How To Use Anticlinal In A Sentence
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The salt continued moving along lines of least resistance and began to push upward, bowing up the overlying sedimentary rocks to form the classic elongated anticlinal structure.
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The ridge trended north-west, as most others did in this extensive basin; and this direction being nearly parallel to that of the coast ranges further northward, seemed to afford additional reason for expecting to find anticlinal and synclinal lines, and, consequently, rivers, much in the same direction.
Journal of an Expedition into the Interior of Tropical Australia
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The expelled hydrothermal fluids were trapped in cap-rock situations inside anticlinal zones, such as the major lithological contrast between siliceous limestones and black shales at the flanks of the Arnsberg anticline.
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This process is initiated by anticlinal and periclinal divisions of a few callus cells only.
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Strain differences between anticlinal and synclinal domains of concentric fold stacks require discontinuities between the two types of domain to maintain overall strain compatibility.
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These metamorphic and plutonic igneous rocks form the uplifted core of the broadly anticlinal Owl Creek Mountains, a mountain range that formed during the Late Cretaceous.
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Low-grade volcanic and sedimentary rocks are widely exposed within this elongate anticlinal window.
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The rocks are on the west flank of the Monument uplift, a 60-mile-long north-trending anticlinal structure.
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The precise form of the anticlinal folds at the base of the overburden layer is uncertain because of both limited seismic resolution and complexities due to the near convergence of conjugate-fault pairs.
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The origin of this circular anticlinal structure has been the subject of a longstanding debate.
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Anticlinal structures that include some landward-verging reverse faults (referred to as antithetic) are produced, with create the tectonic ridges that you can see in the bathymetric map in Figs. 7 and 8 above.
Clastic Detritus
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Fulongquan gas field is situated in transition zone between the massif in southeast of Songliao basin and the center depressed area. It is made up of south and north anticlinal high.
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Polygon boundaries coincide with anticlinal ridges on the interface between the faulted sequence and an underlying 35 m thick low velocity, low density, overpressured layer.
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These subterranean muds are being uplifted into steeply dipping, anticlinal structures cored by strike-slip faulting.
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The Yakima Folds ecoregion consists of unforested anticlinal ridges composed of layer upon layer of basalt many thousands of feet thick.
Ecoregions of Oregon (EPA)
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The fluids were trapped in permeability-controlled positions within anticlinal zones, where fluid cooling induced deposition of stibnite and sulphosalts.
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However, with progressive deformation, markers above anticlinal crests were extended in the shortening direction.
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However, as the thrust sheets grow, the outer area of their anticlinal crest is extended.
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Watterson et al. explained that this situation can arise due to local extension and thinning associated with anticlinal folding of the beds overlying the ridges in the low velocity layer.
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Fulongquan gas field is situated in transition zone between the massif in southeast of Songliao basin and the center depressed area. It is made up of south and north anticlinal high.
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This mountain illustrates both anticlinal and synclinal folding and the way in which the two different fold types react to weathering and erosion.
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Their macrostructures are similar to those of present-day soils, with pseudo-anticlinal structures and cuspate structures comparable to those produced by the expansion and contraction of swelling clays.
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Features shared by the Lake Hope structures and many physical diapiric models are local ductile extension and thinning of the overburden overlying anticlinal ridges of the active boundary.
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The later collapse of the mutual hanging walls of conjugate fault pairs has therefore created graben along the original anticlinal ridges that preserve the form of the anticlines but have destroyed the ridges.
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There are favorable condition for formation of non anticlinal oil & gas pools in the Tarim Basin.
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There are favorable condition for formation of non anticlinal oil & gas pools in the Tarim Basin.
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The concavo-concave shape of the anticlinal cell walls adjacent to the guard cells, reflects the bowed shape of the guard cells.
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Although it is counterintuitive for a graben to overlie a ridge, it has long been recognized that graben can result from local extension and thinning in the anticlinal domains that overlie linear ridges.
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Their macrostructures are similar to those of present-day soils, with pseudo-anticlinal structures and cuspate structures comparable to those produced by the expansion and contraction of swelling clays.
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Moreover, in sun leaves, anticlinal and periclinal divisions occur almost synchronously.
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The principal Formation is orientated in an east-west direction, and comprises both a long anticlinal and synclinal, the latter elevated over some degrees.
Miguasha Provincial Park, Canada
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Anticlinal folds occupy the mutual hanging walls of conjugate fault pairs with synclines occupying mutual footwalls between adjacent pairs.
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The asymmetry of folds at shallower levels in the overburden sequence suggest that the original anticlinal ridges at the base of the overburden sequence were cuspate.
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The unfaulted model produces an anticlinal uplift that is substantially narrower and more elevated than the uplift of a purely elastic lithosphere without a ductile lower crust.
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These elongate anticlinal domes have gentle to moderate dips on their flanks, and are cut by several thrust faults that may be linked to a deeper system.
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Secondly, along-strike displacement minima, fault jogs and anticlinal intrabasin highs often form at, and represent the location of, palacosegment boundaries and subsequent zones of segment linkage.
