The relationship between serpentinization and geotechnical properties of ophiolites (Case study: Paleotethys ophiolites of the Southwest of Mashhad)

Document Type : Research Article

Authors

• Salameh Afshar ¹
• Mohammad Ghafoori ¹
• Naser Hafezi Moghaddas ¹
• Gholam Reza Lashkaripour ²

¹ Ferdowsi University of Mashhad

² University of Mashhad

10.22067/econg.v11i4.74244

Abstract

Introduction
In the southern margin of the Mashhad plain in Northeastern Iran, there are strips with tens of kilometers length consisting of metamorphic rocks and ophiolite complexes with the NE-SW trend. Ophiolites are fragments of ancient Oceanic crust (Ghaseminejad and Torabi, 2015; Khanchuk et al., 2016; Shirdashtzadeh et al, 2017) most of which consists of ultramafic rocks. Ophiolites are formed during tectonic displacement in the southern part of the Mashhad plain (Alavi, 1991; Karimpour et al., 2010; Sheikholeslami and Kouhpeyma, 2012; Zanchetta et al., 2013; Shafaii Moghadam and Stern, 2014). These undergoing metamorphosed regions ultimately lead to the formation of serpentines complex due to factors of pressure and temperature. Subsequently, tectonic variations create different levels of serpentinization in the region. Different degrees of serpentines have different geotechnical properties that are discussed in this study.
 
Materials and methods
To conduct the lithological studies, 313 samples were collected from surface and trenches in the studied area. Following the preparation of the microscopic cross-section of all specimens, the mineralogical characteristics, texture changes, color changes, degradation and microcrack development were studied. Then, the samples were classified based on the general classification of ultramafic rocks (Streckeisen, 1974). According to this classification, the ultramafics extracted from the studied area were classified in the metaperidotite and metapyroxenite groups. After separating various metaperidotites and metapyroxenites the percentage of serpentinization in all specimens were determined and 60 samples with different serpentinite percentages were selected. Also, the stone blocks were provided for preparing the core samples. Physical tests (such as dry and saturated unit weights, porosity, and water absorption percentage), and mechanical tests (such as uniaxial compressive strength, point load strength, and Brazilian tensile strength) were performed based on the Brown (1981) method in the laboratory of the Ferdowsi University of Mashhad.
 
Results
The results show that there is a good relationship between the percentage of serpentinization of samples and uniaxial compressive strength (the most important geotechnical parameter in rocks). The ultramafic rocks are divided into three groups based on uniaxial strength and 25 to 40% of serpentine are very strong, 40 to 60% of serpentine are strong and 60 to 75% serpentine are of medium strength. Also, the ultramafics with 75% to 95% of serpentine, are named as serpentinite rocks with weak uniaxial compressive strength.
 
Discussion
Although most of the ultramafic rocks have good strength as the foundation for building, the construction of a structure on these rocks has numerous problems due to the formation of minerals such as serpentine and talc with one-directional cleavage. With increasing the degree of serpentinization, some phenomena such as slope instability, sliding, excavation collapse will occur. The results of the present research indicated the priority of serpentinization degree of ultramafic rocks compared to their strength. As it is seen, although in a high degree of serpentinization, the metapyroxenites have higher strength and lower water absorption compared to metaperidotites. Therefore, the mentioned issues demonstrated the importance of the degree of serpentinization compared to strength in ultramafic rocks.  
 
Acknowledgements
The authors would like to thank Professor Mohammad Hassan Karimpour for his helpful and effective guidance on the petrography of ultramafics rocks in this paper.
 
