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au.\*:("TZANKOV TV")

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UEBER DEN TERMINUS ANTIKLINORIUM (LE TERME ANTICLINORIUM).TZANKOV TV.1965; CARPATHO-BALK.GEOL.ASS.7TH.CONGR.REP.; 1965, NUM. 001 , P. 169 A 173Miscellaneous

UEBER DIE NATURE DER SIP-STOERUNG BEIM DORFE PODVRSKA (OSTSERBIEN). = SUR LA NATURE DE LA FAILLE DE SIP, PRES DE PODVRSKA (W DE LA SERBIE).GOCEV PM; TZANKOV TV.1971; IZVEST. GEOL. INST., GEOTEKTON., SOFIJA; BGR; 1971, VOL. 20, P. 69 A 73Miscellaneous

STRAIN VARIATION IN A PART OF THE SKRINO ANTICLINE, DISTRICT OF KJUSTENDIL, DETERMINED FROM DEFORMED REDUCTION SPOTS.ZAGORCEV IS; TZANKOV TV; SAPUNDZIEV KM et al.1976; C.R. ACAD. BULG. SCI.; BULG.; DA. 1976; VOL. 29; NO 9; PP. 1333-1336; BIBL. 4 REF.; 2 ILL.Article

N THE FAULT PREDETERMINATION OF THE PANAGYURISHTE STRIP EAST OF THE TOPOLNITSA RIVERKARAGJULEVA JD; KOSTADINOV VT; TZANKOV TV et al.1972; C.R. ACAD. BUL. SCI.; BULG.; 1972, VOL. 25, NUM. 0001, P. 95 A 97Serial Issue

THRUST ZONE OF THE KRIZNA NAPPE AT STOLY IN THE TATRA MTS (POLAND) = ZONE D'AVANCEE DE LA NAPPE KRIZNA A STOLY DANS LES MONTS TATRAS (POLOGNE)BAC MOSZASZWILI M; GAMKRELIDZE IP; JAROSZEWSKI W et al.1981; STUD. GEOL. POL.; ISSN 502219; POL; DA. 1981; VOL. 68; PP. 61-73; H.T. 4; ABS. RUS/POL; BIBL. 11 REF.; 4 PLANCH. ; ESQUISSE/ESQUISSE GEOL./ILL./PL.Article

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