Corrigendum to "A database of plagioclase crystal preferred orientations (CPO) and microstructures - implications for CPO origin, strength, symmetry and seismic anisotropy in gabbroic rocks (vol 4, pg 511, 2013)"

Takako Satsukawa, Benoit Ildefonse, David Mainprice, Luis Morales, K.

Michibayashi, Fabrice Barou

► To cite this version:

Takako Satsukawa, Benoit Ildefonse, David Mainprice, Luis Morales, K. Michibayashi, et al. Corrigendum to "A database of plagioclase crystal preferred orientations (CPO) and microstructures - implications for CPO origin, strength, symmetry and seismic anisotropy in gabbroic rocks (vol 4, pg 511, 2013)". Solid Earth, 2014, 5 (1), pp.509. 10.5194/se-5-509-2014. hal-01115507

HAL Id: hal-01115507

https://hal.science/hal-01115507

Submitted on 6 Sep 2020

HAL is a multi-disciplinary open access
archive for the deposit and dissemination of sci-
entific research documents, whether they are pub-
lished or not. The documents may come from
teaching and research institutions in France or
abroad, or from public or private research centers.

L'archive ouverte pluridisciplinaire HAL, est
destinée au dépôt et à la diffusion de documents
scientifiques de niveau recherche, publiés ou non,
émanant des établissements d'enseignement et de
recherche français ou étrangers, des laboratoires
publics ou privés.

<figure><img src="image_1.png" /></figure>

Distributed under a Creative Commons Attribution 4.0 International License
<figure><img src="image_2.png" /></figure>

<figure><img src="image_3.png" /></figure>

Corrigendum to

“A database of plagioclase crystal preferred orientations (CPO) and microstructures – implications for CPO origin, strength, symmetry and seismic anisotropy in gabbroic rocks” published in Solid Earth, 4, 511–542, 2013

T. Satsukawa<fnref n="1" />,<fnref n="2" />*, B. Ildefonse<fnref n="2" />, D. Mainprice<fnref n="2" />, L. F. G. Morales<fnref n="3" />, K. Michibayashi<fnref n="1" />,<fnref n="4" />, and F. Barou<fnref n="2" />

Correspondence to: T. Satsukawa (takako.satsukawa@mq.edu.au)

In the paper “A database of plagioclase crystal preferred orientations (CPO) and microstructures – implications for CPO origin, strength, symmetry and seismic anisotropy in gabbroic rocks” by T. Satsukawa et al. (Solid Earth, 4, 511–542, doi:10.5194/se-4-511-2013, 2013) an error occured in the second paragraph of Sect. 5.7. The correct paragraph should be as follows:

In the present study, there is a clear variation of the (010) and [100] pole figures from point maxima to girdle distributions, with associated changes in the (001) pole figures. We introduce the BA-index (similar to the LS index used Ulrich and Mainprice (2005) to described variations between the symmetry of (010) and [001] pole figures in omphacite) to characterize the symmetry variation of the (010) and [100] pole figures, which is defined as $1/2[2 - P_{(010)}/(G_{(010)} + P_{(010)}) - G_{[100]}/(G_{[100]} + P_{[100]})]$. P and G are defined in Sect. 3.2 above.

<footnote n="1">¹Graduate School of Science and Technology, Shizuoka University, Ohya 836, Shizuoka 422-8529, Japan</footnote>

<footnote n="2">²Géosciences Montpellier, Université Montpellier 2 and CNRS, CC 060, 34095 Montpellier cedex 5, France</footnote>

<footnote n="3">³Helmholtz Zentrum Potsdam, Deutsches GeoForschungsZentrum (GFZ), Telegrafenberg, 14473 Potsdam, Germany</footnote>

<footnote n="4">⁴Institute of Geosciences, Shizuoka University, Ohya 836, Shizuoka 422-8529, Japan</footnote>

<footnote>*present address: ARC Center of Excellence for Core to Crust Fluid Systems (CCFS) and GEMOC National Key Centre, Department of Earth and Planetary Sciences, Macquarie University, Sydney, NSW 2109, Australia</footnote>