References
Alavi, M., 1991. Sedimentary and structural characteristics of the Paleo-Tethys remnants in northeastern Iran. Geological Society of America Bulletin, 103(8): 983–992.
Brown, E.T. 1981. Rock characterization, Testing and monitoring ISRM suggested methods. Pergamon press, Oxford, 211 pp.
Ghaseminejad, F. and Torabi, Gh., 2015. Petrography and mineral chemistry of Twehrlites in contact zone of gabbro intrusions and mantle peridotites of the Naein ophiolite. Journal of Economic Geology, 6(2): 291–304. (in Persian with English abstract)
Karimpour, M.H., Stern, C.R. and Farmer, G.L., 2010. Zircon U–Pb geochronology, Sr–Nd isotope analyses, and petrogenetic study of the Dehnow diorite and Kuhsangi granodiorite (Paleo-Tethys), NE Iran. Journal of Asian Earth Sciences, 37(4): 384–393.
Khanchuk, A.I. and Vysotsky, S.V., 2016. Different-depth gabbro–ultrabasite associations in the Sikhote-Alin ophiolites (Russian Far East).  Russian Geology and Geophysics, 57(1): 141–154.
Shafaii Moghadam, H. and Stern, R.J., 2014. Ophiolites of Iran: Keys to understanding the tectonic evolution of SW Asia: (I) Paleozoic ophiolites. Journal of Asian Earth Sciences, 91(1): 19–38.
Sheikholeslami, M.R. and Kouhpeyma, M., 2012. Structural analysis and tectonic evolution of the eastern Binalud Mountains, NE Iran. Journal of Geodynamics, 61(1): 23–46.
Shirdashtzadeh, N., Torabi, GH. and Samadi, R., 2017. Petrography and mineral chemistry of metamorphosed mantle peridotites of Nain Ophiolite (Central Iran). Journal of Economic Geology, 9(1): 57–72. (in persian with English abstract)
Streckeisen, A., 1974. Classification and nomenclature of plutonic rocks recommendations of the IUGS subcommission on the systematics of igneous rocks. Geologische Rundschau, 63(2): 773–786.

Keywords

• percentage of serpentinization
• uniaxial compressive strength
• geotechnical properties
• Paleotethys ophiolites
• North East of Iran

20.1001.1.20087306.1398.11.4.5.1

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References

Abdelaziz, R., Abdel-Rahman, Y. and Wilhelm, S., 2018. Landsat-8 data for chromite prospecting in the Logar Massif, Afghanistan. Heliyon, 4(2): 1–18

Alavi, M., 1991. Sedimentary and structural characteristics of the Paleo-Tethys remnants in northeastern Iran. Geological Society of America Bulletin, 103(8): 983–992.

Bieniawski, Z.T., 1974. Estimating the strength of rock materials. Journal of the South African Institute of Mining and Metallurgy, 74(8): 312–320.

Bieniawski, Z.T. and Bernede, M.J., 1979. Suggested methods for determining the uniaxial compressive strength and deformability of rock materials. International Journal of Rock Mechanics and Mining Sciences and Geomechanics abstracts, 16(2): 138–140.

Boulin, J., 1988. Hercynian and Eocimmerian events in Afghanistan and adjoining regions. Tectonophysics, 148(3): 253–278.

Brown, E.T. 1981. Rock characterization, Testing and monitoring ISRM suggested methods. Pergamon press, Oxford, 211 pp.

Cargill, J.S. and Shakoor, A. 1990. Evaluation of empirical methods for measuring the uniaxial compressive strength of rock. International Journal of Rock Mechanics and Mining Sciences, 27(6): 495–503.

Gamble, J.C., 1971. Durability-plasticity classification of shale and other argillaceous rocks. Ph.D. Theses, University of Illinois, Urbana, Illinois, 161 pp.

Ghaseminejad, F. and Torabi, Gh., 2015. Petrography and mineral chemistry of Twehrlites in contact zone of gabbro intrusions and mantle peridotites of the Naein ophiolite. Journal of Economic Geology, 6(2): 291–304. (in Persian with English abstract)

IAEG, 1979. Classification of rocks and soils for engineering geological mapping. Part 1: Rock and Soil Materials. Bulletin of the International Association of Engineering Geology, 19(1): 355–371.

