Articles | Volume 5, issue 1
Solid Earth, 5, 509–509, 2014
https://doi.org/10.5194/se-5-509-2014
Solid Earth, 5, 509–509, 2014
https://doi.org/10.5194/se-5-509-2014

  11 Jun 2014

11 Jun 2014

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. Satsukawa1,2,*, B. Ildefonse2, D. Mainprice2, L. F. G. Morales3, K. Michibayashi1,4, and F. Barou2 T. Satsukawa et al.
  • 1Graduate School of Science and Technology, Shizuoka University, Ohya 836, Shizuoka 422-8529, Japan
  • 2Géosciences Montpellier, Université Montpellier 2 and CNRS, CC 060, 34095 Montpellier cedex 5, France
  • 3Helmholtz Zentrum Potsdam, Deutsches GeoForschungsZentrum (GFZ), Telegrafenberg, 14473 Potsdam, Germany
  • 4Institute of Geosciences, Shizuoka University, Ohya 836, Shizuoka 422-8529, Japan
  • *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