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We use a combination of variable-temperature high-resolution synchrotron X-ray powder diffraction measurements and Monte Carlo simulations to characterize the evolution of two different types of ferroic multipolar order in a series of cyanoelpasolite
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::659a8ae1e1965ebff69fdc5eac979e3f
