Discussion of Ophiolites in Northeast and East Africa: Implications for Proterozoic Crustal Growth Journal
Abstract
W. R. Church writes: In discussing the Pan-African geology of Northeast and East Africa, Berhe (1990) affirms that ophiolite decorated lineaments in the Arabian-Nubian Shield represent suture zones. The difference of opinion between Berhe (1990) and Stern et al. (1989) concerning the location of the supposed suture zones of northern Sudan and southern Egypt, is a clear illustration of the ambiguity that may arise through the uncritical use of this paradigm. Whereas Berhe considers the Sol Hamed-Wadi Onib ophiolite belt to represent in situ oceanic material located along a north-south trending extension of the Saudi Arabian Yanbu-Sol Hamed ‘suture’, Stern et al. 1989 link the latter with the east-west trending Allaqi-Heiani ophiolite belt, which they consider to be a major east-west suture ‘extending well into the interior of North Africa. This important difference in opinion is a clear indication of the arbitrary nature of suture selection based solely on the distribution of ophiolitic rocks. Furthermore, neither explanation may be correct.
Recommended Citation
W. R. Church et al., "Discussion of Ophiolites in Northeast and East Africa: Implications for Proterozoic Crustal Growth Journal," Journal of the Geological Society, vol. 148, no. 3, pp. 600 - 606, Geological Society, May 1991.
The definitive version is available at https://doi.org/10.1144/gsjgs.148.3.0600
Department(s)
Geosciences and Geological and Petroleum Engineering
Geographic Coverage
Africa
Time Period
Proterozoic
International Standard Serial Number (ISSN)
0016-7649
Document Type
Article - Journal
Document Version
Citation
File Type
text
Language(s)
English
Rights
© 1991 Geological Society, All rights reserved.
Publication Date
01 May 1991