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Sarmatian biomicritic limestone with ooids from unknown locality used in building of Medieval St. Emmeram Church of Nitra

机译:萨玛提亚生物微晶灰岩,含来自未知地区的Ooids,用于建造尼特拉中世纪圣埃默拉姆教堂

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摘要

The most of stone building blocks on faces of Romanic St. Emmeram Church of Nitra is cut from Sarmatian limestone. The blocks in secondary position probably come from the first stone church in our territory of the 9th century that was built by Pribina prince (Pivko, 2007). The stone blocks are from whitish porous biomicritic limestone. It is the most often homogenous, medium-grained (to coarse-grained) limestone with grains about 0.3-0.5 mm, rarely it is evidently oomicritic, sometimes fine-grained biomicrite. Micrites are locally washed. Many shells are dissolved. Locally there are large fossils diffused in finer matrix or as very coarse layer with gastropods and bivalve molds, worm tubes and algaes. In one stone block the lumachelle with probably carbonate clasts up to 4 cm also bored are present.
机译:尼特拉古罗马圣埃默拉姆教堂的表面上,大多数石材都是从萨尔马蒂石灰岩切割而成的。处于次要位置的砖块可能来自我们9世纪时由Pribina王子建造的第一座石教堂(Pivko,2007年)。石块来自发白的多孔生物微石灰石。它是最均匀的中粒(至粗粒)石灰石,颗粒约0.3-0.5毫米,很少是明显的卵石质,有时是细粒的生物陨石。微晶石被局部洗涤。许多贝壳都溶解了。局部有大型化石,散布在较细的基质中或极粗的层中,有腹足动物和双壳类霉菌,蠕虫管和藻类。在一个石头砌块中,存在着可能长达4厘米的碳酸盐岩屑,也很无聊。

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