feet (270m) of structural closure with a 450-foot (150M) oi

...ion is from the ''Trim A'' and ''Glob alt'' reservoirs within the rollover anticline downthrown to the north bounding fault A′. Fault A′ splays southwest of

* Anticline: older rocks on the inside [[File:Structural_Geology_Fig-4.2.png|center|300px|{{figure number|12}}Anticline and syncline folds]]

...mation has expanded north and south along the main structure of the Nesson anticline, along with expansion into the central Williston Basin (North Dakota) and e

...c. For example, we might classify East Anschutz as an elongated asymmetric anticline with a gently dipping back limb and a steeply to overturned forelimb.

...w and C. W. Spencer, eds., Geology of tight gas reservoirs in the Pinedale anticline area, Wyoming and at the Multiwell Experiment site, Colorado: U.S. Geologic

* anticline http://www.glossary.oilfield.slb.com/en/Terms/a/anticline.aspx

...ld]]s. A distinct example of fractured porosity due to tectonics occurs in anticline. Outer arc of a fold bears extension, generating tensional fractures and fa

...are consistent with folding by progressive limb rotation. The core of the anticline is filled with salt, which presumably thickened during [[deformation]], lea

...lies along the crest of the Barrow Arch, an east-west-trending, Cretaceous anticline formed by the northward thrusting of the Brooks Range ([[:file:Mth14ch07f03

...oduction in a stratigraphic accumulation on the north-dipping flank of the anticline also ([[:file:Mth14ch02f01.jpg|Figure 1]]). Consequently, Yowlumne Unit B w

...een 1.3 Ma and the present. The result was the development of the rollover anticline downthrown to fault A′, which is a splay off regional fault A ([[:file:se

Synthetic seismic view of Sand A on an asymmetrical anticline structure is shown on [[:file:GeoWikiWriteOff2021-Muamamr-Figure7.png|Figur

| Fields along the Cabin Creek anticline, Willisten basin || Combined lithological and petrophysical parameters of O

...tratigraphic cross section along part of the north flank of the Wilmington anticline in the Long Beach unit showing log displays. Distance scale is irregular to

...rvoirs_fig3.png|'''Figure 3.''' Cross section through an asymmetrical ramp anticline, Whitney Canyon field, Wyoming, with SCAT and isogen data superimposed. Unc

...to note here that we do not require an actual "structure," such as a domal anticline or a fault closure, only that prospect maps and sections accurately depict

...Except in the narrow foothills ring where the structures are [[thrust]] [[anticline]]s, the structural [[trap]]s consist mainly in the crest of faulted blocks

...zestan, and Fars. Lurestan and Fars are mountainous with deeply breached [[anticline]]s. Khuzestan is divided into two morphological zones: the mountainous Izeh

| Dissolution occurs at crest of anticline or at updip pinchout of a reservoir unit

...C. W. Spencer, eds., 1989, Geology of tight gas reservoirs in the Pinedale anticline area, Wyoming and at the Multiwell Experiment site, Colorado: U.S. Geologic

...sediment units on the downthrown side of the fault and the small rollover anticline or reverse-drag characteristic of this type of fault.

...epositional history of the Greenhorn regressive hemicyclothem, Rock Canyon Anticline, Pueblo, Colorado: SEPM Field Trip Guidebook 4, p. 170–183.</ref> date th

...Antelope Field, fracture development over a basement fault/flexure, Nesson anticline structure; Elm Coulee, a stratigraphic pitchout trap on the southwestern pa ...r et al. at Gulf<ref name=Lindsy2018 /> thought they had found the largest anticline in the world<ref name=Lindsy2018 />. Others<ref> West Texas Geological Soci

...ch and Cincinnati arch to the west, the Cambridge arch and Burning Springs anticline farther eastward, the Rome trough, and the anticlinal fold belts in the App