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MATHEMATICAL MODELING OF SEDIMENT ACCUMULATION IN PROGRADING DELTAIC SYSTEMS.HOROWITZ DH.1976; IN: QUANT. TECH. ANAL. SEDIMENTS. PROC. INT. SYMP. IX INT. SEDIMENTOL. CONGR.; NICE; 1975; OXFORD; PERGAMON; DA. 1976; PP. 105-119; BIBL. 9 REF.; 8 ILL.Conference Paper

DIAGENETIC SIGNIFICANCE OF COLOR BOUNDARY BETWEEN JUNIATA AND BALD EAGLE FORMATIONS, PENNSYLVANIA.HOROWITZ DH.1971; J. SEDIMENT. PETROL.; USA; 1971, VOL. 41, NUM. 0004, P. 1134 A 1136Miscellaneous

DIAGENETIC REDUCTION AND ALTERATION OF THE UPPER ORDOVICIAN OSWEGO FORMATION IN THE CENTRAL APPALACHIAN MOUNTAINS (ABSTRACT).HOROWITZ DH.1969; GEOL. SOC. AMER., ABSTR. PROGRAMS; USA; 1969(11), NUM. 007Miscellaneous

EVIDENCE FOR DELTAIC ORIGIN OF AN UPPER ORDOVICIAN SEQUENCE IN THE CENTRAL APPALACHIANS.HOROWITZ DH.1966; DELTAS.IN.THEIR.GEOLOGIC.FRAMEWORK.; 1966, P. 159 A 169Miscellaneous

GEOMETRY AND ORIGIN OF LARGE-SCALE DEFORMATION STRUCTURES IN SOME ANCIENT WIND-BLOWN SAND DEPOSITS = GEOMETRIE ET ORIGINE DES STRUCTURES DE DEFORMATION A GRANDE ECHELLE DANS CERTAINES ANCIENNES FORMATIONS DE SABLE DUES AU VENTHOROWITZ DH.1982; SEDIMENTOLOGY; ISSN 0037-0746; NLD; DA. 1982; VOL. 29; NO 2; PP. 155-180; BIBL. 45 REF.; 2 TAB. ; ESQUISSE/ILL./TABL.Article

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