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SUR LA NATURE DES CODA D'ONDESNERSESOV IL; KOPNICHEV YU F.1976; DOKL. AKAD. NAUK S.S.S.R.; S.S.S.R.; DA. 1976; VOL. 229; NO 6; PP. 1341-1344; BIBL. 12 REF.Article

DETERMINATION DU MOMENT SISMIQUE DES SEISMES LOCAUX D'APRES LES CARACTERISTIQUES DE LA CAUDAVOSTRIKOV GA.1975; IZVEST. AKAD. NAUK S.S.S.R., FIZ. ZEMLI; S.S.S.R.; DA. 1975; NO 11; PP. 33-45; BIBL. 12 REF.Article

ESTIMATION DU MOMENT SISMIQUE DES SEISMES LOCAUX D'APRES LA CAUDA DES SISMOGRAMMESVOSTRIKOV GA.1975; DOKL. AKAD. NAUK S.S.S.R.; S.S.S.R.; DA. 1975; VOL. 220; NO 2; PP. 335-338; BIBL. 10 REF.Article

ETALONNAGE MAGNETIQUE D'UN SEISME D'APRES LES ONDES DE CAUDA SUR DES DISTANCES ALLANT JUSQU'A 3000 KMNERSESOV IL; KOPNICHEV YU F; VOSTRIKOV GA et al.1975; DOKL. AKAD. NAUK S.S.S.R.; S.S.S.R.; DA. 1975; VOL. 222; NO 1; PP. 76-78; BIBL. 5 REF.Article

FURTHER INVESTIGATIONS ON CODA WAVES.BISZTRICSANY E.1975; VEROEFF. ZENTRALINST. PHYS. ERDE; DTSCH.; DA. 1975; NO 31 PART. 2; PP. 343-346; ABS. ALLEM.; BIBL. 5 REF.; (SEISMOL. SOLID-EARTH.-PHYS. INT. SYMP.; JENA; 1974)Conference Paper

MODELE DE FORMATION DE LA CAUDA D'UN SISMOGRAMMEKOPNICHEV YU F.1975; DOKL. AKAD. NAUK S.S.S.R.; S.S.S.R.; DA. 1975; VOL. 22; PP. 333-335; BIBL. 6 REF.Article

Heterogeneity of lithosphere in the Lützow-Holm Bay region, East AntarcticaAKAMATSU, J.Proceedings of the NIPR symposium on antarctic geosciences. 1990, Num 4, issn 0914-2029, 243Conference Paper

THE COMPLEX ENVELOPE IN SEISMIC SIGNAL ANALYSIS.FARNBACH JS.1975; BULL. SEISMOL. SOC. AMER.; U.S.A.; DA. 1975; VOL. 65; NO 4; PP. 951-962; BIBL. 13 REF.Article

CODA PATTERN AND MULTIPATH PROPAGATION OF RAYLEIGH WAVES AT NORSAR.BUNGUM H; CAPON J.1974; PHYS. EARTH PLANET. INTER.; NETHERL.; DA. 1974; VOL. 9; NO 2; PP. 111-127; BIBL. 6 REF.Article

Is the single scattering model invalid for the coda excitation at long lapse time? = Le modèle de diffusion simple permet-il d'étudier l'excitation des caudas pour un grand intervalle de temps?SATO, H.Pure and Applied Geophysics. 1988, Vol 128, Num 1-2, pp 43-47, issn 0033-4553Article

PROPERTIES OF CODA WAVES.BISZTRICSANY E.1975; ACTA GEOD. GEOPHYS. MONTANIST. ACAD. SCI. HUNGAR.; HONGR.; DA. 1975; VOL. 10; NO 1-2; PP. 131-135; ABS. RUSSE; BIBL. 6 REF.Article

Analiz tonkoj struktury korotkoperiodnoj kody P-volnyKAAZIK, P.B; KOPNICHEV, YU.F; RAKHMATULLIN, M.KH et al.Vulkanologiâ i sejsmologiâ. 1990, Num 2, pp 75-87, issn 0203-0306, 13 p.Article

Antioxidant Defence System of Boar Cauda Epididymidal Spermatozoa and Reproductive Tract FluidsKOZIOROWSKA-GILUN, M; KOZIOROWSKI, M; FRASER, L et al.Reproduction in domestic animals (1990). 2011, Vol 46, Num 3, pp 527-533, issn 0936-6768, 7 p.Article

