Original Paper
Textural records and geochemistry of the Kermanshah mantle peridotites (Iran): implications for the tectonic evolution of southern Neo-Tethys
Journal of Geosciences, volume 62 (2017), issue 3, 165 - 186
DOI: http://doi.org/10.3190/jgeosci.244
Agard P, Omrani J, Jolivet L, Whitechurch H, Vrielynck B, Spakman W, Monie P, Meyer B, Wortel R )2011( Zagros orogeny: a subduction-dominated process. Geol Mag 148: 692-725
Allahyari K, Saccani E, Rahimzadeh B, Zeda O (2014) Mineral chemistry and petrology of highly magnesian ultramafic cumulates from the Sarve-Abad (Sawlava) ophiolites (Kurdistan, NW Iran): new evidence for boninitic magmatism in intra-oceanic forearc setting in the Neo-Tethys between Arabia and Iran. J Asian Earth Sci 79: 312-328
Ao S, Xiao W, Khalatbari Jafari M, Talebian M, Chen L, Wan B, Ji W, Zhang Z (2016) U-Pb zircon ages, field geology and geochemistry of the Kermanshah Ophiolite (Iran): from continental rifting at 79 Ma to oceanic core complex at ca. 36 Ma in the southern Neo-Tethys. Gondwana Res 3: 305-318
Arai S (1994) Characterisation of spinel peridotites by olivine-spinel compositional relationships: review and interpretation. Chem Geol 113: 191-204
Ashwal L D, Cairncross B (1997) Mineralogy and origin of stichtite in chromite bearing serpentinites. Contrib Mineral Petrol 127: 75-86
Aswad KJA, Aziz NRH, Koyi HA (2011) Cr-spinel compositions in serpentinites and their implications for the petrotectonic history of the Zagros Suture Zone, Kurdistan Region, Iraq. Geol Mag 148: 802-818
Augé T (1987) Chromite deposits in the northern Oman Ophiolite: mineralogical constraints. Miner Depos 22: 1-10
Barnes SJ, Roeder PL (2001) The range of spinel compositions in terrestrial mafic and ultramafic rocks. J Petrol 42: 2279-2302
Bézard R, Hébert R, Wang C, Dostal J, Dai J, Zhong H (2011) Petrology and geochemistry of the Xiugugabu ophiolitic massif, western Yarlung Zangbo suture zone, Tibet. Lithos 125: 347-367
Braud J (1987) Geological map of Kermanshah. 1/250.000 scale. Tehran, Geological Survey of Iran
Cameron WE (1985) Petrology and origin of primitive lavas from the Troodos Ophiolite, Cyprus. Contrib Mineral Petrol 89: 239-255
Choi SH, Shervais JW, Mukasa SB (2008) Supra-subduction and abyssal mantle peridotites of the Coast Range Ophiolite. Contrib Mineral Petrol 156: 551-576
Coleman RG (1971) Plate tectonic emplacement of upper mantle peridotite along continental edges. J Geophys Res 76: 1212-1222
Deer WA, Howie R A, Zussman J (1992) An Introduction to the Rock Forming Minerals. Wiley New York, pp 1-696
Dick HJB, Bullen T (1984) Chromian spinel as a petrogenetic indicator in abyssal and alpine type peridotites and spatially associated lavas. Contrib Mineral Petrol 86: 54-76
Dilek Y, Furnes H (2011) Ophiolite genesis and global tectonics: geochemical and tectonic fingerprinting of ancient oceanic lithosphere. Geol Soc Am Bull 123: 387-411
Dilek Y, Thy P (2009) Island arc tholeiite to boninitic melt evolution of the Cretaceous Kizildag (Turkey) Ophiolite: model for multi-stage early arc-forearc magmatism in Tethyan subduction factories. Lithos 113: 68-87
Droop GTR (1987) A general equation for estimating Fe3+ concentrations in ferromagnesian silicates and oxides from microprobe analyses, using stoichiometric criteria. Mineral Mag 51: 431-435
