FN Archimer Export Format
PT J
TI Sea-level change and free gas occurrence influencing a submarine landslide and pockmark formation and distribution in deepwater Nigeria
BT 
AF RIBOULOT, Vincent
   CATTANEO, Antonio
   SULTAN, Nabil
   GARZIGLIA, Sebastien
   KER, Stephan
   IMBERT, Patrice
   VOISSET, Michel
AS 1:1,2;2:1;3:1;4:1;5:1;6:3;7:1;
FF 1:PDG-REM-GM-LES;2:PDG-REM-GM-LES;3:PDG-REM-GM-LES;4:PDG-REM-GM-LES;5:PDG-REM-GM;6:;7:PDG-REM-GM-CTDI;
C1 IFREMER, Ctr Brest, Inst CARNOT EDROME, Brest, France.
   Univ Perpignan, F-66025 Perpignan, France.
   TOTAL, Pau, France.
C2 IFREMER, FRANCE
   UNIV PERPIGNAN, FRANCE
   TOTAL, FRANCE
SI BREST
   AUTRE
SE PDG-REM-GM-LES
   PDG-REM-GM
   AUTRE
   PDG-REM-GM-CTDI
IN WOS Ifremer jusqu'en 2018
   copubli-france
   copubli-univ-france
IF 4.724
TC 56
UR https://archimer.ifremer.fr/doc/00159/27031/31906.pdf
LA English
DT Article
CR ERIG 3D
   ERIG3D RECUPIEZO
BO Pourquoi pas ?
   Antea
DE ;pockmarks;fluid seepage;submarine landslide;sea-level changes;piezocone;Niger Delta
AB A series of pockmarks observed at the seabed matches well the perimeter of a large submarine landslide, called NG1, located on the outer shelf and continental slope of the Eastern Gulf of Guinea. NG1 extends over 200 km2, is covered by a 120-m thick sedimentary layer which tapers downslope, and has an internal structure clearly identified in 3D seismic data consisting of three adjacent units on the upper continental slope. The pockmarks above NG1 have a diameter of several tens of meters and reveal distinct origins: (1) linked to >500 m deep fluid reservoirs, (2) rooted in NG1 internal discontinuities between NG1 units, and (3) well above NG1, superficially rooted in a regional conformity (D40), which marks the lowest sea level of the Marine Isotope Stage 6.  The regional stratigraphic pattern of the study area is composed of muddy sedimentary sequences separated by correlative conformities and transgressive condensed units of coarser grain size. Mud-confined coarser-grained units constitute transient gas reservoirs favoring lateral gas migration and formation of pockmarks rooted in the condensed units. The buried NG1 landslide modifies the layered structure of the sedimentary column providing (1) overall, a barrier to fluid migration, and (2) localized pathways for fluid migration. The triggering factor for the formation of pockmarks above NG1 can be the variation of hydrostatic pressure driven by relative sea-level fall during Marine Isotopic Stages 6 and 2 and consequent gas exsolution and fluid flow. We anticipate our result to be a starting point for understanding the role of gas seeps on climate change worldwide. Furthermore, gas release intensifies during lowstands with relevant implication on global warming after ice ages.
PY 2013
PD AUG
SO Earth And Planetary Science Letters
SN 0012-821X
PU Elsevier Science Bv
VL 375
UT 000324847300007
BP 78
EP 91
DI 10.1016/j.epsl.2013.05.013
ID 27031
ER

EF