Skip to main content
Log in

Some carbonate rocks utilized as a building material rocks, Egypt

  • Original Article
  • Published:
Carbonates and Evaporites Aims and scope Submit manuscript

Abstract

Studies of the geochemical, mineralogical, petrographical characteristics and the physicochemical properties were carried out on some carbonate rocks, so as to throw light on the possibility of utilizing them as a building stones. The dolomitic and dolostone rocks of Gebel Ataqa and Giran El-Ful quarries have been acquiring potential application in building and industry. Petrographically, the dolomite rocks of the Gebel Ataqa quarries are characterized by dolo-biomicrosparite and dolomitic limestone microfacies for Hassan Alaam quarry and dolosparite microfacies for Arab Contractors quarry, while those of Giran El-Ful (Abu Roash area) are mainly dolo-biomicite microfacies and dolostones. They are deposited in mixing zone environment. Mineralogically, XRD patterns indicate the dolomites of the Ataqa and Giran El-Ful quarries are non-stoichiometric. XRD with DTA revealed that the rocks of the three quarries are consisting mainly of dolomite (Ataqa quarries), calcite and ankarite (Abo Roash quarry), as the main constituents, besides quartz and halite as minor constituents. Geochemically, the normative dolomite contents in the studied rocks with an average ~ 90, ~ 35, and ~ 31% for Arab Contractors, Hassan Alaam and Giran El-Ful quarries; respectively. Thus, the dolomitization was more effective in the Cretaceous carbonates at Arab Contractors quarry than those in the Middle Eocene in Hassan Alaam and Giran El-Ful quarries. Arab Contractors have very high Mg content followed by Hassan Alaam, though impoverished in Na2O, K2O, Al2O3, Fe2O3, SO3, SiO2, TiO2, and Cl. Giran El-Ful quarry has very high Fe2O3 and MgO contents; on the other hand, poor in Na2O, K2O, Al2O3, SO3, SiO2, TiO2, and Cl. Sr contents indicate that the dolomite crystals were deposited in mixing zone environments. The total radioactivity measurements are ranging from 2 to 8 ppm for U and from 3 to 9 ppm for Th. The radioactivity measurements are approximately against to the background level of carbonates, and they are in the permissible limits for carbonates used in cement industries and as building stones. The dolomitic and dolostone rocks of the three quarries are proved chemically suitable for the industries relevant to crushed aggregates and lime production. Physically–mechanically examination revealed that the youngest carbonate deposits in the Middle Eocene (Hassan Alaam quarry) rocks have relatively low porosity, water absorption, and crushability, and highest compressive strength compared with those carbonate rocks of the two other quarries of Upper Cretaceous (Arab Contractors and Giran El-Ful). The petrographical, geochemical, and physical–mechanical observations recommended that the carbonates rocks of Hassan Alaam and Arab Contractors quarries in Gebel Ataqa area clearly can be used in the production of crushed aggregates to utilize in the concrete works. On the other hand, Giran El-Ful quarry can be used only in the mechanical sawing and in the production of limestone blocks.

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
Fig. 2
Fig. 3
Fig. 4
Fig. 5

Similar content being viewed by others

References

  • Aadland AJ, Hassan AA (1972) Hydrocarbon potential of Abu-Gharading basin in Western Desert, Egypt. In: 8th Arab Petrol. Cong., Algiers (8): (B-3)

  • Abou El- Anwar EA (2006) Petrography, geochemistry and genesis of some Middle Eocene rocks at Qattamia area, Cairo-Suez Road, Egypt. NRC Egypt 3(6):519–543

    Google Scholar 

  • Abou El- Anwar EA (2007) Diagenesis and geochemistry of the reefal facies of the Shagra Formation, Ras Benas, Red Sea coast, Egypt. NRC Egypt 32(5):511–536

    Google Scholar 

  • Abou El- Anwar EA (2011) Petrographical, geochemical and diagenetic studies of the middle Eocene carbonates, Mokattam Formation of Darb El-Fayium area. In: Int. Conf. on Geological Sciences and Engineering, Farance, Paris, Augustus 24–26, vol 80, pp 1315–1325

  • Abou El- Anwar EA (2012) Contribution to the composition and origin of the reef Terraces in Ras Mohamed, Sharm El-Sheikh Coast, Southern Sinai, Egypt. Geol Soc Egypt. 56:33–48

