Trace element systematics and ore-forming processes in mafic VMS deposits: Evidence from the Troodos ophiolite, Cyprus

Journal article


Publication Details

Author(s): Martin AJ, Keith M, Mcdonald I, Haase K, Mcfall KA, Klemd R, Macleod CJ
Journal: Ore Geology Reviews
Publication year: 2019
Volume: 106
Pages range: 205-225
ISSN: 0169-1368


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.


FAU Authors / FAU Editors

Haase, Karsten Prof. Dr.
Lehrstuhl für Endogene Geodynamik
Klemd, Reiner Prof. Dr.
Professur für Geochemie und Lagerstättenkunde


External institutions
Cardiff University
University of Leicester


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://dx.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.

BibTeX: 

Last updated on 2019-09-04 at 17:08