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Erratum to “Lowermost mantle anisotropy beneath the Pacific: Imaging the source of the Hawaiian plume”
Earth and Planetary Science Letters 195 (2002) 299^300
Erratum
www.elsevier.com/locate/epsl
Erratum to ``Lowermost mantle anisotropy beneath the Paci¢c: Imaging the source of the Hawaiian plume'' [Earth Planet. Sci. Lett. 190 (2001) 167^180]C Matthew J. Fouch a; *, Karen M. Fischer b , Michael E. Wysession c a
Department of Terrestrial Magnetism, Carnegie Institution of Washington, Washington, DC 20015, USA b Department of Geological Sciences, Brown University, Providence, RI 02912, USA c Department of Earth and Planetary Sciences, Washington University, St. Louis, MO 63130, USA
In the above article there was an error in Fig. 6B. Fig. 6 is therefore published below again. The publishers would like to apologize for any inconvenience caused by this error.
C
PII of original article S0012-821X(01)00380-6.
* Corresponding author. Present address: Department of Geological Sciences, Arizona State University, Tempe, AZ 85287, USA. Tel.: +1-480-965-9292; Fax: +1-480-965-8102. E-mail address: [email protected] (M.J. Fouch). 0012-821X / 02 / $ ^ see front matter ß 2002 Elsevier Science B.V. All rights reserved. PII: S 0 0 1 2 - 8 2 1 X ( 0 1 ) 0 0 5 7 0 - 2
EPSL 6068 11-2-02 Cyaan Magenta Geel Zwart
300
M.J. Fouch et al. / Earth and Planetary Science Letters 195 (2002) 299^300
Fig. 6. (A) Lowermost mantle ray coverage for the central Paci¢c. Rays were traced assuming the M1 velocity model of [5]. All rays sample the upper and central regions of DQ, but distant phases also sample the CMB. (B) Cross-sectional view of anisotropy along line in Fig. 5. Of primary interest is a lateral decrease in strength from NW to SE in the middle of DQ, and a laterally varying region of strong anisotropy at the top of DQ £anking the Hawaiian hotspot.
EPSL 6068 11-2-02 Cyaan Magenta Geel Zwart
Erratum
www.elsevier.com/locate/epsl
Erratum to ``Lowermost mantle anisotropy beneath the Paci¢c: Imaging the source of the Hawaiian plume'' [Earth Planet. Sci. Lett. 190 (2001) 167^180]C Matthew J. Fouch a; *, Karen M. Fischer b , Michael E. Wysession c a
Department of Terrestrial Magnetism, Carnegie Institution of Washington, Washington, DC 20015, USA b Department of Geological Sciences, Brown University, Providence, RI 02912, USA c Department of Earth and Planetary Sciences, Washington University, St. Louis, MO 63130, USA
In the above article there was an error in Fig. 6B. Fig. 6 is therefore published below again. The publishers would like to apologize for any inconvenience caused by this error.
C
PII of original article S0012-821X(01)00380-6.
* Corresponding author. Present address: Department of Geological Sciences, Arizona State University, Tempe, AZ 85287, USA. Tel.: +1-480-965-9292; Fax: +1-480-965-8102. E-mail address: [email protected] (M.J. Fouch). 0012-821X / 02 / $ ^ see front matter ß 2002 Elsevier Science B.V. All rights reserved. PII: S 0 0 1 2 - 8 2 1 X ( 0 1 ) 0 0 5 7 0 - 2
EPSL 6068 11-2-02 Cyaan Magenta Geel Zwart
300
M.J. Fouch et al. / Earth and Planetary Science Letters 195 (2002) 299^300
Fig. 6. (A) Lowermost mantle ray coverage for the central Paci¢c. Rays were traced assuming the M1 velocity model of [5]. All rays sample the upper and central regions of DQ, but distant phases also sample the CMB. (B) Cross-sectional view of anisotropy along line in Fig. 5. Of primary interest is a lateral decrease in strength from NW to SE in the middle of DQ, and a laterally varying region of strong anisotropy at the top of DQ £anking the Hawaiian hotspot.
EPSL 6068 11-2-02 Cyaan Magenta Geel Zwart