Origin of arc magmatic signature: A temperature-dependent process for trace element (re)-mobilization in subduction zones

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Origin of arc magmatic signature: A temperature-dependent process for trace element (re)-mobilization in subduction zones

Serpentinite is a major carrier of fluid-mobile elements in subduction zones, which influences the geochemical signature of arc magmatism (e.g. high abundances of Li, Ba, Sr, B, As, Mo and Pb). Based on results from Neoproterozoic serpentinites in the Arabian-Nubian Shield, we herein report the role...

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Bibliographic Details
Main Authors:	Gamal El Dien, Hamed, Li, Zheng-Xiang, Kil, Y., Abu-Alam, T.
Format:	Journal Article
Language:	English
Published:	NATURE PUBLISHING GROUP 2019
Subjects:	Science & Technology Multidisciplinary Sciences Science & Technology - Other Topics FLUID-MOBILE ELEMENTS ARABIAN-NUBIAN SHIELD MID-ATLANTIC RIDGE EASTERN DESERT ABYSSAL PERIDOTITES SERPENTINITES MANTLE COMPLEX GEOCHEMISTRY OPHIOLITE
Online Access:	http://purl.org/au-research/grants/arc/FL150100133 http://hdl.handle.net/20.500.11937/90612

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