- Startpagina tijdschrift
- Volume 101 (1978)
- Volume complet
- Structural and sedimentological evolution of the Mesopotamian geosyncline (N.-Iraq)
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Weergave(s): 203 (5 ULiège)
Download(s): 233 (1 ULiège)
Weergave(s): 203 (5 ULiège)
Download(s): 233 (1 ULiège)
Dhya Al-Rawi 
Structural and sedimentological evolution of the Mesopotamian geosyncline (N.-Iraq)
(Volume 101 (1978) — Volume complet)
Article
Abstract
The type and the facies of the sediments are discussed in relation to the various kinds of tectonic movements.
A facies change from NW to SE in the Lower Jurassic indicates the existence of NE-SW trending basement blocks, along which horizontal and vertical movements took place.
Facies changes and the variation in thickness of the Gercus Formation (Eocene) observed in a number of structural units provides proof of synsedimentary folding.
A shift in the axis of the northern basin from a NW-SE trend in the SE part of Iraq to E-W strike in NW Iraq was apparently controlled by faults.
Om dit artikel te citeren:
Dhya Al-Rawi, «Structural and sedimentological evolution of the Mesopotamian geosyncline (N.-Iraq)», Annales de la Société géologique de Belgique [En ligne], Volume 101 (1978), Volume complet, 173 - 177 URL : https://popups.uliege.be/0037-9395/index.php?id=4458.
Over : Dhya Al-Rawi
Geology Department, University of Mosul, Iraq.