Abstract
Interpretation of the mineralizing environment of magnetite-apatite deposits remains controversial with theories that include a hydrothermal or magmatic origin or a combination of those two processes. To address this controversy, we have analyzed the trace element content of magnetite from precisely known geographic locations and geologic environments from the Precambrian magnetite-apatite ore and host rocks in Kiruna, Sweden, and the Pliocene-Holocene El Laco volcano in the Atacama desert of Chile. Magnetite samples from Kiruna have low trace element concentrations with little chemical variation between the ore, host, and related intrusive rocks. Magnetite from andesite at El Laco, and dacite from the nearby Láscar volcano, has high trace element concentrations typical of magmatic magnetite. El Laco ore magnetite have low trace element concentrations and displays growth zoning in incompatible elements (Si, Ca, and Ce), compatible elements (Mg, Al, and Mn), large-ion lithophile element (Sr), and high field strength element (Y, Nb, and Th). The El Laco ore magnetite are similar in composition to magnetite that has been previously interpreted to have crystallized from hydrothermal fluids; however, there is a significant difference in the internal zoning patterns. At El Laco, each zoned element is either enriched or depleted in the same layers, suggesting the magnetite crystallized from a volatile-rich, iron-oxide melt. In general, the compositions of magnetite from these two deposits plot in very wide fields that are not restricted to the proposed fields in published discriminant diagrams. This suggests that the use of these diagrams and genetic models based on them should be used with caution.
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Acknowledgements
We would like to thank the Natural Sciences and Engineering Research Council of Canada (NSERC) discovery grant to JMH. The contribution of FT has been funded by the project SEIDI 2014 CGL2014-55949-R. Thanks to Luossavaara-Kiirunavaara Aktiebolag (LKAB) and Compañía Minera del Pacífico (CMP) for the help in logistics and permission to sample and granting access to the mine sites. We thank the reviewers (P. Williams and N. Oliver) for the thorough and constructive criticism of the original manuscript and to P. Williams for the comments on the revised manuscript. Thanks also to B. Lehmann for his review and editorial additions and handling of this paper.
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Broughm, S.G., Hanchar, J.M., Tornos, F. et al. Mineral chemistry of magnetite from magnetite-apatite mineralization and their host rocks: examples from Kiruna, Sweden, and El Laco, Chile. Miner Deposita 52, 1223–1244 (2017). https://doi.org/10.1007/s00126-017-0718-8
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DOI: https://doi.org/10.1007/s00126-017-0718-8