Abstract The Deccan Volcanic Province (DVP), covering presently an area of 0.5 million km
2, and estimated to be 2–3 times larger during the Upper Cretaceous-Paleocene, is one of …

Fractures generated by internal fluid pressure, for example, dykes, mineral veins, many
joints and man-made hydraulic fractures, are referred to as hydrofractures. Together with …

This is the first detailed report and analyses of deformation from the W part of the Deccan
large igneous province (DLIP), Maharashtra, India. This deformation, related to the India …

Three large dike systems are exposed in the Deccan Traps flood basalt province of India:
the dominantly north–south-trending west coast swarm, the east–west-trending Narmada …

The stages of landscape brought by Wainganga river cycle of erosion are precisely
characterized and determined by progressive returns of maximum relief ratio (above 70%) …

Giant circumferential dyke swarms have a primary geometry that is quasi-circular or quasi-
elliptical. Examples and possible examples described previously or identified in this study …

A review of the existing knowledge on the Deccan Volcanic Province of India shows that it
has a significant geographic bias towards the western parts, while the rest of the province is …

During a volcanic unrest period with magma-chamber rupture, fluid-driven fractures (dykes)
are injected either from deep reservoirs or shallow magma chambers. Subsequently, the …

Lava flows with preserved bases and brecciated upper crusts constitute a morphological
type that differs in character from typical pahoehoe and a'a: such flows have been reported …

Although subparallel swarms of dikes are thought to be the primary feeders to voluminous
volcanic eruptions, increasing recognition of volumetrically significant sill complexes …