2022年6月21日阿富汗地震造成的地表破裂和土地变形

IF 2.4 Q2 GEOSCIENCES, MULTIDISCIPLINARY VIETNAM JOURNAL OF EARTH SCIENCES Pub Date : 2022-07-04 DOI:10.15625/2615-9783/17258
Khac Dang Vu, Trinh Phan Trong, P. Tapponnier
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引用次数: 1

摘要

2022年阿富汗地震于2022年6月21日20:54:36(UTC)发生在阿富汗和巴基斯坦边境。据美国地质调查局称,此次地震造成5.9级振动,震源位于10公里深处,震中位于33092°N,69514°E。据欧洲公民保护和人道主义援助行动称,这一事件造成了人类灾难,帕克蒂卡省和霍斯特省1039人死亡,2949人受伤,房屋受损,4500栋房屋的基础设施部分或全部被毁。有必要提高对这一现象的认识。一方面,必须迅速确定受灾地区的范围,以便及时提供救援服务。另一方面,有必要确定地震引起的断裂带的变形特征,以最大限度地减少未来的破坏。传统的DInSAR技术分别应用于2022年6月18日和6月30日地震前后拍摄的两张图像,显示了最大位移为78.4 cm的断裂带,位于先前确定的东北-西南断层的左侧。该地带位于震中向南15公里处。干涉条纹显示,与原始位置相比,研究区域以东的大片区域发生了位移。然而,与古近系地层相对应的西北地区受地震的影响要小得多。地震发生在印度和欧亚大陆板块边界碰撞西北边缘的左侧走滑断层上。
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Surface ruptures and land deformation from the 21 June 2022 Afghanistan earthquake
The 2022 Afghanistan earthquake occurred at the border between Afghanistan and Pakistan at 20:54:36 (UTC) on June 21, 2022. According to the USGS, the earthquake caused vibrations with a magnitude of 5.9, a hypocenter located at a depth of 10 km, and an epicenter at 33,092°N, 69,514°E.  According to European Civil Protection and Humanitarian Aid Operations, this event resulted in disaster for human beings 1039 people died, 2949 people were injured, and damaged to homes and infrastructures of 4500 houses were partially or fully destroyed across Paktika and Khost provinces. It is necessary to improve the knowledge of this phenomenon. On the one hand, it is essential to quickly determine the extent of the affected area to provide timely relief services. On the other hand, it is necessary to determine the deformation characteristics of the fractured zone caused by earthquakes to minimize future damages. Conventional DInSAR technique applied to two images captured on June 18, 2022, and June 30, 2022, respectively, before and after the earthquake event shows the fractured zone with a maximum displacement of 78.4 cm, which locates on the left side of the previously identified northeast–southwest fault. The location of this zone is 15 km in the southward direction of the earthquake epicenter. The interferometric fringes show that a large area to the East of the study area is displaced in comparison to the original position. However, its Northwest region, which corresponds to the Paleogene formations, is much less affected by earthquakes. The earthquake occurred along a left lateral strike-slip fault in the plate boundary between India and Eurasia plates at the Northwestern margin of the collision.
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来源期刊
VIETNAM JOURNAL OF EARTH SCIENCES
VIETNAM JOURNAL OF EARTH SCIENCES GEOSCIENCES, MULTIDISCIPLINARY-
CiteScore
3.60
自引率
20.00%
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0
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