References

X. References

Burnham, Antony D., and Andrew J. Berry. “An Experimental Study of Trace Element Partitioning between Zircon and Melt as a Function of Oxygen Fugacity.” Geochimica Et Cosmochimica Acta, vol. 95, 2012, pp. 196–212., https://doi.org/10.1016/j.gca.2012.07.034.

Drake, Michael J. “The Oxidation State of Europium as an Indicator of Oxygen Fugacity.” Geochimica Et Cosmochimica Acta, vol. 39, no. 1, Jan. 1975, pp. 55–64., https://doi.org/10.1016/0016-7037(75)90184-2.

Hayden, Leslie A., and E. Bruce Watson. “Rutile Saturation in Hydrous Siliceous Melts and Its Bearing on TI-Thermometry of Quartz and Zircon.” Earth and Planetary Science Letters, vol. 258, no. 3-4, 30 June 2007, pp. 561–568., https://doi.org/10.1016/j.epsl.2007.04.020.

Loucks, Robert R., et al. “Divergent T–ƑO2 Paths during Crystallisation of H2O-Rich and H2O-Poor Magmas as Recorded by CE and U in Zircon, with Implications for Titaniq and Titaniz Geothermometry.” Contributions to Mineralogy and Petrology, vol. 173, no. 12, 2018, https://doi.org/10.1007/s00410-018-1529-3.

Nakamura, Noboru. “Determination of Ree, Ba, Fe, Mg, Na and K in Carbonaceous and Ordinary Chondrites.” Geochimica Et Cosmochimica Acta, vol. 38, no. 5, 1974, pp. 757–775., https://doi.org/10.1016/0016-7037(74)90149-5.

PEARCE, NICHOLAS J. “Towards a Protocol for the Trace Element Analysis of Glass from Rhyolitic Shards in Tephra Deposits by Laser Ablation Icp-Ms.” Journal of Quaternary Science, vol. 29, 640 7, 15 Oct. 2014, pp. 627–640., https://doi.org/10.1002/jqs.2727.

Paton, C., Hellstrom, J., Paul, B.,Woodhead, J. and Hergt, J., 2011, Iolite: Freeware for the visualisation and processing of mass spectrometric data: Journal of Analytical Atomic Spectrometry, v. 26, no. 12, p. 2508-2518, doi:10.1039/c1ja10172b.

Trail, Dustin, et al. “CE and EU Anomalies in Zircon as Proxies for the Oxidation State of Magmas.” Geochimica Et Cosmochimica Acta, vol. 97, 6 Sept. 2012, pp. 70–87., https://doi.org/10.1016/j.gca.2012.08.032.

Smythe, Duane J., and James M. Brenan. “Magmatic Oxygen Fugacity Estimated Using Zircon-Melt Partitioning of Cerium.” Earth and Planetary Science Letters, vol. 453, June 2016, pp. 260–266., https://doi.org/10.1016/j.epsl.2016.08.013.

Spell, T.L., Kyle, P.R., Thirlwall, M.F., and Campbell, A.R., 1993, Isotopic and Geochemical Constraints on the Origin and Evolution of Postcollapse Rhyolites in the Valles Caldera, New Mexico: Journal of Geophysical Research, v. 98, no. B11, p. 19723-19739 https://doi.org/10.1029/93JB01569.

Spell, T.L., McDougall, I., and Doulgeris, A.P, 1996a, Cerro Toledo Rhyol te, Jemez Volcanic Field, New Mexico: 40Ar/39Ar geochronology of eruptions between two caldera-forming events: GSA Bulletin, v. 108, no. 12, p. 1,549-1,566, https://doi.org/10.1130/00167606(1996)- 108%3C1549:CTRJVF%3E2.3.CO;2.

Stix, J., and Gorton, P., 1993, Replenishment and crystallization in epicontinental silicic magma chambers: evidence from the Bandelier magmatic system: Journal of Volcanology and Geothermal Research, v. 55, p. 201-215.

Watson E. B. and Green T. H. (1981) Apatite/liquid partition coefficients for the rare earth elements and strontium. Earth Planet. Sci. Lett. 56, 405–421.

Woodhead, Jon D., et al. “Isotopic and Elemental Imaging of Geological Materials by Laser Ablation Inductively Coupled Plasma-Mass Spectrometry.” Geostandards and Geoanalytical Research, 2007, https://doi.org/10.1111/j.1751-908x.2007.00104.x.

Yuguchi, Takashi, et al. “Simultaneous Determination of Zircon U–Pb Age and Titanium Concentration Using LA-ICP-MS for Crystallization Age and Temperature.” Lithos, vol. 372-373, 1 Nov. 2020, https://doi.org/10.1016/j.lithos.2020.105682.

Zhong, Shihua, et al. “Can Magmatic Zircon Be Distinguished from Hydrothermal Zircon by Trace Element Composition? the Effect of Mineral Inclusions on Zircon Trace Element Composition.” Lithos, vol. 314-315, Aug. 2018, pp. 646–657., https://doi.org/10.1016/j.lithos.2018.06.029.