Abstract
The rocks of the Oligocene Asmari Formation represent the outer ridges surrounding Jabal Hafit anticline. The carbonate beds of this formation dip gently under the northern and western sides of Al-Ain city. The beds are dissected by several sets of joints and characterized by the abundance of the connected caves of different sizes, particularly in the thick chalky beds. In this study, petrographic and mineralogical studies by X-ray diffraction analysis and scanning electron microscope revealed that the examined carbonate rock samples are made up mainly of calcite and minor of authigenic dolomite and quartz minerals. The 87Sr/86Sr data obtained from the 8 fossils of Asmari Formation range between 0.707989 and 0.707835. The age of the analyzed rocks was estimated from the 87Sr/86Sr values that suggest a range from approximately 29.6 to 33.5 my (late Rupelian stage of the Oligocene).
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Acknowledgments
This study was financially supported by the Research Affairs (RA) at the UAE University (03-05-2-IV 09). The authors would like to thank the UAE University-RA for financial support. Sincere thanks to Prof. Ala Aldahan from the UAE University for chemical analyses.
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El Tokhi, M., Arman, H., Abdelghany, O. et al. Isotope Stratigraphy of Oligocene Limestone in Al-Ain City, United Arab Emirates. Arab J Sci Eng 37, 1439–1449 (2012). https://doi.org/10.1007/s13369-012-0253-y
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DOI: https://doi.org/10.1007/s13369-012-0253-y