Environmental signal propagation in sedimentary systems across timescales
Earth-surface processes operate across erosionally dominated landscapes and deliver
sediment to depositional systems that can be preserved over a range of timescales. The …
sediment to depositional systems that can be preserved over a range of timescales. The …
Turbidity currents and their deposits
E Meiburg, B Kneller - Annual review of fluid mechanics, 2010 - annualreviews.org
The article surveys the current state of our understanding of turbidity currents, with an
emphasis on their fluid mechanics. It highlights the significant role these currents play within …
emphasis on their fluid mechanics. It highlights the significant role these currents play within …
Mudstone diversity: Origin and implications for source, seal, and reservoir properties in petroleum systems
AC Aplin, JHS Macquaker - AAPG bulletin, 2011 - archives.datapages.com
Mudstone is the most abundant sedimentary rock and variously acts as sources, seals, and
shale gas reservoirs in petroleum systems. Many important physicochemical properties of …
shale gas reservoirs in petroleum systems. Many important physicochemical properties of …
Marine hyperpycnal flows: initiation, behavior and related deposits. A review
T Mulder, JPM Syvitski, S Migeon, JC Faugères… - Marine and Petroleum …, 2003 - Elsevier
Hyperpycnal flows form in the marine environment when river discharge enters the ocean
with suspended concentrations in excess of 36 kg m− 3 due to buoyancy considerations, or …
with suspended concentrations in excess of 36 kg m− 3 due to buoyancy considerations, or …
On the triggers, resulting flow types and frequencies of subaqueous sediment density flows in different settings
PJ Talling - Marine Geology, 2014 - Elsevier
Turbidity currents, and other types of underwater sediment density flow, are arguably the
most important flow process for moving sediment across our planet. Direct monitoring …
most important flow process for moving sediment across our planet. Direct monitoring …
Trajectory analysis: concepts and applications
Shoreline and shelf‐edge trajectories describe the migration through time of sedimentary
systems, using geomorphological breaks‐in‐slope that are associated with key changes in …
systems, using geomorphological breaks‐in‐slope that are associated with key changes in …
Transport and transformation of dissolved and particulate materials on continental margins influenced by major rivers: benthic boundary layer and seabed processes
Within the benthic boundary layer (BBL) and seabed of river-dominated ocean margins
(RiOMars), the timing, kinetics and extent of important biogeochemical processes are greatly …
(RiOMars), the timing, kinetics and extent of important biogeochemical processes are greatly …
Processes that initiate turbidity currents and their influence on turbidites: a marine geology perspective
DJW Piper, WR Normark - Journal of Sedimentary …, 2009 - pubs.geoscienceworld.org
How the processes that initiate turbidity currents influence turbidite deposition is poorly
understood, and many discussions in the literature rely on concepts that are overly …
understood, and many discussions in the literature rely on concepts that are overly …
How are subaqueous sediment density flows triggered, what is their internal structure and how does it evolve? Direct observations from monitoring of active flows
PJ Talling, CK Paull, DJW Piper - Earth-Science Reviews, 2013 - Elsevier
Subaqueous sediment density flows are one of the volumetrically most important processes
for moving sediment across our planet, and form the largest sediment accumulations on …
for moving sediment across our planet, and form the largest sediment accumulations on …
Depositional processes, bedform development and hybrid bed formation in rapidly decelerated cohesive (mud–sand) sediment flows
Flows with high suspended sediment concentrations are common in many sedimentary
environments, and their flow properties may show a transitional behaviour between fully …
environments, and their flow properties may show a transitional behaviour between fully …