A survey of presumably hydrocarbons-containing water ponds in the Kog hills (Pannonian Basin, NE Slovenia)

In 2011, we were called to survey several shallow water ponds (wp) in the Kog (KOG) area, which geologically belongs to an antiform termed the Ormož-Selnica Antiform (OSA) (Fig.1). It is built of Neogene marls, sands to sandstones, shales, limestones,Read more