Corrigendum to “Simultaneous determination of melting phase relations of mantle peridotite and mid-ocean ridge basalt at the uppermost lower mantle conditions” [Phys. Earth Planet. Inter. 284 (2018) 36–50]. (Physics of the Earth and Planetary Interiors (2018) 284 (36–50), (S003192011730362X), (10.1016/j.pepi.2018.08.012))

Hideharu Kuwahara, Ryuichi Nomura, Ryoichi Nakada, Tetsuo Irifune

Research output: Contribution to journalComment/debatepeer-review

Abstract

The authors sincerely regret the lack of pressure and temperature conditions for Run No. OT2121B in Table 5 and the error of the unit of Y-axis in Fig. 11. Corrections are as follows: Pressure and temperature conditions for Run No. OT2121B in Table 5 are 27 GPa and 2673 K, respectively. The unit of Y-axis in Fig. 11 should be “g/cm3”, not “cm3/g”. We attached corrected Table 5 and Fig. 11. The authors would like to apologise for any inconvenience caused.

Original languageEnglish
Article number106473
JournalPhysics of the Earth and Planetary Interiors
Volume303
DOIs
Publication statusPublished - Jun 2020

ASJC Scopus subject areas

  • Astronomy and Astrophysics
  • Geophysics
  • Physics and Astronomy (miscellaneous)
  • Space and Planetary Science

Fingerprint Dive into the research topics of 'Corrigendum to “Simultaneous determination of melting phase relations of mantle peridotite and mid-ocean ridge basalt at the uppermost lower mantle conditions” [Phys. Earth Planet. Inter. 284 (2018) 36–50]. (Physics of the Earth and Planetary Interiors (2018) 284 (36–50), (S003192011730362X), (10.1016/j.pepi.2018.08.012))'. Together they form a unique fingerprint.

Cite this