Abstract
Central Oman includes the vast desert areas south of the main Oman Mountain range and north of Dhofar province (Figs. 14.1 and 14.2). This area includes the major oil field provinces from west to east, the Lekhwair High, the Fahud salt basin (Natih, Fahud, Yibal, Al Huwaysar oil fields), the Ghaba salt basin, including six surface-piercing salt domes, and the Haushi-Huqf basement high. Both the Fahud and Ghaba salt basins extend northwards up to, and even beneath, the mountain front, with minor salt intrusions penetrating the Hawasina and Haybi complex thrust sheets beneath the ophiolite recently found in the Hawasina Window and at Jebel Qumayrah (Chap. 9). The Fahud and Ghaba salt basins are separated by the NE-SW aligned Makarem High. The salt is the Proterozoic–Early Cambrian Ara Group salt that extends all across Arabia and northwards to the Zagros mountains in Iran where it is termed the Hormuz salt.
Access this chapter
Tax calculation will be finalised at checkout
Purchases are for personal use only
References
Al-Kindy MH, Richard P (2014) The main structural styles of the hydrocarbon reservoirs in Oman. In: Rollinson HR, Searle MP, Abbasi IA, Al-Lazki A, Al-Kindy MH (eds) Tectonic evolution of the Oman Mountains. Geological Society, London, Special Publication, vol 392, pp 409–446
Clarinbould JS, Hyden B, Sarg JF, Trudgill BD (2013) Structural evolution of a salt-cored, domed, reactivated fault complex, Jebel Madar, Oman. J Struct Geol 51:118–131
Dutton RW (ed) (1988) Scientific results of the royal geographical society’s Oman Wahiba Sands Project 1985–1987. J Oman Stud (Special report no. 3). Diwan of the Royal Court, Muscat, Oman, 576 p
Eriksen H, Eriksen J (2005) Common birds in Oman, Reprinted 2017. Al Roya Press and Publishing, Muscat, p 271
Filbrandt JB, Al-Dhahab S, Al-Habsy A, Harris K, Keating J, Al-Mahruqi S, Ozkaya I, Richard PD, Robertson T (2006) Kinematic interpretation and structural evolution of North Oman, Block 6, since the Late Cretaceous and implications for timing of hydrocarbon migration into Cretaceous reservoirs. GeoArabia 11(1):97–139
Gallagher M, Woodcock MW (1980) The birds of Oman. Quartet books, London, p 310
Gardner RAM (1988) Aeolianites and marine deposits of the Wahiba Sands: character and palaeo-environments, In: Dutton RW (ed) The scientific results of the royal geographical society Oman Wahiba sands project 1985–1987. Journal of Oman studies special report 3; Ministry of National heitage and Culture, Muscat, pp 75–94
Glennie KW (2005) The deserts of Southeast Arabia GeoArabia. Manama, Bahrain, 215 p
Gorin GE, Racz LG, Walter MR (1982) Late Precambrian–Cambrian sediments of Huqf Group, Sultanate of Oman. Am Asso Petrol Geol Bull 66:2609–2627
Heward AP (1990) Salt removal and sedimentation in Southern Oman. In: Roberston AHF, Searle MP, Ries AC (eds) The geology and tectonics of the Oman region. Geological Society, London, Special Publication no 49, pp 637–652
Heward AP, Al-Rawahi Z (2008) Qarn Sahmah salt dome. Petroleum Development Oman Field Guide 27
Heward A, Penny RA (2014) Al-Khalta glacial deposits in the Oman Mountains and their implications. In: Rollinson HR, Searle MP, Abbasi IA, Al-Lazki A, Al-Kindy MH (eds) Tectonic evolution of the Oman Mountains. Geological Society, London, Special Publication, vol 392, pp 279–302
Hughes-Clark M (1990) Oman’s geological heritage. Petroleum Development Oman Ltd. 247 p
