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- W2227758323 abstract "Intermediate to felsic volcanic and granitic rocks with high Na2O concentrations (5.2–9.1 wt.%) are widely distributed in the Harsin area along the Zagros thrust zone in western Iran. Most of these rocks are classified as low-potassium tholeiite, display affinity with oceanic plagiogranite and contain somewhat high Na content and low concentrations of K2O, Al2O3, Rb, Sr and Ca. Thus, we prefer to apply the term Na-rich felsic rocks to this complex. U–Pb dating yielded ages of 94.6 ± 2.7 Ma (2σ) from baddeleyite and 95.0 ± 2.4 Ma (2σ) from zircon grains, indicating that the complex crystallized in the Late Cretaceous. Based on the mineral compositions, the crystallization occurred at low pressures (mostly < 2 kbar) and low temperatures (< 750 °C). High initial ratios of 143Nd/144Nd (0.51288–0.51304) and positive values of ɛNd(t) (+ 7.0 to + 11.5) are consistent with those of mid-oceanic ridge basalt (MORB). During collision of the Arabian plate and Biston-Avoraman block in the Late Cretaceous, an increasing geothermal gradient was responsible for partial melting of altered mafic rocks and for producing the Na-rich felsic rocks in the Harsin area. The presence of these types of rocks along the main Zagros fault indicates local collisions. These collisions were caused by southwestward subduction under the Arabian plate in the southern branch of the Neo-Tethys. This event was the first stage of the Zagros collision, which was followed by collision of the Arabian and Iranian plates during the Eocene through Neogene." @default.
- W2227758323 created "2016-06-24" @default.
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- W2227758323 date "2016-03-01" @default.
- W2227758323 modified "2023-10-18" @default.
- W2227758323 title "Age and petrogenesis of Na-rich felsic rocks in western Iran: Evidence for closure of the southern branch of the Neo-Tethys in the Late Cretaceous" @default.
- W2227758323 cites W1491216466 @default.
- W2227758323 cites W1499677798 @default.
- W2227758323 cites W1543566518 @default.
- W2227758323 cites W1574573824 @default.
- W2227758323 cites W1896208096 @default.
- W2227758323 cites W1968318197 @default.
- W2227758323 cites W1972495686 @default.
- W2227758323 cites W1974501258 @default.
- W2227758323 cites W1978776740 @default.
- W2227758323 cites W1979427870 @default.
- W2227758323 cites W1980000874 @default.
- W2227758323 cites W1981054075 @default.
- W2227758323 cites W1981951332 @default.
- W2227758323 cites W1987539111 @default.
- W2227758323 cites W1990305818 @default.
- W2227758323 cites W1994440181 @default.
- W2227758323 cites W1998191744 @default.
- W2227758323 cites W1999229976 @default.
- W2227758323 cites W2003919078 @default.
- W2227758323 cites W2005236071 @default.
- W2227758323 cites W2005485422 @default.
- W2227758323 cites W2007105153 @default.
- W2227758323 cites W2009280852 @default.
- W2227758323 cites W2017102456 @default.
- W2227758323 cites W2018555510 @default.
- W2227758323 cites W2021642760 @default.
- W2227758323 cites W2022865523 @default.
- W2227758323 cites W2023644752 @default.
- W2227758323 cites W2024800224 @default.
- W2227758323 cites W2026780623 @default.
- W2227758323 cites W2028858476 @default.
- W2227758323 cites W2033745814 @default.
- W2227758323 cites W2034817985 @default.
- W2227758323 cites W2040120198 @default.
- W2227758323 cites W2040549377 @default.
- W2227758323 cites W2045594539 @default.
- W2227758323 cites W2046961523 @default.
- W2227758323 cites W2052623580 @default.
- W2227758323 cites W2054899142 @default.
- W2227758323 cites W2055758231 @default.
- W2227758323 cites W2063728739 @default.
- W2227758323 cites W2064648794 @default.
- W2227758323 cites W2068907164 @default.
- W2227758323 cites W2070287079 @default.
- W2227758323 cites W2070734742 @default.
- W2227758323 cites W2071020772 @default.
- W2227758323 cites W2073426602 @default.
- W2227758323 cites W2075156900 @default.
- W2227758323 cites W2075789958 @default.
- W2227758323 cites W2079376467 @default.
- W2227758323 cites W2079548990 @default.
- W2227758323 cites W2079979463 @default.
- W2227758323 cites W2081673195 @default.
- W2227758323 cites W2084564434 @default.
- W2227758323 cites W2084682037 @default.
- W2227758323 cites W2085400311 @default.
- W2227758323 cites W2088223235 @default.
- W2227758323 cites W2091212007 @default.
- W2227758323 cites W2091693693 @default.
- W2227758323 cites W2096144056 @default.
- W2227758323 cites W2098960611 @default.
- W2227758323 cites W2105662998 @default.
- W2227758323 cites W2108971421 @default.
- W2227758323 cites W2109539500 @default.
- W2227758323 cites W2109567422 @default.
- W2227758323 cites W2121394503 @default.
- W2227758323 cites W2134736347 @default.
- W2227758323 cites W2142900602 @default.
- W2227758323 cites W2155135323 @default.
- W2227758323 cites W2157099954 @default.
- W2227758323 cites W2161405009 @default.
- W2227758323 cites W2163015998 @default.
- W2227758323 cites W2163042763 @default.
- W2227758323 cites W2163762918 @default.
- W2227758323 cites W2172106141 @default.
- W2227758323 cites W2316957776 @default.
- W2227758323 cites W2515641725 @default.
- W2227758323 cites W3035349676 @default.
- W2227758323 doi "https://doi.org/10.1016/j.tecto.2015.12.014" @default.
- W2227758323 hasPublicationYear "2016" @default.
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