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Halalate Mountains

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Journal Article
Journal: AAPG Bulletin
Published: 01 January 1953
AAPG Bulletin (1953) 37 (1): 1–113.
..., bordered on the east by the barren trench of Wadi Araba and on the west by Sinai (Egypt). North of the Negev are the Judean and Ephraim mountains, a broad arch bordered on the east by the Dead Sea-Jordan Valley and with a steep west flank. The steep flank flattens into a foothills belt that merges westward...
FIGURES | View All (64)
Series: Geological Society, London, Special Publications, Geological Society, London, Special Publications
Published: 01 January 2010
DOI: 10.1144/SP341.3
EISBN: 9781862395893
.... (Gebel, mountain) Yelleg, G. Halal and G. Maghara are the most prominent of these hillocks and are 1090, 890 and 735 m above sea level, respectively. The three hills represent three large anticlines among other smaller anticlines in northern Sinai. Similar folds exist farther to the NE in the Naqb Desert...
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Journal Article
Published: 07 December 2016
Journal of the Geological Society (2017) 174 (2): 336–352.
...-linkage transfer zones between the inverted rift-parallel fault segments. The Gebel Halal inverted basin ( Fig. 2 ) contains a Jurassic synrift section with maximum thickness of 3234 m (Halal-1 well, cross-section BB' in Fig. 2 ). The exposed Cretaceous rocks are folded by a 43 km long, highly...
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Journal Article
Published: 01 December 1996
Bulletin of Canadian Petroleum Geology (1996) 44 (4): 615–631.
... by rigid Precambrian basement rocks that reach elevations of 2640 m in Jebel Katherine (Said, 1962) (Fig. 1). The central and northern sectors of the Sinai Peninsula are covered with a northward-draining limestone plateau with a series of northeast-trending anticlinal and syn- clinal jebels (mountains...
Journal Article
Published: 25 November 2013
Journal of the Geological Society (2014) 171 (2): 239–254.
... Sinai (namely G. (Gebel = mountain) Maghara, G. Yelleq and G. Halal folds, Fig. 1 ). The Syrian Arc folds in northern Sinai are Late Cretaceous–Early Tertiary, NE–SW-oriented, doubly plunging anticlines. The Triassic rocks of the area are ≥185 m thick and include two units ( Fig. 2 ); a lower...
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Journal Article
Journal: AAPG Bulletin
Published: 01 July 2010
AAPG Bulletin (2010) 94 (7): 937–955.
... risk in this region. The Junggar Basin, approximately 13.4 × 10 4 km 2 (5.17 × 10 4 mi 2 ), is bounded by the Kelameili and Qinggelidi Mountains to the northeast, by the Yilinheibiergen and Bogeda Mountains of the Tianshan range to the south, and by the Zhayier and Halalate Mountains...
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Journal Article
Journal: AAPG Bulletin
Published: 15 July 2019
AAPG Bulletin (2019) 103 (7): 1553–1574.
... to the south, and by the Zhayier and Halalate Mountains to the northwest ( Figure 1B ). The basin is an upper Paleozoic, Mesozoic, and Cenozoic superimposed basin at the junction of the Kazakhstan, Siberia, and Tarim tectonic blocks ( Cao et al., 2006 ). The basin comprises six tectonic units, namely...
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Journal Article
Journal: AAPG Bulletin
Published: 01 December 2017
AAPG Bulletin (2017) 101 (12): 1995–2019.
... in global basins. The Junggar Basin is a petroliferous basin in the northwestern China ( Figure 1A ), covering an area of approximately 13 × 10 4 km 2 (50,000 mi 2 ), and is surrounded by mountains including Yilinheibiergen Mountains in the south, Halalate Mountains in the north, Zhayier Mountains...
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Journal Article
Journal: Interpretation
Published: 06 April 2018
Interpretation (2018) 6 (2): T431–T447.
