Petrographic and geochemical investigation of a stone adze made of nephrite from the site Balatonőszöd – Temetői dűlő (Hungary)

Péterdi, B.; Szakmány, G.; Judik, K.; Dobosi, G.; Kasztovszky, Z.; Szilágyi, V.; Maróti, B.; Bendő, Z.; Gil, G.

doi:10.7306/gq.1146

Artykuł - szczegóły

Tytuł artykułu

Petrographic and geochemical investigation of a stone adze made of nephrite from the site Balatonőszöd – Temetői dűlő (Hungary)

Autorzy

Péterdi B. , Szakmány G. , Judik K. , Dobosi G. , Kasztovszky Z. , Szilágyi V. , Maróti B. , Bendő Z. , Gil G.

Treść / Zawartość

Pełne teksty:

Peterdi_B_Petrographic_Geol. Quart_Vol.58_No 1_2014.pdf

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Identyfikatory

DOI

10.7306/gq.1146

Warianty tytułu

Języki publikacji

Abstrakty

The present study reports on results of petrographic and geochemical analyses on a stone adze from the archaeological site Balatonőszöd – Temetői dűlő (Hungary). This is the largest excavated site of the Baden Culture in Hungary (more than 200.000 m2) and has the longest continuous settlement history. In the site, features of the Balaton-Lasinja Culture (Middle Copper Age) and the Boleraz Culture were also found. Altogether 500 stone artefacts were found and registered. The present study reports on the results of the investigation of a unique stone adze made of nephrite, found on the site. The nephrite adze found in Balatonőszöd – Temetői dűlő has proved to be the first find made of nephrite having an established archaeological context in Hungarian prehistory. By applying detailed petrographic, geochemical and petrophysical methods as well as comparing data from technical literature we located the origin of the raw material of the nephrite adze. Its most probable source is the Northern part of the Bohemian Massif, Lower Silesia, a geological site near Jordanów (Poland).

Słowa kluczowe

archaeometry polished stone tools baden culture nephrite Balatonőszöd Hungary Jordanów Poland

Wydawca

Państwowy Instytut Geologiczny - Państwowy Instytut Badawczy

Czasopismo

Geological Quarterly

Rocznik

2014

Tom

Vol. 58, No. 1

Strony

181--192

Opis fizyczny

Bibliogr. 44 poz., rys., tab., wykr.

Twórcy

autor

Péterdi B.

peterdi.balint@gmail.com

Geological and Geophysical Institute of Hungary, Department of Geological and Geophysical Collections, H-1143, Stefánia út 14, Budapest, Hungary

autor

Szakmány G.

Eötvös Loránd University, Faculty of Science, Institute of Geography and Earth Sciences, Department of Petrology and Geochemistry, H-1117, Pázmány Péter sétány 1/C, Budapest, Hungary

autor

Judik K.

Hungarian Academy of Sciences, Research Centre for Astronomy and Earth Sciences, Institute for Geological and Geochemical Research, H-1112, Budaörsi út 45, Budapest, Hungary

autor

Dobosi G.

Hungarian Academy of Sciences, Research Centre for Astronomy and Earth Sciences, Institute for Geological and Geochemical Research, H-1112, Budaörsi út 45, Budapest, Hungary

autor

Kasztovszky Z.

Hungarian Academy of Sciences, Centre for Energy Research, Nuclear Analysis and Radiography Department, H-1121, Konkoly Thege Miklós út 29-33, Budapest, Hungary

autor

Szilágyi V.

Hungarian Academy of Sciences, Centre for Energy Research, Nuclear Analysis and Radiography Department, H-1121, Konkoly Thege Miklós út 29-33, Budapest, Hungary

autor

Maróti B.

Hungarian Academy of Sciences, Centre for Energy Research, Nuclear Analysis and Radiography Department, H-1121, Konkoly Thege Miklós út 29-33, Budapest, Hungary

autor

Bendő Z.

Eötvös Loránd University, Faculty of Science, Institute of Geography and Earth Sciences, Department of Petrology and Geochemistry, H-1117, Pázmány Péter sétány 1/C, Budapest, Hungary

autor

Gil G.

University of Wrocław, Institute of Geological Sciences, Pl. Maksa Borna 9, 50-205 Wrocław, Poland

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