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 …

The present study is probably the first of its kind in the Deccan Volcanic Province (DVP) that
deals in detail with the morphology and emplacement of the Deccan Trap flows, and …

Unlike pahoehoe, documentation of true a′ a lavas from a modern volcanological
perspective is a relatively recent phenomenon in the Deccan Trap (eg Brown et al., 2011 …

Squeeze-ups are common features of basaltic lava flow-fields on Earth. Squeeze-ups,
rootless autointrusions of lava, drive intraflow resurfacing of active flow-fields, and the term is …

The physical features and morphologies of collections of lava bodies emplaced during
single eruptions (known as flow fields) can be used to understand flood basalt emplacement …

We geomorphometrically characterize the tectonics near the microseismically active Nanded
region, Maharashtra, India. We used the geomorphic indices of active tectonics in 32 sub …

Large igneous provinces (LIPs) form in both oceanic and continental settings by the
emplacement and eruption of voluminous magmas ranging from basalt to rhyolite in …

The pahoehoe–aa transition for a flow exposed near Bodshil village from the western part of
the Deccan Volcanic Province (DVP) is reported for the first time. The∼ 1-km-long Bodshil …

Geoheritage, geoconservation, and geotourism studies are of increasing interest worldwide
because of their scientific, societal, cultural, and aesthetic value. Volcanic areas (whether …

Inflated and compound pahoehoe flows have been identified within the central Paraná
Continental Flood Basalts based upon their morphology, surface features, and internal …