Evaluation of the Waras Serpentinite Rocks for Dimension Stone, Mawat Ophiolite Complex, Kurdistan Region, NE Iraq

Main Article Content

Rezan Qadir Faraj

Abstract

The Mawat ophiolite complex (MOC) is a part of the Zagros Suture Zone, which extends of about 2000 km from southeastern Turkey through northern Syria and Iraq to western and southern Iran. The serpentinite rocks are exposed at Waras area near Betwat village. Serpentinite rocks from this area have been studied to assess their suitability for use as dimension stone. Ten samples were collected in the studied area to establish their physical and mechanical properties. Petrographic studies indicate that the serpentinite rocks in the studied area are composed mostly of serpentine minerals so the results of the color measurement show multiple colors of the studied samples after polishing which are grayish green, greenish black, brownish black, olive brown and dark yellowish green. Physical properties for the studied samples were determined they show low bulk density while the water absorption for all the studied samples except sample (10) show suitability for the interior uses, as well as only the samples (4, 6, 7, 8 and 9) exhibit suitable range of interior and exterior uses. The results of the compressive strength and modulus of rupture of the studied samples are below the requirement. According to the American Standard for Testing and Materials, ASTM C1526-02(2002) the serpentinite rocks from Waras area is not suitable for the use as dimension stone.

Article Details

How to Cite
Rezan Qadir Faraj. (2023). Evaluation of the Waras Serpentinite Rocks for Dimension Stone, Mawat Ophiolite Complex, Kurdistan Region, NE Iraq. Tikrit Journal of Pure Science, 27(6), 43–50. https://doi.org/10.25130/tjps.v27i6.757
Section
Articles

References

[1] Smith, M.R. (1999). Stone: Building stone, rock fill and armourstone in construction. Geological Society Engineering Geology Special Publication No.16.

[2] Nasir, S. et al. (2015). Geotechnical Assessment of Dimension stone Resources in Oman. International Journal of Chemical, Environmental & Biological Sciences (IJCEBS) Volume 3, Issue 6.

[3] Ashmole, I. (2004).Dimension Stone: The Small Scale Mining Potential in South Africa. Paper presented at Small Scale Mining 2004, Johannesburg.

[4] Thrush, P.W. et al. (1968).A dictionary of mining, mineral, and related terms.p1269, US Bureau of Mines.

[5] Carvalho, J.F.et al, (2008).Decision criteria for the exploration of ornamental-stone deposits: Application to the marbles of the Portuguese Estremoz Anticline.International Journal of Rock Mechanics and Mining Sciences.

[6] Ghazal, M.M. , Salih, A.M. and Mohammed, A.H., (2018). Serpentinite Rocks of Mawat Ophiolite Complex, Northeastern Iraq, Beetwat Village: 1-Petrography and Diffractometry. Tikrit Journal of Pure Science 23 (7): 1813 – 1662.

[7]Aqrawi, A.M., Elias, E.M and Mohammad, Y.O.(2007). Oxygen and Hydrogen Isotope Study of Serpentinized Peridotite Rocks, Thrust Zone, North East Iraq. Iraqi Journal of Earth Sciences, 7(1):13-20.

[8] Meierding, T.C. (2005).Weathering of serpentine stone buildings in the Philadelphia region: a geographic approachrelated to acidic deposition. In Stone Decay in the Architectural Environment; Turkington, A.V., Ed.Geological Society of America: Denver, CO, USA; Vol.399, pp. 17–25.

[9] Navarro, R. et al.(2015). The Sierra Nevada serpentinites:The serpentinites most used in Spanish heritage buildings. In Global Heritage Stone: Towards International

Recognition of Building and Ornamental Stones. Geological Society: London, UK, Vol. 407, pp. 101–108.

[10] Ozsoy, E.A.; Yilmaz, G. and Arman, H.(2010). Physical, mechanical and mineralogical properties of ophiolitic rocks at the Yakakayi dam site, Eskisehir, Turkey. Sci. Res. Essays, 5, 2579–2587.

