This study describes and analyses an extraordinary array of pockmarks at the modern seabed of the Lower Congo Basin (offshore Angola), in order to understand the fluid migration routes and shallow plumbing system of the area. The 3D seismic visualization of feeding conduits (pipes) allowed the identification of the source interval for the fluids expelled during pockmark formation. Spatial statistics are used to show the relationship between the underlying (polarised) polygonal fault (PPFs) patterns and seabed pockmarks distributions. Our results show PPFs control the linear arrangement of pockmarks and feeder pipes along fault strike, but faults do not act as conduits. Spatial statistics also revealed pockmark occurrence is not considered t...
Based on high-resolution 3D seismic data sets, we document the subsurface reservoir architecture and...
This study documents the suite of processes associated with source-to-seafloor fluid migration in th...
Using high quality 3D seismic data within the Lower Congo Basin (LCB), we have identified pockmarks ...
This study describes and analyses an extraordinary array of pockmarks at the modern seabed of the Lo...
In marine geological settings, pockmarks are evidence of highly focused fluid expulsion at the seab...
Fluid venting structures are used to evaluate fluid migration in the subsurface and vertical changes...
A synthesis of backscatter imagery coupled with a large 3D seismic dataset in the Lower Congo Basin ...
A synthesis of backscatter imagery coupled with a large 3D seismic dataset in the Lower Congo Basin ...
Pockmarks are seafloor depressions commonly associated with fluid escape from the seabed and are bel...
Pockmarks in Pliocene-Quaternary continental slope deposits offshore Angola show features related to...
Over 25,300 seabed pockmarks were mapped from the Rosetta Channel region of the Western NileDeepSeaF...
Pockmarks in Pliocene-Quaternary continental slope deposits offshore Angola show features related t...
Using high quality 3D seismic data within the Lower Congo Basin (LCB), we have identified pockmarks ...
Underwater gas and liquid escape from the seafloor has long been treated as a mere curiosity. It was...
International audienceInactive and mostly elongated pockmarks of 100-200 m in dimension were recentl...
Based on high-resolution 3D seismic data sets, we document the subsurface reservoir architecture and...
This study documents the suite of processes associated with source-to-seafloor fluid migration in th...
Using high quality 3D seismic data within the Lower Congo Basin (LCB), we have identified pockmarks ...
This study describes and analyses an extraordinary array of pockmarks at the modern seabed of the Lo...
In marine geological settings, pockmarks are evidence of highly focused fluid expulsion at the seab...
Fluid venting structures are used to evaluate fluid migration in the subsurface and vertical changes...
A synthesis of backscatter imagery coupled with a large 3D seismic dataset in the Lower Congo Basin ...
A synthesis of backscatter imagery coupled with a large 3D seismic dataset in the Lower Congo Basin ...
Pockmarks are seafloor depressions commonly associated with fluid escape from the seabed and are bel...
Pockmarks in Pliocene-Quaternary continental slope deposits offshore Angola show features related to...
Over 25,300 seabed pockmarks were mapped from the Rosetta Channel region of the Western NileDeepSeaF...
Pockmarks in Pliocene-Quaternary continental slope deposits offshore Angola show features related t...
Using high quality 3D seismic data within the Lower Congo Basin (LCB), we have identified pockmarks ...
Underwater gas and liquid escape from the seafloor has long been treated as a mere curiosity. It was...
International audienceInactive and mostly elongated pockmarks of 100-200 m in dimension were recentl...
Based on high-resolution 3D seismic data sets, we document the subsurface reservoir architecture and...
This study documents the suite of processes associated with source-to-seafloor fluid migration in th...
Using high quality 3D seismic data within the Lower Congo Basin (LCB), we have identified pockmarks ...