A research group was interested in studying the origin of moldavites found in Poland. In particular, they wanted to find out if the moldavites were transported from the Lusatian sub-strewn field or if they were deposited directly at the time of impact forming a new separate sub-strewn field.
The TESCAN SEM VEGA3 XM was used to image the surface and polished thin sections of the moldavite specimens.