Crinoidal limestones as Ordovician–Cretaceous geological heritage

IF 1.1 4区 地球科学 Q3 GEOLOGY
Dmitry A. Ruban
{"title":"Crinoidal limestones as Ordovician–Cretaceous geological heritage","authors":"Dmitry A. Ruban","doi":"10.1007/s13146-024-00959-0","DOIUrl":null,"url":null,"abstract":"<p>Attention to carbonate rocks is important in the contemporary geoheritage studies, although the related knowledge is yet to be complete. The consideration of the already published information can help to fill this gap. The present study offers interpretation of crinoidal limestones (encrinites) in the terms of geoheritage. A total of 180 literature sources (chiefly articles in international journals) were selected, and their content was analyzed. These sources trace the history of crinoidal limestones from the Ordovician to the Cretaceous; these carbonate rocks were especially common in the Carboniferous and Jurassic. Nonetheless, crinoidal limestones are relatively rare in the world’s sedimentary records, and, thus, they constitute a geoheritage resource. The multiple lines of evidence imply that these rocks can be assigned to ten geoheritage types. The existing works stress their scientific and educational utility. Their touristic importance is linked, particularly to the colors of these rocks, which associate with the common people’s emotions. The collected literature suggests that crinoidal limestones are chiefly a potential, not yet proven geoheritage resource. However, several in-situ and ex-situ geoheritage objects representing these rocks have already been established. Generally, the present study demonstrates a novel perspective for the application of carbonate sedimentology.</p>","PeriodicalId":9612,"journal":{"name":"Carbonates and Evaporites","volume":"77 1","pages":""},"PeriodicalIF":1.1000,"publicationDate":"2024-04-08","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Carbonates and Evaporites","FirstCategoryId":"89","ListUrlMain":"https://doi.org/10.1007/s13146-024-00959-0","RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q3","JCRName":"GEOLOGY","Score":null,"Total":0}
引用次数: 0

Abstract

Attention to carbonate rocks is important in the contemporary geoheritage studies, although the related knowledge is yet to be complete. The consideration of the already published information can help to fill this gap. The present study offers interpretation of crinoidal limestones (encrinites) in the terms of geoheritage. A total of 180 literature sources (chiefly articles in international journals) were selected, and their content was analyzed. These sources trace the history of crinoidal limestones from the Ordovician to the Cretaceous; these carbonate rocks were especially common in the Carboniferous and Jurassic. Nonetheless, crinoidal limestones are relatively rare in the world’s sedimentary records, and, thus, they constitute a geoheritage resource. The multiple lines of evidence imply that these rocks can be assigned to ten geoheritage types. The existing works stress their scientific and educational utility. Their touristic importance is linked, particularly to the colors of these rocks, which associate with the common people’s emotions. The collected literature suggests that crinoidal limestones are chiefly a potential, not yet proven geoheritage resource. However, several in-situ and ex-situ geoheritage objects representing these rocks have already been established. Generally, the present study demonstrates a novel perspective for the application of carbonate sedimentology.

Abstract Image

作为奥陶纪-白垩纪地质遗产的碎屑岩灰岩
在当代地质遗产研究中,对碳酸盐岩的关注十分重要,尽管相关知识尚不完备。对已出版资料的研究有助于填补这一空白。本研究从地质遗产的角度对皱纹石灰岩( encrinites)进行了解读。共选取了 180 篇文献资料(主要是国际期刊上的文章),并对其内容进行了分析。这些资料追溯了从奥陶纪到白垩纪的碎屑岩历史;这些碳酸盐岩在石炭纪和侏罗纪尤为常见。然而,在世界沉积记录中,碎屑岩灰岩相对罕见,因此,它们构成了一种地质遗产资源。多种证据表明,这些岩石可归入十种地质遗产类型。现有著作强调其科学和教育用途。它们在旅游方面的重要性,尤其与这些岩石的颜色有关,这些颜色与普通人的情感息息相关。收集到的文献表明,皱纹石灰岩主要是一种潜在的地质遗产资源,尚未得到证实。然而,代表这些岩石的一些原地和非原地地质遗产已被确立。总体而言,本研究为碳酸盐沉积学的应用展示了一个新的视角。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
求助全文
约1分钟内获得全文 求助全文
来源期刊
Carbonates and Evaporites
Carbonates and Evaporites 地学-地质学
CiteScore
2.80
自引率
14.30%
发文量
70
审稿时长
3 months
期刊介绍: Established in 1979, the international journal Carbonates and Evaporites provides a forum for the exchange of concepts, research and applications on all aspects of carbonate and evaporite geology. This includes the origin and stratigraphy of carbonate and evaporite rocks and issues unique to these rock types: weathering phenomena, notably karst; engineering and environmental issues; mining and minerals extraction; and caves and permeability. The journal publishes current information in the form of original peer-reviewed articles, invited papers, and reports from meetings, editorials, and book and software reviews. The target audience includes professional geologists, hydrogeologists, engineers, geochemists, and other researchers, libraries, and educational centers.
×
引用
GB/T 7714-2015
复制
MLA
复制
APA
复制
导出至
BibTeX EndNote RefMan NoteFirst NoteExpress
×
提示
您的信息不完整,为了账户安全,请先补充。
现在去补充
×
提示
您因"违规操作"
具体请查看互助需知
我知道了
×
提示
确定
请完成安全验证×
copy
已复制链接
快去分享给好友吧!
我知道了
右上角分享
点击右上角分享
0
联系我们:info@booksci.cn Book学术提供免费学术资源搜索服务,方便国内外学者检索中英文文献。致力于提供最便捷和优质的服务体验。 Copyright © 2023 布克学术 All rights reserved.
京ICP备2023020795号-1
ghs 京公网安备 11010802042870号
Book学术文献互助
Book学术文献互助群
群 号:481959085
Book学术官方微信