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The Chrysoberyl- and Phosphate-Bearing Albite Pegmatite of Malga Garbella, Val Di Rabbi, Trento Province, Italy
Plumbopharmacosiderite, Pb 0.5 Fe 3+ 4 (AsO 4 ) 3 (OH) 4 ·5H 2 O, a New Mineral Species from the Monte FalÒ Pb-zn Mine Near the Village of Coiromonte in the Armeno Municipality, Novara Province, Italy
Arrojadite-(bana), BaNa 3 (Na,Ca)Fe 2+ 13 Al(PO 4 ) 11 (PO 3 OH)(OH) 2 , a New Phosphate Mineral from the Luna Albite Pegmatite, Dorio Commune, Lecco Province, Italy
On the Crystal-chemistry of Bjarebyite, BaMn 2+ 2 Al 2 (PO 4 ) 3 (OH) 3 , from the Palermo #1 Pegmatite, Grafton County, New Hampshire, Usa
High-temperature and high-pressure behavior of carbonates in the ternary diagram CaCO 3 -MgCO 3 -FeCO 3
Green andradite stones: gemmological and mineralogical characterisation
Elastic behavior and phase stability of pollucite, a potential host for nuclear waste
High-temperature treatment, hydrogen behaviour and cation partitioning of a Fe–Ti bearing volcanic phlogopite by in situ neutron powder diffraction and FTIR spectroscopy
Leucite at high pressure: Elastic behavior, phase stability, and petrological implications
P - V equation of State, thermal expansion, and P - T stability of synthetic zincochromite (ZnCr 2 O 4 spinel)
High-pressure synchrotron X-ray diffraction study of spessartine and uvarovite: A comparison between different equation of state models
Equation of state and compressibility of phlogopite by in-situ high-pressure X-ray powder diffraction
Deprotonation and order-disorder reactions as a function of temperature in a phengite 3 T (Cima Pal, western Alps) by neutron diffraction and Mössbauer spectroscopy
Synthetic MgAl 2 O 4 (spinel) at high-pressure conditions (0.0001–30 GPa): A synchrotron X-ray powder diffraction study
Neutron powder diffraction and Rietveld analysis; applications to crystal-chemical studies of minerals at non-ambient conditions
Behavior of Micas at High-Pressure and High-Temperature
Abstract Symmetry plays a crucial role in most formalisms of physics, and provides an elegant way to get a variety of results starting from a fully general mathematical basis. Such a principle of course applies to the realm of vibrational modes too. The structural symmetry of crystals, due to the ordered arrangement of atoms, causes particular properties of the vibrational modes, in terms of both the eigenvectors and eigenvalues of the dynamic matrix. The mathematical link that relates a space group, describing a geometrical symmetry, to the dynamics of a crystal, i.e. to a physical phenomenon, is provided by the theory of representations. Vibrational spectroscopy involved with lattice dynamics heavily benefits from the inferences attainable by combining the dynamics of the atomic motion in crystals with symmetry. Such a synergy has led to results of great practical use: selection rules, for instance, are a well-known powerful tool in interpreting experimental spectroscopic data. This presentation aims at the following objectives: (1) illustrating the basic mathematical notions which underlie a rigorous approach to the relationships between lattice dynamics and symmetry, through the concept of group representations; (2) showing how the dynamic equations can be re-cast into a form leading straight to group representations; (3) providing the main links between lattice dynamics and crystal spectroscopy, in terms of theoretical inferences stemming from a combination of symmetry and dynamics, and experimental issues. The points above have been developed with a particular care to the formal aspects, for three reasons: