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Subduction de la Ride de Carnegie au niveau de l'Equateur ? Impact géodynamique et sismique = Subduction of the Carnegie Ridge at the level of the Equador ? Geodynamical and seismic impactGUTSCHER, M.-A; MALAVIEILLE, J; LALLEMAND, S. E et al.Réunion des sciences de la terre. 1998, p. 126Conference Paper

THE CARNEGIE RIDGE NEAR 86OW.: STRUCTURE, SEDIMENTATION AND NEAR BOTTOM OBSERVATIONS.MALFAIT BT.1975; DISSERT. ABSTR. INTERNATION., B; USA; RESUME,1975, VOL. 35, NUM. 0008, P. 4065Serial Issue

MANGANESE-NODULE BEDFORMS AND THERMOHALINE DENSITY FLOWS IN A DEEP-SEA VALLEY ON CARNEGIE-RIDGE, PANAMA BASIN = LITS A NODULES DE MANGANESE ET ECOULEMENT THERMOHALIN DE DENSITE DANS UNE VALLEE EN EAU PROFONDE DE LA DORSALE CARNEGIE, BASSIN DE PANAMALONSDALE P.1980; J. SEDIMENT. PETROL.; ISSN 0022-4472; USA; DA. 1980; VOL. 50; NO 4; PP. 1033-1048; BIBL. 2 P.Article

ABYSSAL SAND WAVES ON THE CARNEGIE RIDGE.LONSDALE P.1972; GEOL. SOC. AMER., ABSTR. PROGRAMS; USA; 1972, VOL. 4, NUM. 0007, P. 579 A 580Serial Issue

A MODERN OCEANIC HARDGROUND ON THE CARNEGIE RIDGE IN THE EASTERN EQUATORIAL PACIFIC = UN HARDGROUND OCEANIQUE ACTUEL SUR LA DORSALE CARNEGIE DANS L'EST DE L'OCEAN PACIFIQUE EQUATORIALMALFAIT BT; VAN ANDEL TH.1980; SEDIMENTOLOGY; ISSN 0037-0746; NLD; DA. 1980; VOL. 27; NO 5; PP. 467-496; BIBL. 39 REF.; ESQUISSE GEOL./ILL.Article

ECUADORIAN SUBDUCTION SYSTEMLONSDALE P.1978; AMER. ASS. PETROLEUM GEOLOGISTS BULL.; USA; DA. 1978; VOL. 62; NO 12; PP. 2454-2477; BIBL. 3 P.; 9 ILL.Article

Seismicity and tectonics of southern central America and adjacent regions with special attention to the surroundings of Panama = Sismicité et tectonique d'Amérique Centrale Sud et des régions adjacentes avec une étude particulière des environnements de PanamaWOLTERS, B.Tectonophysics. 1986, Vol 128, Num 1-2, pp 21-46, issn 0040-1951Article

Carbon isotope data in core V19-30 confirm reduced carbon dioxide concentration in the ice age atmosphere = La composition isotopique du carbone dans la carotte V19-30 confirme une réduction de la concentration en gaz carbonique dans l'atmosphère de l'époque glaciaireSHACKLETON, N. J; HALL, M. A; LINE, J et al.Nature (London). 1983, Vol 306, Num 5941, pp 319-322, issn 0028-0836Article

DIRECT OBSERVATIONS ON OCEAN-FLOOR HOT SPRINGS IN THE GALAPAGOS ZONE AND THE HESS DEPRESSION = OBSERVATIONS DIRECTES DES SOURCES THERMALES DU FOND DE L'OCEAN DANS LA ZONE DES GALAPAGOS ET LA DEPRESSION DE HESSGORGEYEV VV; GORDEEV VV; DEMINA LL et al.1979; GEOCHEM. INT.; ISSN 0016-7029; USA; DA. 1979; VOL. 16; NO 3; PP. 132-146; BIBL. 20 REF.; DE RUSSE EN ANGLAIS; 2 TAB. ; ESQUISSE/ESQUISSE GEOL./TABL./ILL.;[GEOKHIMIJA; SUN; DA. 1979; NO 6; PP. 902-917]Article

INCREASED PRODUCTIVITY IN THE EASTERN EQUATORIAL PACIFIC DURING THE LAST GLACIAL MAXIMUM (19,000 TO 14,000 YR B.P.) = AUGMENTATION DE LA PRODUCTIVITE DANS LE PACIFIQUE EQUATORIAL ORIENTAL AU MAXIMUM DU DERNIER EPISODE GLACIAIRE (19000 A 14000 ANS B.P.)PEDERSEN THOMAS F.1983; GEOL. (BOULDER); ISSN 0091-7613; USA; DA. 1983-01; VOL. 11; NO 1; PP. 16-19; BIBL. 22 REF.; ILL.Article

ESTIMATING ACOUSTIC ATTENUATION FROM A QUANTITATIVE SEISMIC PROFILER = ESTIMATION DE L'ATTENUATION ACOUSTIQUE D'APRES UNE METHODE QUANTITATIVE DE LEVE SISMIQUETYCE ROBERT C.1981; GEOPHYSICS; ISSN 0016-8033; USA; DA. 1981-10; VOL. 46; NO 10; PP. 1364-1378; BIBL. 31 REF.; 1 TAB. ; ILL.Article

Is the Cauca-Patia and Romeral fault system left or rightlateral ?EGO, F; SEBRIER, M; YEPES, H et al.Geophysical research letters. 1995, Vol 22, Num 1, pp 33-36, issn 0094-8276Article

Deep structures of the Ecuador convergent margin and the Carnegie Ridge, possible consequence on great earthquakes recurrence intervalGRAINDORGE, David; CALAHORRANO, Alcinoe; CHARVIS, Philippe et al.Geophysical research letters. 2004, Vol 31, Num 4, pp L04603.1-L04603.5, issn 0094-8276Article

Historical 1942 Ecuador and 1942 Peru subduction earthquakes, and earthquake cycles along Colombia-Ecuador and Peru subduction segments : Historic earthquakesSWENSON, J. L; BECK, S. L.Pure and Applied Geophysics. 1996, Vol 146, Num 1, pp 67-101, issn 0033-4553Article

Are rupture zone limits of great subduction earthquakes controlled by upper plate structures? Evidence from multichannel seismic reflection data acquired across the northern Ecuador-southwest Colombia marginCOLLET, Jean-Yves; MARCAILLOU, Boris; SAGE, Francoise et al.Journal of geophysical research. 2004, Vol 109, Num B11, pp B11103.1-B11103.14, issn 0148-0227Article

Geochemical and petrological constraints on rear-arc magma genesis processes in Ecuador : The Puyo cones and Mera lavas volcanic formationsHOFFER, Géraldine; EISSEN, Jean-Philippe; BEATE, Bernardo et al.Journal of volcanology and geothermal research. 2008, Vol 176, Num 1, pp 107-118, issn 0377-0273, 12 p.Article

Transition entre magmatismes calco-alcalin et adakitique dans le cas d'une subduction impliquant une ride océanique : le Volcan Cayambe (Equateur) = Transition from calc-alkaline to adakitic magmatism at Cayambe volcano (Ecuador) : the influence of Carnegie ridge subductionSamaniego Eguiguren, Pablo; Martin, Hervé.2001, 306 p.Thesis

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