Revised Ti-in-biotite geothermometer for ilmenite- or rutile-bearing crustal metapelites

In the present study, the Ti-in-biotite geother- mometer was revised using more than 300 natural rutile- or ilmenite-bearing metapelites collected worldwide. The formulation was empirically calibrated as ln[T(℃)]= 6.313 +0.22 41n(XTi ) -0.2881n(XFe ) -0. 4491n(XMg) + 0.15P (GPa), with Xj=j/(Fe+Mg+Al...

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Bibliographic Details
Published inChinese science bulletin Vol. 60; no. 1; pp. 116 - 121
Main Authors Wu, Chun-Ming, Chen, Hong-Xu
Format Journal Article
LanguageEnglish
Published Beijing Elsevier B.V 01.01.2015
Springer-Verlag
Science China Press
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ISSN1001-6538
2095-9273
1861-9541
2095-9281
DOI10.1007/s11434-014-0674-y

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Summary:In the present study, the Ti-in-biotite geother- mometer was revised using more than 300 natural rutile- or ilmenite-bearing metapelites collected worldwide. The formulation was empirically calibrated as ln[T(℃)]= 6.313 +0.22 41n(XTi ) -0.2881n(XFe ) -0. 4491n(XMg) + 0.15P (GPa), with Xj=j/(Fe+Mg+Al^Ⅵ+Ti) in biotite, assuming ferric iron content of 11.6 mol% of the total iron in biotite. This thermometer is consistent with the well-calibrated garnet-biotite thermometer within error of i50 ℃ for most of the calibrant samples and can successfully distin- guish systematic temperature changes of different meta- morphic zones in both prograde and inverted metamorphic terranes as well as thermal contact aureoles. Thus, the thermometer truthfully reflects real geologic conditions and can be applied to TiO2-saturated metapelites metamor- phosed at the crustal level within the calibration ranges (450-840 ℃, 0.1-1.9 GPa, XTi = 0.02-0.14 in biotite).
Bibliography:11-1785/N
Ti content ; Biotite ; Calibration -Geothermometer ; Application ; Error
In the present study, the Ti-in-biotite geother- mometer was revised using more than 300 natural rutile- or ilmenite-bearing metapelites collected worldwide. The formulation was empirically calibrated as ln[T(℃)]= 6.313 +0.22 41n(XTi ) -0.2881n(XFe ) -0. 4491n(XMg) + 0.15P (GPa), with Xj=j/(Fe+Mg+Al^Ⅵ+Ti) in biotite, assuming ferric iron content of 11.6 mol% of the total iron in biotite. This thermometer is consistent with the well-calibrated garnet-biotite thermometer within error of i50 ℃ for most of the calibrant samples and can successfully distin- guish systematic temperature changes of different meta- morphic zones in both prograde and inverted metamorphic terranes as well as thermal contact aureoles. Thus, the thermometer truthfully reflects real geologic conditions and can be applied to TiO2-saturated metapelites metamor- phosed at the crustal level within the calibration ranges (450-840 ℃, 0.1-1.9 GPa, XTi = 0.02-0.14 in biotite).
http://dx.doi.org/10.1007/s11434-014-0674-y
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ISSN:1001-6538
2095-9273
1861-9541
2095-9281
DOI:10.1007/s11434-014-0674-y