Origin and variability of a terminal Proterozoic primary silica precipitate, Athel Silicilyte, South Oman Salt Basin, Sultanate of Oman

Author:

Al Rajaibi Ibrahim M.12,Hollis Cathy2,Macquaker Joe H.2

Affiliation:

1. Petroleum Development Oman, Exploration Department; P.O.Box 81, Muscat 100 Sultanate of Oman

2. School of Earth, Atmospheric and Environmental Sciences; University of Manchester; Williamson Building, Oxford Road Manchester M13 9PL UK

Funder

Petroleum Development Oman

Publisher

Wiley

Subject

Stratigraphy,Geology

Reference94 articles.

1. Hydrothermal chert and associated siliceous rocks from the northern Pacific - their geological significance as indication of ocean ridge activity;Adachi;Sed. Geol.,1986

2. Iron(III)-reduction in a low-organic-carbon brackish-marine system;Adams;J. Sed. Res.,2006

3. Sedimentological evidence for bottom-water oxygenation during deposition of the Natih-B intrashelf basin sediments: Upper Cretaceous carbonate source rock, Natih Formation, North Oman;Al Balushi;GeoArabia,2011

4. Influence of oxic diagenesis on source potential and lithofacies cyclicity: insight from Cenomanian Natih-B Member intrashelf basinal carbonates;Al Balushi;Oman. Petrol. Geosci.,2011

5. Al Rajaibi , I 2011 Origin and variability of the Late Precambrian-Cambrian Athel Silicilyte, South Oman Salt Basin University of Manchester 301

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