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The Neoproterozoic Fiq glaciation and its aftermath, Huqf supergroup of Oman

Abstract:

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 and siltstones of the Masirah Bay Formation. The Fiq Member and Hadash-Masirah Bay Formations are well exposed in the core of the Jebel Akhdar of northern Oman and provide a valuable insight into the ...

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Publication status:
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Institution:
University of Oxford
Division:
MPLS
Department:
Earth Sciences
Role:
Author
Journal:
BASIN RESEARCH More from this journal
Volume:
16
Issue:
4
Pages:
507-534
Publication date:
2004-12-01
DOI:
EISSN:
1365-2117
ISSN:
0950-091X
Language:
English
Pubs id:
pubs:82542
UUID:
uuid:8fc80bb8-36b3-440f-bb8c-5554c600ff7c
Local pid:
pubs:82542
Source identifiers:
82542
Deposit date:
2012-12-19

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