[11] Navarro, R. et al. (2013). A serpentinite wrongly referred to as amarble. Geoscience, 3, 102–113.

[12] Smirnov, V. A., and Nelidov, V. P. (1962).Report on 1:200000 prospecting-correlation of the Sulaimani-Chowarta and Penjwin area. Unpublished Report, NIMCO, Baghdad, Iraq.

[13] Etabi, W. (1972).Petrography of Mawat igneous complex. Unpublished Report, NIMCO, Baghdad, Iraq.

[14] Jassim, S. Z., (1972).Geology of the Central sector of Mawat complex. Journal of Geological Society, Iraq, 6, 82-92.

[15] Al-Mehaidi, H. M., (1974). Geological investigation of Mawat-Chwarta area, NE Iraq. Unpublished report, G.S.M Library. Baghdad, Iraq. 54p.

[16] Al-Hassan, M. I. (1975). Comparative petrology study between Mawat and Penjwin igneous complexes, NE Iraq. Unpublished M.Sc Thesis, Baghdad University. 114p.

[17] Jassim, S. Z., and Al-Hassan, M. I. (1977). Petrography and origin of the Mawat and Penjwin igneous complexes: A comparison. Journal of Geological Society, Iraq. Special Issue, 169-210.

[18] Buda, G., and Al-Hashimi, W. S. (1977).Petrology of Mawat ophiolite complex, Northeastern Iraq. Journal of Geological Society, Iraq. Vol. X, 69-98.

[19] Buday, T., and Jassim, S. Z. (1987).The Regional Geology of Iraq. Vol.2, Tectonism, Magmatism, and Metamorphism. Geological Survey and Mining Investigation. Baghdad, 352p.

[20] Aswad, K. J., (1999). Arc-continent collision in Northeastern Iraq as evidenced by the Mawat and Penjwin ophiolite complexes. Raf. Journal of Science, 10 (No.1), 51-61.

[21] Aqrawi, A. M., (1990). Petrochemistry and petrogenesis of ultramafic and gabbroic rocks around Root mountain Mawat ophiolite complex, NE Iraq. Unpublished M.Sc Thesis, University of Mosul, 155p. (In Arabic).

[22] Jassim S. Z. and Goff J. C.,(2006). Geology of Iraq. Parague and Moravian Museum Brno. 341p.

[23] Farjo, S. F. Y., (2006). Geochemistry and petrogenesis of the volcanic rocks of Mawat ophiolite complex, NE Iraq. Unpublished M.Sc Thesis, Mosul University, 158p.

[24] Koyi, A.M.A., (2006). Petrochemistry, petrogenesis and Isotope dating of Walash volcanic rocks at Mawat-Chowarta area, NE Iraq, Unpublished MSc. Thesis, Universty of Mosul 230p. (In Arabic).

[25] Mirza, T. A., and Ismail, S. A., (2007). Origin of plagiogranite in the Mawat ophiolite complex, Kurdistan Region, NE Iraq. Journal of Kirkuk University-Scientific studies, 2 (No. 1), 1-25.

[26] Musa, E. O., (2007). Petrography, Geochemistry and Genesis of copper-iron mineralization and associated rocks in Waraz area, Sulaimani, NE Iraq. Unpublished M.Sc Thesis, University of Baghdad, 155p.

[27] Mirza, T.A.,(2008). Petrogensis of the Mawat Ophiolite Complex and the Associated Chromitite, Kurdistan Region, NE ,Iraq. Unpub. Ph.D. Thesis, University of Sulaimani.

[28] Mohammad, Y. O., (2008). Petrology of ultramafic and related rocks along Iraqi Zagros Thrust Zone. Unpublished D.Sc Thesis, Osaka Prefecture University, Japan, 154p.

[29] Aziz, N. R. H., (2008).Petrogenesis, Evolution, and Tectonics of the Serpentinites of the Zagros Suture Zone, Kurdistan Region, NE Iraq. Unpub. Ph.D. Thesis, University of Sulaimani, 250p.

