The N-S trending Tuludimtu Belt in the extreme west of Ethiopia has been subdivided into five lithotectonic domains, from east to west, the Didesa, Kemashi, Dengi, Sirkole and Daka domains. The Kemashi, Dengi and Sirkole Domains, forming the core of the belt, contain volcano-sedimentary successions,
Discussion of “Geological setting and tectonic subdivision of the Neoproterozoic Orogenic Belt of Tuludimtu, Western Ethiopia” [Journal of African Earth Sciences 36 (2003) 329–343]
✍ Scribed by Tadesse Alemu
- Publisher
- Elsevier Science
- Year
- 2005
- Tongue
- English
- Weight
- 318 KB
- Volume
- 41
- Category
- Article
- ISSN
- 1464-343X
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✦ Synopsis
The paper of [Geological setting and tectonic subdivision of the Neoproterozoic orogenic belt of Tuludimtu, Western Ethiopia, Journal of African Earth Sciences 36 (2003) 329-343] describes the lithology and structure, and discusses the tectonic evolution of the Tulu Dimtu belt in the Precambrian of Western Ethiopia. There can be no doubt that the paper adds knowledge to the understanding of the geology of the Precambrian of Western Ethiopia in particular and to the Precambrian geology of the country as a whole. Moreover, the paper adds to a growing body of literature about the geology of the country. However, I disagree with Allen and Tadesse on the following points: (1) tectonic subdivision of the belt, (2) interpretation of structural evolution of the belt, and (3) interpretation of the tectonic setting of the belt.
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