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Acta Crystallographica. Section A, Foundations and Advances|April 28, 2017
Resonant and non-resonant magnetic scatterings with circularly polarized X-rays: magnetic scattering factor and electron density of gadolinium iron garnetYo Sasaki, Maki Okube, Satoshi SasakiJournal of Synchrotron Radiation|August 18, 2012
Residual-density mapping and site-selective determination of anomalous scattering factors to examine the origin of the Fe K pre-edge peak of magnetiteMaki Okube, Takuya Yasue, Satoshi SasakiJournal of Synchrotron Radiation|October 15, 2011
Titanium local structure in tektite probed by X-ray absorption fine structure spectroscopyLing Wang, Akira Yoshiasa, Maki Okube, et al.Acta Crystallographica Section B, Structural Science, Crystal Engineering and Materials|November 21, 2013
Single-crystal metastable high-temperature C2/c clinoenstatite quenched rapidly from high temperature and high pressureAkira Yoshiasa, Akihiko Nakatsuka, Maki Okube, et al.Acta Crystallographica Section B, Structural Science, Crystal Engineering and Materials|June 1, 2016
High-temperature single-crystal X-ray diffraction study of tetragonal and cubic perovskite-type PbTiO3 phasesAkira Yoshiasa, Tomotaka Nakatani, Akihiko Nakatsuka, et al.Journal of Synchrotron Radiation|June 15, 2013
Temperature dependence of pre-edge features in Ti K-edge XANES spectra for ATiO₃ (A = Ca and Sr), A₂TiO₄ (A = Mg and Fe), TiO₂ rutile and TiO₂ anataseTatsuya Hiratoko, Akira Yoshiasa, Tomotaka Nakatani, et al.Langmuir : the ACS Journal of Surfaces and Colloids|July 3, 2013
Surface stability of Pt3Ni nanoparticulate alloy electrocatalysts in hydrogen adsorptionHana Hoffmannová, Maki Okube, Valery Petrykin, et al.Acta Crystallographica Section B, Structural Science, Crystal Engineering and Materials|February 3, 2016
Variable-temperature single-crystal X-ray diffraction study of tetragonal and cubic perovskite-type barium titanate phasesTomotaka Nakatani, Akira Yoshiasa, Akihiko Nakatsuka, et al.Journal of Synchrotron Radiation|November 9, 2018
Site occupancy of Fe<sup>2+</sup>, Fe<sup>3+</sup> and Ti<sup>4+</sup> in titanomagnetite determined by valence-difference contrast in synchrotron X-ray resonant scatteringMaki Okube, Taro Oshiumi, Toshiro Nagase, et al.Pageof 1