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Tectonic transition from Ediacaran continental arc to early Cambrian rift in the NE Ardakan region, central Iran: Constraints from geochronology and geochemistry of magmatic rocks

Nouri, Fatemeh; Davoudian, Ali Reza; Shabanian, Nahid; Allen, Mark B.; Asahara, Yoshihiro; Azizi, Hossein; Anma, Ryo; Khodami, Mahnaz; Tsuboi, Motohiro

Authors

Fatemeh Nouri

Ali Reza Davoudian

Nahid Shabanian

Yoshihiro Asahara

Hossein Azizi

Ryo Anma

Mahnaz Khodami

Motohiro Tsuboi



Abstract

Ediacaran-early Cambrian magmatic rocks from the Ardakan region of central Iran include deformed granites from deformed granitic plutons and dolerites from doleritic sills. The granites contain zircon grains with U-Pb ages of 552–550 Ma, and dolerites have a zircon U-Pb age of 528 Ma. These granites are high K calc-alkaline in nature and have variable concentrations of SiO2 (69.1–76.3 wt%), Na2O (2.06–4.82 wt%), K2O (3.08–4.79 wt%) and MgO (0.57–2.02 wt%). They represent I-type granite and are metaluminous to weakly peraluminous, with negative primitive mantle-normalized Nb, Ti and Eu anomalies. 87Sr/86Sr(i) and εNd(t) in the granites vary from 0.7075 to 0.7120 and from −3.0 to +7.3, respectively. Dolerites are alkaline, with low contents of SiO2 (45.7–48.6 wt%), Cr and Ni (13.6–313 and 15.7–146 ppm, respectively) and overall high contents of TiO2 (2.0–4.6 wt%). TiO2 contents define high-Ti and low-Ti dolerite types, which show similar high field strength and rare earth element abundances. The high-Ti dolerites may be evolved equivalents of the low-Ti type. The 87Sr/86Sr(i) and εNd(t) values of both types are highly variable (0.7029 to 0.7077 and −6.1 to +7.7, respectively). The data indicate melting of an asthenospheric mantle source, with additional fractionation, and mixing with crustal melts to produce the evolved dolerites. Geochemical data from granites in NE Ardakan are consistent with late Ediacaran arc magmatism ∼550 Ma. The ∼528 Ma OIB-like dolerites may indicate continental extension at this time.

Citation

Nouri, F., Davoudian, A. R., Shabanian, N., Allen, M. B., Asahara, Y., Azizi, H., …Tsuboi, M. (2022). Tectonic transition from Ediacaran continental arc to early Cambrian rift in the NE Ardakan region, central Iran: Constraints from geochronology and geochemistry of magmatic rocks. Journal of Asian Earth Sciences, 224, Article 105011. https://doi.org/10.1016/j.jseaes.2021.105011

Journal Article Type Article
Acceptance Date Nov 12, 2021
Online Publication Date Nov 19, 2021
Publication Date 2022-02
Deposit Date Feb 27, 2023
Journal Journal of Asian Earth Sciences
Print ISSN 1367-9120
Publisher Elsevier
Peer Reviewed Peer Reviewed
Volume 224
Article Number 105011
DOI https://doi.org/10.1016/j.jseaes.2021.105011
Public URL https://durham-repository.worktribe.com/output/1180757