A morphotectonic study of an extensional fault zone in a magma-rich rift: the Baringo Trachyte Fault System, central Kenya Rift
- 1 May 2000
- journal article
- Published by Elsevier in Tectonophysics
- Vol. 320 (2) , 87-106
- https://doi.org/10.1016/s0040-1951(00)00069-x
Abstract
No abstract availableKeywords
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