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au.\*:("PETRUNIN GI")

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NATURE DE LA TRANSITION A LA LIMITE NOYAU-MANTEAUPETRUNIN GI.1976; IZVEST. AKAD. NAUK S.S.S.R., FIZ. ZEMLI; S.S.S.R.; DA. 1976; NO 9; PP. 14-20; BIBL. 21 REF.Article

ON THE NATURE OF THE TRANSITION AT THE CORE-MANTLE BOUNDARY.PETRUNIN GI.1977; IZVEST. AKAD. SCI. U.S.S.R., PHYS. SOLID EARTH; U.S.A.; DA. 1977; VOL. 12; NO 9; PP. 559-562; BIBL. 21 REF.; 3 ILL.; DU RUSSE: IZVEST. AKAD. NAUK SSSR., FIZ. ZEMLI, S.S.S.R. 1976; NO 9, 14-20Article

CONDUCTION THERMIQUE DE QUELQUES FELDSPATHS A 300-1200 DEGRES K.MAGNICKIJ VA; PETRUNIN GI; JURCHAK RP et al.1971; DOKL. AKAD. NAUK S.S.S.R.; SUN; 1971(8), VOL. 199, NUM. 0005, P. 1058 A 1060Miscellaneous

TEMPERATURE CONDUCTIVITY OF BASALTS AT TEMPERATURES FROM 300 TO 1200 DEGREES K.PETRUNIN GI; JURCHAK RI; TKACH GF et al.1971; IZVEST. ACAD. SCI. U.S.S.R., PHYS. SOLID EARTH; USA; 1971, NUM. 0002, P. 126 A 127Miscellaneous

CONDUCTIBILITE DE LA TEMPERATURE DANS LES BASALTES DE 300 A 1200 DEGRES K.PETRUNIN GI; JURCHAK RP; TKACH GF et al.1971; IZVEST. AKAD. NAUK S.S.S.R., FIZ. ZEMLI; SUN; 1971(2), NUM. 0002, P. 65 A 68Miscellaneous

COMPORTEMENT DE LA CONDUCTIVITE THERMIQUE DE QUELQUES FELDSPATHS POTASSIQUES ET DES PLAGIOCLASES ENTRE 300 A 1200OK.MAGNICKIJ VA; PETRUNIN GI; JURCHAK RP et al.1971; DOKL. AKAD. NAUK S.S.S.R.; SUN; 1971, VOL. 199, NUM. 0005, P. 1058 A 1060Miscellaneous

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