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  1. 2 Študijné zvesti

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  1. 2 Jahn J.

  2. 2 Samuel M.

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  1. 1 2013

  2. 1 2009

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PETROGRAFICKÁ ANALÝZA STAVEBNÉHO MATERIÁLU Z VÝSKUMU KOSTOLA NARODENIA PANNY MÁRIE VO VEĽKÝCH CHYNDICIACH

100%
Jahn J., Samuel M.
Študijné zvesti
|
2013
|
issue 53
149 - 158
EN
During the rescue exploration of the Church of the Nativity of Virgin Mary in Veľké Chyndice (Nitra district) were taken ten samples of rocks, which had been used as building material in various stages of its construction and historical development. Their petrographic characteristics were defined by macroscopic analysis, and, subsequently, possible provenance of the rocks was verified. From the oldest Roman part of the church (13th century) built with bricks comes the sample of stone lining of a portal made of rhyolite, or rhyodacite, and neovulcanites brought from the mountains of central Slovak, i.e. from the distance of 30–50 km. The remains of the portal´s threshold are from red organogenic limestone, coming probably from the quarries at the village of Tardos in Hungary. These quarries of “red marble” had been used already by the end of the 12th century and they supplied an extensive territory of the Kingdom of Hungary in Middle Ages. Two other samples, obtained from the stone-brick foundations of a perished medieval sacristy, were determined as ignimbrites taken from a quarry in the 20 km distant Obyce. It was found out that for the foundations of the Baroque annex building (18th century) were exclusively used the crinoid limestones, quarried in the cadastre of a nearby (10 km) village of Kolíňany. The cover of a crypt, attached in the 18th century, or in the 19th century, to the northern wall of the Baroque aisle, was made of the pyroxenic andesite. Its closest occurrences are known from the quarries with historical mining at Machulince (16 km) and Obyce (20 km) in Pohronský Inovec. The samples were also taken from three different parts of a gravestone of the local priest G. Alapy (+1746). It was found out that the gravestone´s cross was made of crystalloclastic ashy tuff, with a probable source of the raw material being central Slovak neovulcanites, situated in a wider vicinity of Banská Štiavnica. The upper and lateral part of the gravestone is made of crystalloclastic sand tuff, also coming from Middle Slovak neovulcanites.
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INDÍCIE SKLÁRSKEJ(?) VÝROBY V POHORÍ TRIBEČ

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Jahn J., Samuel M.
Študijné zvesti
|
2009
|
issue 46
87 - 90
EN
The contribution gives information on evidences of extinct metallurgy in the Tribeč mountain range area, to which no historical sources exist and both kind and chronology of which have not been acceptably answered until recently. The results of surface prospection on some of these sites make us assume their connection with a modern-era glass production.
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