都柏林中部冰川前河道砾石沉积物特征

Q4 Earth and Planetary Sciences Irish Journal of Earth Sciences Pub Date : 2022-01-07 DOI:10.3318/ijes.2021.39.4
Stephen Kealy, M. Long, S. Mccarron, M. Fleming, M. Friedman
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引用次数: 0

摘要

摘要:本文报道了都柏林市冰期前河道特征关键路段的交互式三维模型的制作。研究区域规划了重要的基础设施发展,最重要的是都柏林地铁线路项目。这里提出的模型代表了第四纪期间由几个离散的冰川和消冰川阶段产生的复杂沉积环境,与以前发表的关于该地区的报告一致。研究区典型的地质特征为:石炭系灰岩基岩中的第四纪河道、间歇式下冰碛、大型河流-冰川砂砾石沉积和间歇式上冰碛。描述了用于管理和创建三维地面模型的数字软件,该软件由几个商用模块组成。数字三维地面模型作为单一数据存储库特别有用,可以在获得新数据时轻松更新。大量岩土工程试验的解释证实,河流-冰川砂和砾石矿床相对不均匀,但可以大致表征为中等至非常致密的微砂质至砂质砾石。简单的指数测试,如粒度分布分析和标准渗透测试,对于材料表征和剖面解释都非常有用,尽管后一种测试结果可能会受到鹅卵石或巨石存在的影响。地球物理测试,特别是横波速度剖面,被证明是这些矿床非常有用的表征工具。这项工作的发现与都柏林研究地区的侵蚀特征、冰川沉积模式和一般地质历史的总体认识是一致的。这是一篇基于知识共享署名许可的开放获取文章,该许可允许在任何媒体上使用、分发和复制,前提是正确引用原始作品。由IReL提供的开放获取资金。
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Characterisation of gravel deposits in the pre-glacial channel, Central Dublin
Abstract:This paper reports on the production of an interactive 3-dimensional model over a key section of a pre-glacial channel feature in Dublin City. Significant infrastructural developments, most importantly the Dublin MetroLink project, are planned in the study area. The model presented here represents a complex depositional environment produced by several discrete phases of glaciation and deglaciation during the Quaternary and is consistent with previous published reports on the area. The geology in the study area typically consists of a Quaternary channel cut into the Carboniferous limestone bedrock, an intermittent lower glacial till, a large fluvio-glacial sand and gravel deposit and an intermittent upper glacial till.The digital software used to manage and create a 3-dimensional ground model is described and is comprised of several commercially available modules. The digital 3-dimensional ground models are particularly useful as a single data repository which can easily be updated as new data becomes available. Interpretation of a large body of geotechnical tests confirmed the fluvio-glacial sand and gravel deposit is relatively non-homogenous but can be broadly characterised as a medium to very dense slightly sandy to sandy gravel. Simple index tests, such as particle size distribution analyses and standard penetration testing, are very useful for both material characterisation and interpretation of profiles, albeit the latter test results can be influenced by the presence of cobbles or boulders. Geophysical testing, especially shear wave velocity profiling, was shown to be a very useful characterisation tool in these deposits. The findings of this work are consistent with the overall understanding of the erosional features, pattern of glacial deposition and general geological history of the study area in Dublin.This is an open access article under the terms of the Creative Commons attribution license, which permits use, distribution and reproduction in any medium, provided the original work is properly cited. Open Access funding provided by IReL.
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来源期刊
Irish Journal of Earth Sciences
Irish Journal of Earth Sciences Earth and Planetary Sciences-Earth and Planetary Sciences (all)
CiteScore
0.90
自引率
0.00%
发文量
2
期刊最新文献
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