| Reference Type | Journal (article/letter/editorial) |
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| Title | The Development of the Mid-Zambezi Valley in Northern Rhodesia since Early Karroo Times |
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| Journal | Geological Magazine |
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| Authors | Tavener-Smith, R. | Author |
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| Year | 1958 (April) | Volume | 95 |
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| Issue | 2 |
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| Publisher | Cambridge University Press (CUP) |
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| DOI | doi:10.1017/s0016756800062683 |
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| Generate Citation Formats |
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| Mindat Ref. ID | 248757 | Long-form Identifier | mindat:1:5:248757:5 |
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| GUID | 0 |
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| Full Reference | Tavener-Smith, R. (1958) The Development of the Mid-Zambezi Valley in Northern Rhodesia since Early Karroo Times. Geological Magazine, 95 (2) 105-118 doi:10.1017/s0016756800062683 |
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| Plain Text | Tavener-Smith, R. (1958) The Development of the Mid-Zambezi Valley in Northern Rhodesia since Early Karroo Times. Geological Magazine, 95 (2) 105-118 doi:10.1017/s0016756800062683 |
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| In | (1958, April) Geological Magazine Vol. 95 (2) Cambridge University Press (CUP) |
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| Abstract/Notes | AbstractKarroo sedimentation in the mid-Zambezi area presents an instance of deposition in an intra-cratonic basin during a complete climatic semi-cycle. Mention is made of the tectonic factors which controlled the course of Karroo sedimentation in the area, and the nature of the pre-Karroo surface is commented upon. An account is given of the depositional history of the mid-Zambezi basin during the Karroo period. The structural development of the region since Karroo times is outlined, and it is suggested that the present valley is essentially a downwarped and eroded part of the peneplain which still forms the adjacent plateau to the north-west. |
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These are possibly similar items as determined by title/reference text matching only.
