Zircon Thermometer Reveals Minimum Melting Conditions on Earliest Earth
By H Htoon, M. O 'connell, P. J. Cox, S. Doorn, P. Avouris, M. Hybertsen, M. Loy, P. Kim, V. Perebeinos, M. Sfeir and 2 more. Science, 2005
890 citations recorded by the source corpus.
Subfields: Astronomy and Astrophysics, Geophysics, Paleontology
View Paper: https://www.semanticscholar.org/paper/68f66ea2b975c41097cece4307f3283c745bb976
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In Astronomy and Astrophysics
In Geophysics
- L. Perchuk
- J. Ferry
- E. Bruce Watson
- E. Sizova
- Michael Brown
- Leslie A. Hayden
- A. Antignano
- C. Manning
In Paleontology
Citations in the corpus
- Rutile saturation in hydrous siliceous melts and its bearing on Ti-thermometry of quartz and zircon (2007, background): “If FM is known, magmatic temperature can be inferred and the corresponding rutile solubility can be read off of the contours (see [10], supporting online materials for further discussion).”
- New thermodynamic models and revised calibrations for the Ti-in-zircon and Zr-in-rutile thermometers (2007, background): “Hills, Australia, by Watson and Harrison (2005) and the conclusions drawn from them do not require significant revision.”
- Subduction styles in the Precambrian: Insight from numerical experiments (2009, background): “A form of plate tectonics may have operated earlier in the Hadean, Eoarchean and Paleoarchean (de Wit, 1998; Watson and Harrison, 2005; Hopkins et al., 2008), but subductionmight have been very shallow and at low dips (e.g. Abbott et al., 1994a; de Wit, 1998; Smithies et al., 2003).”
- Rutile solubility in H2O, H2O–SiO2, and H2O–NaAlSi3O8 fluids at 0.7–2.0 GPa and 700–1000 °C: Implications for mobility of nominally insoluble elements (2008, background): “…occurrence makes it useful for net-transfer and exchange thermobarometry (e.g., Bohlen et al., 1983; Manning and Bohlen, 1991; Zack et al., 2004a; Watson and Harrison, 2005; Watson et al., 2006; Zack and Luvizottow, 2006; Tomkins et al., 2007; Tropper and Manning, in press) and U–Pb…”
- Ti-in-zircon thermometry: applications and limitations (2008, methodology): “The average drops to 699 ± 66°C (27 zircons; or 692 ± 65°C, 41 analyses) if those with high Ti-in-zircon temperatures ([750°C) are excluded, as suggested by Watson and Harrison (2005, 2006) and Harrison et al. (2007).”