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Hammam Faraun Fault

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Journal Article

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

C.A.L. Jackson, R.L. Gawthorpe, C.W. Leppard, I.R. Sharp
Published: 01 January 2006
Journal of the Geological Society (2006) 163 (1): 165–183.
DOI: https://doi.org/10.1144/0016-764904-164
...C.A.L. Jackson; R.L. Gawthorpe; C.W. Leppard; I.R. Sharp Abstract 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...
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Evolution and structural style of relay zones in layered limestone–shale sequences: insights from the Hammam Faraun Fault Block, Suez rift, Egypt

E. Bastesen, A. Rotevatn
Published: 01 July 2012
Journal of the Geological Society (2012) 169 (4): 477–488.
DOI: https://doi.org/10.1144/0016-76492011-100
... transform, which accommodates continued extension in the Red Sea rift ( Cochran 1983 ). Fig. 1. ( a ) Simplified geological map of the Hammam Faraun Fault Block, modified from Moustafa (2004) and Sharp et al . (2000) . Inset shows regional map. ( b ) Simplified geological map of the study area...
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( a ) Simplified geological map of the <span class="search-highlight">Hammam</span> <span class="search-highlight">Faraun</span> <span class="search-highlight">fault</span> block (modified ...

( a ) Simplified geological map of the Hammam Faraun fault block (modified ...

Published: 01 March 2002
Fig. 3 ( a ) Simplified geological map of the Hammam Faraun fault block (modified from Moustafa 1993 ). Inset shows the regional geographical setting. Boxed area is shown in Figure 4 . ( b ) Simplified cross-section through the Hammam Faraun fault block, illustrating the half-graben and intra
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( a ) Simplified geological map of the <span class="search-highlight">Hammam</span> <span class="search-highlight">Faraun</span> <span class="search-highlight">Fault</span> Block, modified ...

( a ) Simplified geological map of the Hammam Faraun Fault Block, modified ...

Published: 01 July 2012
Fig. 1. ( a ) Simplified geological map of the Hammam Faraun Fault Block, modified from Moustafa (2004) and Sharp et al . (2000) . Inset shows regional map. ( b ) Simplified geological map of the study area. Location is indicated in ( a ). The location of Figure 4 is shown.
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Stratigraphy of the <span class="search-highlight">Hammam</span> <span class="search-highlight">Faraun</span> <span class="search-highlight">Fault</span> Block. Host rocks studied are shade...

Stratigraphy of the Hammam Faraun Fault Block. Host rocks studied are shade...

Published: 01 July 2012
Fig. 2. Stratigraphy of the Hammam Faraun Fault Block. Host rocks studied are shaded grey.
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( a ) Simplified geological map of the <span class="search-highlight">Hammam</span> <span class="search-highlight">Faraun</span> <span class="search-highlight">fault</span> block (modified ...

( a ) Simplified geological map of the Hammam Faraun fault block (modified ...

Published: 01 January 2006
Fig. 1.  ( a ) Simplified geological map of the Hammam Faraun fault block (modified from Moustafa 1993 ; Sharp et al . 2000 a ). Faults discussed (STFZ, South Thal fault zone; WTFZ, Wadi Thal fault zone; ETFZ, East Tanka fault zone; NFZ, Nukhul fault zone; BMFZ, Baba-Markha fault zone
Journal Article

Fault-controlled dolomitization in a rift basin

Cathy Hollis, Eivind Bastesen, Adrian Boyce, Hilary Corlett, Robert Gawthorpe, Jesal Hirani, Atle Rotevatn, Fiona Whitaker
Journal: Geology
Published: 01 March 2017
Geology (2017) 45 (3): 219–222.
DOI: https://doi.org/10.1130/G38s394.1
... structurally complex dolomite bodies. The Suez Rift in Egypt ( Fig. 1 ) is the aborted arm of the Red Sea rift. The Hammam Faraun fault (HFF) defines the western side of the HFF block and tips out northward ( Fig. 1 ). The partially dolomitized Eocene (Ypresian) Thebes Formation ( Fig. 1B ) is exposed...
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Sedimentology and Sequence Stratigraphy of Early Syn-Rift Tidal Sediments: The Nukhul Formation, Suez Rift, Egypt

Ian D. Carr, Rob L. Gawthorpe, Christopher A.L. Jackson, Ian R. Sharp, Ali Sadek
Published: 01 May 2003
Journal of Sedimentary Research (2003) 73 (3): 407–420.
DOI: https://doi.org/10.1306/111402730407
...Ian D. Carr; Rob L. Gawthorpe; Christopher A.L. Jackson; Ian R. Sharp; Ali Sadek Abstract Facies and tectono-stratigraphic models for the tidally influenced Miocene Nukhul Formation are presented, based on outcrop data from Hammam Faraun fault block, Suez Rift, Egypt. Deposits of the Nukhul...
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Interpretation of major <span class="search-highlight">faults</span> and shear zones in the Gulf of Suez area. HF...

Interpretation of major faults and shear zones in the Gulf of Suez area. HF...

