FORMATION OF CLAY MINERALS IN BASALTS.COLE WF; LANCUCKI CJ.sdIN: 25. INT. GEOL. CONGR. ABS.; SYDNEY; 1976; CANBERRA; PRINT. UNION OFFSET; DA. S.D.; VOL. 3; PP. 751Conference Paper

PRODUCTS FORMED IN AN AGED CONCRETE. THE OCCURRENCE OF OKENITE = LES PRODUITS FORMES DANS UN BETON VIEILLI. LA PRESENCE D'OKENITECOLE WF; LANCUCKI CJ.1983; CEM. CONCR. RES.; ISSN 0008-8846; USA; DA. 1983; VOL. 13; NO 5; PP. 611-618; BIBL. 9 REF.Article

HYDROGEN BONDING IN GYPSUMCOLE WF; LANCUCKI CJ.1973; NATURE PHYS. SCI.; G.B.; DA. 1973; VOL. 242; NO 120; PP. 104-105; BIBL. 3 REF.; 1 ILL.; 1 ANAL.Serial Issue

MONTMORILLONITE PSEUDOMORPHS AFTER AMPHIBOLE FROM MELBOURNE, AUSTRALIA.COLE WF; LANCUCKI CJ.1976; CLAYS CLAY MINER.; G.B.; DA. 1976; VOL. 24; NO 2; PP. 79-83; H.T. 1; BIBL. 16 REF.; 4 ILL.Article

HUNTITE FROM DEER PARK, VICTORIA, AUSTRALIA.COLE WF; LANCUCKI CJ.1975; AMER. MINERALOGIST; U.S.A.; 1975, VOL. 60, NUM. 0011-0012, P. 1130 A 1131Serial Issue

SYMMETRY OF SO₄ ION IN GYPSUMCOLE WF; LANCUCKI CJ.1972; NATURE PHYS. SCI.; G.B.; 1972, VOL. 268, NUM. 0084, P. 95 A 96Serial Issue

ON THE CHARACTERIZATION OF CERAMIC CLAYS.COLE WF; LANCUCKI CJ; POWELL DA et al.1971; CLAY MINER. BULL., G.B; GBR; 1971(7), VOL. 9, NUM. 0001, P. 35 A 46Miscellaneous