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Wadi Wasit

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Series: GCSSEPM
Published: 01 December 1997
DOI: 10.5724/gcs.97.18.0377
EISBN: 978-1-944966-31-7
... surfaces) is therefore less than the number of paleontologically defined sequences. Terraces T 00 and T 20 are sequence boundaries, and subsurface evidence suggests that T 40 is a condensed interval and that T 50 is an erosional unconformity (sequence boundary). Field observations of T 10 at Wadi Thal...
Image
Four sub-basins of the Hammam Farraun fault block. From north to south, Wad...
Published: 01 May 2003
Figure 9 Four sub-basins of the Hammam Farraun fault block. From north to south, Wadi Wasit, Thal Ridge, Wadi Tanka, and Wadi Nukhul, have different sediment thicknesses, reflecting unique fault movement histories during early syn-rift times. See Figure 1 for locations.
Image
Figure 2. Lithostratigraphy, conodont zones, and faunal ranges of upper par...
in > Geology
Published: 01 September 2004
Figure 2. Lithostratigraphy, conodont zones, and faunal ranges of upper part of Wasit block. Dots indicate sample horizons. Ammonoid and conodont ranges are from Krystyn et al. (2003) . Inset: Location of Wadi Wasit. RL—Reef Limestone unit; ML—Marly Limestone unit; DI—Dienerian; ku — kummeli
Image
Field views showing examples of the transfer zones and fan-delta systems in...
Published: 03 November 2016
Fig. 11. Field views showing examples of the transfer zones and fan-delta systems in the Gulf of Suez and Red Sea. ( a ) Quaternary alluvial fan located at the mouth of Wadi Gharandal (Lagia Plain); ( b ) Miocene fan delta in Wadi Wasit; ( c ) relay ramp controlling the Miocene fan delta at Wadi
Image
Paleogeographic map showing Shangsi (32.31926°N; 105.45440°E) section (Chin...
in > Geology
Published: 01 July 2017
Figure 1. Paleogeographic map showing Shangsi (32.31926°N; 105.45440°E) section (China) and other localities. Closed red stars indicate Griesbachian echinoids; open stars are younger. 1—Wadi Wasit block, Oman (late Griesbachian); 2—Salt Range, Pakistan (early Griesbachian); 3—late Griesbachian
Image
Figure 1. Paleogeographic reconstruction of Griesbachian indicating approxi...
in > Geology
Published: 01 September 2004
Figure 1. Paleogeographic reconstruction of Griesbachian indicating approximate positions of localities mentioned in text: 1—western United States; 2—northern Italy; 3—Wadi Wasit; 4—Salt Ranges of Pakistan; 5—southern Tibet. Paleogeography after Scotese (1994) ; land areas shaded, shallow-shelf
Journal Article
Journal: Geology
Published: 01 September 2004
Geology (2004) 32 (9): 805-808.
...Figure 2. Lithostratigraphy, conodont zones, and faunal ranges of upper part of Wasit block. Dots indicate sample horizons. Ammonoid and conodont ranges are from Krystyn et al. (2003) . Inset: Location of Wadi Wasit. RL—Reef Limestone unit; ML—Marly Limestone unit; DI—Dienerian; ku — kummeli...
FIGURES
Journal Article
Published: 03 November 2016
Journal of the Geological Society (2016) 174 (2): 318-335.
...Fig. 11. Field views showing examples of the transfer zones and fan-delta systems in the Gulf of Suez and Red Sea. ( a ) Quaternary alluvial fan located at the mouth of Wadi Gharandal (Lagia Plain); ( b ) Miocene fan delta in Wadi Wasit; ( c ) relay ramp controlling the Miocene fan delta at Wadi...
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Journal Article
Journal: GeoArabia
Publisher: Gulf Petrolink
Published: 01 April 1996
GeoArabia (1996) 1 (2): 343-358.
... on the hanging wall of larger, younger basins. An example of one of these small, kilometer-scale basins that exhibit marked changes in thickness of the Nukhul strata over a lateral distance of a few hundred meters is visible in outcrop at Wadi Wasit. Patton et al. (1994) argue, based upon isopach maps...
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Journal Article
Journal: GeoArabia
Publisher: Gulf Petrolink
Published: 01 April 2001
GeoArabia (2001) 6 (2): 271-334.
... velocity behaviour. Geostatistical modelling demonstrates that the expected depth uncertainty after application of the residual depth correction is less than 35 m within a 5 km distance from the well control. In the basinal Wadi Wasit deposits, a unique decametric boulder from a hudge Dienerian debris...
