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
✦ LIBER ✦
Reply to Discussion of “Geological setting and tectonic subdivision of the Neoproterozoic Orogenic Belt of Tuludimtu, Western Ethiopia” [A. Allen, G. Tadesse, Journal of African Earth Sciences 36 (2003) 329–343]
✍ Scribed by Alistair Allen; Gebremedhin Tadesse
- Book ID
- 108155298
- Publisher
- Elsevier Science
- Year
- 2005
- Tongue
- English
- Weight
- 242 KB
- Volume
- 41
- Category
- Article
- ISSN
- 1464-343X
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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,