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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Published in | Chinese science bulletin Vol. 60; no. 1; pp. 116 - 121 |
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Main Authors | , |
Format | Journal Article |
Language | English |
Published |
Beijing
Elsevier B.V
01.01.2015
Springer-Verlag Science China Press |
Subjects | |
Online Access | Get full text |
ISSN | 1001-6538 2095-9273 1861-9541 2095-9281 |
DOI | 10.1007/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). |
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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 ObjectType-Article-1 SourceType-Scholarly Journals-1 ObjectType-Feature-2 content type line 23 |
ISSN: | 1001-6538 2095-9273 1861-9541 2095-9281 |
DOI: | 10.1007/s11434-014-0674-y |