The following article is from The Great Soviet Encyclopedia (1979). It might be outdated or ideologically biased.



a form of bedding in which the strata are inclined in such a way that the dips are directed toward some central point and the strikes describe an arc around the central point

Figure 1. The bedding of rocks in a centrocline

(see Figure 1). Younger rocks occur in the central parts of the arc, while older rocks are found in the lateral parts. A centrocline usually originates at the termination of a syncline where the hinge of the fold rises and the strata forming the fold are closed.

The Great Soviet Encyclopedia, 3rd Edition (1970-1979). © 2010 The Gale Group, Inc. All rights reserved.