Skip to main content
Log in

Facies development and sedimentology of the Middle Miocene carbonates of the Raghama Formation, northeastern Saudi Arabia

  • Original Article
  • Published:
Acta Geochimica Aims and scope Submit manuscript

Abstract

Ragahama Formation comprises a siliciclastic continental deposits followed by marine carbonates, representing prograding alluvial fans from adjacent high hinterlands seaward into lagoons and fringing reef environments. The present work aimed to document the facies development and sedimentology of the Raghama carbonates exposed along the eastern coastal plain of the Red Sea, northwestern Saudi Arabia. Four stratigraphic sections were measured and sampled (D1–D4) and thin sections and major and trace element analyses were prepared and applied for petrographic and geochemical approaches. The carbonates were subdivided into three successive fore-reef, reef-core, and back-reef depositional facies. Sandy stromatolitic boundstone, microbial laminites, dolomitic ooidal grainstone, bioclastic coralline algal wackestone, sandy bioclastic wackestone, and coral boundstones were the reported microfacies types. Petrographic analysis reveals that the studied carbonates were affected by dissolution, dolomitization, and aggrading recrystallization, which affects both the original micrite matrix and grains or acts as fracture and veinlet filling leading to widespread vuggy and moldic porosity. No evidence of physical compaction, suggesting rapid lithification and recrystallization during early diagenesis and prior to substantial burial and intensive flushing by meteoric waters. Most of the original microstructure of corals were leached and destructed. This is indicated by the higher depletion in Sr and Ca levels and increase in Mg, Na, Fe, and Mn levels, especially in section D1, in comparison with the worldwide carbonates.

This is a preview of subscription content, log in via an institution to check access.

Access this article

Price excludes VAT (USA)
Tax calculation will be finalised during checkout.

Instant access to the full article PDF.

Fig. 1

(Modified from Tawfik et al. 2021)

Fig. 2
Fig. 3
Fig. 4
Fig. 5
Fig. 6
Fig. 7
Fig. 8

Similar content being viewed by others

References

  • Abu El-Enain F, El-Sorogy AS (1994) Microfacies, depositional environments and geochemistry of the Miocene carbonate succession of Gabal El-Safra, southern Sinai, Egypt. Middle East Res Center Ain Shams Univ Earth Sci Ser 8:167–177

    Google Scholar 

  • Adefris D, Nton ME, Boboye OA, Atnafu B (2020) Petrography and stable oxygen and carbon isotopic composition of the Antalo Limestone, Mekelle Basin, Northern Ethiopia: implications for marine environment and deep-burial diagenesis. Carbonates Evaporites 35:124

    Article  CAS  Google Scholar 

  • Al-Kahtany KM (2017) Facies development of the Middle Miocene reefal limestone in Northwest Saudi Arabia. J Afr Earth Sci 130:134–140

    Article  Google Scholar 

  • Al-Ramadan K (2017) Geochemical signatures of pervasive meteoric diagenesis of Early Miocene syn-rift carbonate platform, Red Sea, NW Saudi Arabia. Geol Q 61(1):239–250

    Google Scholar 

  • Bathurst RC (1975) Carbonate sediments and their diagenesis. Elsevier, Amsterdam, p 658

    Google Scholar 

  • Booker S, Jones B, Li L (2020) Diagenesis in Pleistocene (80 to 500 ka) corals from the Ironshore formation: implications for paleoclimate reconstruction. Sed Geol 399:105615

    Article  CAS  Google Scholar 

  • Bosworth W (2015) Geological evolution of the Red Sea: historical background, review, and synthesis. In: Rasul NM, Stewart IC (eds) The Red Sea. Springer, Berlin, pp 45–78

    Chapter  Google Scholar 

  • Bosworth W, Huchon P, McClay K (2005) The Red Sea and Gulf of Aden basins. J Afr Earth Sci 43(1–3):334–378

    Article  Google Scholar 

  • Braithwaite CJR, Camoin GF (2011) Diagenesis and sea-level change: lessons from Moruroa, French Polynesia. Sedimentology 58:259–284

    Article  ADS  Google Scholar 

  • Bramkamp RA, Brown GF, Holm DA, Layne NM Jr (1963) Geologic map of the Wadi as Sirhan quadrangle, Kingdom of Saudi Arabia. U.S. Geological Survey, p 200–A

  • Brown GF, Jackson RO, Boogue RG, Elberg EL (1963) Geologic map of northwestern Hijaz quadrangle: U.S. Geological Survey Miscellaneous Geologic Investigations Map 1–204A, 1:500000 scale

  • Budd DA, Land LS (1990) Geochemical imprint of meteoric diagenesis in Holocene ooid sands, Schooner Cays, Bahamas: correlation of calcite cement geochemistry with extent ground waters. J Sediment Petrol 60:361–378

    Google Scholar 

  • Cochran JK, Kallenberg K, Landman NH, Harries PJ, Weinreb D, Turekian KK, Beck AJ, Cobban WA (2010) Effect of diagenesis on the Sr, o, and C isotope composition of late cretaceous mollusks from the western interior seaway of North America. Am J Sci 310:69–88

