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Tectonic evolution of the western Kunlun orogenic belt, western China

โœ Scribed by Wang Zhihong


Book ID
116700502
Publisher
Elsevier Science
Year
2004
Tongue
English
Weight
515 KB
Volume
24
Category
Article
ISSN
0743-9547

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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,