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Geotechnical properties of Precambrian carbonate, Saudi Arabia

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Abstract

The effect of post depositional processes (e.g., diagenesis) on geotechnical properties of the studied Fatima carbonates has been evaluated on 32 oriented samples of Precambrian carbonate of Fatima Group, Jeddah, Saudi Arabia where Fatima carbonate considered as the oldest sedimentary rock unit. Fatima carbonate sequence represents the middle part of Fatima Group and attains 90–130 m thick. Fatima carbonate composes mainly of alternating cycles of highly deformed, folded, and faulted stromatolitic carbonates. Algal laminates with scattered dolomite pseudomorphs are recorded within these carbonates and are shown clearly in cut-slabs. The laminae are millimetric in thickness. The Fatima carbonate has a relative abundance of nearly uniform-sized dolomite crystals. Dolomite crystal are represented by small-sized rhombs of euhedral, subhedral, and non-rhombic. The larger euhedral rhomb-shaped dolomite crystals are occurred as cavity filling dolomite. The silicification features are recognized as patches of cryptocrystalline quartz replacing laminated carbonates. It is believed that this type of silicification represents late diagenetic stage and not influenced by the depositional environment or by physicochemical conditions of water. XRD charts indicate that the Fatima carbonate is consisted mainly of dolomite, quartz, and minor constitutes of gypsum. These carbonates are mostly barren in marine fossils and it is clear that these carbonates were deposited within restricted (lagoonal) marine environment. The rock unit weight values of the studied Fatima carbonate range from 29.429 to 25.993 kN/m3. The total porosity varies from 9.147 to 6.112%. The uniaxial compressive strength (UCS, measured by Schmidt Hammer) values of Fatima carbonate range from 22.6 to 110 MPa for the horizontal direction and from 19.7 to 71.8 MPa for the vertical direction). The abovementioned results implicate that the studied Fatima carbonate rock samples are classified as medium to strong rocks.

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Acknowledgements

The authors are deeply grateful to Prof. Dr. A.M. Al-Amri (Editor-in-Chief) and the anonymous reviewers for insightful comments and criticism that improved the original manuscript.

Funding

This project was funded by the Deanship of Scientific Research (DSR), King Abdulaziz University, Jeddah, under grant no. 64-145-1437. The authors, therefore, acknowledge and thank the Deanship of Scientific Research (DSR) for the technical and financial support.

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Authors and Affiliations

  1. Faculty of Earth Sciences, King Abdulaziz University, Jeddah, Saudi Arabia

    El-Sayed Sedek Abu Seif & Abdulelah A. Bahabri

  2. Geology Department, Faculty of Science, Sohag University, Sohag, Egypt

    El-Sayed Sedek Abu Seif & Abd El-Hamed El-Shater Abd El-Hamed

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  1. El-Sayed Sedek Abu Seif
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  2. Abdulelah A. Bahabri
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Correspondence to El-Sayed Sedek Abu Seif.

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Seif, ES.S.A., Bahabri, A.A. & El-Hamed, A.EH.ES.A. Geotechnical properties of Precambrian carbonate, Saudi Arabia. Arab J Geosci 11, 500 (2018). https://doi.org/10.1007/s12517-018-3821-y

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