Bonatti E;Hamlyn P R,Peridotites from the Island of Zabargad(St.Jone).Red Sea:Petrology and geochemistry,J Geophys Rec,1986(81).
[17]
Dick H J B;Bullen T,Chromium spinel as a petrogenetic indicator in abyssal and Alpine-type peridotites and spatially associated lavas,Contributions to Mineralogy & Petrology,1984.
[18]
Dubois-C(o)té V;Hébert R;Dupuis C;Wang C S Li Y L and Dostal J,Petrological and geochemical evidence for the origin of the Yarlung Zangbo ophiolites,southern Tibet,Chemical Geology,2005.
[19]
El-Rus M A A;Neumann E R;Peters V,Serpentinization and dehydration in the upper mantle beneath Fuerteventura(eastern Canary Islands):Evidence from mantle xenoliths,Lithos,2006.
[20]
Falloon T J;Berry R F;Robinson P;Stolz A J,Whole-rock geochemistry of the Hill Manu peridotite,East Timor:implications for the origin of Timor ophiolites,Australian Journal of Earth Sciences,2006.
[21]
Frey F A;Stockman H W,The Roda high temperature peridotite:geochemistry and petrogenesis,Geochimica et Cosmochimica Acta,1985.
[22]
Frey F A,Rare earth element abundances in upper mantle rocks,1984.
[23]
Gao J;Klemd R;Zhang L;Wang Z and Xiao X,P-T path of high pressure low temperature rocks and tectonic implications in the western Tianshan Mountains(NW China),Journal of Metamorphic Geology,1999.
[24]
Godard M;Jousselin D;Bodinier J-L,Relationships between geochemistry and structure beneath a palaeo-spreading centre:a study of the mantle section in the Oman ophiolite,Earth and Planetary Science Letters,2000.
[25]
Grégoire M;McInnes BIA;O\' Reilly S Y,Hydrous metasomatism of oceanic sub-arc mantle,Lihir,Papua New Guinea,Part 2:Trace element characteristics of slab-derived fluids,Lithos,2001(59).
[26]
Hart S R;Zindler A,In search of a bulk Earth composition,Chemical Geology,1986.
[27]
Ivonov, DA ;Chazot, G ;Chauvel, C ;Merlet, C ;Bodinier, JL,Trace element distribution in peridotite xenoliths from Tok, SE Siberian craton: A record of pervasive, multi-stage metasomatism in shallow refractory mantle,Geochimica et Cosmochimica Acta?,2006, 70(5).
[28]
Jagoutz E;Palme H;Baddenhausen H;Blum K,Cendales M,Dreibus G,Spettel B,Lorentz V an,The abundance of major,minor and trace elements in the Earth\' s mantle as derived from primitive ultramafic nodules,1979.
[29]
Jan M Q;Windley B F,Chromian spinel-silicate chemistry in ultramafic rocks of the Jijal complex,Northwestern Pakistan,Journal of Petrology,1990.
[30]
Kelemen P B;Rilling J L;Parmentier E M;Mehl L and Hacker B R,Thermal structure due to solid-state flow in the mantle wedge beneath arcs,AGU,Washington,DC,2003.
[31]
Kessel R;Sshmidt MW;Ulmer P;Pettke T,Trace element signature of subduction-zone fluids,melts and super-critical liquids at 120~ 180 km depth,Nature,2005.
[32]
Khedr M Z;Arai S,Hydrous peridotites with Ti-rich chromian spinel as a low-temperature forearc mantle facies:evidence from the Happo-O\'ne metaperidotites(Japan),Contributions to Mineralogy & Petrology,2010.
[33]
Kretz R,Symbols for rock-forming minerals,American Mineralogist,1983.
[34]
Lenoir X;Ganido C J;Bodiniere J-L;Dautria J-L and Gervilla F,The recrystallization front of the Ronda Peridotite:evidence for melting and thermal erosion of sub-continental lithospheric mantle beneath the Alboran Basin,Journal of Petrology,2001.
[35]
McDonough W F;Sun S S,The composition of the Earth,Chemical Geology,1995.
[36]
Melchera F;Meisel T;Puhl J;Kolle F,Petrogenesis and geotectonic setting of ulramafic rocks in the Eastern Alps:constraints from geochemistry,Lithos,2002.
[37]
Mctcalf R V;Shervais J W,Suprasubduction-zone ophiolites:Is there really an ophiolite conundrum,Geological Society of America Special Paper,2008.
[38]
Niu Y,Bulk-rock major and trace element compositions of abyssal peridotites:implications for mantle melting,melt extraction and post-melting processes beneath mid-ocean ridges,Journal of Petrology,2004.
[39]
Ohara Y;Ishii T,Peridotites from the southern Mariana forearc:heterogeneous fluid supply in mantle wedge,Island Arc,1998(3).
