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DER WAERMEFLUSS ZWISCHEN HARZ UND PRIGNITZ.(LE FLUX GEOTHERMIQUE ENTRE LE HARZ ET PRIGNITZ).BECHER D; MEINCKE W.1968; Z. ANGEW. GEOL.; DDR; 1968(6), VOL. 14, NUM. 0006, P. 291 A 297Miscellaneous

SUBSURFACE TEMPERATURE, HEAT CONDUCTIVITY AND HEAT FLOW IN THE THURINGIA BASIN AND SURROUNDING AREAS, GDR.HURTIG E; MEINCKE W.1969; BULL. VOLCANOL.; ITA; 1969, VOL. 33, NUM. 0001, P. 229 A 242Miscellaneous

TEMPERATURVERTEILUNG,WAERMELEITFAEHIGKEIT UND WAERMEFLUSS IM THUERINGER BECKEN.(DISTRIBUTION DES TEMPERATURES,DES CONDUCTIVITES THERMIQUES ET DES FLUX GEOTHERMIQUES DANS LA DEPRESSION DE THURINGE).MEINCKE W; HURTIG E; WEINER J et al.1967; GEOPHYS. UND GEOL., DTSCH; DDR; 1967, VOL. 11, P. 40 A 71Miscellaneous

STUDY OF ELECTROPRODUCTION WITH A STREAMER CHAMBER FOR 0.3<Q2<1.5(GEV)2, 1.3<W<2.8 GEVECKARDT V; GEBAUER HJ; JOOS P et al.1973; LETTERE NUOVO CIMENTO; ITAL.; DA. 1973; VOL. 6; NO 14; PP. 551-556; BIBL. 7 REF.Serial Issue

STUDY OF ELECTROPRODUCTION WITH A STREAMER CHAMBER FOR 0.3<Q2<1.5 GEV2, MP <OU= W<2.8 GEVECKARDT V; GEBAUER HJ; JOOS P et al.1973; NUCL. PHYS., B; NETHERL.; DA. 1973; VOL. 55; NO 1; PP. 45-82; BIBL. 1 P.Serial Issue

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