Effect of permo-carboniferous climate on illite-smectite, Haushi Group Sultanate of Oman
The Late Westphalian to Artinskian Haushi Group in the Sultanate of Oman consists of the glaciogenic Al Khlata Formation and the Gharif Formation which contains marginal marine, coastal plain, and fluvial sediments. The sequence was deposited during a global-warming event following the Permo-Carboni...
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Veröffentlicht in: | Clays and clay minerals 1999-04, Vol.47 (2), p.131-143 |
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