Karimpour, M.H., Stern, C.R. and Farmer, G.L., 2010. Zircon U–Pb geochronology, Sr–Nd isotope analyses, and petrogenetic study of the Dehnow diorite and Kuhsangi granodiorite (Paleo-Tethys), NE Iran. Journal of Asian Earth Sciences, 37(4): 384–393.

Khanchuk, A.I. and Vysotsky, S.V., 2016. Different-depth gabbro–ultrabasite associations in the Sikhote-Alin ophiolites (Russian Far East). Russian Geology and Geophysics, 57(1): 141–154.

Kurtulus, C., Bozkurt, A. and Endes, H., 2011. Physical and mechanical properties of serpentinized ultrabasic rocks in NW Turkey. Pure and applied geophysics, 169(7): 1205–1215.

Peltier, L.C., 1950. The Geographic Cycle in Periglacial Regions as it is Related to Climatic Geomorphology. Annals of the Association of American Geographers, 40(3): 214–236.

Rigopoulos, I., Tsikouras, B., Pomonis, P. and Hatzipanagiotou, K., 2015. Assessment of the engineering behavior of ultramafic and mafic rocks using chemical indices. Engineering Geology, 196(1): 222–237.

Shafaii Moghadam, H., Hua Li, X., Xiao Ling, X., Stern, R., Zaki Khedr, M., Chiaradia, M., Ghorbani, Gh., Arai, Sh. and Tamura, A., 2014. Devonian to Permian evolution of the Paleo-Tethys Ocean: New evidence from U–Pb zircon dating and Sr–Nd–Pb isotopes of the Darrehanjir – Mashhad “ophiolites”, NE Iran. Gondwana Research, 28(1): 781–799.

Shafaii Moghadam, H. and Stern, R.J., 2014. Ophiolites of Iran: Keys to understanding the tectonic evolution of SW Asia: (I) Paleozoic ophiolites. Journal of Asian Earth Sciences, 91(1): 19–38.

Sheikholeslami, M.R. and Kouhpeyma, M., 2012. Structural analysis and tectonic evolution of the eastern Binalud Mountains, NE Iran. Journal of Geodynamics, 61(1): 23–46.

Shirdashtzadeh, N., Torabi, GH. and Samadi, R., 2017. Petrography and mineral chemistry of metamorphosed mantle peridotites of Nain Ophiolite (Central Iran). Journal of Economic Geology, 9(1): 57–72. (in persian with English abstract)

Stampfli, G.M., 1996. The intra-alpine terrain: a Paleo-Tethyan remnant in the alpine variscides. Eclogae Geologicae Helvetiae, 89(1): 13–42.

Streckeisen, A., 1974. Classification and nomenclature of plutonic rocks recommendations of the IUGS subcommission on the systematics of igneous rocks. Geologische Rundschau, 63(2): 773–786.

Styles, M.T., Sanna, A., Lacinska, A.M., Naden, J. and Maroto-Valer, M., 2014. The variation in composition of ultramafi c rocks and the effect on their suitability for carbon dioxide sequestration by mineralization following acid leaching. Modeling and Analysis, 4(1): 1–12.

Whitney, D.L. and Evans B.W., 2010. Abbreviations for names of rock-forming minerals. American Mineralogist, 95(1): 185–187.

Zanchetta, S., Berra, F., Zanchi, A., Bergomi, M., Caridroit, M., Nicora, A. and Heidarzadeh, G., 2013. The record of the Late Palaeozoic active margin of the Palaeotethys in NE Iran: constraints on the Cimmerian orogeny. Gondwana Research, 24(3): 1237–1266.

Zanchi, A., Zanchetta, S., Berra, F., Mattei, M., Garzanti, E., Molyneux, S., Nawab, A. and Sabouri, J., 2009. The Eo-Cimmerian (Late? Triassic) orogeny in north Iran. In: M.F. Brunet, M. Wilmsen and J.W. Granath (Editors), South Caspian to Central Iran Basins. Geological Society, London Special Publication, pp. 31–55.