Subsurface sediment remobilization and fluid flow processes and their products are
increasingly being recognized as significant dynamic components of sedimentary basins …

Subsurface sediment mobilization (SSM)-which includes soft sediment deformations, sand
injections, shale diapirs and mud volcanoes-is more widespread than previously thought …

Deep‐water mudstones are often considered as background sediments, deposited by
vertical suspension fallout, and the range of transport and depositional processes are poorly …

An architectural hierarchy of clastic sills is recognized in the Panoche Giant Injection
Complex in which staggered, stepped with erosive top surfaces, and multi-layered …

Few studies describe and compare the transport mechanisms operating to disperse mud in
different parts of basins. Instead, the physical processes operating to disperse mud in …

The complexity of flow and wide variety of depositional processes operating in subaqueous
density flows, combined with post‐depositional consolidation and soft‐sediment …

In accretionary wedges, often morphologically similar sedimentary intrusions, when
observed by remote geophysical means, may have one of two quite different driving …

Sand‐rich injectites are a common attribute of clastic sedimentary successions, and they
have received increased attention in the last decade by geoscientists and engineers dealing …

Fine grained clastic sediments are very common in the interior deposits of ancient
epicontinental seas. Not only do they make up the gross lithology in these basins, but they …

Clastic injection and surface expression of subsurface sediment remobilization is a
phenomenon which is becoming increasingly recognized. However, understanding of the …