COMPARISON OF ORIENTATIONS OF OH-BONDS IN LAYER SILICATES BY DIFFRACTION METHODS AND ELECTROSTATIC CALCULATIONS = COMPARAISON DES ORIENTATIONS DES LIAISONS OH DANS LES PHYLLOSILICATES PAR DES METHODES DE DIFFRACTION ET DES CALCULS ELECTROSTATIQUESBOOKIN AS; DRITS VA; ROZDESTVENSKAYA IV et al.1982; CLAYS CLAY MINER.; ISSN 0009-8604; USA; DA. 1982-12; VOL. 30; NO 6; PP. 409-414; ABS. RUS/UND/UND/FRE; BIBL. 28 REF.; 2 TAB. ; ILL.Article

Clay minerals from ancient deposits of Eastern SiberiaFAIER, M.M; TSIPURSKY, S.I.Geologica. Conference on clay mineralogy and petrology. 1993, pp 157-163Conference Paper

USE OF DIFFRACTION AND MOESSBAUER METHODS FOR THE STRUCTURAL AND CRYSTALLOCHEMICAL CHARACTERIZATION OF NONTRONITES = UTILISATION DES METHODES DE DIFFRACTION ET MOESSBAUER POUR LA CARACTERISATION STRUCTURALE ET CRISTALLOCHIMIQUE DES NONTRONITESBESSON G; BOOKIN AS; DAINYAK LG et al.1983; JOURNAL OF APPLIED CRYSTALLOGRAPHY; ISSN 0021-8898; DNK; DA. 1983; VOL. 16; NO 4; PP. 374-383; BIBL. 39 REF.; ILL./TABL.Article

Structure of magnesian calcite from sea urchinsTSIPURSKY, S. J; BUSECK, P. R.The American mineralogist. 1993, Vol 78, Num 7-8, pp 775-781, issn 0003-004XArticle

The distribution of octahedral cations in the 2:1 layers of dioctahedral smectites studies by oblique-texture electron diffraction = Répartition des cations octaédriques dans les couches 2:1 des smectites dioctaédriques par diffraction électronique de texture obliqueTSIPURSKY, S. I; DRITS, V. A.Clay minerals. 1984, Vol 19, Num 2, pp 177-193, issn 0009-8558Article

Globular and tabular Al-glauconite, the Lower Riphean, Northern SiberiaIVANOVSKAYA, T.A; GEPTNER, A; TSIPURSKY, S.O et al.International geological congress. 1992, p.712Conference Paper

Photodynamic Therapy of Choroidal Hemangioma in Sturge-Weber Syndrome, with a Review of Treatments for Diffuse and Circumscribed Choroidal HemangiomasTSIPURSKY, Michael S; GOLCHET, Pamela R; JAMPOL, Lee M et al.Survey of ophthalmology. 2011, Vol 56, Num 1, pp 68-85, issn 0039-6257, 18 p.Article

Dehydroxylation of Fe3+, Mg-rich dioctahedral micas : (II) cation migrationMULLER, F; DRITS, V. A; TSIPURSKY, S. I et al.Clay minerals. 2000, Vol 35, Num 3, pp 505-514, issn 0009-8558Article

Structural transformations of Fe³⁺-containing 2:1 dioctahedral phyllosilicates in the course of dehydration = Transformation de structure des phyllosilicates dioctaédriques en Fe³⁺ 2 à 1 pendant la déshydratationTSIPURSKY, S. I; KAMENEVA, M. YU; DRITS, V. A et al.Euroclay meeting. 1985, pp 569-577Conference Paper

Measurement of fundamental illite particle thicknesses by X-ray diffraction using PVP-10 intercalationEBERL, D. D; NÜESCH, R; SUCHA, V et al.Clays and clay minerals. 1998, Vol 46, Num 1, pp 89-97, issn 0009-8604Article

Structural transformations of Fe³⁺-containing 2:1 dioctahedral phyllosilicates in the course of dehydration = Les transformations structurales des phyllosilicates dioctaédriques 2:1 contenant Fe³⁺ au cours de la déshydratationTSIPURSKY, S. I; KAMENEVA, M. YU; DRITS, V. A et al.European Clays groups. Meeting. 5. 1985, pp 569-577Conference Paper

Origins of fullerenes in rocks. Authors' replyEBBESEN, T. W; HIURA, H; HEDENQUIST, J. W et al.Science (Washington, D.C.). 1995, Vol 268, Num 5217, pp 1634-1635, issn 0036-8075Article