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Midyan Plate

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Image
False-color landsat image of the Ifal Basin, Midyan area, northwest Saudi Arabia. The basin is located between the Gulf of Aqaba and Red Sea footwall uplifts, both of which bring basement to the surface (shown in transparent red). West of the Midyan area a pull-apart basin in the Gulf of Aqaba has opened 26 km perpendicular to the Aqaba/Dead Sea strike-slip fault system due to a slight rotation of the Arabian Plate as it migrated northward. Major faults are shown in white. Midyan Field wells are labeled A, B and C. The Midyan 3-D seismic survey is shown in orange.
Published: 01 July 2014
of Aqaba has opened 26 km perpendicular to the Aqaba/Dead Sea strike-slip fault system due to a slight rotation of the Arabian Plate as it migrated northward. Major faults are shown in white. Midyan Field wells are labeled A, B and C. The Midyan 3-D seismic survey is shown in orange.
Journal Article
Journal: GeoArabia
Publisher: Gulf Petrolink
Published: 01 October 1999
GeoArabia (1999) 4 (4): 503–542.
.... (1988) , and which has been considered as a transitional phase between continental and oceanic rifting by Cochran and Martinez (1988) . It is believed to be responsible for the triangular shape of the Midyan region that lies within the zone bounded by the Red Sea rift margin and the new plate boundary...
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First thumbnail for: Lithostratigraphy and Depositional History of Part...
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Third thumbnail for: Lithostratigraphy and Depositional History of Part...
Journal Article
Journal: GeoArabia
Publisher: Gulf Petrolink
Published: 01 January 2005
GeoArabia (2005) 10 (1): 97–124.
.... This continuous, point-sourced sedimentation is indicative of stable drainage and by inference, a stable eastern border fault system. We attribute this stable border fault system to a stress heterogeneity related to the pre-existing Najd Shear Zone, and polarity reversals in upper-plate transport direction...
FIGURES
First thumbnail for: Preferential deposition and preservation of struct...
Second thumbnail for: Preferential deposition and preservation of struct...
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Journal Article
Journal: GeoArabia
Publisher: Gulf Petrolink
Published: 01 July 2014
GeoArabia (2014) 19 (3): 165–184.
... of Aqaba has opened 26 km perpendicular to the Aqaba/Dead Sea strike-slip fault system due to a slight rotation of the Arabian Plate as it migrated northward. Major faults are shown in white. Midyan Field wells are labeled A, B and C. The Midyan 3-D seismic survey is shown in orange. ...
FIGURES
First thumbnail for: <span class="search-highlight">Midyan</span> Penin...
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Schematic reconstruction of the accretionary evolution of the Arabian Plate. By 715 Ma, the Asir, Hijaz and Midyan terranes formed the western part of the Arabian Shield. Between about 680 and 640 Ma the Afif terrane collided with the western Shield along the Nabitah Suture. At about 670 Ma, a subduction complex formed west of the Amar Arc. The Amar Collision lasted from about 640 to 620 Ma when the Rayn micro-plate and Afif terrane collided along the Amar Suture. The N-trending Rayn anticlines and conjugate NW and NE fractures and faults may have formed at this time.
Published: 01 October 2000
Figure 2: Schematic reconstruction of the accretionary evolution of the Arabian Plate. By 715 Ma, the Asir, Hijaz and Midyan terranes formed the western part of the Arabian Shield. Between about 680 and 640 Ma the Afif terrane collided with the western Shield along the Nabitah Suture. At about
Journal Article
Journal: GeoArabia
Publisher: Gulf Petrolink
Published: 01 July 2005
GeoArabia (2005) 10 (3): 49–126.
... is proposed in a lexicon format that integrates biostratigraphic, sedimentological, seismic and field studies from the Midyan Peninsula in the north, to the Jizan Coastal Plain in the south. In view of the economic aspect of the Neogene succession and greater accessibility to Neogene subsurface samples...
FIGURES
First thumbnail for: Lithostratigraphy of the Red Sea Region
Second thumbnail for: Lithostratigraphy of the Red Sea Region
Third thumbnail for: Lithostratigraphy of the Red Sea Region
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The Midyan, Hijaz, Asir and Afif terranes, and Amar Arc of the Rayn micro-plate form the Arabian Shield (Stoeser and Camp, 1985; Husseini 1989). The Rayn micro-plate (green) forms the eastern part of the Arabian Plate. The Amar Collision (about 640-620 Ma) fused the Rayn micro-plate and Afif terrane along the Amar Suture, and formed the N-trending, basement-controlled blocks (Summan Platform, Khurais-Burgan Anticline, En Nala-Ghawar Anticline and Qatar Arch). These giant anticlines are bounded by the orthogonal NE-trending Wadi Batin and NW-trending Abu Jifan strike-slip faults that appear to be syn-collisional. The much younger Najd Fault System (about 570-530 Ma) dislocated the older Nabitah Suture (about 680-640 Ma) by about 250-300 km.
