The structure of denisovite, ideally K14Ca42Na6[Si60(O,OH)162]F16(O,OH)8*2H2O : An asbestiform, nano-crystalline, polytypic, disordered, 'very complex' mineral, studied by a synergetic, multi-disciplinary approach employing methods of electron crystallography and x-ray powder diffraction

Autor: Rozhdestvenskaya, I. V., Enrico Mugnaioli, Schowalter, M., Schmidt, M. U., Czank, M., Depmeier, W., Rosenauer, A.
Rok vydání: 2016
Zdroj: Università degli Studi di Siena-IRIS
Databáze: OpenAIRE