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- W4214897036 abstract "Dr F. Moseley said that having recently had the opportunity to walk over these old volcanoes he had much enjoyed this paper. He observed that the late-Cretaceous early-Tertiary Aden Traps and the late-Tertiary Aden Volcanics, together with similar rocks in Ethiopia covered many thousands of square miles of unmapped country with tremendous research potential, particularly so on this critical segment of the Earth’s surface. There were a number of more obvious queries to which Dr Moseley thought the authors may be able to provide some answers. The first concerned the relation between the Aden Traps and the Aden Volcanics. Were they in fact completely separate from each other, or were there some areas where vulcanicity had been continuous throughout the Tertiary? The similarity of volcanic sequences in both suggested that this might be the case. It was also unusual that there was a near absence of olivine basalt from the Aden volcanoes, when such rocks were common if not predominant in other outcrops of Aden Volcanics, for example at Ataq, along the northern margin (at least) of the Shuqra mass and on the Red Sea islands, not to mention the ten thousand feet plus of olivine basalts within the Aden Traps near Dhala. Another item of interest was the linear, almost east-west trend of volcanoes from the mouth of the Red Sea to Aden, presumably related to the Gulf of Aden rift, but the much more impressive Shuqra mass was to the north-east and did not continue this line. Was" @default.
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- W4214897036 date "1968-10-01" @default.
- W4214897036 modified "2023-09-27" @default.
- W4214897036 title "Discussion" @default.
- W4214897036 doi "https://doi.org/10.1144/gsjgs.124.1.0307" @default.
- W4214897036 hasPublicationYear "1968" @default.
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