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PHYSICAL CHEMISTRY OF HIGH-TEMPERATURE POSTMAGMATIC METASOMATISM OF HERCYNIAN GRANITOID ROCKS OF NORMAL ALKALINITY IN THE CENTRAL CAUCASUS, AND ITS EFFECT ON ORE CONCENTRATION.MOSKALEV YE L; MOSKALEV EL.1976; DOKL. EARTH SCI. SECT.; U.S.A.; DA. 1976; VOL. 227; PP. 172-176; BIBL. 12 REF.; 5 ILL.; 7 ANAL.; DU RUSSE: DOKL. AKAD. NAUK S.S.S.R., S.S.S.R. 1976; 227, NO 6, 1446-1449Article

THERMODYNAMIC CONDITIONS OF EMPLACEMENT OF HERCYNIAN GRANITOIDS IN GORNAYA BALKARIA, NORTHERN CAUCASUS.MOSKALEV YE L; MOSKALEV EL.1975; DOKL. EARTH SCI. SECT.; U.S.A.; DA. 1975; VOL. 224; PP. 144-147; BIBL. 3 REF.; 4 ILL.; 22 ANAL.; DU RUSSE: DOKL. AKAD. NAUK S.S.S.R., S.S.S.R. 1975; 224, NO 6, 1410-1413Article

ECLOGITE AT THE EAST END OF THE FRONT RANGE OF THE CENTRAL CAUCASUS.MOSKALEV YE L; MOSKALEV EL.1973; DOKL. EARTH SCI. SECT.; USA; DU RUSSE: DOKL. AKAD. NAUK S.S.S.R., S.S.S.R. 1973; 212, NO 2, 471-474,1973, VOL. 212, P. 157 A 160Miscellaneous

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