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The provenance of stone tabernacle and altar table from the St. Emmeram's Cathedral (Nitra City)

机译:圣埃默拉姆大教堂(尼特拉市)的石头帐幕和坛台的出处

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An unique stone Renaissance tabernacle (1497) was discovered in the upper church of the St. Emmeram's Cathedral (Nitra) in the year 2007. The rocks from the tabernacle and probably altar table of the same age come from the Gerecse Mts. in northern Hungary. The parts of the tabernacle and altar table are from the Liassic red nodular limestone, which was quarried between Tardos and Lábatlan also in time when the tabernacle was made. On the basis of the stable oxygen and carbon isotope the analysed sample can be compared with the samples from Bányahegy quarry near Tardos and the samples from Late Gothic and Renaissance fountains and font of Matthias Corvinus king palace in Visegrád of the 15th century. Parts of the tabernacle are also from yellowish crinoidal limestone of the Lower Cretaceous which is probably from the Tata quarry. The altar table was prolonged to both sides by tuff from Obyce probably during the building of new Baroque main altar in the 18th century. "Gerecse red marble" was used almost in the same time in Gothic tombstone (1492) and Renaissance tabernacle (1497) both from the upper church of the St. Emmeram's Cathedral.
机译:2007年,在圣埃默拉姆大教堂(Nitra)的上层教堂发现了一个独特的文艺复兴时期的会幕(1497)。会幕和同年龄的祭坛上的岩石来自盖雷塞(Gerecse)山。在匈牙利北部。会幕和祭坛的桌子部分来自Liassic红色节状石灰岩,也是在制造会幕时在Tardos和Lábatlan之间开采的。在稳定的氧和碳同位素的基础上,可以将分析后的样品与塔多斯附近的Bányahegy采石场的样品以及15世纪维谢格拉德维特格拉德的Matthias Corvinus王宫的字体和晚期哥特式和文艺复兴时期喷泉的样品进行比较。会幕的某些部分也来自下白垩统的淡黄色海百合状灰岩,可能来自塔塔采石场。奥比斯(Obyce)的凝灰岩使祭坛的台面向两侧延长,大概是在18世纪建造新的巴洛克式主祭坛时。圣埃梅拉姆大教堂的上层教堂的哥特式墓碑(1492年)和文艺复兴时期的会堂(1497年)几乎同时使用了“希腊红色大理石”。

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