标题：Különösen gazdag kőbalta és csiszolt kőeszköz leletegyüttes előzetes vizsgálati eredményei Diósviszlóról = Preliminary results on a unique collection of axes and polished stone tools from Diósviszló67
摘要：The goal of this study was the petrological and geochemical investigation of the polished stone artefacts of the Korinek-collection, as well as the grouping of the raw materials and the determination of the possible provenance areas of the artefacts. These artefacts were collected as straight finds by Dr. L¨¢szl¨® Korinek from a plow-land area that located between Di¨®sviszl¨® and M¨¢rfa villages (South Hungary). The collection contains more than one hundred chipped stone tools and fragments, also ceramics and 87 pieces of polished stone artefacts. The artefacts are predominantly axes, but some adzes, chisels, grinding stones, handstones and perforated pendants also belong to the collection. The majority of the artefacts are fragmented, but some entire finished and semi-finished tools also occur in the collection. The ceramics found together with them suggest that some of the artefacts originated from the Transdanubian Linear Pottery culture. Beyond the provenance analysis the authors tried to link between particular artefacts of the collection and stone artefacts that derived from the recently excavated archaeological site of HT 104 near Di¨®sviszl¨® village. The track of this excavation partially overlaps the source area of the Korinek-collection.Macroscopic description and magnetic susceptibility measurements were done on all samples, polarising microscopic petrography, mineral chemistry by SEM-EDX and PGNAA bulk chemical analyses were used on selected representative artefacts. The entire artefacts were analysed by non destructive methods only. We used a completely non-destructive SEM-EDX method, which is absolutely new developing in the analyses of polished stone tools. As regards the raw materials the majority of the artefacts were made from the late Cretaceous fine grained dyke or subvolcanic alkaline magmatic rocks of the closely Mecsek Mountains. Although a few alkaline magmatic rock samples come from ulterior localities. The provenance of the rare, hainite bearing sodalite phonolite is the Moldanubian zone, most probably .elenicky Vrch. There is relatively high amount of greenschists-metabasites-contact metabasites which have high varieties. We could identify Fels.csat¨¢r, Pezinok and .elezn. Brod types amongst them while one of them presumably derived from the Engadin tectonic window of the Western Alps. The majority of the grindstone raw materials derived from the Permian red sandstones of the Balaton Highland. Other raw materials are represented by few pieces only: basanite, serpentinite, milonite, siltstone, volcanoclastic siltstone, limestone and quartzite. We found connection between the Korinek-collection and the samples from Di¨®sviszl¨® excavation site. Regarding the raw materials of the collection and the excavation site the alkaline magmatic rock types are very similar and two artefacts types made of sandstone are completely identical
