Abstract

Lava-flow structure and morphology help to understand the eruption style, emplacement mechanisms, and post-emplacement alterations such as weathering. It is challenging to quantify the subsurface structure like dike and the extent of multiple generations of lava flows that are buried under soil and vegetation cover. In this study, limitations of seismic methods for imaging a Dike in the Dive Ghat region of the Pune district located in the Deccan Volcanic Province are examined