Deformations formed in unconsolidated sediments are known as soft-sediment deformation
structures. Their nature, the time of their genesis, and the state in which the sediments …

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

Injecting fluids in the crust, or their extraction, changes pore pressure and poroelastic
stresses. Both pressure and stress changes can promote seismicity and, hence, the seismic …

Petroleum Geoscience, 2nd edition is a comprehensive introduction to the application of
geology and geophysics to the search for and production of oil and gas. The aim this …

Geofluids (2010) 10, 206–216 Abstract Hydrologic responses to earthquakes, including
liquefaction, changes in stream and spring discharge, changes in the properties of …

Mud volcanoes sometimes erupt within days after nearby earthquakes. The number of such
nearly coincident events is larger than would be expected by chance and the eruptions are …

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 …

Piercement structures such as hydrothermal vent complexes, pockmarks, and mud
volcanoes, are found in various geological settings but are often associated with faults or …

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 …

The mud volcano known as LUSI first erupted in May 2006 in East Java, Indonesia. The
eruption has continued for over two years, and potentially will continue for many years to …