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A long, narrow depression that borders an orogenic belt, such as an island arc, on the convex side.
McGraw-Hill Dictionary of Scientific & Technical Terms, 6E, Copyright © 2003 by The McGraw-Hill Companies, Inc.
The following article is from The Great Soviet Encyclopedia (1979). It might be outdated or ideologically biased.



(1) Another term for a marginal deep.

(2) The late developmental stage of a marginal deep, characterized by the accumulation of an upper molasse, formed by coarse continental sediment.

The Great Soviet Encyclopedia, 3rd Edition (1970-1979). © 2010 The Gale Group, Inc. All rights reserved.
References in periodicals archive ?
Recent studies carried on in the Carpathian Foredeep [13] demonstrated that such migration can be recorded in the seismic sections as so-called "gas chimneys." One chimney was confirmed by surface geochemical survey by Marzec et al.
The Safed Koh Block is situated in the tribal areas of District Dera Ghazi Khan of Punjab Province and located west of Sulaiman Foredeep in the Middle Indus Basin of Pakistan.
Eastern Venezuela remained a continental passive margin until the gradual arrival of the peripheral bulge by Late Eocene time and the Caribbean foredeep by Oligocene time [7].
Late Cenozoic tectonics and sedimentation in the northwestern Himalayan foredeep, Eastern limb of the northwest Syntaxis and regional synthesis.
The foredeep depression started to develop in the inner Zagros after deposition of the widespread Upper Oligocene platform carbonate (Lower Asmari Formation) [23] and migrated southwestward down to its present position in the Persian Gulf [1].
The area of interest is found in the northern part of Western Carpathian Foredeep at the contact of geological units of the Bohemian Massif and the Carpathian System [18].
Ancient river systems in the Himalayan foredeep, Chinji village area, northern Pakistan.
They suggested a rough equilibrium between the modelled northward plate motion of the Indian subcontinent and the southward displacement of depositional processes within the foredeep. There is an increase in sedimentation in all the basins at ~ 10 Ma (the onset of Nagri Formation).
The Rharb Basin is a foredeep basin located in the external zone of the Rif Folded belt.
The Sebou permit lies to the north-east of Rabat in the Rharb Basin, which is a foredeep basin located in the external zone of the Rif Folded belt.