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The Wajid Sandstone around Abha/Khamis Mushayt and in its type area: lithostratigraphic architecture and correlations

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Abstract

The Wajid Sandstone of southeastern Saudi Arabia is a prolific aquifer and a recent target for hydrocarbon exploration, but a sedimentologic model and the stratigraphic architecture of the sediments have only recently been presented for the type area of the Wajid Group around Wadi Dawasir. Farther to the west, the Wajid Sandstone was also recognized, but stratigraphic architecture and sedimentology are poorly known. This paper presents the preliminary results of investigations targeted at the outcrops west and south of the type area, covering the area between Wadi Dawasir, Najran in the south, and Abha in the west. Two successions are recognized, a lower red one and an upper beige one. Although the lower one sedimentologically shares several features with the lowermost unit in the type area, the marine Dibsiyah Formation, a correlation remains doubtful. The red succession lacks the Skolithos fauna of the Dibsiyah Formation, and its facies associations point to a fluvial depositional environment. From its stratigraphic position and from its lithology, the red succession is similar to the Siq Formation of the northern Kingdom and it will be discussed whether the red succession might be a yet unrecognized equivalent of the Siq Formation. The lower red unit is bounded by a major unconformity, separating it from the underlying basement. This pan-African unconformity developed during a latest Neoproterozoic–Cambrian episode of intensive weathering and peneplanation. It is characterized by a thick weathering zone and an overlying coarse but thin quartz pebble breccia to conglomerate, which together represent a regolith. The beige succession is definitely correlated to the Khusayyayn Formation. Both successions are characterized by macro-scale to giant 2D and 3D submarine dunes and share many other phenomena. The basal unconformity also shows regolith development with a quartz pebble conglomerate, whose clasts seem to have been reworked from the pan-African regolith.

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References

  • Al Ajmi FH, Keller M, Hinderer M, Filomena CM (2015) Lithofacies, depositional environments, and stratigraphic architecture of the Wajid Group outcrops in southern Saudi Arabia. GeoArabia 20:49–94

    Google Scholar 

  • Allen JRL (1980) Sand waves; a model of origin and internal structure. Sed Geol 26:281–328

    Article  Google Scholar 

  • Allen JRL, Collinson J (1979) The superposition and classification of dunes formed by unidirectional flow. Sed Geol 12:169–178

    Article  Google Scholar 

  • Ashley GM (1990) Classification of large-scale subaqueous bedform: a new look at an old problem. J Sed Pet 60:160–172

    Article  Google Scholar 

  • Avigard A, Sandler A, Kolodner K, Stern RJ, McWilliams M, Miller N, Beyth M (2005) Mass-production of Cambro–Ordovician quartz-rich sandstone as a consequence of chemical weathering of Pan-African terranes: environmental implications. Earth Planet Sci Let 240:818–826

    Article  Google Scholar 

  • Babalola LO (1999) Depositional environments and provenance of the Wajid Sandstone, Abha-Khamis Mushayt Area, Southwestern Saudi Arabia. MS Thesis, King Fahd University of Petroleum and Minerals, Dhahran, Saudi Arabia, 239 p

  • Babalola LO, Hussain M, Hariri MM (2003) Origin of iron-rich beds in the basal Wajid Sandstone, Abha-Khamis Mushayt Area, Southwest Saudi Arabia. Arab J Sci Eng 28:3–24

    Google Scholar 

  • Bokunewiecz HJ, Gordon RB, Kastens KA (1977) Form and migration of sand waves in a large estuary, Long Island Sound. Mar Geol 24:185–199

    Article  Google Scholar 

  • Byers CW, Dott RH Jr (1995) Sedimentology and depositional sequences of the Jordan Formation (Upper Cambrian), northern Mississippi valley. J Sed Res B5:289–305

    Google Scholar 

  • Cheel RJ (1984) Heavy mineral shadows, a new sedimentary structure formed under upper-flow-regime conditions: its directional and hydraulic significance. J Sed Pet 54:1175–1182

    Google Scholar 

  • Conaghan PJ (1980) The Hawkesbury Sandstone: gross characteristics and depositional environment. In: Herbert C, Helby R (eds) A Guide to the Sydney Basin. Geol Surv New South Wales Bull 26:188–253

  • Conaghan PJ, Jones JG (1975) The Hawkesbury Sandstone and the Brahmaputra: a depositional model for a continental sheet sandstone. J Geol Soc Australia 22:275–283

    Article  Google Scholar 

  • Dalrymple RW, Rhodes RN (1995) Estuarine dunes and bars. In: Perillo GME (ed) Geomorphology and Sedimentology of Estuaries. Dev Sedim 53:359–422

  • Eschner TB, Kocurek G (1986) Marine destruction of eolian sand seas: origin of mass flows. J Sed Pet 56:401–411

    Google Scholar 

  • Fairer GM (1985) Geologic map of the Wadi Baysh quadrangle, sheet 17F, Kingdom of Saudi Arabia. Saudi Arabian Deputy Ministry for Mineral Resources Geoscience Map GM-77C, scale 1:250,000, 40 p

  • Flemming BW (1982) Dynamics of large transverse bedforms on the southeast African continental shelf. 11th Int Congr Sedim Abstracts:73

  • Greenwood WR (1985) Geologic map of the Abha quadrangle, sheet 18F, Kingdom of Saudi Arabia. Saudi Arabian Deputy Ministry for Mineral Resources Geoscience Map GM-138, scale 1:250,000, 40 p

