U-Pb age dating on zircon crystals, Sr-Nd isotope ratios and geochemistry of Neogene adakitic domes of Quchan-Esfarayen magmatic belt,NE Iran

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geology, mineralization, u-pb dating and sr-nd isotope geochemistry of intrusive bodies in northeast of kashmar

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keybarkuh area is located 70 km southwest of khaf, khorasan razavi province. the study area is situated in northeastern lut block. the rock units in the area are paleozoic metamorphic rocks and cretaceous to tertiary subvolcanic intrusions intruded as dike, stock and batholith; their composition varies from granite to diorite. based on magnetic susceptibility, the intrusive rocks are divided in...

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سن‌سنجی U-Pb بر بلورهای زیرکن، نسبت‌های ایزوتوپی Sr-Nd و زمین شیمی گنبدهای آداکیتی نئوژن کمان ماگمایی قوچان- اسفراین، شمال شرق ایران

Quchan- Esfarayen magmatic belt (north of Sabzevar) include Neogene adakitic domes with andesite to rhyolite in composition which is cut by Jurasic sedimentary rocks, Eocene volcano-sedimentary rocks, Miocene sedimentary rocks and even occasionally Peliocene conglomerate. The main minerals of these rocks are plagioclase and amphibole with various textures such as felsitic porphyry, microlitic p...

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sr-nd isotopic characteristic, u-pb zircon geochronology, and petrogenesis of najmabad granodiorite batholith, eastern iran

the study area is located south of ghonabad in eastern iran. this area is situated between two major faults, darouneh to the north and dashtbyaz to the south. the movements of these faults cased major dislocation of this block. najmabad granodiorite to granite batholith is elongated trending east-west 2×8 km2. mineralization is associated with granite and monzonite. alteration zones are: propyl...

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geology, mineralization, rb-sr & sm-nd geochemistry, and u–pb zircon geochronology of kalateh ahani cretaceous intrusive rocks, southeast gonabad

kalateh ahani is located 27 km southeast of gonabad within the khorasan razavi province. the area is part of lut block. sub-volcanic monzonitic rocks intruded regional metamorphosed shemshak formation (jurassic age). magnetic susceptibility of less altered monzonitic rocks is 0.6%., as, pb and zn > 1%, au up to 150 ppb and sn = 133 ppm. the sn content of vein in the northern part of kalateh aha...

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ژورنال

عنوان ژورنال: Iranian Journal of Crystallography and Mineralogy

سال: 2018

ISSN: 1726-3689,2588-4719

DOI: 10.29252/ijcm.26.2.455