人为引起的休眠流的重新激活?奥地利Ischl盐矿历史矿物图的地貌学解释

IF 1.3 4区 工程技术 Q3 ENGINEERING, GEOLOGICAL Quarterly Journal of Engineering Geology and Hydrogeology Pub Date : 2023-03-02 DOI:10.1144/qjegh2022-012
H. J. Laimer
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引用次数: 0

摘要

这个来自北钙质阿尔卑斯山脉的案例研究展示了历史采矿文件在地貌学目的中的应用,特别是在滑坡事件记录方面。对奥地利Ischl盐矿长达200年的采矿地图进行地貌测绘和解释,揭示了在一个工程地质调查充分的地区存在一条500米长的土流。基于cad创建的多专题地图(地表和地下特征)得出的结论是,1850年至1934年间,由于采矿沉陷,史前土流部分重新激活。历史土流的衰竭带位于矿山主要塌陷带的正上方。恢复活动最有可能是由于延展性的Haselgebirge组内沉降槽的缓慢发展导致斜坡底部下降。特别是对于采矿后地区的工程地貌学任务,在那里地下设施不再可用,历史采矿图分析和地貌学测绘相结合的方法可以被认为是一个有前途和具有成本效益的工作概念。补充资料:表1所列的历史平面图和剖面图可在:https://doi.org/10.6084/m9.figshare.21740459.v1上找到。专题文集:本文是人类世工程地质学和水文地质学文集的一部分,可在https://www.lyellcollection.org/topic/collections/engineering-geology-and-hydrogeology-of-the-anthropocene上找到
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Human-induced reactivation of a dormant earthflow? A geomorphological interpretation of historical mining maps of the Ischl salt mine (Austria)
This case study from the Northern Calcareous Alps demonstrates the utilization of historical mining documents for geomorphological purposes, especially for landslide event documentation. The combination of geomorphological mapping and interpretation of up to 200 years old mining maps of the Ischl salt mine (Austria) revealed the existence of a 500 m long earthflow in an engineering geologically well-investigated area. The CAD-based creation of a polythematic map (surface and subsurface features) led to the conclusion that a prehistoric earthflow has been partly reactivated between 1850 and 1934 due to mining subsidence. The depletion zone of the historical earthflow is situated directly above the major collapse zone of the mine. Reactivation was most likely caused by the lowering of the slope base due to slow development of a subsidence trough within the ductile Haselgebirge Formation. Particularly for engineering geomorphological tasks in post-mining-areas, where subsurface facilities are no longer accessible, a combined approach of historical mining map analysis and geomorphological mapping can be regarded as a promising and cost-effective working concept. Supplementary material: historical ground plans and cross sections which are listed in Tab. 1 are available at: https://doi.org/10.6084/m9.figshare.21740459.v1 Thematic collection: This article is part of the Engineering Geology and Hydrogeology of the Anthropocene collection available at: https://www.lyellcollection.org/topic/collections/engineering-geology-and-hydrogeology-of-the-anthropocene
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来源期刊
CiteScore
3.40
自引率
14.30%
发文量
66
审稿时长
6 months
期刊介绍: Quarterly Journal of Engineering Geology and Hydrogeology is owned by the Geological Society of London and published by the Geological Society Publishing House. Quarterly Journal of Engineering Geology & Hydrogeology (QJEGH) is an established peer reviewed international journal featuring papers on geology as applied to civil engineering mining practice and water resources. Papers are invited from, and about, all areas of the world on engineering geology and hydrogeology topics. This includes but is not limited to: applied geophysics, engineering geomorphology, environmental geology, hydrogeology, groundwater quality, ground source heat, contaminated land, waste management, land use planning, geotechnics, rock mechanics, geomaterials and geological hazards. The journal publishes the prestigious Glossop and Ineson lectures, research papers, case studies, review articles, technical notes, photographic features, thematic sets, discussion papers, editorial opinion and book reviews.
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