Journal Article
Journal: Geology
Published: 01 July 2017
Geology (2017) 45 (7): 607-610.
...Figure 1. Paleogeographic map showing Shangsi (32.31926°N; 105.45440°E) section (China) and other localities. Closed red stars indicate Griesbachian echinoids; open stars are younger. 1—Wadi Wasit block, Oman (late Griesbachian); 2—Salt Range, Pakistan (early Griesbachian); 3—late Griesbachian...
FIGURES | View All (4)
Journal Article
Journal: GeoArabia
Publisher: Gulf Petrolink
Published: 01 January 2012
GeoArabia (2012) 17 (1): 181-239.
... or alkali basalt-related ( Maury et al., 2003 ; Lapierre et al., 2004 ). The volcanic succession is filled and overlain by red ammonoid limestones dated as Middle Permian (Capitanian) followed by radiolarian chert and shales newly dated as Lopingian in Buday’ah. In the Wadi Wasit area, the volcanic series...
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Journal Article
Journal: GeoArabia
Publisher: Gulf Petrolink
Published: 01 July 2013
GeoArabia (2013) 18 (3): 135-178.
.... and B.R. Wardlaw 2010 . The Guadalupian conodont fauna of Rustaq and Wadi Wasit, Oman and a West Texas connection . Micropaleontology , v. 56 , no. 1 , p. 213 – 233 . Leven , E. Ya. 1997 . Permian stratigraphy and Fusulinida of Afghanistan with their paleogeographic...
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Journal Article
Journal: GeoArabia
Publisher: Gulf Petrolink
Published: 01 April 2012
GeoArabia (2012) 17 (2): 189-256.
FIGURES | View All (32)
Journal Article
Published: 01 May 2003
Journal of Sedimentary Research (2003) 73 (3): 407-420.
...Figure 9 Four sub-basins of the Hammam Farraun fault block. From north to south, Wadi Wasit, Thal Ridge, Wadi Tanka, and Wadi Nukhul, have different sediment thicknesses, reflecting unique fault movement histories during early syn-rift times. See Figure 1 for locations. ...
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Journal Article
Journal: AAPG Bulletin
Published: 01 June 2002
AAPG Bulletin (2002) 86 (6): 979-1002.
... evolution of the northern Hammam Faraun block (Wadi Wasit-Wadi Wardan area), eastern side of the Suez rift : Kuwait Journal of Science and Engineering , v. 23 , p. 105 – 132 . Moustafa , A. R. , 1997a , Controls on the development and evolution of transfer zones: the influence of basement...
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Journal Article
Journal: GeoArabia
Publisher: Gulf Petrolink
Published: 01 July 2012
GeoArabia (2012) 17 (3): 180-234.
... for material, and a complementary detailed field study has been performed on sections at Wadi Alwa, Wadi Sahtan, Wadi Aday, the Saiq Plateau, Wadi Wasit, Al Buday’ah, Wadi Maqam, Wadi Shuy’ab and the Batain Plain. All samples have been processed using buffered acetic acid and formic acid digestion techniques...
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Journal Article
Published: 16 May 2014
Geological Magazine (2014) 152 (1): 106-142.
... are needed in order to clarify the full apparatus of M. siciliensis , its ontogeny, intraspecific variation and geographic and stratigraphic range. Pa elements from the deep-water Permian of Rustaq and Wadi Wasit in Oman have been studied by Mei & Henderson ( 2002...
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Series: Geological Society, London, Special Publications
Published: 01 January 2007
DOI: 10.1144/GSL.SP.2007.275.01.15
EISBN: 9781862395237
... Lopingian blocks are rare-absent. Data from a well-exposed section at Wadi Wasit (23°06′20″N, 58°18T0″E) were used for this paper (Fig. 3 ). In the field, carbonate-rich sediment of the Saiwan Formation is characterized by horizontal bedding (Fig. 4 a), planar cross-bedding (Fig. 4 b), erosional...
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Journal Article
Journal: PALAIOS
Published: 12 June 2018
PALAIOS (2018) 33 (6): 266-281.
... change ( Hautmann et al. 2015 ). The pace of recovery of taxonomic diversity in the Servino Formation is, however, much lower and less ecologically complex than recorded in other Early Triassic localities, e.g., Kesennuma, Japan ( Kashiyama and Oji 2004 ); Wadi Wasit, Oman ( Twitchett et al. 2004...
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