图拉的化石矿床位于Kotel附近的Garnyovitsa地区,这是一个对保加利亚地质学具有历史价值的地质遗址

IF 0.2 Q4 GEOSCIENCES, MULTIDISCIPLINARY
D. Sinnyovsky, R. Stoilov
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引用次数: 0

摘要

Franz Toula于1890年首次描述了科特尔附近Garnyovitsa地区的化石矿床,该矿床被估计为具有国家意义的地质岩,对保加利亚地质具有历史价值。这是一个巨大的泥灰岩,镶嵌在科特Olistostrome组的中侏罗纪浊积岩中。它包含晚三叠纪(诺里安)的水生生物和珊瑚,早在19世纪末,保加利亚土地上的第一批探险家就发现了它们。鉴于该地区地理多样性高,且靠近科特尔,该地质点在未来的“东巴尔干”地质公园内具有巨大的地质旅游潜力。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Toula’s fossil deposit in the Garnyovitsa area near Kotel – a geosite of historical value for the Bulgarian geology
Fossil deposit first described by Franz Toula in 1890, in the Garnyovitsa area near Kotel is estimated as a geosite of a national significance with historical value for the Bulgarian geology. Here is cropping out a huge marl olistolith embedded among Middle Jurassic turbidites of the Kotel Olistostrome Formation. It contains Late Triassic (Norian) hydrozoa and corals, identified by the first explorers of the Bulgarian lands as early as the end of the 19th century. Given the high geodiversity of the area and the proximity to Kotel, this geosite has great potential for geotourism within the future geopark “East Balkan”.
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