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COUP D'OEIL SUR L'EVOLUTION DES THEORIES DE LA LOESSOGENESE.MAROSI P.1970; STUD. UNIV. BABES-BOLYAI, SER. GEOL.-MINERAL.; ROM; 1970, NUM. 0001, P. 61 A 74Miscellaneous

HYDROGEOCHEMICAL ZONALITY OF THE ARTESIAM BASIN OF TRANSYLVANIA.MAROSI P.1976; IN: HYDROGEOL. GREAT SEDIMENT. BASINS. INT. HYDROGEOL. CONF.; BUDAPEST; 1976; BUDAPEST; HUNG. GEOL. INST.; DA. 1976; PP. 103-106; RESUME. MEME DOC. FR.Conference Paper

HYDROGEOCHEMICAL ZONALITY OF THE ARTESIAN BASIN OF TRANSYLVANIA.MAROSI P.1976; IN: HYDROGEOL. GREAT SEDIMENT. BASINS. INT. HYDROGEOL. CONF. ABS.; BUDAPEST; 1976; BUDAPEST; HUNG. GEOL. INST.; DA. 1976; PP. 103-106; MEME DOC. FRConference Paper

PRINCIPLES OF GENETIC CLASSIFICATION OF PIEDMONT FORMATIONS AND OF THEIR HYDROGEOLOGICAL ZONAL DIVISION,WITH A SPECIAL VIEW UPON THE TERRITORY OF THE SOCIALIST REPUBLIC OF ROMANIA(1).THE GEOLOGY OF THE PIEDMONT FORMATIONS.MAROSI P.1968; STUD. UNIV. BABES-BOLYAI, GEOL. GEOGR.; ROM; 1968, NUM. 0002, P. 27 A 35Miscellaneous

ORIGINE DE LA MINERALISATION DES EAUX PHREATIQUES DE LA PLAINE INTERFLUVIALE BUZAU - R. SARAT.MAROSI P.1967; STUD.TEHN.ECON.HIDROGEOL.ROM; ROM; 1967, NUM. 0007, P. 105 A 150Miscellaneous

PRINCIPES DE LA CLASSIFICATION GENETIQUE DES FORMATIONS PIEDMONTANES ET DE LEUR ZONALITE HYDROGEOLOGIQUE, CONCERNANT SPECIALEMENT LE TERRITOIRE DE LA ROUMANIE (2). LES EAUX PHREATIQUES DES FORMATIONS PIEDMONTANES.MAROSI P.1969; STUD. UNIV. BABES-BOLYAI, GEOL. GEOGR.; ROM; 1969, VOL. 14, NUM. 0001, P. 41 A 52Miscellaneous

LES HORIZONS AQUIFERES DES ENVIRONS DE LA VILLE DE CLUJ.MESZAROS N; MAROSI P.1967; STUD. UNIV. BABES-BOLYAI, GEOL. GEOGR.; ROM; 1967, NUM. 002 , P. 215 A 223Miscellaneous

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