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Tollan, Peter M. E., O’Neill, Hugh St. C., Hermann, Jörg (2018) The role of trace elements in controlling H incorporation in San Carlos olivine. Contributions to Mineralogy and Petrology, 173 (11). 89 doi:10.1007/s00410-018-1517-7

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Reference TypeJournal (article/letter/editorial)
TitleThe role of trace elements in controlling H incorporation in San Carlos olivine
JournalContributions to Mineralogy and Petrology
AuthorsTollan, Peter M. E.Author
O’Neill, Hugh St. C.Author
Hermann, JörgAuthor
Year2018 (November)Volume173
Page(s)89Issue11
PublisherSpringer Science and Business Media LLC
DOIdoi:10.1007/s00410-018-1517-7Search in ResearchGate
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Mindat Ref. ID80123Long-form Identifiermindat:1:5:80123:6
GUID0
Full ReferenceTollan, Peter M. E., O’Neill, Hugh St. C., Hermann, Jörg (2018) The role of trace elements in controlling H incorporation in San Carlos olivine. Contributions to Mineralogy and Petrology, 173 (11). 89 doi:10.1007/s00410-018-1517-7
Plain TextTollan, Peter M. E., O’Neill, Hugh St. C., Hermann, Jörg (2018) The role of trace elements in controlling H incorporation in San Carlos olivine. Contributions to Mineralogy and Petrology, 173 (11). 89 doi:10.1007/s00410-018-1517-7
In(2018, November) Contributions to Mineralogy and Petrology Vol. 173 (11) Springer Science and Business Media LLC

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LocalityCitation Details
Peridot Mesa (Peridot occurrence 38), San Carlos, Gila County, Arizona, USA

See Also

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Jollands, Michael C., O’Neill, Hugh St. C., Hermann, Jörg (2014) The importance of defining chemical potentials, substitution mechanisms and solubility in trace element diffusion studies: the case of Zr and Hf in olivine. Contributions to Mineralogy and Petrology, 168 (3) doi:10.1007/s00410-014-1055-x
Spandler, Carl, O’Neill, Hugh St.C. (2010) Diffusion and partition coefficients of minor and trace elements in San Carlos olivine at 1,300°C with some geochemical implications. Contributions to Mineralogy and Petrology, 159 (6) 791-818 doi:10.1007/s00410-009-0456-8
Le Losq, Charles, Jollands, Michael C., Tollan, Peter M. E., Hawkins, Rhys, O’Neill, Hugh St. C. (2019) Point defect populations of forsterite revealed by two-stage metastable hydroxylation experiments. Contributions to Mineralogy and Petrology, 174 (6) doi:10.1007/s00410-019-1590-6
Foley, Stephen F., Jacob, Dorrit E., O’Neill, Hugh St. C. (2011) Trace element variations in olivine phenocrysts from Ugandan potassic rocks as clues to the chemical characteristics of parental magmas. Contributions to Mineralogy and Petrology, 162 (1) 1-20 doi:10.1007/s00410-010-0579-y
Schoneveld, Louise, O’Neill, Hugh St. C. (2019) The influence of melt composition on the partitioning of trace elements between anorthite and silicate melt. Contributions to Mineralogy and Petrology, 174 (2) doi:10.1007/s00410-019-1548-8
Reynes, Julien, Jollands, Michael, Hermann, Jörg, Ireland, Trevor (2018) Experimental constraints on hydrogen diffusion in garnet. Contributions to Mineralogy and Petrology, 173 (9) doi:10.1007/s00410-018-1492-z
Hammerli, Johannes, Hermann, Jörg, Tollan, Peter, Naab, Fabian (2021) Measuring in situ CO2 and H2O in apatite via ATR-FTIR. Contributions to Mineralogy and Petrology, 176 (12) doi:10.1007/s00410-021-01858-6
Sossi, Paolo A., Prytulak, Julie, O’Neill, Hugh St. C. (2018) Experimental calibration of vanadium partitioning and stable isotope fractionation between hydrous granitic melt and magnetite at 800 °C and 0.5 GPa. Contributions to Mineralogy and Petrology, 173 (4) doi:10.1007/s00410-018-1451-8
Sossi, Paolo A., O’Neill, Hugh St. C. (2016) Liquidus temperatures of komatiites and the effect of cooling rate on element partitioning between olivine and komatiitic melt. Contributions to Mineralogy and Petrology, 171 (5) doi:10.1007/s00410-016-1260-x
Berry, Andrew J., O’Neill, Hugh St. C., Foran, Garry J. (2021) The effects of temperature and pressure on the oxidation state of chromium in silicate melts. Contributions to Mineralogy and Petrology, 176 (5) doi:10.1007/s00410-021-01776-7
Mallmann, Guilherme, O’Neill, Hugh St. C., Klemme, Stephan (2009) Heterogeneous distribution of phosphorus in olivine from otherwise well-equilibrated spinel peridotite xenoliths and its implications for the mantle geochemistry of lithium. Contributions to Mineralogy and Petrology, 158 (4) 485-504 doi:10.1007/s00410-009-0393-6
 
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