Purang ultramafic complex and their geological origin, SouthwestTibet

来源 :International Workshop on: Ophiolites, Mantle Processes and | 被引量 : 0次 | 上传用户:water11
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Purang ultramafic complex of western Tibet consists of spinel peridotites,olivine websterite,rodingite and later intruded gabbro-diabase veins.The spinel peridotites consist of lherzolite,harzburgite and dunite.All Purang peridotites are rich in MgO,but depleted in Al2O3,CaO and TiO2 relative to primary mantle values,indicating depletion by several episodes of partial melting.The olivine websterite probably formed by melt/rock reaction between an evolved basaltic melt and harzburgite or dunite.The evolution of the Purang ultramafic rocks from lherzolite through harzburgite,and dunite to olivine websterite indicates multistage melting and melt/rock reaction processes.Decompression-related textures such as exsolution lamellae of clinopyroxene and spinel in orthopyroxene,and melting,melt/rock textures such as embayed,flame-like grains of spinel and partial chain spinel textures are widespread in the ultramafic rocks.Impregnation textures are reflected by the presence of late intergranular and interstitial clinopyroxene in the harzburgite,dunite and olivine websterite.Bulk rock chemistry and minerlaogical chemistries of the spinel,clinopyroxene and orthopyroxene all recorded both abyssal/back arc basin and supra-subduction zone affinity.
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