2021
DOI: 10.1016/j.gr.2020.12.033
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Neoproterozoic evolution of northern Gondwana recorded in detrital zircon grains from the Gheshlagh bauxite deposit, Alborz Mountains, Iran Block

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Cited by 15 publications
(1 citation statement)
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“…The CEIM, Northwest Iran, the Alborz Mountains, and the Binalud Mountains form the Iran Plate that, as an element of the ribbon-like Cimmerian terrane assemblage, split off from the northern margin of Gondwana towards the end of the Palaeozoic Era (Late Permian; e.g. Stampfli and Borel 2002;Shamanian and Hattori 2021). The northward-directed drift of the Cimmerian terranes opened the Neotethys, and their collision with the southern Aistov et al (1984) and Wilmsen et al (2015).…”
Section: Geological Setting and Stratigraphymentioning
confidence: 99%
“…The CEIM, Northwest Iran, the Alborz Mountains, and the Binalud Mountains form the Iran Plate that, as an element of the ribbon-like Cimmerian terrane assemblage, split off from the northern margin of Gondwana towards the end of the Palaeozoic Era (Late Permian; e.g. Stampfli and Borel 2002;Shamanian and Hattori 2021). The northward-directed drift of the Cimmerian terranes opened the Neotethys, and their collision with the southern Aistov et al (1984) and Wilmsen et al (2015).…”
Section: Geological Setting and Stratigraphymentioning
confidence: 99%