Please use this identifier to cite or link to this item: http://hdl.handle.net/2381/46101
Title: Effects of magmatic volatile influx in mafic VMS hydrothermal systems: evidence from the Troodos ophiolite, Cyprus
Authors: Martin, A
Keith, M
Parvaz, D
McDonald, I
Boyce, A
McFall, K
Jenkin, G
Strauss, H
MacLeod, C
First Published: 2019
Publisher: Elsevier for European Association of Geochemistry
Citation: Chemical Geology, 2019, In Press
Abstract: The Troodos ophiolite, Cyprus is the principal on-land analogue for mafic-hosted volcanogenic massive sulfide (VMS) deposits. This study, for the first time, presents sulfur isotope (δ34S) data on a regional scale from VMS deposits and other mineralised zones across the Troodos ophiolite. In combination δ34S, Se/S ratios and trace element chemistry (e.g., Se, Cu and Au) of different hydrothermal sulfides are used to assess variations in magmatic volatile influx and the source of metals and sulfur in ancient hydrothermal systems.
DOI Link: TBA
ISSN: 0009-2541
Links: TBA
http://hdl.handle.net/2381/46101
Version: Post-print
Status: Peer-reviewed
Type: Journal Article
Rights: Copyright © Elsevier for European Association of Geochemistry2019. After an embargo period this version of the paper will be an open-access article distributed under the terms of the Creative Commons Attribution-Non Commercial-No Derivatives License (http://creativecommons.org/licenses/by-nc-nd/4.0/), which permits use and distribution in any medium, provided the original work is properly cited, the use is non-commercial and no modifications or adaptations are made.
Description: The file associated with this record is under embargo until 12 months after publication, in accordance with the publisher's self-archiving policy. The full text may be available through the publisher links provided above.
Appears in Collections:Published Articles, Dept. of Geology

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