Original paper

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

Volume: 9, Issue: 1
Published: May 8, 2019
Abstract
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 of antigorite in the transportation of fluid-mobile elements (FME) and light rare earth elements (LREE) from the subducted slab to arc-related magma...
Paper Details
Title
Origin of arc magmatic signature: A temperature-dependent process for trace element (re)-mobilization in subduction zones
Published Date
May 8, 2019
Volume
9
Issue
1
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