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Strain analysis and microstructural evolution characteristic of neoproterozoic rocks associations of Wadi El Falek, centre Eastern Desert, Egypt

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Abstract

The estimation of finite strain in rocks is fundamental to a meaningful understanding of deformational processes and products on all scales from microscopic fabric development to regional structural analyses. The Rf/φ and Fry methods on feldspar porphyroclasts and mafic grains from 5 granite, 1 metavolcanic, 3 metasedimentary and 1 granodiorite samples were used in Wadi El Falek region. Finite-strain data shows that a high to moderate range of deformation of the granitic to metavolcano-sedimentary samples and axial ratios in the XZ section range from 1.60 to 4.10 for the Rf/φ method and from 2.80 to 4.90 for the Fry method. Furthermore, the short axes are subvertical associated with a subhorizontal foliation. We conclude that finite strain in the deformed granite rocks is of the same order of magnitude as that from metavolcano-sedimentary rocks. Furthermore, contacts formed during intrusion of plutons with some faults in the Wadi El Falek area under brittle to semi-ductile deformation conditions. In this case, finite strain accumulated during superimposed deformation on the already assembled nappe structure. It indicates that the nappe contacts formed during the accumulation of finite strain.

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Authors and Affiliations

  1. SGSRC, Department of Geology, Science faculty, King Saud University, P.O. Box 2455, Riyadh, 11451, Kingdom of Saudi Arabia

    Osama M. K. Kassem

  2. Department of Geology, National Research Center, Al-Behoos str., Dokki, Cairo, 12622, Egypt

    Osama M. K. Kassem, Said H. Abd El Rahim & El Said R. El Nashar

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  1. Osama M. K. Kassem
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  2. Said H. Abd El Rahim
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  3. El Said R. El Nashar
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Correspondence to Osama M. K. Kassem.

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Kassem, O.M.K., Rahim, S.H.A.E. & Nashar, E.S.R.E. Strain analysis and microstructural evolution characteristic of neoproterozoic rocks associations of Wadi El Falek, centre Eastern Desert, Egypt. Geotecton. 46, 379–388 (2012). https://doi.org/10.1134/S0016852112050032

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