    Google Scholar 

  • Abou El- Anwar EA (2014) Composition and origin of the dolostones of Um Bogma formation, lower carboniferous, West Central Sinai, Egypt. Carbonates Evaporates 29:239–250

    Article  Google Scholar 

  • Abou El-Anwar EA (2010) Petrographical, geochemical and environmental studies of the subsurface carbonate sediments of El-Azima Well, western Samalut, Samalut Formation, El-Minia, Egypt. Sedimentol Egypt 18:98–100

    Google Scholar 

  • Abou El-Anwar EA, Melegy AA (2005) Hazards and possible application of carbonate deposits from Abu-Roash. Southwest Cairo, Sedimentology of Egypt. 13:189–199

    Google Scholar 

  • Abou El-Anwar EA, Mekky HS, Darweesh HS, Aita SK (2016) Utilization of some Miocene Limestones as building materials from Egyptian north western coastal area (Abu– Sir Ridge). Carbonates Evaporates. https://doi.org/10.1007/s13146-016-0326-1

    Article  Google Scholar 

  • ASTM C88-13, Standard Test Method for Soundness of Aggregates by Use of Sodium Sulfate or Magnesium Sulfate, ASTM International, West Conshohocken, PA

  • Badiozamani K (1973) The Dorag dolomitization model-application to the Ordovician of Wisconsin. J Sediment Pet 43:965–984

    Google Scholar 

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

    Google Scholar 

  • Brand V, Veizer J (1980) Chemical diagenesis of a multicomponant carbonate systems—1. Trace elements. J Sediment Pet 50:1219–1236

    Google Scholar 

  • El- Akkad S, Abdallah AM (1971) Contribution to the geology of Gebel Ataqa area. Ann Geol Surv Egypt 1:1–21

    Google Scholar 

  • Harrison DJ (1993) Industrial minerals laboratory manual, limestone: British Geological Survey, Technical Report WG./92/29, p. 4

  • IAEA (International Atomic Energy Agency) (1979) Gamma ray surveys in uranium exploration. Technical Report Series No. 186, STI/DOC/10/186, IAEA, Vienna, 90 p

  • Ismail MM, El-Mahdy OR, El-Nozahi FA (1974) Geological studies of Gebel Ataqa surface section. Bull Inst Desert Egypt. 24:1–11

    Google Scholar 

  • Loukina S, Abou El-Anwar EA (1991) Petrography, mineralogy and diagenesis of Gebel Ataqa dolostones. Egypt J Geol 35(1–2):133–145

    Google Scholar 

  • Loukina S, Abou El-Anwar EA (1994) Geochemistry of Gebel Ataqa dolostones. Egypt J Geol 38(1):141–156

    Google Scholar 

  • Lumsden DN (1979) Discrepancy between thin-section and X-Ray estimates of dolomite in limestone. J Sediment Pet 49(2):424–436

    Google Scholar 

  • Matolin M. (1990) A report to the Government of the Arab Republic of Egypt, construction and use of spectrometric calibration pads, Egy/4/030-03, Laboratory of Gamma-ray Spectrometry

  • Pagano MA, Cardy PD (1982) A Chemical approach to the problem of alkalies—reactive carbonates aggregates. Cem Concr Res 12:1–12

    Article  Google Scholar 

  • Said R (1962) The geology of Egypt. Elsevier, Amsterdam

    Google Scholar 

  • Siegel FR (1967) Properties and uses of the carbonates. - Kap. 9. In: Chilingar GV, Bissell HJ, Fairbridge RW (eds) Carbonate rocks, Dev. Sedimentol.9B, 343–393, 4 Abb., 29 Tab. Elsevier, Amsterdam-London-New York

  • Zatout MA (1956) The dolomite and dolomitic rocks of Gebel 'Ataqa. (Eastern cliff — Suez sheet). Geol. Survey Egyp, 27 p

Download references

Author information

Authors and Affiliations

Authors

Corresponding author

Correspondence to Esmat Ahmed Abou El-Anwar.

Rights and permissions

Reprints and permissions

About this article

Check for updates. Verify currency and authenticity via CrossMark

Cite this article

El-Anwar, E.A.A. Some carbonate rocks utilized as a building material rocks, Egypt. Carbonates Evaporites 34, 1333–1341 (2019). https://doi.org/10.1007/s13146-018-0423-4

Download citation

  • Accepted:

  • Published:

  • Issue Date:

  • DOI: https://doi.org/10.1007/s13146-018-0423-4

Keywords

Navigation