Volcaniclastic sediments, broadly defined as clastic deposits derived from the transport,
deposition and/or redeposition of the products of volcanic activity, have long been a …

This study presents a review on palaeogeographic implications and temporal variations of
glaucony covering both modern and ancient records. Phanerozoic glaucony preferably …

Plate motion and associated tectonics explain the location of magmatic systems along plate
boundaries [1], however, they cannot give satisfactory explanations of the origin of intraplate …

The urgent need to accelerate permanent anthropogenic carbon dioxide (CO 2) abatement
has led to a growing interest in in-situ CO 2 mineralisation globally. This review outlines the …

Hydrovolcanism is a type of volcanism where magma and water interact either explosively or
non-explosively. The less frequently used term, hydromagmatism, includes all the processes …

Density currents fed directly from subaqueous eruptions can be divided conceptually into
three groups based on modes of fragmentation and transport:(I) explosive fragmentation …

Volcanic-associated massive sulfide deposits (VMS deposits) have been studied in more
detail than their volcanic host rocks. Over the last 10 years, however, there has been a …

The study of volcano-ice interactions, or'glaciovolcanism', is a field experiencing exponential
growth. This comprehensive volume presents a discussion of the distinctive processes and …

The subaqueous phases of an eruption initiated approximately 85 m beneath the surface of
Pleistocene Lake Bonneville produced a broad mound of tephra. A variety of distinctive …

A new and detailed bathymetric map of the Myo**sho shallow submarine volcano provides
a framework to interpret the physical volcanology of its 1952–1953 eruption, especially how …