Original paper
Rhenium enrichment in the northwest Pacific arc
Abstract
Rhenium (Re) is one of the least abundant elements in the silicate Earth. However, independent rhenium sulfide was reported in the Usu and Kudryavy volcanos, namely rheniite (ReS2, 74.5 wt% of Re). This raises questions about the sources of the Kurile–Kamchatka volcanic island arc magmas and geochemical cycling of Re. The oxidation-reduction cycle on the Earth’s surface is the major process that concentrates Re in reduced sediments. The...
Paper Details
Title
Rhenium enrichment in the northwest Pacific arc
Published Date
Dec 1, 2019
Journal
Volume
115
Pages
103176 - 103176
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Notes
History