  • GTZ/DCo (2009) Detailed water resources studies of Wajid and overlying aquifers, volume 10, drilling investigations. Ministry of Water and Electricity, KSA

    Google Scholar 

  • Gutiérrez-Alonso G, Blanco JA, Macfarlane A, Fernández-Suárez J (2004) Paleometeorización vs. Paleoalteración en la superficie de discordancia Proterozoico-Cámbrico en el Antiforme del Narcea. Geogaceta 36:7–10

    Google Scholar 

  • Harms JC, Southard JB, Walker RG (1982) Structures and sequences in clastic rocks. Soc Sed Res Short Course 9

  • Janjou D, Halawani MA, Memesh A, Razin P, Jaques R, Roobol MJ, Shorbaji H (1998) Geologic map of the Jibal al Misma quadrangle, sheet 27D, Kingdom of Saudi Arabia. Saudi Arabian Deputy Ministry for Mineral Resources Geoscience Map GM-138, scale 1:250,000, 40 p

  • Jones BG, Rust BR (1983) Massive sandstone facies in the Hawkesbury Sandstone, a Triassic fluvial deposit near Sydney, Australia. J Sed Pet 53:1249–1261

    Google Scholar 

  • Kellogg KS, Janjou D, Minoux L, Fourniguet F (1986) Geologic map of the Wadi Tathlith quadrangle, sheet 20G, Kingdom of Saudi Arabia. Saudi Arabian Deputy Ministry for Mineral Resources Geoscience Map GM-103C, scale 1:250,000, 27 p

  • Kolodner K, Avigad D, McWilliams M, Wooden JL, Weissbrod T, Feinstein S (2006) Provenance of north Gondwana Cambrian–Ordovician sandstone: U–Pb SHRIMP dating of detrital zircons from Israel and Jordan. Geol Mag 143:367–391

    Article  Google Scholar 

  • Martin CAL (1995) The origin of massive sandstone facies in an ancient braided river deposits. Dissertation, Durham University. http://etheses.dur.ac.uk/5326/

  • Miall A (2006) The geology of fluvial deposits . Springer Verlag, Berlin582 p

    Book  Google Scholar 

  • Miller KG, Kominz MA, Browning JV, Wright JD, Mountain GS, Katz ME, Sugarman PJ, Cramer BS, Christie-Blick N, Pekar NF (2005) The Phanerozoic record of global sea-level change. Science 310:1293–1298

    Article  Google Scholar 

  • Moscariello A, Spaak P, Jourdan A, Azzouni AH (2009) The Ordovician glaciation in Saudi Arabia—exploration challenges part 1: geology (outcrop, subsurface, analogues). http://www.searchanddiscovery.com/pdfz/documents/2009/50175moscariello/presentation.pdf.html

  • Nemec W (1990) Aspects of sediment movements on steep delta slopes. In: Collela a, prior DB (eds). Coarse grained deltas. Int Ass Sedim Spec Pub 10:29–73

    Google Scholar 

  • Paola C, Wiele SM, Reinhart MA (1989) Upper-regime parallel lamination as the result of turbulent sediment transport and low-amplitude bed forms. Sedimentology 36:47–59

    Article  Google Scholar 

  • Powers, RW, Ramirez LF, Redmond CD, Elberg EL (1966) Geology of the Arabian Peninsula— sedimentary geology of Saudi Arabia. USGS, Prof Paper 560-D

  • Reineck HE, Singh IB (1970) Depositional sedimentary environments. Springer, Berlin

    Google Scholar 

  • Ross CA, Ross JRP (1988) Late Paleozoic transgressive-regressive deposition. Soc Sed Geol Spec Publ 42:227–247

    Google Scholar 

  • Ross CA, Ross JRP (1995) North American Ordovician depositional sequences and correlations. In: Cooper JD, Droser ML, Finney SC (eds.) Ordovician Odyssey. Pacific section SEPM: 77:309–313

  • Runkel AC (1994) Deposition of the uppermost Cambrian (Croixan) Jordan Sandstone, and the nature of the Cambrian–Ordovician boundary in the Upper Mississippi Valley. Geol Soc Am Bull 106:492–506

    Article  Google Scholar 

  • Rust BR, Jones GG (1987) The Hawkesbury Sandstone south of Sydney, Australia, Triassic analogue for the deposit of a large braided river. J Sed Pet 57:222–233

    Google Scholar 

  • Saudi Stratigraphic Committee (2013) Phanerozoic stratigraphy of Saudi Arabia. Part 1—Paleozoic successions of the Arabian Shelf (cover rocks). Saudi Stratigraphic Committee Special Publication 1: 69 p

  • Stump TE, van der Eem GLA (1995) The stratigraphy, depositional environments and periods of deformation of the Wajid outcrop belt, southwestern Saudi Arabia. J Afr Earth Sci 21:421–441

    Article  Google Scholar 

  • Turner B, Monro M (1987) Channel formation and migration by mass-flow processes in the Lower Carboniferous fluviatile Fell Sandstone Group, north-east England. Sedimentology 34:1107–1122

    Article  Google Scholar 

Download references

Acknowledgements

We would like to express our thanks to the anonymous reviewer, whose meticulously worked out comments helped to improve the manuscript considerably.

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Correspondence to Martin Keller.

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Keller, M., Amarah, B.A. & Al Ajmi, H.F. The Wajid Sandstone around Abha/Khamis Mushayt and in its type area: lithostratigraphic architecture and correlations. Arab J Geosci 10, 55 (2017). https://doi.org/10.1007/s12517-016-2800-4

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  • DOI: https://doi.org/10.1007/s12517-016-2800-4

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