内沃夫斯基古暗礁及相关深海地层:来自鲁德阿尔泰的高价值晚泥盆世地质遗产

Heritage Pub Date : 2024-05-01 DOI:10.3390/heritage7050113
Jaroslav M. Gutak, D. Ruban
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引用次数: 0

摘要

鲁德尼阿尔泰是阿尔泰造山带的西段。其丰富的地质资源使其地质遗产勘探成为当务之急。在 Loktevsky 地区(俄罗斯联邦阿尔泰地区)进行的调查发现了三个著名的地点,建议将其作为地质遗迹。为确定这些地方的地质遗产特征和价值,进行了实地调查和定性与半定量(按标准评分)研究。内沃夫斯基古礁石是一个相对较大的地质复合体,代表了在火山建筑物上发育的弗拉斯尼安礁石。Zolotukha段和Razdolnoe段是较小的地质群,分别代表吉文特-弗雷西尼亚过渡时期和弗雷西尼亚晚期的深海面貌。在内维夫斯基古礁石中确定了七种地质遗产类型,在其他两个地质群落中确定了四种地质遗产类型。通过对稀有性、可获取性、脆弱性和其他特性的研究,可以对内维夫斯基古礁石进行全球排名,对其他两个地质群落进行区域排名。这三个拟议的地质群需要采取特别的地质保护措施(尤其是其丰富的化石含量)。古礁石可用于促进当地旅游业的发展。
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Neverovsky Palaeoreef and Associated Deep-Marine Facies: High-Value Late Devonian Geoheritage from the Rudny Altai
The Rudny Altai is a western segment of the Altai orogenic belt. Its geological richness makes its geoheritage exploration an urgent matter. Investigations in the Loktevsky District (Altai Region, Russian Federation) have led to the finding of three notable localities, which are proposed as geosites. Field investigations and both qualitative and semi-quantitative (scoring by criteria) studies were carried out to characterize and value the geoheritage properties of these localities. The Neverovsky palaeoreef is a relatively large geosite, representing a Frasnian reef developed on a volcanic edifice. The Zolotukha section and the Razdolnoe section are smaller geosites representing deep-marine facies of the Giventian–Frasnian transition and the late Frasnian, respectively. Seven geoheritage types are established in the Neverovsky palaeoreef, and four geoheritage types are established in the other two geosites. Examination of rarity, accessibility, vulnerability, and other properties allows the ranking of the Neverovsky palaeoreef globally and the other two geosites regionally. The three proposed geosites need special geoconservation measures (especially regarding their rich fossil content). The palaeoreef can be used for the promotion of local tourism.
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