Dungan MA (1979) A microprobe study of antigorite and some serpentine pseudomorphs. Canad Mineral 17: 711-784
Franz L, Wirth R (2000) Spinel inclusions in olivine of peridotite xenoliths from TUBAF seamount (Bismarck Archipelago/Papua New Guinea): evidence for the thermal and tectonic evolution of the oceanic lithosphere. Contrib Mineral Petrol 140: 283-295
Harnois L, Trottier J, Morency M (1990) Rare earth element geochemistry of Thetford Mines Ophiolite Complex, Northern Appalachians, Canada. Contrib Mineral Petrol, 105: 433-445
Kamenetsky VS, Crawford AJ, Meffre S (2001) Factors controlling chemistry of magmatic spinel: an empirical study of associated olivine, Cr-spinel and melt inclusions from primitive rocks. J Petrol 42: 655-671
Li XP, Chen HK, Wang ZL, Wang LJ, Yang JS, Robinson P (2015) Spinel peridotite, olivine websterite and the textural evolution of the Purang Ophiolite Complex, western Tibet. J Asian Earth Sci 110: 55-71
Maurel C, Maurel P (1982) Etude expérimental de la distribution de l’aluminium entre bain silicate basique et spinelle chromifère. Implications pétrogenetiques: teneur en chrome des spinelles. Bull Mineral 105:197-202
Morimoto N (1989) Nomenclature of pyroxenes. Canad Mineral 27: 143-156
Mouthereau F, Lacombe O, Vergés J (2012) Building the Zagros collisional orogen: timing, strain distribution and the dynamics of Arabia/Eurasia plate convergence. Tectonophysics 532-535: 27-60
Neumann ER (1991) Ultramafic and mafic xenoliths from Hierro, Canary Islands: evidence for melt infiltration in the upper mantle. Contrib Mineral Petrol 106: 236-252
O’Driscoll B, Emeleus CH, Donaldson CH, Daly JS (2010) Cr-spinel seam petrogenesis in the Rum layered suite, NW Scotland: cumulate assimilation and in situ crystallization in a deforming crystal mush. J Petrol 51: 1171-1201
Page P, Barnes SJ (2009) Using trace elements in chromites to constrain the origin of podiform chromitites in the Thetford Mines Ophiolite, Québec, Canada. Econ Geol 104: 997-1018
Parkinson IJ, Pearce JA (1998) Peridotites from the Izu-Bonin-Mariana forearc (ODP Leg 125): evidence for mantle melting and melt-mantle interaction in a suprasubduction zone setting. J Petrol 39: 1577-1618
Pearce JA, Norry MJ (1979) Petrogenetic implications of Ti, Zr, Y, and Nb variations in volcanic rocks. Contrib Mineral Petrol 69: 33-47
Pearce JA, Barker PF, Edwards S, Parkinson IJ, Leat PT (2000) Geochemistry and tectonic significance of peridotites from the South Sandwich arc-basin system, South Atlantic. Contrib Mineral Petrol 139: 36-53
Presnall DC, Hoover JD (1987) High pressure phase equilibrium constraints on the origin of mid-ocean ridge basalts. In: Mysen BO (ed) Magmatic Processes: Physicochemical Principles. The Geochemical Society Special Papers 1: 75-89
Rafia R, Shahidi A (1999) Geological map of Mianrahan, 1/100.000 scale. Geological Survey of Iran, Tehran
Rajabzadeh MA, Nazari Dehkordi T, Caran S (2013) Mineralogy, geochemistry and geotectonic significance of mantle peridotites with high-Cr chromitites in the Neyriz Ophiolite from the outer Zagros ophiolite belts, Iran. J Asian Earth Sci 78: 1-15
