Pare-Usambara mountain chain

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Journal Article
Journal: GSA Bulletin
Published: 01 March 2004
GSA Bulletin (2004) 116 (3-4): 490–510.
... of (1) Neogene half- graben morphology (<2–3-km-deep basins) and (2) amount of extension. A similar half-graben system, but with a western-tilted polarity, is suspected to lie further east, at the foot of the 1000-m-high PareUsambara fault scarp in the Pangani rift arm ( Fig. 11...
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