Lyell Collection

Journal of the Geological Society

Lyell Centre  |   Lyell Collection  |   Subscriptions   |   Geological Society  |   Email alerts  |   Online bookshop  |   Help


Keywords:
Author:
Advanced search>>
This Article
Right arrow Figures Only
Right arrow Full Text
Right arrow Full Text (PDF)
Right arrow Alert me when this article is cited
Right arrow Alert me if a correction is posted
Right arrow Citation Map
Services
Right arrow Email this article to a friend
Right arrow Similar articles in this journal
Right arrow Alert me to new issues of the journal
Right arrow Download to citation manager
Right arrow Request Permissions
Citing Articles
Right arrow Citing Articles via HighWire
Right arrow Citing Articles via Web of Science (51)
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by BLASBAND, B.
Right arrow Articles by VISSER, W.
Right arrow Search for Related Content
GeoRef
Right arrow GeoRef Citation
Journal of the Geological Society; 2000; v. 157; issue.3; p. 615-628
© 2000 Geological Society of London

Regular Article

Late Proterozoic extensional collapse in the Arabian–Nubian Shield

B. BLASBAND1, S. WHITE1, P. BROOIJMANS1, H. DE BOORDER1 & W. VISSER1

1 Structural Geology, Geodynamics Research Institute, The University of Utrecht, PO Box 80021, 3508 TA Utrecht, The Netherlands (e-mail: B.Blasband{at}inter.nl.net)

Scientific editing by Alex Maltman.

A structural and petrological study of the Late Proterozoic rocks in the Wadi Kid area, Sinai, Egypt indicates the presence of an extensional metamorphic core complex in the northern Arabian–Nubian Shield. Gneissic domes throughout the Arabian–Nubian Shield resemble the core complex of the Wadi Kid area and as a result, they are interpreted as extensional metamorphic core complexes. The presence of a widespread phase of extension at the end of the Pan-African period in the Arabian–Nubian Shield requires a new interpretation of the tectonic history of this shield. Three main tectonic phases are recognized in the Late Proterozoic of the Arabian–Nubian Shield. Ophiolites and island-arc remnants are relicts of an oceanic phase, the oldest one. This phase was followed by arc-accretion, well established in the Arabian–Nubian Shield from the presence of individual terranes bordered by sutures, which was responsible for lithospheric thickening. The Late Proterozoic ended with widespread NW–SE extension. The metamorphic core complexes, late-orogenic extensional basins and large strike slip zones were formed during this phase. Similarity of the tectonic evolution of the Arabian–Nubian Shield with the Mesozoic and Early Cenozoic evolution of western North America lead us to conclude that gravitational instability at the final stages of the arc-accretion phase caused the collapse and resulted in extension at the latest stages of the Pan-African orogeny in the Arabian–Nubian Shield.


Keywords: Arabian–Nubian Shield, Wadi Kid area, Pan-African Orogeny, metamorphic core complexes, extension.




This article has been cited by other articles:


Home page
Journal of the Geological SocietyHome page
Y. Be'eri-Shlevin, Y. Katzir, and M. Whitehouse
Post-collisional tectonomagmatic evolution in the northern Arabian-Nubian Shield: time constraints from ion-probe U-Pb dating of zircon
Journal of the Geological Society, 2009; 166: 71 - 85.
[Abstract] [Full Text] [PDF]


Home page
Geological Society, London, Special PublicationsHome page
R. D. Nance, J. B. Murphy, R. A. Strachan, J. D. Keppie, G. Gutierrez-Alonso, J. Fernandez-Suarez, C. Quesada, U. Linnemann, R. D'lemos, and S. A. Pisarevsky
Neoproterozoic-early Palaeozoic tectonostratigraphy and palaeogeography of the peri-Gondwanan terranes: Amazonian v. West African connections
Geological Society, London, Special Publications, 2008; 297: 345 - 383.
[Abstract] [Full Text] [PDF]


Home page
Geological Society of America Special PapersHome page
G. Zulauf, S.S. Romano, W. Dorr, and J. Fiala
Crete and the Minoan terranes: Age constraints from U-Pb dating of detrital zircons
Geological Society of America Special Papers, 2007; 423: 401 - 411.
[Abstract] [Full Text] [PDF]


Home page
Mineral MagHome page
A. M. Abdel-Rahman
Petrogenesis of anorogenic peralkaline granitic complexes from eastern Egypt
Mineralogical Magazine, 2006; 70: 27 - 50.
[Abstract] [Full Text] [PDF]


Home page
Geological MagazineHome page
A. K. ENGVIK and S. ELVEVOLD
Pan-African extension and near-isothermal exhumation of a granulite facies terrain, Dronning Maud Land, Antarctica
Geological Magazine, 2004; 141: 649 - 660.
[Abstract] [Full Text] [PDF]


Home page
Geological MagazineHome page
T. Grenne, T. GRENNE, R. B. PEDERSEN, T. BJERKGARD, A. BRAATHEN, M. G. SELASSIE, and T. WORKU
Neoproterozoic evolution of Western Ethiopia: igneous geochemistry, isotope systematics and U-Pb ages
Geological Magazine, 2003; 140: 373 - 395.
[Abstract] [Full Text] [PDF]


Home page
Geological Society, London, Special PublicationsHome page
B. F. Windley
Continental growth in the Proterozoic: a global perspective
Geological Society, London, Special Publications, 2003; 206: 23 - 33.
[Abstract] [PDF]


Home page
Geological Society, London, Special PublicationsHome page
J. Jacobs, R. Klemd, C. M. Fanning, W. Bauer, and F. Colombo
Extensional collapse of the late Neoproterozoic-early Palaeozoic East African-Antarctic Orogen in central Dronning Maud Land, East Antarctica
Geological Society, London, Special Publications, 2003; 206: 271 - 287.
[Abstract] [PDF]


Home page
Geological Society, London, Special PublicationsHome page
P. R. Johnson and B. Woldehaimanot
Development of the Arabian-Nubian Shield: perspectives on accretion and deformation in the northern East African Orogen and the assembly of Gondwana
Geological Society, London, Special Publications, 2003; 206: 289 - 325.
[Abstract] [PDF]