کد مقاله | کد نشریه | سال انتشار | مقاله انگلیسی | نسخه تمام متن |
---|---|---|---|---|
4692652 | 1636809 | 2012 | 13 صفحه PDF | دانلود رایگان |
عنوان انگلیسی مقاله ISI
Geochemical characteristics of basaltic rocks from the Nain ophiolite (Central Iran); constraints on mantle wedge source evolution in an oceanic back arc basin and a geodynamical model
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موضوعات مرتبط
مهندسی و علوم پایه
علوم زمین و سیارات
فرآیندهای سطح زمین
پیش نمایش صفحه اول مقاله
![عکس صفحه اول مقاله: Geochemical characteristics of basaltic rocks from the Nain ophiolite (Central Iran); constraints on mantle wedge source evolution in an oceanic back arc basin and a geodynamical model Geochemical characteristics of basaltic rocks from the Nain ophiolite (Central Iran); constraints on mantle wedge source evolution in an oceanic back arc basin and a geodynamical model](/preview/png/4692652.png)
چکیده انگلیسی
⺠We studied geochemistry of mafic rocks from the Nain ophiolites in Iran. ⺠The rocks show characters of island arc tholeiite/mid-ocean ridge basalt magma types. ⺠They are originated in an oceanic back arc basin, and subsequently have been enriched by slab-derived fluids. ⺠The arc volcanic-like magmas were produced at the early stage. ⺠The MORB-like basalts were generated at the later stage of evolution of the Nain ophiolitic complex.
ناشر
Database: Elsevier - ScienceDirect (ساینس دایرکت)
Journal: Tectonophysics - Volumes 574â575, 29 October 2012, Pages 92-104
Journal: Tectonophysics - Volumes 574â575, 29 October 2012, Pages 92-104
نویسندگان
Javad Mehdipour Ghazi, Mohssen Moazzen, Mohammad Rahgoshay, Hadi Shafaii Moghadam,