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An anticlinorium is a large anticline in which a series of minor anticlinal folds are superimposed. Examples include the Late Jurassic to Early Cretaceous Purcell Anticlinorium in British Columbia [ 1 ] and the Blue Ridge anticlinorium of northern Virginia and Maryland in the Appalachians, [ 6 ] or the Nittany Valley in central Pennsylvania.
Anticlinal trap. An anticline is an area of the subsurface where the strata have been pushed into forming a domed shape. If there is a layer of impermeable rock present in this dome shape, then water-insoluble hydrocarbons can accumulate at the crest until the anticline is filled to the spill point (the highest point where hydrocarbons can escape the anticline).
Anticlinal traps are formed by folding of rock. For example, if a porous sandstone unit covered with low permeability shale is folded into an anticline, it may form a hydrocarbons trap, oil accumulating in the crest of the fold. Most anticlinal traps are produced as a result of sideways pressure, folding the layers of rock, but can also occur ...
Between 2012 and 2019, cervical cancer incidence among women ages 20 to 24 dropped by 65%, an American Cancer Society report found. In addition, fewer teens and young adults get genital warts as a ...
Anticlinal may refer to: Anticline , in structural geology, an anticline is a fold that is convex up and has its oldest beds at its core Anticlinal, in stereochemistry, a torsion angle between 90° to 150°, and –90° to –150°; see Alkane_stereochemistry
A 2022 KFF Women's Health Survey found that 42% of uninsured women had received a cervical cancer screening in the past year, compared to 64% with private insurance and 56% of those with Medicaid.
President Donald Trump, from left, actress Cheryl Hines, and Robert F. Kennedy Jr., the new secretary of Health and Human Services (HHS), during a ceremony in the White House in Washington, D.C ...
The Weald–Artois Anticline, or Wealden Anticline, is a large anticline, a geological structure running between the regions of the Weald in southern England and Artois in northern France. The fold formed during the Alpine orogeny , from the late Oligocene to middle Miocene as an uplifted form of the Weald basin through inversion of the basin.