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ABSTRACTThe Biarjmand granitoids and granitic gneisses in northeast Iran are part of the Torud–Biarjmand metamorphic complex, where previous zircon U–Pb geochronology show ages of ca. 554–530 Ma for orthogneissic rocks. Our new U–Pb zircon ages confirm a Cadomian age and show that the granitic gneiss is ~30 million years older (561.3 ± 4.7 Ma) than ...
Xian-Hua Li +2 more
exaly +6 more sources
Abstract Small granitic plutons and associated granitic dykes that intrude the pre-Devonian basement of the Bitlis Massif were previously inferred to have a broadly Late Palaeozoic crystallisation age related to the Hercynian orogeny; this was tested during this work.
Timur Ustaömer +2 more
exaly +8 more sources
Abstract The ChahJam–Biarjmand complex (CJBC), flanked by the Alborz Mountains in the north and the Lut–Tabas block to the south, is part of Central Iranian block, where the oldest continental crust of Iran is found. This complex contains granitic to tonalitic orthogneissic rocks (old plutons) and associated metasediments, amphibolites and ...
Hadi Shafaii Moghadam +2 more
exaly +5 more sources
The work was supported by the Ministerio de Ciencia, Innovación y Universidades Ministerio de Ciencia, Innovación y Universidades [PID2021-122467NB-C22]; Ministerio de Ciencia, Innovación y Universidades [PID2021-125585NB-I00].
Esther Rojo-Pérez +3 more
semanticscholar +4 more sources
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Cadomian magmatism in the North Armorican Massif
Geological Society Special Publication, 1990Abstract This review concerns intrusive magmatism related to the Cadomian orogeny in the northeastern part of the Armorican Massif of France. The Cadomian orogeny is interpreted to represent tectono-thermal activity in a continental margin above a subduction zone. The North Armorican Shear Zone (NASZ) separates two major Cadomian
G M Power, R S D'Lemos
exaly +3 more sources
Cadomian Magmatic Rocks from Zarand (SE Iran) Formed in a Retro-Arc Basin
Abstract A major arc-related magmatic episode is recorded in the Ediacaran-Early Cambrian (Cadomian) crust of Iran and Anatolia due to the southward subduction of Prototethyan oceanic lithosphere beneath N Gondwana. This magmatism was generated at a convergent margin, fragments of which can be traced for thousands of kilometres, from west Avalonia to
Fatemeh Sepidbar +5 more
semanticscholar +4 more sources
Short Paper: Cadomian terrane tectonics and magmatism in the Armorican Massif
Journal of the Geological Society, 1989The North Armorican composite terrane, NW France, is a collage of displaced terranes which result from the amalgamation of Cadomian continental arcs and marginal basin complexes by sinistral transpression along a continental margin above a subduction zone. Early Cadomian arc activity occurred at c.
Peter J Treloar, Richard S D'Lemos
exaly +3 more sources
Lithos, 2015
Hormuz Island, a salt-gypsum dome in the Persian Gulf in southern Iran, is a complex halotectonic melange comprising evaporites, carbonates, volcanic and volcaniclastic rocks, as well as low-grade metamorphic and sedimentary rocks. Based on trace element (including rare earth elements REE) compositions of whole rocks and zircon, Hormuz rhyolites are ...
Jamshid Hassanzadeh, Kevin D Mckeegan
exaly +4 more sources
Hormuz Island, a salt-gypsum dome in the Persian Gulf in southern Iran, is a complex halotectonic melange comprising evaporites, carbonates, volcanic and volcaniclastic rocks, as well as low-grade metamorphic and sedimentary rocks. Based on trace element (including rare earth elements REE) compositions of whole rocks and zircon, Hormuz rhyolites are ...
Jamshid Hassanzadeh, Kevin D Mckeegan
exaly +4 more sources

