Fluid flow structures of the Miocene-Holocene succession, western slope, Niger Delta

U. Benjamin*, M. Huuse

*Corresponding author for this work

Research output: Chapter in Book/Conference proceedingConference contribution

Abstract

The analysis of a 3D seismic data from western slope of the Niger Delta reveals several fluid flow structures in the Miocene to Holocene stratigraphic succession. These structures, imaged on attribute maps and seismic sections, include seafloor features such as mud volcanoes and their collapse structures as well as pockmarks. Others include buried seafloor mounds; amplitude anomalies as well as bottom-simulating reflectors (BSRs). The fluid flow activity in study area appears to be controlled mainly by mobile shale tectonics and dewatering of mini-basin sediments. These structures can be used to investigate fluid flow history, timing and migration, particularly with regards to hydrocarbons.

Original languageEnglish
Title of host publication74th European Association of Geoscientists and Engineers Conference and Exhibition 2012 Incorporating SPE EUROPEC 2012
Subtitle of host publicationResponsibly Securing Natural Resources
Place of PublicationBunnik
PublisherEAGE Publishing BV
Pages2280-2284
Number of pages5
ISBN (Electronic)9781629937908
DOIs
Publication statusPublished - Jun 2012
Event74th European Association of Geoscientists and Engineers Conference and Exhibition 2012 Incorporating SPE EUROPEC 2012: Responsibly Securing Natural Resources - Copenhagen, Denmark
Duration: 4 Jun 20127 Jun 2012

Conference

Conference74th European Association of Geoscientists and Engineers Conference and Exhibition 2012 Incorporating SPE EUROPEC 2012: Responsibly Securing Natural Resources
Country/TerritoryDenmark
CityCopenhagen
Period4/06/127/06/12

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