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NARROW
GeoRef Subject
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all geography including DSDP/ODP Sites and Legs
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Commonwealth of Independent States
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Russian Federation
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Murmansk Russian Federation
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Khibiny Mountains (2)
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Kola Peninsula (2)
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Lovozero Massif (1)
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Europe
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Murmansk Russian Federation
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Khibiny Mountains (2)
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Kola Peninsula (2)
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Lovozero Massif (1)
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commodities
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phosphate deposits (1)
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elements, isotopes
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metals
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rare earths
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cerium (1)
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titanium (1)
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vanadium (1)
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igneous rocks
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igneous rocks
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feldspathoid rocks (1)
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plutonic rocks
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urtite (1)
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minerals
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halides
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fluorides (1)
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minerals (1)
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oxides (1)
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silicates
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chain silicates
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amphibole group
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clinoamphibole
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arfvedsonite (1)
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-
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astrophyllite (1)
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pyroxene group
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clinopyroxene
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aegirine (1)
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framework silicates
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feldspar group
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alkali feldspar
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microcline (1)
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plagioclase
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albite (1)
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-
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sodalite group
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sodalite (1)
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orthosilicates
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nesosilicates
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garnet group
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schorlomite (1)
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vanadates (1)
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Primary terms
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crystal chemistry (3)
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crystal structure (4)
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Europe
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Murmansk Russian Federation
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Khibiny Mountains (2)
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Kola Peninsula (2)
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Lovozero Massif (1)
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-
-
igneous rocks
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feldspathoid rocks (1)
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plutonic rocks
-
urtite (1)
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-
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metals
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rare earths
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cerium (1)
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-
titanium (1)
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vanadium (1)
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minerals (1)
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phosphate deposits (1)
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paranatisite
RECONSIDERATION OF THE CRYSTAL STRUCTURE OF PARANATISITE AND THE CRYSTAL CHEMISTRY OF [ [6] M 2 [4] T 2 ϕ 12 ] SHEETS
MISCELLANEOUS INFORMATION FOR PARANATISITE
FINAL ATOM PARAMETERS FOR PARANATISITE
BOND-VALENCE TABLE FOR PARANATISITE*
SELECTED INTERATOMIC DISTANCES (Å) FOR PARANATISITE
CHEMICAL COMPOSITION (wt. %)* AND UNIT FORMULA ( apfu ) FOR PARANATISITE
Three (100) sheets in the crystal structure of paranatisite: (a) a sheet of...
Four sheets [(010) (a)–(b); (001) (c)–(d)] in the crystal structure of para...
Empirical Electronic Polarizabilities for Use in Refractive Index Measurements III. Structures with Short [5] Ti–O and Vanadyl Bonds
New Mineral Names
Khibiny.: By V.N. Yakovenchuk, G.Yu. Ivanyuk, Ya.A. Pakhomovsky and Yu.P. Men’shikov. Edited by F. Wall. Laplandia Minerals, Apatity, Russia. 2005. 472 pages, hardcover (with dust jacket). ISBN 5–900395–48–0. CDN$220 plus shipping in Canada. Available from the Ed Leith Cretaceous Menagerie, Department of Geological Sciences, University of Manitoba, Winnipeg, Manitoba R3T 2N2 (contact: Sharon Kirsch, [email protected] ). US$179 plus $15 shipping and handling in the United States. Also available from Excalibur Mineral Corp., 1000 North Division Street, Peekskill, N.Y. 10566, U.S.A. (e-mail: [email protected] ).
Polezhaevaite-(Ce), NaSrCeF 6 , a new mineral from the Khibiny massif (Kola Peninsula, Russia)
CNMNC guidelines for the nomenclature of polymorphs and polysomes
Nomenclature of the garnet supergroup
Abstract Layered materials have much potential for applications as ion exchangers, gas sorbents and catalysts. Layered titanosilicates are of particular interest because on the one hand they possess large amounts of titanium and, on the other, they exhibit a wide variety of crystal structures. This chapter summarizes the main structural features in the family of heteropolyhedral layered titanosilicates and presents briefly the synthesis and application studies on some of these materials. The most representative members have been described in terms of the construction of each individual sheet from the individual building blocks. In general, the structures of these materials encompass single layers, micatype layers (heterophyllosilicates) and perforated ‘microporous’ layers. The most commonly used synthesis process and potential applications of some layered titanosilicates are reviewed briefly. The materials with perforated ‘microporous’ sheets are particularly interesting because they can be considered as microporous materials with one of the dimensions in the nano size regime, meaning the materials have fast transport properties. Most of the structures reviewed are known only as minerals. Both the synthesis and potential applications of layered titanosilicates have been significantly underexplored and still present a great number of challenges and opportunities for future research.