U–Pb zircon geochronology, petrochemical and Sr–Nd isotopic characteristic of Late Neoproterozoic granitoid of the Bornaward Complex (Bardaskan-NE Iran). (1st November 2015)

• Record Type: Journal Article
• Authors: Bagherzadeh, R. Monazzami; Karimpour, M.H.; Farmer, G. Lang; Stern, C.R.; Santos, J.F.; Rahimi, B.; Heidarian Shahri, M.R.
• Is Part Of: Journal of Asian earth sciences. Volume 111(2015)
• Page Start: 54
• Page End: 71
• Publication Date: 2015-11-01
• Subjects: Taknar -- Bornaward -- U–Pb dating -- Zircon -- Sr–Nd -- Late Neoproterozoic; Earth sciences -- Asia -- Periodicals; Sciences de la terre -- Asie -- Périodiques; Earth sciences; Asia; Periodicals; 555.05
• DOI: 10.1016/j.jseaes.2015.05.019
• Languages: English
• ISSNs: 1367-9120

Abstract

Abstract: The Bornaward Granitoid Complex (BGC) in the Taknar Zone is located in the northeast of Central Iranian Block. The BGC consists of granite, alkaligranite, syenogranite, leucogranite, granophyre, monzogranite, granodiorite, tonalite and diorite that have intruded into the center of Taknar Zone. These intrusive rocks affected by low grade metamorphism. Because of there are no reliable isotope dating data, for the Bornaward Granitoid Complex rocks have been proposed discordant ages (Jurassic, Cretaceous or even younger ages) by many studies. In the present study, new isotopic information based on zircon U–Pb dating has revealed the origin and time of the formation of the BGC. These new results do not confirm previously proposed ages. The results obtained from zircon U–Pb dating of the BGC rocks suggest late-Neoproterozoic (Precambrian) age (540–550 Ma). The Bornaward Granitoid Complex is middle-high metaluminous to lower-middle peraluminous and belongs to tholeiite, calc-alkaline to high-K calc-alkaline rock series with enrichment in LIL (Cs, Rb and Ba, U, K, Zr, Y, Th) and depletion in HIL (Sr and Nb, Ta, Ti) elements. Chondrite-normalized Rare Earth Elements (REE) plots indicate minor enrichment of LREE compared to HREE, and strong negative anomaly of Eu compared to other Rare Earth Elements. Furthermore, initial 87 Sr/ 86 Sr and 143 Nd/ 144 Nd range from 0.70351 to 0.71689 and 0.511585 to 0.512061, respectively, and initial εNd isotope values for granite, granodiorite and diorite range from −6.73 to 2.52. These all indicate that the BGC has derived from partial melting of distinct basement source regions with very high initial 87 Sr/ 86 Sr and undergoing extensive crustal contamination (S-type granite).