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ROLE OF DEFORMATIONS IN FORMING CONTACT HORNFELS IN CRYSTALLINE ROCKS.DUK GG.1970; INTERNATION. GEOL. REV.; SUN; 1970, VOL. 12, NUM. 0012, P. 1454 A 1462Miscellaneous

GRANITISATION REPETITIVE DES FORMATIONS ARCHEENNES DE LA REGION DE KIROVSKIJ DANS LA REGION DE L'AMOUR.DUK GG.sdUL'TRAMETAMORPHISM I METASOMATOSE DOKEMBRIJSKIKH FORMACIJ.S.S.S.R.MOSCOU.NAUKA.; , P. 132 A 155Miscellaneous

METAMORPHISME DE LA ZONE DE LA FRACTURE MONGOLIE-OKHOTSKDUK GG.1972; IZVEST. AKAD. NAUK S.S.S.R., SER. GEOL.; S.S.S.R. ; 1972, NUM. 0003, P. 45 A 54Serial Issue

THE ROLE OF DEFORMATIONS DURING THE FORMATION OF CONTACT HORNFELS IN CRYSTALLINE ROCKS.DUK GG.1970; ZAP. VSESOJUZ. MINERAL. OBSHCHEST.; SUN; 1970, VOL. 99, NUM. 0001, P. 35 A 44Miscellaneous

LES DIAPHTORITES MESOZOIQUES DE LA ZONE DE CASSURE TUKURINGR-SUD (REGION DU HAUT AMOUR).DUK GG; SUDOVIKOV NG.1965; MOSKVA.LENINGRAD.NAUKA.; 1965, P. 76 A 91Miscellaneous

PARTICULARITES DE LA COMPOSITION DES BIOTITES DES GRANITOIDES DE L'ENCADREMENT SUD DU MASSIF DE L'ALDAN.SEDOVA IS; DUK GG.1970; ZAP. VSESOJUZN. MINERAL. OBSHCH., S.S.S.R.; 1970(8), VOL. 99, NUM. 0004, P. 399 A 410Miscellaneous

LES DIAPHTORITES MESOZOIQUES DE LA ZONE DE CASSURE TUKURINGR-SUD (REGION DU HAUT AMOUR).DUK GG; SUDOVIKOV NG.1965; MOSKVA.LENINGRAD.NAUKA.; 1965, P. 76 A 91Miscellaneous

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