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1. The crystal structure of Pb$_{10}$(PO$_4$)$_6$O revisited: the evidence of superstructure

10. On the Origin of Crystallinity: a Lower Bound for the Regularity Radius of Delone Sets

11. Functionality in metal–organic framework minerals: proton conductivity, stability and potential for polymorphism

12. Polymorphism and topological features of compounds with the general formula [formula omitted] {[formula omitted] [BP2O8(OH)]} (where x = 0, 1): Synthesis and structure refinement of Rb{V[BP2O8(OH)]}, analysis of the ion-migration paths, and comparative crystal chemistry of vanadium borophosphates

13. On the Polymorphism of Cu 2 V 2 O 7 : Synthesis and Crystal Structure of δ-Cu 2 V 2 O 7 , a New Polymorph.

14. The Crystal Chemistry of Boussingaultite, (NH 4) 2 Mg(SO 4) 2 ·6H 2 O, and Its Derivatives in a Wide Temperature Range.

15. 'Rhythmite', Ca 29 (SiO 4) 8 Cl 26 , an Anthropogenic Phase from the Chelyabinsk Coal Basin (Ural, Russia) with a Complex Modular Structure Related to α-Ca 3 SiO 4 Cl 2 ('Albovite'): Crystal Structure, Raman Spectra, and Thermal Expansion.

19. Nefedovite, Na5Ca4(PO4)4F: thermal evolution, phase transition and crystal structure refinement.

23. The AM-4 Family of Layered Titanosilicates: Single-Crystal-to-Single-Crystal Transformation, Synthesis and Ionic Conductivity

29. Arctic Mineral Resources : Science and Technology

34. Zn(NH3)2Cl2, a Mineral-like Anthropogenic Phase with Ammine Complexes from the Burned Dumps of the Chelyabinsk Coal Basin, South Urals, Russia: Crystal Structure, Spectroscopy and Thermal Evolution

36. On the Attributes of Mineral Paragenetic Modes

39. Insights into crystal chemistry of the vesuvianite-group: manaevite-(Ce), a new mineral with complex mechanisms of its hydration

41. The AM-4 Family of Layered Titanosilicates: Single-Crystal-to-Single-Crystal Transformation, Synthesis and Ionic Conductivity.

45. Ca3SiO4Cl2—An Anthropogenic Phase from Burnt Mine Dumps of the Chelyabinsk Coal Basin: Crystal Structure Refinement, Spectroscopic Study and Thermal Evolution

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