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جستجوی مقالات
سه شنبه 25 آذر 1404
Journal of Mining and Environment
، جلد ۱۶، شماره ۲، صفحات ۷۳۷-۷۶۵
عنوان فارسی
چکیده فارسی مقاله
کلیدواژههای فارسی مقاله
عنوان انگلیسی
Plio-Quaternary Adakite Genesis and Post-collisional Processes: Whole Rock Constraints and Sr, Nd Isotopic Compositions in Alborz Magmatic Belt, Ardabil, Iran
چکیده انگلیسی مقاله
The Plio-quaternary sub-volcanic domes are the products of magmatism in the Turkish-Iranian plateau in the collision zone between Eurasia and Arabia. Intermediate-felsic volcanic rocks are found 50 km west of Ardabil. These volcanic domes make a significant part of the Sabalan volcanic, a Plio-quaternary stratovolcano in northwest Iran. The igneous rocks (adakitic) include dacite, trachyte, andesite, trachy-andesite, and trachydacite, associated with ignimbrite and pyroclastic equivalents. They mainly comprise phenocrysts and a microcrystalline groundmass of pyroxene, amphibole, and plagioclase, with biotite and titanomagnetite. These rocks are enriched in Light Rare Earth Elements (LRREs) and Large Ion Lithophile Elements (LILEs) and depleted from Heavy Rare Earth Elements (HRREs) and High-Field Strength Elements (HFSEs). In these rocks, the SiO
2
content is 56-66 wt%, Na
2
O is > 3.5 wt%, Al
2
O
3
> 15 wt%, Yb < 0.2 ppm, and Y < 7 ppm, which are typical of high silica adakitic rocks. The initial ratios of the
143
Nd/
144
Nd range from 0.5127 to 0.5129
and the initial ratios of
87
Sr/
86
Sr for the adakites range from 0.7035 to 0.7060, reflecting the heterogeneity of the mantle and different degrees of crystallization. These geological, geochemical, and Sr, and Nd isotopic data indicate that these rocks belong to the post-collisional adakite type, and are derived from low-degree partial melting of a subduction-metasomatized continental lithospheric mantle (eclogite or amphibolite garnet). In the studied area, mineralization related to Plio-quaternary adakitic rocks has not been observed.
کلیدواژههای انگلیسی مقاله
Alborz magmatic belt,Sr-Nd isotopic,Adakite,Sabalan,Iran
نویسندگان مقاله
Akram Abdolahadi |
Department of Geology, Science and Research Branch, Islamic Azad University, Tehran, Iran
Seyed Jamal Sheikhzakariaee |
Department of Geology, Science and Research Branch, Islamic Azad University, Tehran, Iran
Abdollah Yazdi |
Department of Geology, Kahnooj Branch, Islamic Azad University, Kahnooj, Iran
Seyed Zahed Mousavi |
Department of Geology, Meshkinshahr Branch, Islamic Azad University, Meshkinshahr, Iran
نشانی اینترنتی
https://jme.shahroodut.ac.ir/article_3286_26d77c9e046fa427da233201d33ef796.pdf
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