The Neoproterozoic Fiq glaciation and its aftermath, Huqf supergroup of Oman
The < 1.5-km thick Fiq Member of the Ghadir Manqil Formation, Huqf Supergroup, Oman, contains a succession of Marinoan-age glacially and non- glacially influenced deposits overlain by a transgressive, 13C-depleted, deep-water dolostone (Hadash Formation) that deepens up into the marine shales...
| Asıl Yazarlar: | , , |
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| Materyal Türü: | Journal article |
| Dil: | English |
| Baskı/Yayın Bilgisi: |
2004
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