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Titolo:
DEVELOPMENT OF A PASSIVE TRANSFORM MARGIN - COTE-DIVOIRE GHANA TRANSFORM MARGIN - ODP LEG-159 PRELIMINARY-RESULTS
Autore:
MASCLE J; LOHMANN P; CLIFT P; AKAMALUK T; ALLERTON S; ASK M; BARRERA EC; BARTON E; BASILE C; BELLIER JP; BENKHELIL J; BRANTUOH E; EDWARDS R; EWERT E; GONCALVES C; JANIK AG; HOLMES MA; HISADA K; LOHMANN KC; MORITA S; MORTERAGUTIERREZ CA; NORRIS RD; OBOH FE; PLETSCH T; PICKETT EA; RAVIZZA G; SHAFIK S; SHIN IC; STRAND KO; WAGNER T; WATKINS D;
Indirizzi:
GEMCO,URA CNRS 718,LAB GEODYNAM SOUS MARINE,BP 48 F-06230 VILLEFRANCHE MER FRANCE WOODS HOLE OCEANOG INST WOODS HOLE MA 02543 TEXAS A&M UNIV COLLEGE STN TX 77843 UNIV OXFORD OXFORD OX1 2JD ENGLAND ROYAL INST TECHNOL S-10044 STOCKHOLM SWEDEN UNIV MICHIGAN ANN ARBOR MI 48109 UNIV GRENOBLE 1 F-38041 GRENOBLE FRANCE UNIV PARIS 06 PARIS FRANCE UNIV PERPIGNAN F-66025 PERPIGNAN FRANCE UNIV LEICESTER LEICESTER LE1 7RH LEICS ENGLAND UNIV MIAMI CORAL GABLES FL 33124 UNIV NEBRASKA LINCOLN NE 00000 UNIV TSUKUBA TSUKUBA IBARAKI 305 JAPAN UNIV TOKYO,OCEAN RES INST TOKYO 164 JAPAN SCH MINES & MET ROLLA MO 00000 UNIV TUBINGEN TUBINGEN GERMANY UNIV EDINBURGH EDINBURGH EH8 9YL MIDLOTHIAN SCOTLAND UNIV OULU OULU FINLAND UNIV BREMEN D-2800 BREMEN 33 GERMANY
Titolo Testata:
Geo-marine letters
fascicolo: 1, volume: 17, anno: 1997,
pagine: 4 - 11
SICI:
0276-0460(1997)17:1<4:DOAPTM>2.0.ZU;2-7
Fonte:
ISI
Lingua:
ENG
Tipo documento:
Article
Natura:
Periodico
Settore Disciplinare:
Science Citation Index Expanded
Science Citation Index Expanded
Citazioni:
9
Recensione:
Indirizzi per estratti:
Citazione:
J. Mascle et al., "DEVELOPMENT OF A PASSIVE TRANSFORM MARGIN - COTE-DIVOIRE GHANA TRANSFORM MARGIN - ODP LEG-159 PRELIMINARY-RESULTS", Geo-marine letters, 17(1), 1997, pp. 4-11

Abstract

The Cote: d'Ivoire-Ghana transform margin is bounded to the south by a prominent marginal ridge. ODP Leg 159 shipboard analyses on sediments from four sites document three distinct transform margin sedimentaryand tectonic stages of evolution: (1) an intracontinental stage of transform faulting recorded in deformed lacustrine to marine siliciclastic sequences; (2) a marginal ridge uplift stage, recorded by shallow water limestones, appears coeval with the passing of a hot, oceanic spreading center just south of the sediment wedge; and (3) cooling subsidence of the transform margin recorded in bathyal to abyssal sediments emphasizes a passive margin stage, These results are consistent with previously published models of evolution.

ASDD Area Sistemi Dipartimentali e Documentali, Università di Bologna, Catalogo delle riviste ed altri periodici
Documento generato il 26/09/20 alle ore 14:35:08