标题：A regölyi kora vaskori sírhalom kőzetleleteinek előzetes archeometriai vizsgálati eredményei= Preliminary archaeometric study of rock types from the early-iron age mound grave in Regöly
摘要：Reg.ly Tolna megye ¨¦szaki r¨¦sz¨¦n fekszik, a Kapos ¨¦s a Kopp¨¢ny foly¨® .sszefoly¨¢s¨¢n¨¢l. A Strupka-Magyar birtokon l¨¦v. haloms¨ªr felt¨¢r¨¢sa 2011 kora tavasz¨¢n kezd. d.tt. A r¨¦g¨¦szeti megfigyel¨¦sek alapj¨¢n a halmot a kora vaskorban, a Kr.e. 7. sz¨¢zadban egy nagym¨¦ret. boronafal¨² ¨¦p¨¹let f.l¨¦ emelt¨¦k, melynek f.d¨¦mj¨¦t a sz¨¢m¨ªt¨¢sok szerint 54 bels. faoszlop tartotta. A k.zponti r¨¦sz be¨¢s¨¢saiban ¨¦s az ¨¦gett, hamus faszenes felt.lt¨¦s¨¦ben felt.n.en nagy mennyis¨¦g. k. zetanyag is el.ker¨¹lt. Kutat¨¢sunk c¨¦lja ezeknek a k.veknek a vizsg¨¢lata; sz¨¢mbav¨¦tele, t¨ªpusokba sorol¨¢sa, a k.zett¨ªpusok lel. hely¨¦nek, lehets¨¦ges forr¨¢ster¨¹let¨¦nek min¨¦l pontosabb behat¨¢rol¨¢sa. Ehhez makroszk¨®pos ¨¦s polariz¨¢ci¨®s mikroszk¨®pos m¨®dszereket haszn¨¢ltunk. A terepi munka sor¨¢n 4074 darab k.vet vizsg¨¢ltunk meg. Makroszk¨®pos megfigyel¨¦sek alapj¨¢n 8 k. zettani f.csoportot, ezeken bel¨¹l a sz¨ªn, sz.vet ¨¦s ¨¢sv¨¢nyos .sszet¨¦tel alapj¨¢n 27 alcsoportot ¨¢llap¨ªtottunk meg. A makroszk¨®pos megfigyel¨¦sek alapj¨¢n 140 reprezentat¨ªv p¨¦ld¨¢nyb¨®l v¨¦konycsiszolatos mikroszk¨®pos petrogr¨¢fiai elemz¨¦s k¨¦sz¨¹lt. Ennek eredm¨¦nye n¨¦mileg m¨®dos¨ªtotta a makroszk¨®posan kialak¨ªtott csoportokat, ez alapj¨¢n 7 f.- ¨¦s 17 alcsoportot v¨¦gleges¨ªtett¨¹nk. A haloms¨ªrban cs.kken. gyakoris¨¢guk szerint a k.vetkez. f. k. zetcsoportokat k¨¹l.n¨ªtett¨¹k el: karbon¨¢tos k.zetek, gr¨¢nit, homokk. , riolit, kvarcit, bazalt ¨¦s bazaltos piroklasztit. A k.zetek sz¨¢rmaz¨¢si hely¨¦t tekintve, a vizsg¨¢latok jelenlegi ¨¢ll¨¢sa szerint a gr¨¢nit a Velencei- hegys¨¦gb.l, a riolit Polg¨¢rdi-K. sz¨¢rhegyr. l, a homokk. kov¨¢s cement. alcsoportja, illetve a bazalt ¨¦s a bazaltos piroklasztit a Balaton-felvid¨¦kr.l, a kvarcit a Velencei-hegys¨¦gb. l ¨¦s/vagy a Tihanyi-f¨¦lszigetr.l, a karbon¨¢tos k. zetek kov¨¢s alcsoportja szint¨¦n a Tihanyi-f¨¦lszigetr.l val¨®sz¨ªn. s¨ªthet. . Egyes karbon¨¢tos k.zett¨ªpusok ¨¦s homokk.vek nyersanyaglel.hely¨¦nek meghat¨¢roz¨¢sa egyel.re m¨¦g nem volt lehets¨¦ges. A fenti val¨®sz¨ªn. s¨ªthet. lel.helyek Reg.ly mintegy 100 km-es k.rnyezet¨¦ben, att¨®l ¨¦szak, ¨¦szaknyugat fel¨¦ helyezkednek el
其他摘要：Reg.ly is located in the northern part of Tolna County, at the confluence of Kopp¨¢ny and Kapos Rivers. The mound on the Strupka-Magyar land was excavated in the summer of 2011 and according to the archaeological observations it was built in the Early-Iron Age. Rock fragments together with artefacts were mixed with soil and deposited in the middle of the structure. The aim of this research was to study the rock fragments present at the site: list them into types and characterize them from a petrological point of view in order to outline the most probable provenance of the raw materials. Macroscopic analysis and polarizing microscopy analysis were used to achieve this goal. During field work 4074 stone artefacts were examined. According to macroscopic observations 8 main lithotypes were defined and based on the different attributes (colour, mineral composition, fabric) 27 subgroups were determined. Based on macroscopic observations 140 representative specimens were selected for thin section analysis. Detailed petrographic analysis modified the previously established groups: 7 main and 17 subtypes were determined. The main rock types in decreasing frequency are the following: carbonate rocks, granites, sandstones, rhyolites, quartzites, basalts and basaltic pyroclastics. Based on the results the possible provenances of the rock types present at the site are the Velence Mountains for granites, Polg¨¢rdi-K.sz¨¢rhegy for rhyolites, the Balaton Highland for basalts, basaltic pyroclastics and one subgroup of the sandstones, the Velence Mountains and/or Tihany peninsula for quartzites and also Tihany peninsula for the siliceous subgroup of carbonate rocks. The provenance of some carbonate rocks and sandstone subtypes has not been possible to determine until now. My results show that the possible provenances of most of the rock types are to the N-NW of Reg.ly, within 100 km