.... Zhongguai paleouplift is on the east of the Zhayler and Halalate Mountains. Some studies suggested that volcanic rocks of the Carboniferous basement in the uplift have the potential for oil and gas exploration ( Xiao et al., 2010 ); thus, industry has focused on the volcanic rocks of Carboniferous age...
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Series: Geological Society, London, Special Publications, Geological Society, London, Special Publications
Published: 01 January 2010
DOI: 10.1144/SP341.2
EISBN: 9781862395893
... Gaash-2 5508–4595 913+ 4595–2981 1614 2981–2506 475 2506–803 1703 8 Gevim-1 4620–4588 32 4588–4078 510 4078–3870 208 3870–2306 1564 2306–1876 430 1876–567 1309 9 Halal-1 4314–3629 685+ 3629–815 2814 815–457 358 457–0 457 10 Helez Deep-1 6093–5978 115...
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Journal Article
Journal: AAPG Bulletin
Published: 15 September 2019
AAPG Bulletin (2019) 103 (9): 2073–2115.
... in the northwestern Junggar Basin and is surrounded by the Halalate Mountains to the northwest and Zaire Mountains to the west ( Figure 1A, B ). This study is based on core, well-log, and three-dimensional (3-D) seismic data that were provided by the Xinjiang Oilfield, China National Petroleum Corporation...
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Journal Article
Journal: GeoArabia
Publisher: Gulf Petrolink
Published: 01 January 2008
GeoArabia (2008) 13 (1): 59–84.
... of this unique upper Oligocene outcrop is placed in context of the northeast African-Arabian region. The Risan Aneiza Mountains (20 km south of El Arish, Figure 2 ) represent the northernmost outcrop of Mesozoic rocks in the Sinai Peninsula. There are few geological studies in the area, probably due...
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Series: Geological Society, London, Special Publications, Geological Society, London, Special Publications
Published: 01 January 2010
DOI: 10.1144/SP341.6
EISBN: 9781862395893
... (Fig. 1 c). Eight sections from the upper Rizan Aneiza and lower Halal formations (Upper Aptian–Albian) were presented in former publications ( Bachmann & Kuss 1998 ; Bachmann et al. 2003 ); three of them are added in this work (Fig. 1 c) to illustrate facies and sequence stratigraphy...
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Journal Article
Journal: GeoArabia
Publisher: Gulf Petrolink
Published: 01 July 2015
GeoArabia (2015) 20 (3): 175–224.
... is described in Figure 2 . The lower Palaeozoic is known from wells and outcrops in the Amanous Mountains of the Iskenderun region and the Mardin High and Hakkari area of southeast Turkey (Ala and Moss, 1979; Lovelock, 1984 ; Ozcan et al., 1988 ; Hosgör et al., 2014 ) and Jordan ( Basha, 1982...
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Journal Article
Published: 01 August 2007
Mineralogical Magazine (2007) 71 (4): 389–406.
... of limestone, dolomite, marl, shale and sandstone of Jurassic and Cretaceous ages. In places, the folds reach up to 50 km in length (e.g. Halal). The Wadi El Arish system drains a large area of central and northern Sinai and reaches the Mediterranean Sea at the town of El Arish to the east of Lake El Bardawil...
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Journal Article
Journal: AAPG Bulletin
Published: 01 January 1976
AAPG Bulletin (1976) 60 (1): 34–64.
... sedimentary sequences against “basement” buttresses in the southeast. Surface anticlines that resulted from this compressional episode include El Maghara and El Halal anticlines in north Sinai which are associated with northeast-southwest trending thrust or high angle reverse faults. In addition, Abu Roash...
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Series: AAPG Memoir, AAPG Memoir
Published: 01 January 2014
DOI: 10.1306/13431857M106298
EISBN: 9781629812663
... sand dunes, red soil, and several ridges of calcareous sandstone that extends parallel to the modern coastline (Figure 1 ). A mountain belt that exceeds 1000 m (3281 ft) in elevation extends east of the Coastal Plain (Figure 1 ).The mountainous backbone of Israel is composed of Mesozoic rocks...
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