Published: 01 October 2000
Figure 1: The Midyan, Hijaz, Asir and Afif terranes, and Amar Arc of the Rayn micro-plate form the Arabian Shield ( Stoeser and Camp, 1985 ; Husseini 1989 ). The Rayn micro-plate (green) forms the eastern part of the Arabian Plate. The Amar Collision (about 640-620 Ma) fused the Rayn micro-plate
Journal Article
Published: 08 October 2015
The Journal of Geology (2015) 123 (5): 463–489.
... ), these suites are generated in back-arc and within-plate settings and indicate a change in tectonic process from older A-types associated with suture zones. Fortunately, the Midyan and Hijaz terranes in the western Arabian Shield provide an excellent example to explore this petrogenetic transition...
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First thumbnail for: Zircon Geochemical and Geochronological Constraint...
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Journal Article
Journal: PALAIOS
Published: 24 July 2024
PALAIOS (2024) 39 (7): 233–242.
... 6.0 ( Collins et al. 2013 ). Overall, distribution of Miocene corals and coral reefs was influenced by eustasy, plate tectonics, and associated changes in climate and paleoceanographic conditions ( Renema et al. 2008 ; Mathew et al. 2020 ; Steinthorsdottir et al. 2021 ). During the Miocene...
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First thumbnail for: MEDITERRANEAN IMPRINT ON CORAL DIVERSITY IN THE IN...
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Reconstruction of Pannotia Supercontinent at 600 Ma (modified from Scotese, 2009). The Arabian Plate consists of the Rayn and Afif terranes and half of the Hijaz Terrane (Midyan, Hijaz and Asir terranes in the western Arabian Shield). The locations of the Cimmerian Iranian (Sanandaj-Sirjan, Alborz and Central Iran) and Afghan terranes are modified here although their precise locations remain uncertain. The Hun terranes are not shown in Scotese’s maps (see review in Ruban et al., 2007). They may have formed a long belt of terranes extending from along Spain to Iran and may have continued between North Rodinia and Cathysia.
Published: 01 April 2010
Figure 7: Reconstruction of Pannotia Supercontinent at 600 Ma (modified from Scotese, 2009). The Arabian Plate consists of the Rayn and Afif terranes and half of the Hijaz Terrane (Midyan, Hijaz and Asir terranes in the western Arabian Shield). The locations of the Cimmerian Iranian (Sanandaj
Journal Article
Journal: AAPG Bulletin
Published: 11 October 1997
AAPG Bulletin (1997) 81 (10): 1640–1659.
... sector of the Red Sea and is a segment of the East Africa rift system, which acted as a divergent plate boundary between the Arabian and African plates during Oligocene–Miocene rifting. This area is characterized by the exposures of rift shoulders (Precambrian basement massifs) on both sides of the Red...
FIGURES
First thumbnail for: A Common Source Rock for Egyptian and Saudi Hydroc...
Second thumbnail for: A Common Source Rock for Egyptian and Saudi Hydroc...
Third thumbnail for: A Common Source Rock for Egyptian and Saudi Hydroc...
Journal Article
Journal: GeoArabia
Publisher: Gulf Petrolink
Published: 01 October 1999
GeoArabia (1999) 4 (4): 445–464.
...Denis Mougenot; Amir A. Al-Shakhis ABSTRACT In the Midyan Peninsula (onshore northern Red Sea, Saudi Arabia), the current prospective oil and gas exploration targets are sub-salt structures. In this region, conventional time-migrated seismic sections are distorted due to the presence of salt...
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First thumbnail for: Depth Imaging Sub-salt Structures: A Case Study in...
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Journal Article
Published: 26 June 2024
Bulletin de la Société Géologique de France (2024) 195 (1): 12.
... extension of the subducting Arabian Plate below the Eurasian Plate (Bellahsen et al. , 2003) and the thermal weakening of the lithosphere due to the East-Africa hotspot track (Vicente de Gouveia et al. , 2018). Rifting started during the Oligocene and extended from the Gulf of Suez to the southern Red Sea...
