Record number :
2364254
Title of article :
Evidence of Precambrian sedimentation/magmatism and Cambrian metamorphism in the Bitlis Massif, SE Turkey utilising whole-rock geochemistry and U–Pb LA-ICP-MS zircon dating
Author/Authors :
Ustaِmer، نويسنده , , P. Ayda and Ustaِmer، نويسنده , , Timur and Gerdes، نويسنده , , Axel and Robertson، نويسنده , , Alastair H.F. and Collins، نويسنده , , Alan S.، نويسنده ,
Issue Information :
روزنامه با شماره پیاپی سال 2012
Pages :
18
From page :
1001
To page :
1018
Abstract :
The Bitlis Massif is a regional-scale, south-vergent allochthon that was finally emplaced by collision of the Eurasian and Afro-Arabian plates during Miocene time. The Bitlis Massif includes a large outcrop of Precambrian continental crust, the closest counterpart to which is the Arabian–Nubian Shield ~ 1000 km to the south. The Massif is sub-divided into two rock associations: a pre-Middle Devonian high-grade basement and a Middle Devonian-Triassic low-grade cover. The pre-Devonian basement comprises meta-granitic plutons emplaced into high-grade metamorphic rocks, including schist, paragneiss, amphibolite and eclogite. New laser-ablation zircon ages obtained for zircons separated from a meta-granite body and its host paragneiss provide constraints on magmatism, sedimentation and metamorphism. Whole-rock geochemical data indicate that the pluton crystallised from peraluminous I-type melts from an arc-type subduction influenced source. Sm–Nd isotope systematics suggest crustal contamination. Zircon dating yielded a 206Pb/238U age of 572 ± 4.8 Ma, interpreted as the time of crystallisation. Igneous zircons exhibit metamict metamorphic domains dated at 529 Ma (Early Cambrian), interpreted as the time of latest Pan-African metamorphism. Nine detrital zircon grains from host paragneiss yielded Neoproterozoic ages (992–627 Ma). Combined with the crystallisation age data, this suggests that the sedimentary protolith of the paragneiss was deposited from ~ 627 to ~ 572 Ma (Ediacaran). The late Neoproterozoic ages suggest the Bitlis Massif is a peri-Gondwanan terrane with a likely origin in northeast Africa where similar early Neoproterozoic (0.9–1.0 Ga) ages have been reported.
Keywords :
Arc magmatism , Neoproterozoic , U–Pb zircon dating , SE Turkey , Bitlis Massif
Journal title :
Gondwana Research
Serial Year :
2012
Link To Document :
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