Determine the temperature and pressure conditions during the formation of Zahedan igneous intrusive mass,South-East of Iran
Journal Title: International Research Journal of Applied and Basic Sciences - Year 2014, Vol 8, Issue 1
Abstract
Zahedan granitoid mass (upper Eocene - Oligocene), the largest intrusive igneous mass in granitoid belt Zahedan - Saravan the Southwest - West and south to southeast of Zahedan, the exposed populations such as narrow, low, high and larger populations scattered in neighboring Pakistan and Afghanistan that the flyschold in southeastern Iran and is the contact metamorphism of the host rocks.In this research field , petrographic ground conditions and specific mass of plutonic igneous tectonic zone in Zahedan, depending on the specificities of petrographic (microscopic sections) and petrology (chemical analysis) and large rock outcrops high in the batholith Loochan, three front is studied .Petrological diagrams of binary and According to the Pertite and Large amounts of alkaline feldspars orthoclase With Pertite the number of plaques obtained from Loochan batholith and Front of curved mica granite melting curve stability diagram also cited, Batholith intrusive igneous mass of water vapor pressure environment Loochanin Zahedan region About 2Kbar and temperatures of about 700 °C, respectively.According toatransformationoftheoldflyschrocksin the area and Diagramsofalkali-silicaand ThediagramsTAS, Zahedan Mass ofintrusiveigneous, Especiallyin the areaof thebatholithLoochanLandofbirthand thecollisionofcontinentalplates, The origin ofZahedan granitoids,Partial melting ofcontinentalcrustina shallowarea.
Authors and Affiliations
Behrooz Sahebzadeh| FarhangianUniversity, Shahhid Motahhari Campus, Zahedan, Iran, email: Sahebzadeh.geologist@gmail.com
Keywords
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- EP ID EP6527
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