Evidences of early to late fluid migration from an upper Miocene turbiditic channel revealed by 3D seismic coupled to geochemical sampling within seafloor pockmarks, Lower Congo Basin

Marine and Petroleum Geology

Volumn 23, Issue 3, 2006, Pages 387-399

  Gay, A ^a   Lopez, M ^b   Cochonat, P ^c   Levache D ^d   Sermondadaz, G ^d   Seranne, M ^b  

^a NATIONAL OCEANOGRAPHY CENTRE   (United Kingdom)

^b UNIVERSITÉ MONTPELLIER 2   (France)

^c IFREMER   (France)

^d TOTAL   (France)

Author keywords

Fluid migration; Pipes; Pockmarks; Polygonal faults; Seismic chimneys; Turbiditic channels

Indexed keywords

FLUID MIGRATION; GEOCHEMICAL ANALYSIS; GEOCHEMICAL SAMPLING; HIGHLY FAULTED INTERVAL; THERMOGENIC HYDROCARBON; TURBIDITIC CHANNEL;

COMPACTION; CORE SAMPLES; FLUID DYNAMICS; GEOCHEMISTRY; HYDROCARBONS; MOLECULAR WEIGHT; PARAFFINS; SEDIMENTS; SEISMOLOGY; THREE DIMENSIONAL;

PETROLEUM GEOLOGY;

CORE ANALYSIS; MIOCENE; PALEOCHANNEL; POCKMARK; SEAFLOOR; SEISMIC DATA;

AFRICA; CONGO BASIN; SUB-SAHARAN AFRICA;

EID: 33646768640     PISSN: 02648172     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.marpetgeo.2006.02.004     Document Type: Article

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