Reilinger R, McClusky S (2011) Nubia-Arabia-Eurasia plate motions and the dynamics of Mediterranean and Middle East tectonics. Geophys J Int 186: 971-979
Rollinson H (2008) The geochemistry of mantle chromitites from the northern part of the Oman Ophiolite: inferred parental melt compositions. Contrib Mineral Petrol 156: 273-288
Saccani E, Beccaluva L, Photiades A, Zeda O (2011) Petrogenesis and tectonomagmatic significance of basalts and mantle peridotites from the Albanian-Greek ophiolites and sub-ophiolitic mélanges. New constraints for the Triassic-Jurassic evolution of the Neo-Tethys in the Dinaride sector. Lithos 124: 227-242
Saccani E, Allahyari K, Beccaluva L, Bianchini G (2013) Geochemistry and petrology of the Kermanshah ophiolites (Iran): implication for the interaction between passive rifting, oceanic accretion, and OIB-type components in the Southern Neo-Tethys Ocean. Gondwana Res 24: 392-411
Saumur BM, Hattori K (2013) Zoned Cr-spinel and ferritchromite alteration in forearc mantle serpentinites of the Rio San Juan Complex, Dominican Republic. Mineral Mag 77: 117-136
Seyler M, Lorand JP, Dick HJB, Drouin M (2007) Pervasive melt percolation reactions in ultra-depleted refractory harzburgites at the Mid-Atlantic Ridge. Contrib Mineral Petrol 153: 303-319
Shahidi M, Nazari H (1997) Geological map of Harsin, 1/100.000 scale. Geological Survey of Iran, Tehran
Stöcklin J (1968) Structural history and tectonics of Iran; a review. AAPG Bull 52 (7): 1229-1258
Sun SS, McDonough WF (1989) Chemical and isotopic systematics of oceanic basalts: implications for mantle composition and processes. In: Saunders AD, Norry MJ (eds) Magmatism in the Ocean Basins. Geological Society of London Special Publications 42: 313-345
Tamura A, Arai S (2006) Harzburgite-dunite-orthopyroxenite suite as a record of supra-subduction zone setting for the Oman Ophiolite mantle. Lithos 90: 43-56
Vergés J, Saura E, Casciello E, Fernàndez M, Villaseñor A, Jiménez-Munt I, García-Castellanos D (2011) Crustal-scale cross-section across the NW Zagros Belt: implications for the Arabian margin reconstruction, In: Lacombe O, Grasemann B, Simpson G (eds) Geodynamic Evolution of the Zagros. Geol Mag 148: 739-761
Whitechurch H, Omrani J, Agard P, Humbert F, Montigny R, Jolivet L (2013) Evidence for Paleocene-Eocene evolution of the foot of the Eurasian margin (Kermanshah Ophiolite, SW Iran) from back-arc to arc: implications for regional geodynamics and obduction. Lithos 182-183: 11-32
Workman RK, Hart SR (2005) Major and trace element composition of the depleted MORB mantle (DMM). Earth Planet Sci Lett 231: 53-72
Wrobel-Daveau JC, Ringenbach JC, Tavakoli S, Ruiz GMH, Masse P, De Lamotte DF (2010) Evidence for mantle exhumation along the Arabian margin in the Zagros (Kermanshah area, Iran). Arabian J Geosci 3: 499-513
Xia X, Song S, Niu Y (2012) Tholeiite-boninite terrane in the North Qilian suture zone: implications for subduction initiation and back-arc basin development. Chem Geol 328: 259-277
Zarei Sahamieh R, Moradpour A (2015) Geochemistry and petrology of Harsin-Sahneh Ophiolitic Complex (NE of Kermanshah - west of Iran) an evidence of southern Neo-Tethys Ocean tectonic. Arabian J Geosci 8: 8347-836
IF (WoS, 2023): 1.1
5 YEAR IF (WoS, 2023): 1.5
Policy: Open Access
ISSN: 1802-6222
E-ISSN: 1803-1943