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Geochemical and Nd-Sr Isotopic Compositions of Hypabyssal Adakites in the Torud-Ahmad Abad Magmatic Belt, Northern Central Iran Zone : Analysis of Petrogenesis and Geodynamic Implications

Yousefi, Fazilat (author)
Department of Earth Sciences, University of New Brunswick, Fredericton, Canada
Mills, Ryan D. (author)
Department of Geological Sciences, University of North Carolina at Chapel Hill, Chapel Hill, USA
Sadeghian, Mahmoud (author)
Faculty of Earth Sciences, Shahrood University of Technology, Shahrood, Iran
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Lentz, David R. (author)
Department of Earth Sciences, University of New Brunswick, Fredericton, Canada
Wanhainen, Christina (author)
Luleå tekniska universitet,Geovetenskap och miljöteknik
Ghasemi, Habibollah (author)
Faculty of Earth Sciences, Shahrood University of Technology, Shahrood, Iran
Miao, Laicheng (author)
Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing, 100029, China
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 (creator_code:org_t)
2021-01-07
2021
English.
In: Journal of Earth Science. - : Springer Nature. - 1674-487X .- 1867-111X. ; 32:6, s. 1428-1444
  • Journal article (peer-reviewed)
Abstract Subject headings
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  • Eocene intermediate to felsic subvolcanic rocks of the Torud-Ahmad Abad magmatic belt (TAMB), in the northern part of the Central Iran zone, are exposed between the Torud and Ahmad Abad regions in South-Southeast Shahrood. These igneous rocks include hypabyssal dacite, trachyte, andesite, trachy-andesite, and basaltic andesite; they are mainly composed of phenocrysts and microcrystalline groundmass of pyroxene, amphibole, and plagioclase, with minor biotite and titanomagnetite; they form domal structures (plugs and stocks), dikes, and sills that intruded into Neoproterozoic to cogenetic Eocene volcano-sedimentary sequences. Based on isotopic analysis of these intermediate to acidic rocks, initial ratios of 143Nd/144Nd range from 0.512 775 to 0.512 893 and initial ratios of 87Sr/86Sr range from 0.703 746 to 0.705 314, with quite positive εNd(i) values of +3.69 to +6.00. They are enriched in light rare earth elements and large ion lithophile elements and depleted in heavy rare earth elements and high-field strength elements, the SiO2 content is (52–62) wt.%, and Na2O content >3 wt.%, Al2O3 content >16 wt.%, Yb <1.8 ppm, and Y <18 ppm. These geological, geochemical, and Sr and Nd isotopic data are consistent with adakitic signatures originating by partial melting of the subducted Neo-Tethys oceanic slab (Sabzevar branch) and lithospheric suprasubduction zone mantle. The mantle signatures typifying the rapidly emplaced adakitic rocks (slab (high-silica adakite) and suprasubduction zone (low-silica adakite) melts) together with their locally voluminous extent are evidences that support a locally extensional geodynamic setting; and the evidence is consistent with an evolution to local transpression in the Late Eocene in this convergent margin arc environment to rifting (basalts to adakites) towards submarine conditions in the Neogene. © 2021, China University of Geosciences (Wuhan) and Springer-Verlag GmbH Germany, Part of Springer Nature.

Subject headings

NATURVETENSKAP  -- Geovetenskap och miljövetenskap -- Geologi (hsv//swe)
NATURAL SCIENCES  -- Earth and Related Environmental Sciences -- Geology (hsv//eng)

Keyword

isotope geochemistry
adakite rocks
Central Iran zone
Shahrood
Iran
Ore Geology
Malmgeologi

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ref (subject category)
art (subject category)

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