Abstract The South China Sea, which is located to the southeast of Eurasian continent,
developed as the result of intra-continental rifting and seafloor spreading on the South …

The architecture of subsurface magma plumbing systems influences a variety of igneous
processes, including the physiochemical evolution of magma and extrusion sites. Seismic …

Dyke swarms are common on Earth and other planetary bodies, comprising arrays of dykes
that can extend laterally for tens to thousands of kilometres. The vast extent of such dyke …

Continental rifting and ocean basin formation is occurring today in the Red Sea, providing a
possible modern analogue for the creation of mid-ocean ridges. Yet many of the seafloor …

Ancient hydrothermal vent complexes have released large volumes of greenhouse gases in
the past causing global warming, and similar modern vent structures are potential …

Many sedimentary basins host thick evaporite (salt) deposits. Some of these basins also
host extensive igneous intrusion networks. It thus seems inevitable that, in some locations …

Many prospective sedimentary basins contain a variety of extrusive volcanic products that
are ultimately sourced from volcanoes. However, seismic reflection‐based studies of …

Based on 3D and 2D high-resolution multichannel seismic reflection data in the Western
High-Sea of Marmara, this study reviews shallow gas occurrence and related structures and …

There is growing evidence that intrusive magmatic bodies such as sills and dikes can
influence the migration of fluids in the deep subsurface. This influence is largely due to …

Igneous sills emplaced at shallow levels in sedimentary basins commonly uplift the
overburden and free surface. Uplift produces dome-shaped forced folds that may host …