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| Creator | Title | Description | Subject | Date | ||
|---|---|---|---|---|---|---|
| 1 |
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Brown, Francis Harold | Gombe group basalts and initiation of pliocene deposition in the Turkana depression, northern Kenya and southern Ethiopia | A little before 4 Ma ago, deposition of Pliocene and Pleistocene strata described as the Omo Group began in the Turkana and Omo basins of northern Kenya and southern Ethiopia. Soon after, basaltic magma erupted as thin lava flows, and intruded as dykes into the oldest Pliocene strata of the basin. T... | 2004 | |
| 2 |
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Brown, Francis Harold | The lower Omo basin | The boundaries of the Lower Omo Basin have been mapped by Fuchs (1939) and by Butzer (1970, 1971) in a general way. The structural features and physiography of the eastern and central part of the Lower Omo Basin are best expressed on the maps of Davidson et al. (1973). Walsh and Dodson (1969) have m... | 1983 | |
| 3 |
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Brown, Francis Harold | Pliocene/pleistocene formations in the lower omo basin, southern Ethiopia | Following a two month geological reconnaissance by one of us (FHB) in 1966, four seasons of fieldwork by members of the Omo Research Expedition has added greatly to our previous, scanty knowledge of the late Cenozoic history of the lower Omo basin in southern Ethiopia. Eduard Suess (in: von Hohnel ... | 1970 | |
| 4 |
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Chapman, David S.; Picard, M. Dane | Heat flow in the Uinta Basin determined from bottom hole temperature (BHT) data | The thermal resistance (or Bullard) method is used to judge the utility of petroleum well bottom-hole temperature data in determining surface heat flow and subsurface temperature patterns in a sedimentary basin. Thermal resistance, defined as the quotient of a depth parameter AZ and thermal con... | Thermal analysis; Bottom hole temperature | 1984-04 |
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