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First thumbnail for: The tectonostratigraphic latitudinal record of the...
Second thumbnail for: The tectonostratigraphic latitudinal record of the...
Third thumbnail for: The tectonostratigraphic latitudinal record of the...
Journal Article
Journal: GeoArabia
Publisher: Gulf Petrolink
Published: 01 October 2014
GeoArabia (2014) 19 (4): 59–108.
... Waqb Member of the Jabal Kibrit Formation and of the Pliocene Badr Formation of the Lisan Group. The Midyan area of the northern Red Sea offers a unique window into the Cretaceous and Miocene succession that is otherwise only present in the deep subsurface. The sediments are of hydrocarbon interest...
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First thumbnail for: Micropalaeontology and palaeoenvironments of the M...
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Journal Article
Published: 01 April 2005
Journal of Foraminiferal Research (2005) 35 (2): 171–172.
...). E iland , M., and G udmundsson , G., Taxonomy of some Recent Nodosariinae (Foraminifera) from the North Atlantic, with notes on wall lamination.—Micropaleontology, v. 50, no. 2, 2004, p. 195–210, 2 figures, 5 plates, 1 table.—“Morphological characters of twelve Recent species of Nodosariinae...
Journal Article
Journal: AAPG Bulletin
Published: 01 September 1989
AAPG Bulletin (1989) 73 (9): 1117–1131.
... the eastern part of the Arabian plate, western Iran, and central Iran’s Lut block ( Figures 2 - 4 ). The Precambrian tectonic history of the Turkish (Anatolia) and the Levant plates is poorly understood; however, these two plates may have accreted against the Midyan terrane and northeastern Egypt along...
FIGURES
First thumbnail for: Tectonic and Deposition Model of Late Precambrian-...
Second thumbnail for: Tectonic and Deposition Model of Late Precambrian-...
Third thumbnail for: Tectonic and Deposition Model of Late Precambrian-...
Journal Article
Published: 08 November 2019
Petroleum Geoscience (2020) 26 (3): 448–461.
...Khalid Al-Ramadan; Ardiansyah Koeshidayatullah; Dave Cantrell; Peter K. Swart Abstract The early Miocene Wadi Waqb carbonate in the Midyan Peninsula, NE Red Sea is of great interest not only because of its importance as an archive of one of the few pre-salt synrift carbonate platforms in the world...
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First thumbnail for: Impact of basin architecture on diagenesis and dol...
Second thumbnail for: Impact of basin architecture on diagenesis and dol...
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Journal Article
Journal: GeoArabia
Publisher: Gulf Petrolink
Published: 01 October 2000
GeoArabia (2000) 5 (4): 527–542.
...Figure 2: Schematic reconstruction of the accretionary evolution of the Arabian Plate. By 715 Ma, the Asir, Hijaz and Midyan terranes formed the western part of the Arabian Shield. Between about 680 and 640 Ma the Afif terrane collided with the western Shield along the Nabitah Suture. At about...
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First thumbnail for: Origin of the Arabian <span class="search-highligh...
Second thumbnail for: Origin of the Arabian <span class="search-highligh...
Third thumbnail for: Origin of the Arabian <span class="search-highligh...
Journal Article
Journal: The Leading Edge
Published: 01 June 2017
The Leading Edge (2017) 36 (6): 507–511.
... setting of Arabian plate and Red Sea showing the Red Sea rift separating the Arabian and Nubian Shields (image courtesy of https://en.wikipedia.org/wiki/Persian_Gulf_Basin, shared under the CC BY-SA 3.0 Unported License). Postsalt section at the top: this section consists of clastic sediments...
FIGURES
First thumbnail for: KFUPM-KAUST Red Sea model: Digital viscoelastic de...
Second thumbnail for: KFUPM-KAUST Red Sea model: Digital viscoelastic de...
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Journal Article
Published: 11 June 2008
Geological Magazine (2008) 145 (5): 648–654.
.... They comprise part of a widely distributed Late Cretaceous to Neogene succession deposited in troughs of the Maqnah massif and Ifal Basin in the SE Midyan region between the Gulf of Aqaba and Red Sea ( Remond & Teixido, 1980 ; Clark, 1986 ; Hughes et al . 1999 ; Hughes & Johnson, 2005 ). Clark...
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First thumbnail for: Late Cretaceous (Campanian–Maastrichtian) marine r...
Second thumbnail for: Late Cretaceous (Campanian–Maastrichtian) marine r...
Third thumbnail for: Late Cretaceous (Campanian–Maastrichtian) marine r...