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au.\*:("WHITCOMBE DN")

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AN ANALYSIS OF THE VELOCITY STRUCTURE OF THE PRECAMBRIAN ROCKS OF CHARNWOOD FOREST = ANALYSE DE LA STRUCTURE DE VITESSE DES ROCHES PRECAMBRIENNES DE CHARNWOOD FORESTWHITCOMBE DN; MAGUIRE PKH.1980; GEOPHYS. J.R. ASTRON. SOC.; ISSN 0016-8009; GBR; DA. 1980; VOL. 63; NO 2; PP. 405-416; BIBL. 10 REF.Article

THE RESPONSE OF THE TIME-TERM METHOD TO SIMULATED CRUSTAL STRUCTURESWHITCOMBE DN; MAGUIRE PKH.1979; BULL. SEISMOL. SOC. AMER.; USA; DA. 1979; VOL. 69; NO 5; PP. 1455-1473; BIBL. 13 REF.Article

A SEISMIC REFRACTION INVESTIGATION OF THE CHARNIAN BASEMENT AND GRANITIC INTRUSIONS FLANKING CHARNWOOD FOREST = ETUDE PAR SISMIQUE REFRACTION DU BASEMENT CHARNIEN ET DES INTRUSIONS GRANITIQUES BORDANT LA FORET CHARNWOODWHITCOMBE DN; MAGUIRE PKH.1981; J. GEOL. SOC. (LOND.); ISSN 0016-7649; GBR; DA. 1981; VOL. 138; NO 6; PP. 643-651; BIBL. 32 REF.; ILL./ESQUISSE GEOL.Article

DEPTH OF GEOLOGICAL CONTRAST ACROSS THE WEST AFRICAN CRATON MARGIN = PROFONDEUR DU CONTRASTE GEOLOGIQUE DE LA MARGE DU CRATON WEST AFRICAINBRIDEN JC; WHITCOMBE DN; STUART GW et al.1981; NATURE (LOND.); ISSN 0028-0836; GBR; DA. 1981; VOL. 292; NO 5819; PP. 123-128; BIBL. 31 REF.; ILL.Article

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