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Erratum to “Empirical garnet–muscovite geothermometry in metapelites” [Lithos 62 (2002) 1–13]
Lithos 66 (2003) 291 www.elsevier.com/locate/lithos
Erratum
Erratum to ‘‘Empirical garnet–muscovite geothermometry in metapelites’’ $ [Lithos 62 (2002) 1–13] Chun-Ming Wu a,*, Xin-She Wang b, Chong-Hui Yang b, Yuan-Sheng Geng b, Fu-Lai Liu b a
Department of Earth Sciences, The Graduate School, Chinese Academy of Sciences, P.O. Box 3908, Beijing 100039, China b Institute of Geology, Chinese Academy of Geological Sciences, 26 Baiwanzhuang Street, Beijing 100037, China Received 13 September 2002
The molar fractions of the Fe2 +, Mg and AlVI components in the muscovite solid solution are actually defined mus mus mus as XFe = Fe2 +/(Fe2 + + Mg + AlVI), XMg = Mg/(Fe2 + + Mg + AlVI), and XA1 = AlVI/(Fe2 + + Mg + AlVI), respectively. The symbol ‘‘ + ’’ is missing in the original article, Section 2.2. However, this does not have any effect on the calibration. A similar mistake is made for the ferric iron content in muscovite, Section 3, 7th paragraph. This must be Fe3+/ (Fe2++Fe3+).
$
PII of original article S0024-4937(02)00096-8. * Corresponding author. Tel.: +86-10-68229894; fax: +86-10-68226012. E-mail address: [email protected] (C.-M. Wu).
0024-4937/02/$ - see front matter D 2002 Elsevier Science B.V. All rights reserved. PII: S 0 0 2 4 - 4 9 3 7 ( 0 2 ) 0 0 2 5 1 - 7
Erratum
Erratum to ‘‘Empirical garnet–muscovite geothermometry in metapelites’’ $ [Lithos 62 (2002) 1–13] Chun-Ming Wu a,*, Xin-She Wang b, Chong-Hui Yang b, Yuan-Sheng Geng b, Fu-Lai Liu b a
Department of Earth Sciences, The Graduate School, Chinese Academy of Sciences, P.O. Box 3908, Beijing 100039, China b Institute of Geology, Chinese Academy of Geological Sciences, 26 Baiwanzhuang Street, Beijing 100037, China Received 13 September 2002
The molar fractions of the Fe2 +, Mg and AlVI components in the muscovite solid solution are actually defined mus mus mus as XFe = Fe2 +/(Fe2 + + Mg + AlVI), XMg = Mg/(Fe2 + + Mg + AlVI), and XA1 = AlVI/(Fe2 + + Mg + AlVI), respectively. The symbol ‘‘ + ’’ is missing in the original article, Section 2.2. However, this does not have any effect on the calibration. A similar mistake is made for the ferric iron content in muscovite, Section 3, 7th paragraph. This must be Fe3+/ (Fe2++Fe3+).
$
PII of original article S0024-4937(02)00096-8. * Corresponding author. Tel.: +86-10-68229894; fax: +86-10-68226012. E-mail address: [email protected] (C.-M. Wu).
0024-4937/02/$ - see front matter D 2002 Elsevier Science B.V. All rights reserved. PII: S 0 0 2 4 - 4 9 3 7 ( 0 2 ) 0 0 2 5 1 - 7