Abstract
Abstract A boring for water supply at Bjornstorp E of Lund was placed in the south-western faultline of the Archaean horst Romeleasen; it penetrated 66 metres of Ceno. manian greensand at a depth between 61 and 127 metres. As far as concerns Sweden this greensand was not known before, except in two deep borings at Hollviken, the south-westernmost corner of the province of Scania, were it was pierced ten years ago at a depth of 1 200 metres. The greensand contained ostracods, foraminifers, and macroscopic shell fragments, pebbles of sedimentary rocks, a piece of asphalt and probably traces of other bituminous products.
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