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Monocline

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monocline
a local steepening in stratified rocks with an otherwise gentle dip

monocline [′män·ə‚klīn]
(geology)
A stratigraphic unit that dips from the horizontal in one direction only, not as part of an anticline or syncline.

Monocline 

formation of rock strata in which the strata are gently tilted in one direction. It is usually a limb of a broad and gentle uplift or of a depression of strata. Monoclines are especially typical of platforms, where they are confined to the limbs of anteclises and syneclises. An example of a monocline is the structure formed by Paleozoic beds from the southern slope of the Baltic crystalline shield toward the center of the Moscow syneclise; the inclination of the strata is calculated to be 2–2.5 m per kilometer of length.



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We should further discuss the reason why a monocline phase is formed after material received cold work.
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