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Journal of the Geological Society; 2006; v. 163; issue.1; p. 165-183;
DOI: 10.1144/0016-764904-164
© 2006 Geological Society of London

Original Article

Rift-initiation development of normal fault blocks: insights from the Hammam Faraun fault block, Suez Rift, Egypt

C.A.L. Jackson1,2, R.L. Gawthorpe1, C.W. Leppard1,3 & I.R. Sharp1,3

1 Basin and Stratigraphic Studies Group, School of Earth, Atmospheric and Environmental Sciences, University of Manchester, Oxford Road, Manchester M13 9PL, UK
2 Present address: Department of Earth Sciences and Engineering, Prince Consort Road, Imperial College, London SW7 2BP, UK (e-mail: c.jackson@imperial.ac.uk)
3 Present address: Norsk Hydro Research Centre, Sandsliveien 90, 5020, Bergen, Norway

An integrated structural and stratigraphic study of the Hammam Faraun fault block, Suez Rift, Egypt, provides insights into the rift-initiation tectonostratigraphic evolution of the crustal-scale normal fault blocks. The shallow marine to offshore Tayiba Formation (Lower Oligocene) represents the youngest preserved pre-rift unit, and key stratal surface development indicates that relative sea-level variations exerted a marked control on its stratigraphic evolution. A major sea-level fall, which may have been a regional (i.e. eustatic) event, occurred during the mid-Oligocene and was synchronous with the onset of rifting. A major erosional unconformity (the base synrift unconformity) formed in response to the sea-level fall and defines a series of NNE–SSW- to NE–SW-trending palaeovalleys up to 40 m deep by 500 m wide, which are infilled by continental deposits and volcanic rocks of the Abu Zenima Formation (Upper Oligocene–Lower Miocene). During the rift initiation, palaeovalleys controlled depositional patterns and the evolving fault-controlled topography was insufficient to modify drainage patterns. Through time, however, surface-breaking faults began to exert a marked control on deposition. This study indicates the complexity that can occur during the rift-initiation phase caused by extrabasinal factors such as eustatic sea-level variations and antecedent drainage.





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M. KRABBENDAM, T. PRAVE, and D. CHEER
A fluvial origin for the Neoproterozoic Morar Group, NW Scotland; implications for Torridon Morar Group correlation and the Grenville Orogen foreland basin
Journal of the Geological Society, 2008; 165: 379 - 394.
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