Kerman Cenozoic magmatic arc has gone through a different tectonic and magmatic evolution from that of central and northwestern parts of the Urumieh-Dokhtar volcanic belt and has particularly been influenced by the subduction of Neo-Tethys oceanic crust to the east of Nain-Baft transform fault beneath the rotating central Iran micro-continent and its surrounding circum ocean. The arc magmatic activities started from early Eocene with extensive volcanism of Bahr Asemen and Razak complexes which are characterized by silica-satureated magmas with ranges mafic to felsic compositions without feldspathoides, calc-alkaline and locally tholeiitic-like affinity, low enrichment in LILE, weak to moderately REE fractionation (La/Yb<20), non-radiogenic Sr isotopic ratios (0.7041-0.7049), and high ?Nd (6-2.3).
shafiei,B . (2010). Two contrasting volcanic episodes during the Paleogene magmatism in Kerman Cenozoic magmatic arc: geochemical signatures and petrogenetic processes. (e21701). Journal of Science,University of Tehran(not publish), 36(1), e21701
MLA
shafiei,B . "Two contrasting volcanic episodes during the Paleogene magmatism in Kerman Cenozoic magmatic arc: geochemical signatures and petrogenetic processes" .e21701 , Journal of Science,University of Tehran(not publish), 36, 1, 2010, e21701.
HARVARD
shafiei B. (2010). 'Two contrasting volcanic episodes during the Paleogene magmatism in Kerman Cenozoic magmatic arc: geochemical signatures and petrogenetic processes', Journal of Science,University of Tehran(not publish), 36(1), e21701.
CHICAGO
B shafiei, "Two contrasting volcanic episodes during the Paleogene magmatism in Kerman Cenozoic magmatic arc: geochemical signatures and petrogenetic processes," Journal of Science,University of Tehran(not publish), 36 1 (2010): e21701,
VANCOUVER
shafiei B. Two contrasting volcanic episodes during the Paleogene magmatism in Kerman Cenozoic magmatic arc: geochemical signatures and petrogenetic processes. Journal of Science,University of Tehran(not publish). 2010;36(1):e21701 (In Persian).
