INFLUENCE OF CAPILLARY GROUND MOISTURE ON EOLIAN ACCUMULATION OF LOESS.CEGLA J.1969; BULL. ACAD. POL. SCI., SER. SCI. GEOL. GEOGR; POL; 1969, VOL. 17, NUM. 0001, P. 25 A 27Miscellaneous

DEPOSITS OF FOSSIL CLOSED DEPRESSIONS AS INDICATORS OF GROUND MORAINE DEGRADATION IN AREAS OF OLDER GLACIATIONS.CEGLA J; KLIMEK K.1968; PRZEGL. GEOGR.; POL; 1968, VOL. 40, NUM. 0002, P. 333 A 342Miscellaneous

KINK FOLDING IN UNCONSOLIDATED QUATERNARY SEDIMENTS = PLIS EN CHEVRON DANS DES SEDIMENTS MEUBLES QUATERNAIRESBRODZIKOWSKI K; CEGLA J.1981; ROCZ. POL. TOW. GEOL.; ISSN 0079-3663; POL; DA. 1981; VOL. 51; NO 1-2; PP. 63-82; H.T. 4; ABS. POL; BIBL. 1 P.; 4 PLANCH. ; ESQUISSE/ILL./PL.Article

EXPERIMENTS ON FEATHER FRACTURE IN SEDIMENTS.CEGLA J; DZULYNSKI S.1967; ROCZ. POLSK. TOW. GEOL; POL; 1967, VOL. 37, NUM. 0004, P. 489 A 497Miscellaneous

ON THE DEFORMATIONAL STRUCTURES IN SYSTEMS WITH REVERSED DENSITY GRADIENTS.ANKETELL JM; CEGLA J; DZULYNSKI S et al.1970; ROCZ. POLSK. TOW. GEOL; POL; 1970, VOL. 40, NUM. 0001, P. 3 A 30Miscellaneous

MICROTEXTURES OF PARTICLES FROM SOME EUROPEAN LOESS DEPOSITS.CEGLA J; BUCKLEY T; SMALLEY IJ et al.1971; SEDIMENTOLOGY; NLD; 1971, VOL. 17, NUM. 0001-0002, P. 129 A 134Miscellaneous

UNCONFORMABLE SURFACES FORMED IN THE ABSENCE OF CURRENT EROSION.ANKETELL JM; CEGLA J; DZULYNSKI S et al.1969; GEOL., ROMANA.; 1969, VOL. 8, P. 41 A 46Miscellaneous

Penecontemporaneous deformation structures formed within some fine-grained Quaternary sediments (Dalkowskie Hills, SW Poland) = Structures de déformation syngénétique formées dans des sédiments fins Quaternaires (Monts Dalkowskie, Pologne Sud Ouest)BRODZIKOWSKI, K; CEGLA, J; KIDA, J et al.Bulletin of the Polish Academy of Sciences. Earth sciences. 1987, Vol 35, Num 3, pp 221-234, issn 0239-7277Article