[40]
Parkinson I J;Pearce J A,Peridotites from the Izu-Bonin-Mariana forearc(ODP Leg 125):evidence for mantle melting and melt-mantle interaction in a supra-subduction zone setting,Journal of Petrology,1998.
[41]
Paulick H;Bach W;Godard M;Hoog De J C M Suhr G Harvey J,Geochemistry of abssal peridotites(Mid-Atlantic Ridge,15°20'N,ODP Leg 209):Implications for fluid/rock interaction in slow spreading environments,Chemical Geology,2006.
[42]
Takazawa E;Frey A;Shimizu N;Obatan N,Whole rock compositional variations in an upper mantle peridotite(Horoman,Hokkaido,Japan):are they consistent with a partial melting process,Geochimica et Cosmochimica Acta,2000.
[43]
Tatsumi Y;Hamihon D L;Nesbitt R W,Chemical characteristics of fluid phase released from a subducted lithosphere and origin of arc magmas:Evidence from high-pressure experiments and natural rocks,Journal of Volcanology and Geothermal Research,1986.
[44]
Thompson R N;Morrison M A;Hendry G L;Parry S J,An assessment of the relative roles of crust and mantle in magma genesis:an elemental approach,Philosophical Transactions of the Royal Society of London Series A:Mathematical and Physical Sciences,1984.
[45]
Wang B;Chen Y;Zhang S;Shu L S Faure M Cluzel D Charvet J and Laurent C S,Primary Carboniferous and Permian paleomagnetic results from Yili Block(NW China)and their implication on the geodynamic evolution of Chinese Tianshan Belt,Earth and Planetary Science Letters,2007.
[46]
Weyer S;Munker C;Mezger K,Nb/Ta,Zr/Hf and REE in the depleted mantle:implications for the differentiation history of the crust mantle system,Earth and Planetary Science Letters,2003.
[47]
Yoshikawa M;Nakamura E,Geochmical evolution of Horoman peridotite complex:implications for melt extraction,metasomatism and compositional layering in the mantle,Jouranal of Geophysical Research,2000.
[48]
Zhang L;Ai Y;Li X P;Rubatto D Song B Williams S Song S Ellis D Liou J G,Triassic collision of western Tianshan orogenic belt,China:evidences from SHRIMP U-Pb dating of zircon from HP/UHP eclogitic rocks,Lithos,2007.
Arai S,Chemistry of chromian spinel in volcanic rocks as a potential guide to magma chemistry,Mineralogical Magazine,1992.
[60]
Arai S;Okamura H;Kadoshima K;Tanaka C Suzuki K and Ishimaru S,Chemical characteristics of chromian spinel in plutonic rocks:Implications for deep magma processes and discrimination of tectonic setting,Island Arc,2011.
[61]
Arai S;Kadoshima K;Morishita T,Wide-spread arc-related melting in the mantle section of the northern Oman ophiolite as inferred from detrital chromian spinels,Journal of the Geological Society(London),2006.
[62]
Bell D R;Gregoire M;Grove T L;Chatterjee N Carlson R W and Buseck P R,Silica and volatile-element metasomatism of Arehean mantle:a xenolith scale example from the Kaapvaal Craton,Contributions to Mineralogy & Petrology,2005(3).
[63]
Loubet M;Shimnizu N;Allegre C J,Rare earth elements in Alpine peridotites,Contributions to Mineralogy & Petrology,1975.
[64]
Pearce J A;Lippard S J;Roberts S,Characteristics and tectonic significance of supra-subduction zone ophiolites,London:Blaekwell Scientific Publications,1984.
[65]
Pearce J A;Parkinson I J,Trace element models for mantle melting:Application to volcanic arc petro-genesis,1993.
[66]
Pearce J A;Barker P F;Edwards S J;Parkinson I J and Leat P T,Geochemistry and tectonic significance of peridotites from the South Sandwich arc-basin system,South Atlantic,Contributions to Mineralogy & Petrology,2000.
[67]
Polat A;Herzberg C;Münker C;Rodgers R,Kusky T,Li J H,Fryer B and Delaney J,Geochemical and petrological evidence for a suprasubduction zone origin of Neoarchean(ca.2.5 Ga)peridotites,central orogenic belt,North China craton,Bulletin of the Geological Society of America,2006.
[68]
Proenza J;Gervilla F;Melgarejo J C;Bodinier J L,Al-rich and Cr-rich chromitites from the Maya―Baracoa ophiolitic belt(eastern Cuba):consequence of interaction between volatile rich melts and peridotites in suprasubduction mantle,Economic Geology,1999.
[69]
Sun S S;McDonough W F,Chemical and isotopic systematics of oceanic basalts:implications for mantle composition and processes,London:Geological Society,Special Publications,1989.