    Article  ADS  CAS  Google Scholar 

  • Coimbra R, Azeredo AC, Cabral MC (2018) Cretaceous coastal lagoon facies: geochemical insights into multi-stage diagenesis and palaeoclimatic signals. Cretac Res 85:60–77

    Article  Google Scholar 

  • Cole GA, Abu-Ali MA, Coiling EL, Halpern HI, Carrigan WJ, Savage GR, Scolaro RJ, Al-Sharidi SH (1995) Petroleum geochemistry of the Midyan and Jaizan basins of the Red Sea, Saudi Arabia. Mar Pet Geol 12(6):597–614

    Article  CAS  Google Scholar 

  • Dickson JAD (1965) A modified staining technique for carbonates in thin section. Nature 205:587

    Article  ADS  CAS  Google Scholar 

  • El-Safory Y, El-Sorogy AS (1999) Early Miocene Bryozoa of Gebel Gharra, Northwest Gulf of Suez, Egypt. Egypt J Geol 44:19–35

    Google Scholar 

  • El-Sorogy AS (2001) Miocene coral reefs of the northern Red Sea coast, Egypt: facies development and diagenesis. Middle East Research Center, Ain Shams University. Earth Sci Ser 15:184–199

    Google Scholar 

  • El-Sorogy AS (2015) Bryozoan nodules as a frame-builder of bryzoan microreef, Middle Miocene sediments, Egypt. J Earth Sci 26(2):251–258

    Article  CAS  Google Scholar 

  • El-Sorogy AS, Abd-Elmoneim M, Mowafi A, Al-Kahtany K, Gahlan H (2017) Facies analysis and biostratigraphy of the miocene sequence, Cairo–Suez District, Egypt. J Earth Sci 28(1):1–8

    Article  CAS  Google Scholar 

  • El-Sorogy AS, Tsaparas N, Al-Kahtany K (2020) Middle Miocene corals from Midyan area, Northwestern Saudi Arabia. Geol J 55(7):5594–5605

    Article  ADS  Google Scholar 

  • El-Sorogy AS, Ziko A (1999) Facies development and environments of Miocene reefal limestone, Wadi Hagul, Cairo–Suez district, Egypt. Neues Jahrbuch für Geologie und Paläontologie 4:213–226

    Article  Google Scholar 

  • Ghebreab W (1998) Tectonics of the Red Sea region reassessed. Earth Sci Rev 45:1–44

    Article  ADS  Google Scholar 

  • Hughes GW (2014) Micropalaeontology and palaeoenvironments of the Miocene Wadi Waqb carbonate of the northern Saudi Arabian Red Sea. GeoArabia 19(4):59–108

    Article  Google Scholar 

  • Hughes GW, Johnson RS (2005) Lithostratigraphy of the Saudi Arabian Red Sea. GeoArabia 10:49–126

    Article  Google Scholar 

  • Hughes GW, Perincek D, Grainger DJ, Abu-Bshait A, Jarad AM (1999) Lithostratigraphy and depositional history of part of the Midyan region, northwestern Saudi Arabia. GeoArabia 4:503–542

    Article  Google Scholar 

  • Kahal AY, El-Sorogy AS, Alfaifi HJ, Almadani S, Kassem OM (2019) Biofacies and diagenetic alterations of the pleistocene coral reefs, northwest Red Sea coast, Saudi Arabia. Geol J. https://doi.org/10.1002/gj.3503

    Article  Google Scholar 

  • Koeshidayatullah A, Al-Ramadan K, Collier R, Hughes GW (2016) Variations in architecture and cyclicity in fault-bounded carbonate platforms, early Miocene Red Sea rift, NW Saudi Arabia. Mar Pet Geol 70:77–92

    Article  Google Scholar 

  • Ligi M, Bonatti E, Rasul NMA (2015) Seafloor spreading initiation: geophysical and geochemical constraints from the Thetis and Nereus Deeps, Central Red Sea. In: Rasul NMA, Stewart ICF (eds) The Red Sea: the formation, morphology, oceanography andenvironment of a Young Ocean Basin. Springer, Berlin, Heidelberg, pp 79–98

    Chapter  Google Scholar 

  • McGregor HV, Gagan MK (2003) Diagenesis and geochemistry of Porites corals from Papua New Guinea: implications for paleoclimate reconstruction. Geochim Cosmochim Acta 67:2147–2156

    Article  ADS  CAS  Google Scholar 

  • Moon F, Sadek H (1923) Preliminary geological report on Wadi Gharandal area. Petrol Res Bull Cairo 9:1–40

    Google Scholar 

  • Morad S, Al Suwaidi M, Mansurbeg H, Morad D, Ceriani A, Paganoni M, Al-Aasm I (2019) Diagenesis of a limestone reservoir (lower cretaceous), Abu Dhabi, United Arab Emirates: comparison between the anticline crest and flanks. Sed Geol 380:127–142

    Article  Google Scholar 

  • Powers RW, Ramires LF, Redond CD, Elberg EL (1966) Geology of the Arabian peninsula, sedimentary geology of Saudi Arabia. US Geol Surv Prof Paper 560D:147p

