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Lithology and tectonomagmatic setting of volcanic and plutonic rocks from the Lak area, southwest Buin Zahra, NW Iran
Published 2022-12-01“…The purpose of this research is to identify the petrographic and geochemical characteristics of the volcanic and intrusive rocks of the Lak area in NW Iran and also to determine the tectonomagmatic setting of these rocks.GeologyThe Lak area is situated 36 km southwest of Buin Zahra, in the northern part of the UDMA and the western part of the Central Iran zone (Aghanabati, 2006). The UDMA is an Andean magmatic arc with a NW-SE trend, which formed by the oblique subduction of the Neotethys oceanic plate under the central Iranian plate (Shearman et al., 1976; Berberian and King, 1981; Agard et al., 2011; Gohari et al., 2022). …”
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Petrogenesis and tectonic setting of Aftabru-Qlichkandi High-K metaluminous intrusive bodies (South of Buin-Zahra): Evidences from Nd-Sr isotopic Data
Published 2022-06-01“…The mentioned intrusive masses are located in the southwest region of Buin Zahra in Central Iran zone.Geology BackgroundUrmia-Dokhtar magmatic arc with Cenozoic intrusive and Eocene-Quaternary extrusive rocks shows different levels and rock outcrops in terms of time of origin and erosion rate, same what is seen in the subduction arc of the Andean continental margin. The lithospheric stresses caused by the interaction of the African-Eurasian-Indian lithosphere led to the emergence of Paleogene extensive magmatic activity and a magmatic flare-up lasting 30 Myrs during Eocene and Oligocene. …”
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Au-bearing magnetite mineralizaion in Kashmar (alteration, mineralization, geochemistry, geochemistry and fluid inclusions);
Published 2017-02-01“…Iron oxide-copper-gold deposits: An Andean view. Mineralium Deposita, 38(7): 787–812.…”
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