In the original article, there was a mistype in Equation (2) used to simulate the experimental C-O contribution on g(r) (Figure 3B).
A correction has been made to Section 2, Density Measurements, equation 2:
where cC and cO are the atomic proportions of carbon and oxygen, KC and KO are defined as the average effective atomic number over the experimental q-range (Eggert et al., 2002) and calculated using form factors from Hajdu (1972). Other parameters are as defined in the article.
The authors apologize for this error and state that this does not change the scientific conclusions of the article in any way. The original article has been updated.
References
1
EggertJ. H.WeckG.LoubeyreP.MezouarM. (2002). Quantitative structure factor and density measurements of high-pressure in diamond anvil cells by x-ray diffraction: Argon and water. Phys. Rev. B65:174105. 10.1103/PhysRevB.65.174105
2
HajduF. (1972). Revised parameters of the analytic fits for coherent and incoherent scattered X-ray intensities of the first 36 atoms. Acta Cryst. A28, 250–252.
Summary
Keywords
carbonate melts, high pressure, x-ray diffraction, Raman, x-ray Raman, polymerization, deep mantle
Citation
Sanloup C, Hudspeth JM, Afonina V, Cochain B, Konôpková Z, Lelong G, Cormier L and Cavallari C (2019) Corrigendum: Polymerized 4-Fold Coordinated Carbonate Melts in the Deep Mantle. Front. Earth Sci. 7:155. doi: 10.3389/feart.2019.00155
Received
20 May 2019
Accepted
03 June 2019
Published
25 June 2019
Volume
7 - 2019
Edited and reviewed by
Dan J. Bower, University of Bern, Switzerland
Updates
Copyright
© 2019 Sanloup, Hudspeth, Afonina, Cochain, Konôpková, Lelong, Cormier and Cavallari.
This is an open-access article distributed under the terms of the Creative Commons Attribution License (CC BY). The use, distribution or reproduction in other forums is permitted, provided the original author(s) and the copyright owner(s) are credited and that the original publication in this journal is cited, in accordance with accepted academic practice. No use, distribution or reproduction is permitted which does not comply with these terms.
*Correspondence: Chrystèle Sanloup chrystele.sanloup@sorbonne-universite.fr
This article was submitted to Earth and Planetary Materials, a section of the journal Frontiers in Earth Science
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