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Relationship between finite strain and tectonic setting in the Ar-Ruwaydah area, eastern Arabian Shield, Saudi Arabia

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Abstract

Our work deals with structural characteristics of the Ar-Ruwaydah area, which lie between the Al Amar–Idsas fault and the Halaban belt. Our goals are accomplished through field reconnaissance and finite strain analysis, as well as microstructural investigation to estimate the tectonic evolution and structures in the Ar-Ruwaydah area. Our strain data show that Abt schist, metavolcano-sedimentary rocks, and granitic gneiss are characterized by weak to moderate deformation, and the axial ratios for the XZ section range from 1.55 to 2.22. The long axes for ellipsoids (X) have NW–SE and W–E trend directions in the Ar-Ruwaydah area while their short axes (Z) are subhorizontal to subvertical foliations. The strain magnitude does not display any increase towards the tectonic contacts for varying rocks units. Most of the obtained data indicate a dominant oblate with minor prolate strain symmetries in the Abt schist and metavolcano-sedimentary and metagranite rocks. The strain data also display flattening with some constriction. It is concluded that Abt schist, granitic gneiss, and metavolcano-sedimentary rocks have the same deformation behavior. Our finite strain accumulated during the metamorphism which was investigated by thrusting activity in the studied rocks. Furthermore, the nappe contact for different types of rock formed during thrusting activity and intrusion of granitic plutons under semi-brittle to ductile deformation conditions in the Ar-Ruwaydah area.

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References

  • Ali KA, Stern RJ, Manton WI, Kimura JI, Whitehouse MJ, Mukherjee SK, Johnson PR, Griffin WR (2010) Geochemical U_Pb zircon, and Nd isotope investigations of the Neoproterozoic Ghawjah metavolcanic rocks, Northwestern Saudi Arabia. Lithos 120:379–392

    Article  Google Scholar 

  • Al-Saleh AM, Boyle AP (2001) Structural rejuvenation of the eastern Arabian Sshield during continental collision: 40Ar/39Ar evidence from the Ar Ridaniyah ophiolite mélange. J Afr Earth Sci 33:135–141

    Article  Google Scholar 

  • Al-Saleh AM, Kassem OMK (2012) Microstructural, strain analysis and 40Ar/39Ar evidence for the origin of the Mizil gneiss dome, eastern Arabian Shield, Saudi Arabia. J Afr Earth Sci 70:24–35

    Article  Google Scholar 

  • Al-Shanti AM, Gass IG (1983) The upper Proterozoic ophiolite melange zones of the easternmost Arabian Shield. J Geol Soc 140:867–876

    Article  Google Scholar 

  • Calvez JY, Alsac C, Delfour J, Kemp J, Pellaton C, (1983) Geologic evolution of western, central, and eastern parts of the Northern Precambrian Shield, Kingdom of Saudi Arabia. Saudi Arabian Deputy Ministry for Mineral Resources Open-File Report BRGM-OF-02-26, p. 39

  • Collins AS, Pisarevsky SA (2005) Amalgamating eastern Gondwana: the evolution of the Circum-Indian Orogens. Earth-Sci Rev 71:229–270

    Article  Google Scholar 

  • Cox GM, Lewis CJ, Collins AS, Halverson GP, Jourdan F, Foden J, Nettle D, Kattan F (2012) Ediacaran terrane accretion within the Arabian-Nubian Shield. Gondwana Res 21:341–352

    Article  Google Scholar 

  • Delfour J, (1979) Geology of the Nuqrah Quadrangle, 25E, Kingdom of Saudi Arabia. Saudi Arabian Directorate General of Mineral Resources Geologic Map GM 28, scale 1:250,000, p. 32

  • Doebrich JL, Al-Jehani AM, Siddiqui AA, Hayes TS, Saleh Y, Wooden JL, Johnson PR, Kattan FH, Shaikan B, Basahel M, Zahran H, Al-Shammari A (2007) Geology and mineral resources of the Ar Rayn terrane, eastern Arabian Shield, Kingdom of Saudi Arabia. Precambrian Res 158:17–50

    Article  Google Scholar 

  • Flinn D (1962) On folding during three-dimensional progressive deformation. Quarternary Journal of Geological Society of London 118:385–433

    Article  Google Scholar 

  • Fry N (1979) Random point distributions and strain measurement in rocks. Tectonophysics 60:89–105

    Article  Google Scholar 

  • Hossack JR (1968) Pebble deformation and thrusting in the Bygdin area Southern Norway. Tectonophysics 5:315–339

    Article  Google Scholar 

  • Johnson PR (1998) The structural geology of the Samran-Shayban area, Kingdom of Saudi Arabia: Saudi Arabian Deputy Ministry for Mineral Resources Technical Report USGS-TR-98-02, 45 p

  • Johnson PR, Woldehaimanot B (2003) Development of the Arabian–Nubian shield: perspectives on accretion and deformation in the northern East African Orogen and the assembly of Gondwana. In: Yoshida M, Windley BF, Dasgupta S (eds) Proterozoic east Gondwana: supercontinent assembly and breakup: geological society, vol 206. Special Publication, London, pp. 290–325

    Google Scholar 

  • Johnson PR, Andresen A, Collins AS, Fowler AR, Fritz H, Ghebreab W, Kusky T, Stern RJ (2011) Late Cryogenian–Ediacaran history of the Arabian–Nubian Shield: a review of depositional, plutonic, structural, and tectonic events in the closing stages of the northern East African Orogen. J Afr Earth Sci 61:167–232

