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001-es BibID:BIBFORM063004
Első szerző:Farkas-Pető Anna
Cím:Archaeometric investigation of the stone tools of the Vatya culture (Pest county, Hungary) / Farkas-Pető Anna, Horváth Tünde, Papp István, Kovács-Pálffy Péter
Dátum:2014
ISSN:1842-4090 1844-489X
Megjegyzések:With the analysis of the middle Bronze Age (2000-1350 BC) Vatya culture findings in Pest county (Central Hungary) comprising of more than 400 polished stone tools and instrument tools this is the first archaeometric study with such scale in Hungary. In order to characterize petrographically the raw material of the stone tools macroscopic and microscopic stone analyses were made together with mineralogical and geochemical analyses. In the course of the work a new digital database the ArchaeometricStone Tool Database was established. Based on the results, the material of the instrument stones is mainly sandstone and quartzite that were easy to collect from their source areas. Local volcanics, mostly amphibole containing andesite variations dominated among the material of the polished stone tools. Ophiolites (metamorphic basic rocks, serpentinized basic and ultrabasic rocks) were the raw-material of stone axes thatindicate either more distant travels for raw-material or exchange import.
Tárgyszavak:Természettudományok Földtudományok idegen nyelvű folyóiratközlemény külföldi lapban
Archaeometrics
Carpathian Basin
Vatya culture
polished stone tools
instrument tools
Megjelenés:Carpathian Journal of Earth and Environmental Sciences. - 9 : 1 (2014), p. 81-94. -
További szerzők:Horváth Tünde Papp István (1980-) (vegyész) Kovács-Pálffy Péter
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001-es BibID:BIBFORM094891
Első szerző:Vincze László
Cím:Origin of red clays around Miskolc (North Hungary) / László Vincze, Miklós Kozák, Péter Kovács-Pálffy, István Papp, Zoltán Püspöki
Dátum:2006
Megjegyzések:During the geological mapping of the northern foreland of the Bükk Mountains red clay occurrences were identified by the Department of Mineralogy and Geology, University of Debrecen. Red clays are underlain by Triassic limestone and Miocene, mainly Sarmatian siliciclastic sediments containing tuffaceous bentonites. Based on the sedimentological (grain-size distribution), mineralogical (micromineralogy, X-ray diffraction, thermal analysis) and major element geochemical (ICP-OES) examinations, it can be established that the studied red clays belong to the less weathered, so-called ?reddish clay" type. Montmorillonite prevails among clay minerals, while kaolinite is subordinate. Considering the strong sedimentological and mineralogical similarity with the underlying Miocene sediments, the red clays were probably originated by the weathering of the Miocene sediments under a moderately warm and dry climate. Taking lithostratigraphic features into account, the examined red clays can be classified as members of the Pliocene-Pleistocene Tengelic or Kerecsend Red Clay Formation.
Tárgyszavak:Természettudományok Földtudományok idegen nyelvű folyóiratközlemény hazai lapban
folyóiratcikk
red clay
Bükk Mountains
Pliocene
Pleistocene
Megjelenés:Acta Mineralogica-Petrographica. - 46 (2006), p. 15-27.
További szerzők:Kozák Miklós (1948-) (geológus) Kovács-Pálffy Péter Papp István (1980-) (vegyész) Püspöki Zoltán (1972-) (geológus)
Pályázati támogatás:NKFP No. 3/083/2001.
Egyéb
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