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A METHOD TO CLIMINATE THE BACKGROUND IN X-RAY DIFFRACTION PATTERNS OF ORIENTED CLAY MINERAL SAMPLES = METHODES POUR ELIMINER LE FOND CONTINU DANS DES CLICHES DE DIFFRACTION RX D'ECHANTILLONS DE MINERAUX ARGILEUX ORIENTESVAN DER GAAST SJ; VAARS AJ.1981; CLAY MINER.; ISSN 0009-8558; GBR; DA. 1981; VOL. 16; NO 4; PP. 383-393; ABS. FRE/GER/SPA; BIBL. 8 REF.; ILL./TABL.Article

DETERMINATION OF OPAL IN MARINE SEDIMENTS BY X-RAY DIFFRACTION.EISMA D; VAN DER GAAST SJ.1971; NETHERL. J. SEA RES.; NLD; 1971(7), VOL. 5, NUM. 0003, P. 382 A 389Miscellaneous

SUSPENDED MATTER IN THE ZAIRE ESTUARY AND THE ADJACENT ATLANTIC OCEANEISMA D; KALF J; VAN DER GAAST SJ et al.1978; NETHERL. J. SEA RES.; NLD; DA. 1978; VOL. 12; NO 3-4; PP. 382-406; BIBL. 2 P.Article

A COMPARISON OF THE EFFECTIVENESS OF EIGHT METHODS FOR THE REMOVAL OF ORGANIC MATTER FROM CLAYVAN LANGEVELD AD; VAN DER GAAST SJ; EISMA D et al.1978; CLAYS CLAY MINER.; GBR; DA. 1978; VOL. 26; NO 5; PP. 361-364; ABS. RUS/GER/FRE; BIBL. 8 REF.; 1 ILL.Article

SUSPENDED MATTER AND BOTTOM DEPOSITS OF THE ORINOCO DELTA: TURBIDITY, MINERALOGY AND ELEMENTARY COMPOSITIONEISMA D; VAN DER GAAST SJ; MARTIN JM et al.1978; NETHERL. J. SEA RES.; NLD; DA. 1978; VOL. 12; NO 3; PP. 224-251; BIBL. 3 P.Article

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