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Schwarzenbach, Esther M., Gazel, Esteban, Caddick, Mark J. (2014) Hydrothermal processes in partially serpentinized peridotites from Costa Rica: evidence from native copper and complex sulfide assemblages. Contributions to Mineralogy and Petrology, 168 (5) doi:10.1007/s00410-014-1079-2

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Reference TypeJournal (article/letter/editorial)
TitleHydrothermal processes in partially serpentinized peridotites from Costa Rica: evidence from native copper and complex sulfide assemblages
JournalContributions to Mineralogy and Petrology
AuthorsSchwarzenbach, Esther M.Author
Gazel, EstebanAuthor
Caddick, Mark J.Author
Year2014 (November)Volume168
Issue5
PublisherSpringer Science and Business Media LLC
DOIdoi:10.1007/s00410-014-1079-2Search in ResearchGate
Generate Citation Formats
Mindat Ref. ID79718Long-form Identifiermindat:1:5:79718:2
GUID0
Full ReferenceSchwarzenbach, Esther M., Gazel, Esteban, Caddick, Mark J. (2014) Hydrothermal processes in partially serpentinized peridotites from Costa Rica: evidence from native copper and complex sulfide assemblages. Contributions to Mineralogy and Petrology, 168 (5) doi:10.1007/s00410-014-1079-2
Plain TextSchwarzenbach, Esther M., Gazel, Esteban, Caddick, Mark J. (2014) Hydrothermal processes in partially serpentinized peridotites from Costa Rica: evidence from native copper and complex sulfide assemblages. Contributions to Mineralogy and Petrology, 168 (5) doi:10.1007/s00410-014-1079-2
In(2014, November) Contributions to Mineralogy and Petrology Vol. 168 (5) Springer Science and Business Media LLC

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Schwarzenbach, E. M., Gazel, E., & Caddick, M. J. (2014). Hydrothermal processes in partially serpentinized peridotites from Costa Rica: evidence from native copper and complex sulfide assemblages. Contributions to Mineralogy and Petrology, 168(5), 1-21.
Schwarzenbach, E.M., Gazel, E., and Caddick, M.J. (2014) Hydrothermal processes in partially serpentinized peridotites from Costa Rica: evidence from native copper and complex sulfide assemblages. Contributions to Mineralogy and Petrology, 168(5), 1-21.
Schwarzenbach, Esther M., Caddick, Mark J., Beard, James S., Bodnar, Robert J. (2016) Serpentinization, element transfer, and the progressive development of zoning in veins: evidence from a partially serpentinized harzburgite. Contributions to Mineralogy and Petrology, 171 (1) doi:10.1007/s00410-015-1219-3
Farber, Katja, Caddick, Mark J., John, Timm (2014) Controls on solid-phase inclusion during porphyroblast growth: insights from the Barrovian sequence (Scottish Dalradian) Contributions to Mineralogy and Petrology, 168 (6) doi:10.1007/s00410-014-1089-0
Gorve, Timothy L., Hoefs, Jochen, Müntener, Othmar (2014) Editorial. Contributions to Mineralogy and Petrology, 168 (5) doi:10.1007/s00410-014-1080-9
Le Roux, V., Dick, H. J. B., Shimizu, N. (2014) Tracking flux melting and melt percolation in supra-subduction peridotites (Josephine ophiolite, USA) Contributions to Mineralogy and Petrology, 168 (4) doi:10.1007/s00410-014-1064-9
Ziberna, Luca, Klemme, Stephan, Nimis, Paolo (2014) Erratum to: Garnet and spinel in fertile and depleted mantle: insights from thermodynamic modelling. Contributions to Mineralogy and Petrology, 168 (2) doi:10.1007/s00410-014-1036-0
Grove, Timothy L., Hoefs, Jochen, Müntener, Othmar (2014) Erratum to: Editorial. Contributions to Mineralogy and Petrology, 168 (6) doi:10.1007/s00410-014-1087-2
Alex Zirakparvar, N., Mathez, Edmond. A., Scoates, James S., Wall, Corey J. (2014) Zircon Hf isotope evidence for an enriched mantle source for the Bushveld Igneous Complex. Contributions to Mineralogy and Petrology, 168 (3) doi:10.1007/s00410-014-1050-2
Holness, Marian B. (2014) The effect of crystallization time on plagioclase grain shape in dolerites. Contributions to Mineralogy and Petrology, 168 (5) doi:10.1007/s00410-014-1076-5
Chamberlain, Katy J., Morgan, Daniel J., Wilson, Colin J. N. (2014) Timescales of mixing and mobilisation in the Bishop Tuff magma body: perspectives from diffusion chronometry. Contributions to Mineralogy and Petrology, 168 (1) doi:10.1007/s00410-014-1034-2
 
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