Published: 01 June 2002
Figure 3 Interpretation of major faults and shear zones in the Gulf of Suez area. HF = Hammam Faraun fault block; HA = Hadahid fault block; ZAZ = Zaafarana accommodation zone; MAZ = Morgan accommodation zone.
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(A) Simplified geologic map (modified from Moustafa and Abdeen, 1992 ) and...

(A) Simplified geologic map (modified from Moustafa and Abdeen, 1992 ) and...

Published: 01 June 2002
Figure 7 (A) Simplified geologic map (modified from Moustafa and Abdeen, 1992 ) and (B) structural cross section of the southernmost part of the Hammam Faraun block showing the Bir El Markha monocline (relay ramp) between the Baba and Hammam Faraun faults. Symbols designate the following rocks
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Simplified geologic map of the east-central part of the Suez rift showing t...

Simplified geologic map of the east-central part of the Suez rift showing t...

Published: 01 June 2002
Figure 15 Simplified geologic map of the east-central part of the Suez rift showing the major jump (offset) between the Araba and Hammam Faraun faults and their linkage by a zigzag fault array. See Figure 2 for legend.
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Idealized chronostratigraphic diagram illustrating the development of forma...

Idealized chronostratigraphic diagram illustrating the development of forma...

Published: 01 May 2003
Figure 2 Idealized chronostratigraphic diagram illustrating the development of formations across the Hammam Faraun fault block. The Nukhul Formation was deposited in the hanging-wall depocenters of early-formed fault segments. Fault movement was later concentrated on major block-bounding faults.
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A: Regional geological map and location map (inset), Suez Rift, Egypt. B: G...

A: Regional geological map and location map (inset), Suez Rift, Egypt. B: G...

Published: 01 March 2017
Figure 1. A: Regional geological map and location map (inset), Suez Rift, Egypt. B: Geological map of Hammam Faraun fault (HFF) block (modified after Moustafa, 2003 ). C: HFF block viewed looking northeast (see B).
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Interpretative line drawing of a photo panorama illustrating the preservati...

Interpretative line drawing of a photo panorama illustrating the preservati...

Published: 01 January 2006
Fig. 14.  Interpretative line drawing of a photo panorama illustrating the preservation of latest pre-rift units (i.e. Tanka and Tayiba Formations) in a fault-bounded graben along the eastern margin of the Hammam Faraun fault block in the hanging wall of the Thal fault. (See Fig. 1 for location
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Composite stratigraphic log of the late pre-rift (Late Oligocene) to early ...

Composite stratigraphic log of the late pre-rift (Late Oligocene) to early ...

Published: 01 January 2006
Fig. 3.  Composite stratigraphic log of the late pre-rift (Late Oligocene) to early synrift (Late Oligocene–Early Miocene) stratigraphy of the Hammam Faraun fault block. It should be noted that the Tayiba Formation may be locally absent because of erosion along the base synrift unconformity
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Detailed geological map of the Wadi Tanka area, southern <span class="search-highlight">Hammam</span> <span class="search-highlight">Faraun</span> faul...

Detailed geological map of the Wadi Tanka area, southern Hammam Faraun faul...

Published: 01 March 2002
Fig. 4 Detailed geological map of the Wadi Tanka area, southern Hammam Faraun fault block, Suez rift. See Figure 2 a for location. FS refers to fault segments referred to in the text. Cross sections (e.g. Fig. 7 a, b, c) are marked. Inset shows the along-strike footwall uplift profile
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A: δ 18 O and δ 13 C for dolostone and whole-rock unaltered limestone (dash...

A: δ 18 O and δ 13 C for dolostone and whole-rock unaltered limestone (dash...

Published: 01 March 2017
Figure 3. A: δ 18 O and δ 13 C for dolostone and whole-rock unaltered limestone (dashed oval), Hammam Faraun fault area, Egypt. VPDB—Vienna Peedee belemnite. B: Rare earth element data normalized to Post-Archean Australian Shale (PASS). C: Strontium isotope ratios relative to seawater strontium
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Fluid circulation and dolomite formation in response to progressive rifting...

Fluid circulation and dolomite formation in response to progressive rifting...

Published: 01 March 2017
Figure 4. Fluid circulation and dolomite formation in response to progressive rifting and development of faults, Hammam Faraun fault (HFF) area, Egypt. A: Rift initiation. Cool seawater is drawn down discrete open faults on proto-footwall, heated, and convected within Nubian Sandstone. Buoyant
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Fluid circulation and dolomite formation in response to progressive rifting...

Fluid circulation and dolomite formation in response to progressive rifting...

Published: 01 March 2017
Figure 4. Fluid circulation and dolomite formation in response to progressive rifting and development of faults, Hammam Faraun fault (HFF) area, Egypt. A: Rift initiation. Cool seawater is drawn down discrete open faults on proto-footwall, heated, and convected within Nubian Sandstone. Buoyant
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Simplified stratigraphic logs illustrating variations in the magnitude of e...

Simplified stratigraphic logs illustrating variations in the magnitude of e...

Published: 01 January 2006
Fig. 8.  Simplified stratigraphic logs illustrating variations in the magnitude of erosion along the base synrift unconformity across the Hammam Faraun fault block. Erosion estimates are a minimum based on the maximum preserved thickness of the Tayiba Formation ( c . 56 m) and the recorded