Subsurface sediment remobilization and fluid flow in sedimentary basins: an overview
Subsurface sediment remobilization and fluid flow processes and their products are
increasingly being recognized as significant dynamic components of sedimentary basins …
increasingly being recognized as significant dynamic components of sedimentary basins …
Mud volcanoes: indicators of stress orientation and tectonic controls
M Bonini - Earth-Science Reviews, 2012 - Elsevier
This study examines the use of specific mud volcano features (ie, elongated calderas,
aligned vents and elongated volcanoes) as potential indicators of tectonic stress orientation …
aligned vents and elongated volcanoes) as potential indicators of tectonic stress orientation …
Seismic characteristics of fluid escape pipes in sedimentary basins: Implications for pipe genesis
Fluid escape pipes were first documented from 3D seismic data over a decade ago, and
have subsequently been identified in many petroliferous basins worldwide. They are …
have subsequently been identified in many petroliferous basins worldwide. They are …
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 …
A major Miocene deepwater mud canopy system: the North Sabah–Pagasa Wedge, northwestern Borneo
CK Morley, W Promrak, W Apuanram… - …, 2023 - pubs.geoscienceworld.org
Three-dimensional seismic reflection data, well data, and analogues from areas with
extensive shale tectonics indicate that the enigmatic deepwater “shale nappe or thrust …
extensive shale tectonics indicate that the enigmatic deepwater “shale nappe or thrust …
Review of submarine cold seep plumbing systems: leakage to seepage and venting
AR Talukder - Terra Nova, 2012 - Wiley Online Library
Terra Nova, 24, 255–272, 2012 Abstract Cold seep systems comprise three structural
elements: source, plumbing system, and venting structures or see** features at or near the …
elements: source, plumbing system, and venting structures or see** features at or near the …
Proposal for a mechanical model of mobile shales
Structural systems involving mobile shale represent one of the most difficult challenges for
geoscientists dedicated to exploring the subsurface structure of continental margins. Mobile …
geoscientists dedicated to exploring the subsurface structure of continental margins. Mobile …
Shale transformations and physical properties—Implications for seismic expression of mobile shales
Seismic interpretation of mobile shales is challenging, mostly because of their unclear
seismic expression. Imaging of mobile shales is difficult because of their low seismic …
seismic expression. Imaging of mobile shales is difficult because of their low seismic …
Structure of mud volcano systems and pockmarks in the region of the Ceuta Contourite Depositional System (Western Alborán Sea)
New high-resolution seismic and swath bathymetry data reveal the detailed structure of nine
mud volcanoes and two large fields of pockmarks at water depths of 400–1100m in the …
mud volcanoes and two large fields of pockmarks at water depths of 400–1100m in the …
[BOOK][B] Geosciences of Azerbaijan
AA Alizadeh, IS ogly Guliyev, FA Kadirov… - 2016 - Springer
Azerbaijan occupies an area of about 87,000 km2 in the unique tectonic environment (the
Greater and Lesser Caucasus, Talysh Mts., Kur and Caspian Basins, etc.) that finds a …
Greater and Lesser Caucasus, Talysh Mts., Kur and Caspian Basins, etc.) that finds a …