Titlebook: From Differential Geometry to Non-commutative Geometry and Topology; Neculai S. Teleman Book 2019 Springer Nature Switzerland AG 2019 inde

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J. Váradye,Co,Ti). equilibrium phases, are presented. Their structure is explained with a model ground on the R.T. formula (R=rare-earth, s=vacancy rate, T=transition metal) where s Sm atoms are statistically substituted by s transition metal pairs. The Rietveld analysis (RA) provides the stoichiometry of th

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tions of solids at high temperature and pressure indicate that there is a close relation be- tween the electrical conductivity of rocks and temperature. Therefore, measurements of deep conductivity can provide knowledge of the present state and temperature of the Earth‘s crust and upper mantle matte

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