    Google Scholar 

  • Rasul NMA, Stewart ICF, Nawab ZA (2015) Introduction to the Red Sea: its origin, structure, and environment. In: Rasul NMA, Stewart ICF (eds) The Red Sea: the formation, morphology, oceanography and environment of a young ocean Basin. Springer-Verlag, Berlin, p 614

    Chapter  Google Scholar 

  • Ren M, Jones B (2016) Diagenesis in limestone–dolostone successions after 1 million years of rapid sea-level fluctuations: a case study from Grand Cayman, British West Indies. Sed Geol 342:15–30

    Article  Google Scholar 

  • Seibel MJ, James NP (2017) Diagenesis of Miocene, incised valley-filling limestones; Provence, Southern France. Sed Geol 347:21–35

    Article  CAS  Google Scholar 

  • Spencer CH (1987) Provisional stratigraphy and correlation of the tertiary rocks in the Jiddah region. Ministry of the petroleum and mineral resources, deputy ministry for mineral resources open-file report BRGM-580 OF-06-17, p 37

  • Stern RJ (1994) Arc assembly and continental collision in the Neoproterozoic East African Orogen: implications for the consolidation of Gondwanaland. Annu Rev Earth Planet Sci 22:319–351

    Article  ADS  Google Scholar 

  • Stern R, Kroner A (1993) Late precambrian crustal evolution in NE Sudan: isotopic and geochronologic constraints. J Geol 101:555–574

    Article  ADS  CAS  Google Scholar 

  • Stockli DF, Bosworth W (2019) Timing of extensional faulting along the magma-poor central and northern Red Sea rift margin— transition from regional extension to necking along a hyperextended rifted margin. In: Rasul NM, Stewart IC (eds) Geological setting, palaeoenvironment and archaeology of the Red Sea. Springer International, Switzerland, pp 81–111

    Chapter  Google Scholar 

  • Tawfik M, Al-Hashim M, El-Sorogy AS, Alharbi T, Wadani M (2021) Coastal alluvial fans of the Raghama formation, Northern East Red Sea, Saudi Arabia. J Coast Res 37(3):1193–1203

    Google Scholar 

  • Tawfik M, El-Sorogy AS, Mowafi A, Al-Malky M (2015) Facies and sequence stratigraphy of some Miocene sediments in the Cairo–Suez district, Egypt. J Afr Earth Sci 101:84–95

    Article  Google Scholar 

  • Taylor SR (1964) Abundance of chemical elements in the continental crust: a new table. Geochim Cosmochim Acta 28:1273–1285

    Article  ADS  CAS  Google Scholar 

  • Tubbs RE, Aly A, Fouda HG, Afifi AM, Raterman NS, Hughes GW, Fadolalkarem YK (2014) Midyan Peninsula, northern Red Sea, Saudi Arabia: seismic imaging and regional interpretation. GeoArabia 19(3):165–184

    Article  Google Scholar 

  • Turekian KK, Wedepohl KH (1961) Distribution of the elements in some major units of the earth’s crust. Geol Soc Am Bull 72:175–192

    Article  CAS  Google Scholar 

  • United States Geological Survey USGS (1963) Geologic map of the Arabian Peninsula. Washington, DC: United States Government Printing Office, Map1-270-A

  • Veizer J (1983) Chemical diagenesis of carbonates: theory and application of trace element technique. In: Arthur MA, Anderson TF, Kaplan IR, Veizer J, Land LS (eds) Stable isotopes in sedimentary geology. SEPM short course, vol 10. SEPM Society for Sedimentary Geology

    Google Scholar 

  • Wilson JL (1975) Carbonate facies in geologic history. Springer-Verlag, Berlin, p 456

    Book  Google Scholar 

  • Yaroshevsky AA (2006) Abundances of chemical elements in the Earth’s crust. Geochem Int 44:48–55

    Article  Google Scholar 

Download references

Funding

This research was supported and funded by the Researchers Supporting Project number (RSPD2023R781), King Saud University, Riyadh, Saudi Arabia.

Author information

Authors and Affiliations

Authors

Corresponding author

Correspondence to Mansour H. Al-Hashim.

Ethics declarations

Conflict of interest

The authors certify that neither the submitted material nor portions thereof have been published previously or are under consideration for publication elsewhere. The authors declare that they have no known competing financial interests or personal relationships that could have appeared to influence the work reported in this paper.

Rights and permissions

Springer Nature or its licensor (e.g. a society or other partner) holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law.

Reprints and permissions

About this article

Check for updates. Verify currency and authenticity via CrossMark

Cite this article

Al-Hashim, M.H., El-Sorogy, A.S. & Wadani, M. Facies development and sedimentology of the Middle Miocene carbonates of the Raghama Formation, northeastern Saudi Arabia. Acta Geochim 43, 87–96 (2024). https://doi.org/10.1007/s11631-023-00643-5

Download citation

  • Received:

  • Revised:

  • Accepted:

  • Published:

  • Issue Date:

  • DOI: https://doi.org/10.1007/s11631-023-00643-5

Keywords

Navigation