与2020年12月至2021年1月Petrinja地震系列相关的同震地面破坏的初步清单

IF 1.1 4区 地球科学 Q3 GEOLOGY Geologia Croatica Pub Date : 2021-04-27 DOI:10.4154/GC.2021.08
Davor Pollak, Vlatko Gulam, T. Novosel, Radovan Avanić, B. Tomljenović, Nina Hećej, Josip Terzić, J. Stipčević, Mario Bačić, Tomislav Kurečić, Mario Dolić, Iris Bostjančić, L. Wacha, I. Kosovic, Marko Budić, M. Vukovski, N. Belic, M. Špelić, V. Brčić, J. Barbača, B. Kordić, D. Palenik, R. Filjak, Tihomir Frangen, M. Pavić, K. Urumović, Marin Sečanj, B. Matos, Marin Govorcin, M. Kovačević, L. Librić
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引用次数: 8

摘要

最近的一次大地震发生在佩特里尼亚附近(2020年12月29日,里氏6.2级),在佩特里尼亚、西萨克和格利纳等更广泛的地区引发了大面积的地面塌陷。不同的专家和团队已经记录了包括沉降线、液化和滑坡在内的同震地面故障。这些数据存储在新创建的库存中,在本文中公开展示。该清单由克罗地亚地质调查局管理和更新,并将通过网络地图服务(www.hgi-cgs.hr)在线提供。该清单的目的不仅是为绘制易感性地图和更详细地探索可能的补救措施提供数据,而且还为立即采取行动确定优先事项。地震引发了辍学儿童的迅速发展,危及到me en ani村和Borojevići村的当地人口。在房屋附近,这一过程仍在进行中,因此立即开始了现场勘探。与萨瓦河、库帕河和格利纳河冲积沉积物相关的液化几乎全部发生在松散和纯砂中,并伴有砂沸腾、沉降和横向扩张。液化也带来了更大的危害,因为房屋和河堤会发生沉降。横向扩展造成了河流防洪堤防和天然河岸的破坏。根据迄今所知的资料,大多数同震滑坡都以较小的位移重新激活。尽管如此,人们已经认识到,位于滑坡边缘或崩积层的房屋比位于滑坡影响区外的其他房屋遭受的破坏更大。
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The preliminary inventory of coseismic ground failures related to December 2020 – January 2021 Petrinja earthquake series
The most recent major earthquake series struck near Petrinja (December 29th 2020 M 6.2), and triggered extensive ground failures in the wider area of Petrinja, Sisak and Glina. Coseismic ground failures including subsidence dolines, liquefaction and landslides have been documented over a large area by various experts and teams. These data are stored in the newly created inventory, which is openly presented in this paper. This inventory is administered and updated by the Croatian Geological Survey, and will be available online via a Web Map Service (WMS) (www.hgi-cgs.hr). The aim of the inventory is to not only provide data for the development of susceptibility maps and more detailed exploration for possible remediation measures, but also to define the priorities for immediate action. The earthquake triggered the rapid development of dropout dolines which endanger the local populations of the villages of Mečenčani and Borojevići. This is still an ongoing process in the vicinity of the houses and therefore in-situ exploration started immediately. Liquefaction related to alluvial sediments of the Sava, Kupa and Glina rivers occurred almost exclusively in loose and pure sands, and was accompanied by sand boils, subsidence and lateral spreading. Liquefaction also presents a greater hazard because settlement of houses and river embankments occurred. Lateral spreading caused failures of river flood embankments and natural river banks. According to the data known to date, the majority of the coseismic landslides were reactivated with minor displacements. Despite that, it has been recognised that houses at the edge, or in landslide colluvium suffered greater damage than other houses located outside the landslide impact zone.
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来源期刊
Geologia Croatica
Geologia Croatica GEOSCIENCES, MULTIDISCIPLINARY-
CiteScore
2.90
自引率
23.10%
发文量
35
审稿时长
>12 weeks
期刊介绍: Geologia Croatica welcomes original scientific papers dealing with diverse aspects of geology and geological engineering, the history of the Earth, and the physical changes that the Earth has undergone or it is undergoing. The Journal covers a wide spectrum of geology disciplines (palaeontology, stratigraphy, mineralogy, sedimentology, petrology, geochemistry, structural geology, karstology, hydrogeology and engineering geology) including pedogenesis, petroleum geology and environmental geology. Papers especially concerning the Pannonian Basin, Dinarides, the Adriatic/Mediterranean region, as well as notes and reviews interesting to a wider audience (e.g. review papers, book reviews, and notes) are welcome.
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