Trace element systematics and ore-forming processes in mafic VMS deposits: Evidence from the Troodos ophiolite, Cyprus
Martin AJ, Keith M, Mcdonald I, Haase K, Mcfall KA, Klemd R, Macleod CJ (2019)
Publication Type: Journal article
Publication year: 2019
Journal
Book Volume: 106
Pages Range: 205-225
DOI: 10.1016/j.oregeorev.2019.01.024
Abstract
The volcanogenic massive sulfide (VMS) deposits in the Troodos ophiolite (Cyprus) are ancient analogues for modern day seafloor massive sulfide mineralisation formed in a supra-subduction zone environment. In this study we present the first detailed in situ study of trace elements in sulfides from twenty VMS deposits hosted in the Troodos ophiolite to better understand factors that influence the distribution, enrichment and incorporation of trace elements in different sulfide minerals.
Authors with CRIS profile
Manuel Keith
Lehrstuhl für Endogene Geodynamik (LEG)
Karsten Haase
Lehrstuhl für Endogene Geodynamik (LEG)
Reiner Klemd
Professur für Geochemie von Lagerstätten
Involved external institutions
United Kingdom (GB)How to cite
APA:
Martin, A.J., Keith, M., Mcdonald, I., Haase, K., Mcfall, K.A., Klemd, R., & Macleod, C.J. (2019). Trace element systematics and ore-forming processes in mafic VMS deposits: Evidence from the Troodos ophiolite, Cyprus. Ore Geology Reviews, 106, 205-225. https://doi.org/10.1016/j.oregeorev.2019.01.024
MLA:
Martin, Andrew J., et al. "Trace element systematics and ore-forming processes in mafic VMS deposits: Evidence from the Troodos ophiolite, Cyprus." Ore Geology Reviews 106 (2019): 205-225.
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