Is the single scattering model invalid for the coda excitation at long lapse time? = Est-ce que le modèle de diffusion est adapté aux excitations de queue avec un temps d'erreur important?SATO, H.Pure and Applied Geophysics. 1988, Vol 128, Num 1-2, pp 43-47, issn 0033-4553Article

CODA ENERGY DISTRIBUTION AND ATTENUATIONYOSHIMOTO, Kazuo; JIN, Anshu.Advances in geophysics. 2008, Vol 50, pp 265-299, issn 0065-2687, 35 p.Article

Crustal coda-Q in the Iberian Peninsula = Facteur Q d'ondes cauda crustales dans la Péninsule IbériqueCANAS, J. A; EGOZCUE, J. J; PUJADES, L et al.Annales geophysicae. Series B. Terrestrial and planetary physics. 1987, Vol 5, Num 6, pp 657-662Article

ATTENUATION OF SHEAR-WAVES IN THE LITHOSPHERE FOR FREQUENCIES FROM 0.05 TO 25 HZAKI K.1980; PHYS. EARTH PLANET. INTER.; NLD; DA. 1980; VOL. 21; NO 1; PP. 50-60; BIBL. 42 REF.Article

ORIGIN OF CODA WAVES: SOURCE, ATTENUATION, AND SCATTERING EFFECTS.AKI K; CHOUET B.1975; J. GEOPHYS. RES.; U.S.A.; DA. 1975; VOL. 80; NO 23; PP. 3322-3342; BIBL. 1 P.Article

PERIODICITE DES CAUDAS DES SISMOGRAMMES LUNAIRESGALKIN IN; NIKOLAEV AV; KHAVROSHKIN OB et al.1980; IZVEST. AKAD. NAUK S.S.S.R., FIZ. ZEMLI; SUN; DA. 1980; NO 7; PP. 82-85; BIBL. 8 REF.Article

UTILISATION DE LA CODA SISMIQUE POUR L'ETUDE DE L'ATTENUATION DES ONDES SISMIQUES DANS LA REGION DE LA CRIMEEPUSTOVITENKO BG; RAUTIAN TG.1977; GEOFIZ. SBOR., U.S.S.R.; S.S.S.R.; DA. 1977; NO 78; PP. 3-14; ABS. ANGL.; BIBL. 23 REF.Article

ROLE DE LA DIFFUSION MULTIPLE DANS LA FORMATION DE LA QUEUE DU SISMOGRAMMEKOPNICHEV YU F.1977; IZVEST. AKAD. NAUK S.S.S.R., FIZ. ZEMLI; S.S.S.R.; DA. 1977; NO 6; PP. 41-48; BIBL. 10 REF.Article

CIRCULATING ANTIBODIES TO THE NEURITOGENIC MYELIN PROTEIN, P2, IN NEURITIS OF THE CAUDA EQUINA OF THE HORSEKADLUBOWSKI M; INGRAM PL.1981; NATURE (LOND.); ISSN 0028-0836; GBR; DA. 1981; VOL. 293; NO 5830; PP. 299-300; BIBL. 9 REF.Article

DIFFERENCE ENTRE SEISMES PRELIMINAIRES ET ESSAIMS DE SEISME ETUDIEE A PARTIR DE LA SIMILITUDE DES ONDES (RAPPORT PRELIMINAIRE)TSUJIURA M.1979; BULL. EARTHQUAKE RES. INST. UNIV. TOKYO; JPN; DA. 1979; VOL. 54; NO 2; PP. 309-315; ABS. ENG; BIBL. 8 REF.Article

PROPRIETES DES CARDA DES ONDES PANTONOVA DM; YANOVOSKAYA TB.1978; UCHEN. ZAP. LENINGRAD. GOS. UNIV., FIZ. GEOL. NAUK; SUN; DA. 1978; NO 27; PP. 66-76; BIBL. 19 REF.Article

MODELE DE FORMATION D'UN CAUDA D'UNE ONDE LONGITUDINALEKOPNICHEV YU F.1977; DOKL. AKAD. NAUK S.S.S.R.; S.S.S.R.; DA. 1977; VOL. 234; NO 3; PP. 560-563; BIBL. 11 REF.Article

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