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

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

Internet

http://purl.org/au-research/grants/arc/FL150100133
http://hdl.handle.net/20.500.11937/90612

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