[30] Aziz, N. R. H., Aswad, K. J. A., and Koyi, H. A., (2011): Contrasting settings of serpentinite bodies in the northwestern Zagros Suture Zone, Kurdistan Region, Iraq. Geological Magazine, 148, 819-837.

[31] Qaradaghi, J. M. A., (2012) "Petrogenesis and Geochronology of Granitoid Rocks in Mawat Ophiolite from Kurdistan Region, Northeastern Iraq"Unpublished M.Sc Thesis, University of Sulaimania, 219p.

[32] Palinkas, L. A. and Mirza, T.A.(2020). Ridge-axis and Off-axis volcanic massive sulphide, Cyprus-type, in the Mawat Ophiolites, Kurdistan-Iraq, Reconnaissance survey. Journal of Zankoy Sulaimani,v.22,ISS 1. P.103-122.

[33] Mirza, T.A. and Rashid, S.Gh.(2019). Evaluation of the Pila spi Formation carbonate rocks for dimension stone, Qara Dagh area, Kurdistan Region, NE Iraq. Iraqi Bulletin of Geology and Mining, Vol.15, No.2, p 107-120.

[34] Al-Mehaidi, H. M. (1975).Tertiary nappe in Mawat range NE Iraq. J. Geol. Soc. Iraq, Vol. VII, pp. 31–44.

[35] Alavi, M. (2004). Regional stratigraphy of the Zagros fold-thrust Belt of Iran and its proforeland evolution. American Journal of Science, 304, 1-20.

[36] Al-Hashimi, A.R. and Al-Mehaidi, H.M. (1975). Cu-Ni-Cr dispersion in Mawat ophiolite complex, NE Iraq. Jour. Geol. Soc. Iraq, Spec. Issue, pp. 37-44.

[37] ASTM C97-02, (2003). Standard test methods for absorption and bulk specific gravity of test methods of dimension stone. Annual Book of ASTM Standard American Society for Testing and Materials. Vol.4. No.7, 3pp.

[38] ASTM C170-90, (1999). Standard test method for compressive. Annual Book of ASTM Standard American Society for Testing and Materials. Vol. 4. No. 7, 3pp.

[39] ASTM C99-87, (2000). Standard test method for modulus of rapture of dimension stone. Annual Book of ASTM Standard American Society for Testing and Materials. Vol.4. No.7, 3pp.

[40] Harrison, D.J. and Bloodworth, A.J.(1994). Industrial Minerals Laboratory Manual Construction materials Technical Report WG/92/29, Mineralogy and Petrology Series British Geological Survey, 117pp.

[41] ASTM C1526-02, (2002). Standard Specification for Serpentine Dimension Stone. Annual Book of ASTM Standard American Society for Testing and Materials. Vol.4. No.7, 3pp.

[42] Pereira, D. et al., (2015). Characterization of serpentinites to define their appropriate use as dimension stone, Geological Society, London, Special Publications, Vol.271, p. 55 – 62.

[43] DOLLEY. T. P., (2010). Minerals Yearbook: Dimension Stone. U.S. Geological Survey 2012.

[44] Aurangzeb, (2009). Prediction of Effective Thermal Conductivity of Fluid Saturated Porous Media: in situ Thermo Physical Measurements, Ph.D., thesis, Quaidi-Azam University, Department of Physics, 139pp.

[45] Taylor, J. and Harold, A., (1991). A. “Annual Report of Dimensional Stones”, U.S Department of Interior, Bureau of Mines, 18pp.

[46] Marinos, P.; Hoek, E. and Marinos, V. (2005). Variability of the engineering properties of rock masses quantified by the geological strength index: The case of ophiolites with special emphasis on tunnelling. Bull. Eng. Geol. Environ, 65, 129–142.

[47] Currier, L. W., (1960). Geologic appraisal of dimension-stone deposits, Geological Survey Bulletin 1109, Report by United States Government Printing Office, Washington.