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Fluid flow features in hydrocarbon plumbing systems: What do they tell us about the basin evolution?
KJ Andresen - Marine Geology, 2012 - Elsevier
Fluid flow features such as sandstone intrusions, mud volcano systems and pockmarks
represent well-known geological structures generated due to flow of fluids in the subsurface …
represent well-known geological structures generated due to flow of fluids in the subsurface …
The chronology and tectonic style of landscape evolution along the elevated Atlantic continental margin of South Africa resolved by joint apatite fission track and (U‐Th …
Atlantic‐type continental margins have long been considered “passive” tectonic settings
throughout the entire postrift phase. Recent studies question the long‐term stability of these …
throughout the entire postrift phase. Recent studies question the long‐term stability of these …
Rapid South Atlantic spreading changes and coeval vertical motion in surrounding continents: Evidence for temporal changes of pressure‐driven upper mantle flow
Abstract The South Atlantic region displays (1) a topographic gradient across the basin, with
Africa elevated relative to South America,(2) a bimodal spreading history with fast spreading …
Africa elevated relative to South America,(2) a bimodal spreading history with fast spreading …
Origin and evolution of widespread crescentic pockmarks on the western South China Sea margin
L Wang, F Zhao, E Miramontes - Marine and Petroleum Geology, 2024 - Elsevier
Pockmarks are prominent morphological features formed by fluid escape at the seafloor that
provide valuable information on past environmental conditions and ongoing sedimentary …
provide valuable information on past environmental conditions and ongoing sedimentary …
[HTML][HTML] Origin of seafloor pockmarks overlying submarine landslides: Insights from semi-automated map** of 3D seismic horizons (North West Shelf, Australia)
Pockmarks are geohazards that can impact offshore developments, and an understanding of
their formation assists in determination of their physical characteristics and in the prediction …
their formation assists in determination of their physical characteristics and in the prediction …
Segmentation and volcano-tectonic characteristics along the SW African continental margin, South Atlantic, as derived from multichannel seismic and potential field …
H Koopmann, D Franke, B Schreckenberger… - Marine and Petroleum …, 2014 - Elsevier
Regional seismic reflection and potential field data document the South Atlantic's break-up
history, between 39° S and 19° S, from the Early Cretaceous onwards. Previous maps of …
history, between 39° S and 19° S, from the Early Cretaceous onwards. Previous maps of …
Gas hydrate distributions in sediments of pockmarks from the Nigerian margin–Results and interpretation from shallow drilling
A joint research expedition between the French IFREMER and the German MARUM was
conducted in 2011 using the R/V 'Pourquoi pas?'to study gas hydrate distributions in a …
conducted in 2011 using the R/V 'Pourquoi pas?'to study gas hydrate distributions in a …
Post-rift stratigraphic evolution of the Atlantic margin of Namibia and South Africa: Implications for the vertical movements of the margin and the uplift history of the …
The aim of this study is to constrain the post-rift deformations of the Atlantic passive margin
of Namibia and South Africa using an extensive industrial 2D reflection seismic dataset …
of Namibia and South Africa using an extensive industrial 2D reflection seismic dataset …
The late rifting phase and continental break-up of the southern South Atlantic: the mode and timing of volcanic rifting and formation of earliest oceanic crust
H Koopmann, B Schreckenberger, D Franke, K Becker… - 2016 - pubs.geoscienceworld.org
Multichannel seismic and potential field data shed light on the final rifting stage in the
southern South Atlantic. This was associated with major episodes of magmatism during the …
southern South Atlantic. This was associated with major episodes of magmatism during the …
Strato-structural evolution of the deep-water Orange Basin: constraints from 3D reflection seismic data
Deep-water fold-and-thrust belt (DWFTB) systems are gravity-driven collapse structures
often found in passive margin settings and are comprised of a linked up-dip extensional …
often found in passive margin settings and are comprised of a linked up-dip extensional …