Article
Publicly Available
Simulation of the structure and stability of sphalerite (ZnS) surfaces
-
K. Wright
Published/Copyright:
November 13, 2015
Received: 1997-1-27
Accepted: 1997-9-6
Published Online: 2015-11-13
Published in Print: 1998-1-1
© 2015 by Walter de Gruyter Berlin/Boston
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Articles in the same Issue
- Calibration of excess thermodynamic properties and elastic constant variations associated with the α ↔ β phase transition in quartz
- Thermoelastic properties of MgSiO3 perovskite using the Debye approach
- An empirical model for the solubility of H2O in magmas to 3 kilobars
- The influence of water on the environment of transition metals in silicate glasses
- The reaction talc + forsterite = enstatite + H2O: New experimental results and petrological implications
- Hydrothermal synthesis of ammonium illite
- Equation of state of brucite: Single-crystal Brillouin spectroscopy study and polycrystalline pressure-volume-temperature measurement
- Single-crystal Raman spectroscopic study of dickite
- 29Si MAS NMR systematics of calcic and sodic-calcic amphiboles
- Substructure and superstructure of four-layer Ca-exchanged birnessite
- Silanol groups in minerals and inorganic compounds
- A systematic approach to general and structure-type formulas for minerals and other inorganic phases
- High form of pentlandite and its thermal stability
- Simulation of the structure and stability of sphalerite (ZnS) surfaces
- Aqueous Pb sorption by hydroxylapatite: Applications of atomic force microscopy to dissolution, nucleation, and growth studies
- Structural variations induced by thermal treatment in lead feldspar (PbAl2Si2O8)
- Ferri-clinoholmquistite, Li2(Fe2+,Mg)3 Fe3+2Si8O22 (OH)2, a new BLi clinoamphibole from the Pedriza Massif, Sierra de Guadarrama, Spanish Central System
- Bamfordite, Fe3+Mo2O6(OH)3·H2O, a new hydrated iron molybdenum oxyhydroxide from Queensland, Australia: Description and crystal chemistry
- Cordylite-(Ce): A crystal chemical investigation of material from four localities, including type material
