The following article is from The Great Soviet Encyclopedia (1979). It might be outdated or ideologically biased.
an extensive linear uplift formed at a certain stage in the development of the geosynclinal system. Intrageoanticlines are contrasted with the intrageosynclines of equal length (1,000–3,000 km) that separate them.
The Great Soviet Encyclopedia, 3rd Edition (1970-1979). © 2010 The Gale Group, Inc. All rights reserved.