东巴尔干“Belemnitico rosso”相——岩石地层形式化的一个建议

IF 0.2 Q4 GEOSCIENCES, MULTIDISCIPLINARY
D. Sinnyovsky, D. Vangelov
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引用次数: 1

摘要

东巴尔干地区科特尔镇周围的中侏罗纪科特尔Olistostrome地层中,下侏罗纪含化石的红色石灰岩以滑岩的形式暴露,其中含有丰富的贝伦姆岩。在广泛认可的特提斯“菊石-罗索”相之后,我们建议将这一独特的红色含化石水平正式化为岩石地层标记,并命名为“贝伦米科-罗索(belemntico-roso)”。这将有助于创造具有科学和教育价值的有吸引力的地质遗迹,对公众理解科学具有巨大的解释潜力,以及在建筑中用作基石的“非原位”地球多样性元素。以未来“东巴尔干”地质公园的品牌名称创建原创地质旅游产品,旨在让所有人都能接触到地质。很有可能有一天,这个新术语会广受欢迎,并会让人们意识到它最初被定义的地质公园。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
The “Belemnitico rosso” facies in the East Balkan – a proposal of lithostratigraphic formalization
Lower Jurassic fossil-bearing red limestone with abundant belemnite rostra is exposed in the form of olistoliths included in the Middle Jurassic Kotel Olistostrome Formation in the surroundings of the town of Kotel in the East Balkan. Following the widely recognized Tethyan “ammonitico rosso” facies, we propose to formalize this distinctive red fossiliferous level as a lithostratigraphic marker under the name “belemnitico rosso”. This will contribute to the creation of attractive geosites of scientific and educational value with great interpretive potential for public understanding of science, as well as “ex situ” geodiversity elements used as building stones in construction. The creation of original geotourism products under the brand name of the future “East Balkan” Geopark seeks to make geology accessible to all. It is quite possible that someday, the new term will gain widespread popularity and will bring awareness to the geopark where it was first defined.
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