Loosveld RJH, Bell A, Terken JJM (1996) The tectonic evolution of interior Oman. GeoArabia 1(1):28–51
Meyer J, Mercolli I, Immenhauser A (1996) Off-ridge alkaline magmatism and seamount volcanoes in the Masirah island ophiolite, Oman. Tectonophysics 267:187–208
Mountain GS, Prell WL (1990) In: Robertson AFH, Searle MP, Ries AC (eds) The geology and tectonics of the Oman region. Geological Society, London, Special Publication no 49, pp 725–744
Naylor MA (1996) Geological features of outstanding scientific interest in the Huqf area. Petroleum Development Oman Internal Report 168
Peters T, Mercolli I (1998) Extremely thin oceanic crust in the Proto-Indian Ocean: evidence from the Masirah Ophiolite, Sultanate of Oman. J Geophys Res 193:677–689
Peters T, Immenhauser A, Mercolli I, Meyer J (1997) Geological map of Masirah North and Masirah South, scale 1:50,000. Ministry of Petroleum and Minerals, Muscat
Peters T et al (2001) Geological Map of Sur and Al Ashkharah, scale 1:100,000. Ministry of Commerce and Industry, Sultanate of Oman
Peters JM, Filbrandt JB, Grotzinger JP, Newall MJ, Shuster MW, Al-Siyabi HA (2003) Surface-piercing salt domes of interior North Oman and their significance for the Ara carbonate “stringer” hydrocarbon play. GeoArabia 8:231–270
Reuning L et al (2009) Constraints on the diagenesis, stratigraphy and internal dynamics of the surface-piercing salt domes in the Ghaba Salt Basin (Oman): a comparison to the Ara group in the South Oman Salt Basin. GeoArabia 14:83–120
Reuter M, Piller WE, Harzhause M, Kroh A, Basi D (2008) Termination of the Arabian shelf sea: stacked cyclic sedimenatry patterns and timing (Oligocene/Miocene, Oman). Sediment Geol 212:12–24
Rollinson H (2017) Masirah, Oman’s other ophiolite: a better analogue for mid-ocean ridge processes? Geosci Front 8:1253–1262
Schreurs G, Immenhauser A (1999) West-northwest directed obduction of the batain group on the eastern Oman continental margin at the Cretaceous-Tertiary boundary. Tectonics 18:148–160
Shackleton RM, Ries AC (1990) Tectonics of the Masirah fault zone and eastern Oman. In: Robertson AFH, Searle MP, Ries AC (eds) The geology and tectonics of the Oman Region. Geological Society, London, Special Publication, no 49, pp 715–724
Shackleton RM, Ries AC, Bird PR, Filbrandt JB, Lee CW, Cunningham GC (1990) The Batain Melange of NE Oman. In: Robertson AFH, Searle MP, Ries AC (eds) The geology and tectonics of the Oman Region. Geological Society, London, Special Publication, no 49, pp 673–696
Terken J (1999) The Natih petroleum system of North Oman. GeoArabia 4:157–180
Winser N (1989) The sea of sands and mists. Royal Geographical Society, London. Century Hutchinson Ltd., 199 p
Worthing MA, Nasir S (2008) Cambro-Ordovician potassic (alkaline) magmatism in Central Oman: Petrological and geochemical constraints on petrogenesis. Lithos 106:25–38
Author information
Authors and Affiliations
Corresponding author
Rights and permissions
Copyright information
© 2019 Springer Nature Switzerland AG
About this chapter
Cite this chapter
Searle, M. (2019). Central Oman, Wahiba Sands and Al Wusta. In: Geology of the Oman Mountains, Eastern Arabia. GeoGuide. Springer, Cham. https://doi.org/10.1007/978-3-030-18453-7_14
Download citation
DOI: https://doi.org/10.1007/978-3-030-18453-7_14
Published:
Publisher Name: Springer, Cham
Print ISBN: 978-3-030-18452-0
Online ISBN: 978-3-030-18453-7
eBook Packages: Earth and Environmental ScienceEarth and Environmental Science (R0)