Results 71 to 80 of about 230,739 (198)
Analysis on the geo-resistivity anomaly at Baoji Seismic Station of the Jiuzhaigou Ms7.0 earthquake
Abstract According to the geological structure and observation characteristics of Baoji Seismic Station, a variety of methods are used to process and analyze the geo-resistivity data of Baoji Seismic Station from 2014 to 2018, such as the fourier sliding method that removing annual variation, the anisotropic degree method of the geo ...
Yu Sun, Weichao Zhang
openaire +1 more source
Abstract The Xianshuihe fault zone (XSHF) in southwestern China accommodates both aseismic creep and seismic slip, yet geological evidence constraining these processes remains limited. Hence, we conducted microstructural, geochemical, and rock magnetic analyses of fault‐zone materials from the Cuoniulongba River outcrop.
Lei Zhang +6 more
wiley +1 more source
Earthquake source parameters of the 2009 Mw 7.8 Fiordland (New Zealand) earthquake from L-band InSAR observations [PDF]
The 2009 MW7.8 Fiordland (New Zealand) earthquake is the largest to have occurred in New Zealand since the 1931 Mw 7.8 Hawke’s Bay earthquake, 1 000 km to the northwest.
Qu, W. +7 more
core +1 more source
Satellite Image Survey of Landslides Triggered by the 2024 Wushi Earthquake, Xinjiang, China
A satellite imagery survey was used to compile an inventory of 1273 landslides triggered by the 2024 Wushi earthquake in Xinjiang, China. These landslides ranged in area from 9 to 13,418 m2, with a total area of 0.42 km2, and exhibited a notable hanging wall effect.
Tao Li, Chong Xu, Yuandong Huang
wiley +1 more source
ABSTRACT During the excavation of a deep‐buried tunnel by the drilling and blasting method, the dynamic stress of blasting may cause the disorderly release of high energy in the rock mass during the blasting process of deep high‐energy rock. Blasting vibration is one of the main factors inducing dynamic disasters (such as rockbursts) in the surrounding
Chao Ren +5 more
wiley +1 more source
Slip Deficit Rate and Seismic Potential on Crustal Faults in Tibet
Abstract Quantifying slip deficit rates on active faults in Tibet is essential for understanding fault kinematics and assessing seismic hazards, but has not been fully characterized, particularly on secondary faults. In this study, we integrate an updated interseismic Global Navigation Satellite Systems velocity field from 4,458 stations across ...
Yanchuan Li +5 more
wiley +1 more source
Abstract Satellite thermal infrared observation has advantages over other earthquake observation techniques. With MODIS remote-sensing images from the TERRA satellite, the thermal infrared brightness temperature difference variation rate was used to analyze the observation data prior to three Magnitude-7-and-above earthquakes along the ...
Dong Na, Liao Hongyue
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The inventory of landslides includes a total of 169,888 large‐scale landslides, covering a combined area of approximately 1575 km2. The average size of these landslides is approximately 92,734 m2. The scale of these landslides varies widely, with the smallest individual landslide covering an area of 166.25 m2 and the largest reaching 12.9 km2 ...
Liye Feng +13 more
wiley +1 more source
Dynamic Monitoring of Jiuzhaigou Earthquake Damaged Landscape Restoration Based on SBAS-InSAR
On August 8, 2017, Jiuzhaigou earthquake caused a large number of geological disasters in Jiuzhaigou scenic area, and many landscapes were seriously damaged. Sentinel-1A data from July 30, 2017 to January 28, 2020 are selected as the data source. SBAS-InSAR technology is used to obtain the settlement rate changes of Jiuzhaigou earthquake damaged core ...
Maoying Ran +4 more
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Post-Earthquake Recovery of Traditional Tibetan Villages in Jiuzhaigou Valley Scenic and Historic Interest Area Natural World Heritage [PDF]
This paper is based on the survey of the damage and post-earthquake recovery status of the Tibetan traditional villages located in the Jiuzhaigou Valley Scenic and Historic Interest Area a Natural World Heritage property.
Hongtao Liu
core +1 more source

