Structures that facilitate fluid migration are common in sedimentary basins. We document
several possible hydrothermal and/or volcanic vents located above a> 157 km2, late …

We analyse occurrences of gas hydrates and free gases above a 1200 km 2 complex of
igneous volcanoes and sills using newly acquired three-dimensional (3D) seismic data in …

Volcanoes represent one of the most critical geological settings for hazard modelling due to
their propensity to both unpredictably erupt and collapse, even in times of quiescence …

Seafloor mounds are enigmatic features along many continental margins and are often
interpreted as gas hydrate **oes, seep deposits, mud volcanoes, or hydrothermal …

Background Cenozoic rifting in the Arctic and the resulting opening of the Labrador Sea and
the Fram Strait are typically associated with the movement of the Svalbard Archipelago c …

Late Cretaceous magmatism has been widely documented in the Great South Basin (GSB)
of New Zealand, which is mainly relevant to the Gondwana break-up (105–83 Ma) and the …

The Little Minch Sill Complex consists of a series of stacked, multi-leaved Paleocene
dolerite sills, which have primarily intruded into Mesozoic sedimentary rocks and Paleocene …

Long-lasting widespread volcanism in Mars is testified by the Tharsis volcanic province, one
of the largest volcanic provinces with the largest shield volcanoes of the Solar System …

The lateral distribution of strength within the crust is non-uniform, dictated by crustal lithology
and the presence and distribution of heterogeneities within it. During continental extension …

This chapter focuses on two critical and interrelated themes:(1) integration of different
stratigraphical datasets, particularly through quantitative techniques (Section 17.2) to allow …