    Article  Google Scholar 

  • Kassem OMK (2011) Determining heterogeneous deformation for granitic rocks in the northern thrust in Wadi Mubark belt, Eastern Desert, Egypt. Geotectonics Journal 45(3):244–254

    Article  Google Scholar 

  • Kassem OMK (2014) Kinematic analysis of the Migif area in the Eastern Desert of Egypt. J Afr Earth Sci 90:136–149

    Article  Google Scholar 

  • Kassem OMK (2015) Investigation of kinematic analysis in the Tanumah area, Arabian Shield, Saudi Arabia. Journal of Tethys 3(1):16–30

    Google Scholar 

  • Kassem OMK, Abdel Raheim S (2010) Finite strain analysis for the metavolcanic-sedimentary rocks in the Gabel El-Mayet region, Central Eastern Desert, Egypt. J Afr Earth Sci 58:321–330

    Article  Google Scholar 

  • Kassem OMK, Ring U (2004) Underplating-related finite-strain patterns in the Gran Paradiso massif, Western Alps, Italy: heterogeneous ductile strain superimposed on a nappe stack. J Geol Soc Lond 161:875–884

    Article  Google Scholar 

  • Kassem OMK, Abd El Rahim SH, El Nashar ER (2012) Strain analysis and microstructural evolution characteristic of Neoproterozoic rocks associations of Wadi El Falek, Centre Eastern Desert, Egypt. Geotectonics 46(5):379–388

    Article  Google Scholar 

  • Kennedy A, Johnson PR, Kattan, FH (2004) SHRIMP geochronology in the northern Arabian Shield, Part 1: data acquisition, Saudi Geological Survey Open File Report SGS-OF-2004-11, p. 28

  • Nawab ZAH (1978) Evolution of the Al Amar Idasas region of the northern part of the Arabian Shield (Kingdom of Saudi Arabia), Bulletin du BRGM (deuxieme series), 1–19, sec II, no 1–2

  • Nehlig P, Genna A, Asfirane F (2002) A review of the Pan-African evolution of the Arabian Shield. GeoArabia, V 7:103–124

    Google Scholar 

  • Owens WH (1984) The calculation of a best-fit ellipsoid from elliptical sections on arbitrarily oriented planes. J Struct Geol 6:571–578

    Article  Google Scholar 

  • Passchier CW, Trouw RA (1995) Microtectonics. Springer, Berlin Heidelberg 366

    Google Scholar 

  • Peach CJ, Lisle RJ (1979) A fortran IV program for the analysis of tectonic strain using deformed elliptical markers. Computer & Geoscience 5:325–334

    Article  Google Scholar 

  • Ramsay JG (1967) Folding and fracturing of rocks. McGraw Hill, New York

    Google Scholar 

  • Ramsay JG, Huber MI (1983) The techniques of modern structural geology, vol 1. Academic Press, London

    Google Scholar 

  • Ring U, Kassem OMK (2007) The nappe rule: why does it work? J Geol Soc 164:1109–1112

    Article  Google Scholar 

  • Stacey JS, Stoeser DB, Greenwood WR, Fischer LB (1984) U–Pb zircon geochronology and geologic evaluation of the Halaban-Al Amar region of the eastern Arabian Shield. J Geol Soc Lond 141:1043–1055

  • Stern RJ (1994) Arc assembly and continental collision in the Neoproterozoic East African Orogen: implications for the consolidation of Gondwanaland. Annual Reviews of Earth and Planetary Sciences 22:315–319

    Article  Google Scholar 

  • Stern RJ (2002) Crustal evolution in the East African Orogen: a neodymium isotopic perspective. J Afr Earth Sci 34:109–117

    Article  Google Scholar 

  • Stern RJ (2008) Neoproterozoic crustal growth: the solid Earth system during a critical episode of Earth history. Gondwana Res 14:33–50

    Article  Google Scholar 

  • Stern RJ, Johnson PR (2010) Continental lithosphere of the Arabian plate: a geologic, petrologic, and geophysical synthesis. Earth Sci Rev 101:29–67

    Article  Google Scholar 

  • Stoeser DB, Camp VE (1985) Pan-African microplate accretion of the Arabian Shield. Geol Soc Am Bull 96:817–826

    Article  Google Scholar 

  • Stoeser DB, Frost CD (2006) Nb, Pb, Sr, and O isotopic characterization of Saudi Arabian Shield terranes. Chem Geol 226:163–188

    Article  Google Scholar 

  • Stoeser DB, Stacey JS, Greenwood WR, Fischer LB (1984) U/Pb zircon geochronology of the southern part of the Nabitah Mobile Belt and Pan-African continental collision in the Saudi Arabian Shield”, Saudi Arabian Deputy Ministry for Mineral Resources Technical Record USGS-TR-04-5, pp. 88

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Acknowledgments

The authors would like to extend their sincere appreciation to the Deanship of Scientific Research at King Saud University for its funding of this research through the Research Group project no RGP-VPP-230.

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Correspondence to Osama M. K. Kassem.

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Kassem, O.M.K., Almutairi, A.L., Al Bassam, A.A.M. et al. Relationship between finite strain and tectonic setting in the Ar-Ruwaydah area, eastern Arabian Shield, Saudi Arabia. Arab J Geosci 9, 728 (2016). https://doi.org/10.1007/s12517-016-2760-8

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  • DOI: https://doi.org/10.1007/s12517-016-2760-8

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