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PÉTERDI, Bálint; BENDŐ, Zsolt; SZAKMÁNY, György; KASZTOVSZKY, Zsolt: Possible sources of nephrite artefacts found on Hungarian archaeological sites ( preliminary results ). Nephrite artefacts from Hungarian sites. Cca. 25 pcs . 10 pcs . Nephrite artefacts from Hungarian sites.
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PÉTERDI, Bálint; BENDŐ, Zsolt; SZAKMÁNY, György; KASZTOVSZKY, Zsolt: Possiblesources of nephriteartefactsfoundon Hungarianarchaeologicalsites (preliminaryresults)
NephriteartefactsfromHungariansites Cca. 25 pcs. 10 pcs.
NephriteartefactsfromHungariansites Cca. 25 pcs. 10 pcs.
NephriteartefactsfromHungariansites Cca. 25 pcs. 10 pcs.
NephriteartefactsfromHungariansites Cca. 25 pcs. 10 pcs.
NephriteartefactsfromHungariansites Cca. 25 pcs. 10 pcs.
NephriteartefactsfromHungariansites Cca. 25 pcs. 10 pcs.
Classificationaccordingtonephriteformationaltypes (basedonbulk rock chemistry, measuredwith PGAA)
Microscopicfeatures (fabric, enclosedminerals, measuredwithnon-destructive SEM-EDX, the „originalsurfacemethod”) Type 1: „pure” tremolite-nephritewith minor magnetite, limonite, ± ilmenite, ± pseudomorphsafterpyroxenes
Microscopicfeatures (fabric, enclosedminerals, measuredwithnon-destructive SEM-EDX, the „originalsurfacemethod”) Type 1: „pure” tremolite-nephritewith minor magnetite, limonite, ± ilmenite, ± pseudomorphsafterpyroxenes
Microscopicfeatures (fabric, enclosedminerals, measuredwithnon-destructive SEM-EDX, the „originalsurfacemethod”) Type 2: „pure” actinolite-nephrite with minor magnetite, limonite, ± ilmenite Type3: „pure” nephrite (act + trem) with minor chlorite, ± pseudomorphsafterpyroxenes
Microscopicfeatures (fabric, enclosedminerals, measuredwithnon-destructive SEM-EDX, the „originalsurfacemethod”) Type 4: actinolite-nephritewithchlorite, relictclinopyroxenes (diopside), pseudomorphsafterpyroxenes, spinel (chromite), garnet (grossular), (magnetite, limonite, ± apatite, ± titanite)
Microscopicfeatures (fabric, enclosedminerals, measuredwithnon-destructive SEM-EDX, the „originalsurfacemethod”) Type 4: actinolite-nephritewithchlorite, relictclinopyroxenes (diopside), pseudomorphsafterpyroxenes, spinel (chromite), garnet (grossular), (magnetite, limonite, ± apatite, ± titanite)
Microscopicfeatures (fabric, enclosedminerals, measuredwithnon-destructive SEM-EDX, the „originalsurfacemethod”) Type5: nephrite (tremolite ± aktinolite) withchlorite, relictclinopyroxenes, spinel (chromite), butwithoutgarnet
Microscopicfeatures (main amphiboltype, measuredwithnon-destructive SEM-EDX, the „originalsurfacemethod”)
Nephritesourceswith detaileddescriptions and/or chemicaldata (Switzerland, boundaries of theBohemianMassif
Nephritesourceswith detaileddescriptions and/or chemicaldata (Switzerland, boundaries of theBohemianMassif
Nephritesourceswith detaileddescriptions and/or chemicaldata (Switzerland, boundaries of theBohemianMassif
Nephritesourceswith detaileddescriptions and/or chemicaldata (Switzerland, boundaries of theBohemianMassif
Nephritesourceswith detaileddescriptions and/or chemicaldata (Switzerland, boundaries of theBohemianMassif
Nephritesourceswith detaileddescriptions and/or chemicaldata (Switzerland, boundaries of theBohemianMassif
Nephritesourceswith detaileddescriptions and/or chemicaldata (Switzerland, boundaries of theBohemianMassif
Classificationaccordingtonephriteformationaltypes, comparingartefactswithpossiblesources (basedonbulk rock chemistry, fromreferencedata and new PGAA data)
Microscopicfeatures (main amphiboltype, comparingartefactswithpossiblesources measuredwithnon-destructive SEM-EDX, the „originalsurfacemethod” and also EPMA forthegeologicalsources)
Most probablesources (preliminaryresults) Jordanów Mur-river? Oberhalbstein
Acknowledgements Weareindebtedtothearchaeologistsfor affording us the opportunity to study the artefacts (especiallyfor Katalin T. Biró, Tünde Horváth, Erzsébet Nagy, Szilvia Honti, Péter Németh, Judit P. Barna, Csilla Száraz, László Hotváth, Judit Regenye, Marcella Nagy, Ádám Kőszegi, Gábor Ilon, Gyula Kerékgyártó, Ernő Wolf). Wewanttothankthecolleagues and othersforhelpingusinourworkinmanyways (especiallyforVeronika Szilágyi, Katalin Gméling, Boglárka Maróti, Ágnes Veres, Emma P. Szabó, Zoltán Lantos, Péter Papp). Wearegratefultoallthescientists, whoseworkswereusedasreference (Belgya T., Bendő Zs., Bradák B., Cheng H.S., Cholewa P., D’Amico C., De Quervain F., Dietrich V., Dobosi G., Foltyn E. M., Foltyn E., Friedel O., Füri J., Gan F.X., Gasparotto G., Ghedini M., Giess H., Gunia P., Heierli J., Horváth T., Jochemczyk L., Józsa S., Judik K., Kalkowsky E., KasztovszkyZs., Kis Z., Kostov, R.I., KovářJ.J., Kuča M., Majerowicz A., Meyer A.B., Molnár M., Péterdi B., Preiswerk H., Přichystal A., RévayZs., Sachs A., Schmidt C., Schneider A., Skoczylas J., Starnini E., S. Svingor É., Staub R., Szakmány Gy., Szentmiklósi L., Szilágyi V., SzolgayZs., T. Biró K., Traube H., Welter O.A., Wojciechowski W., Wojcik A., Zentai L., Zhang Z.W.) Special thanks go to the Hungarian Scientific Research Fund OTKA Grant No. K 62874 and K 100385 for their financial support.