Results 231 to 240 of about 5,650,087 (284)

Smart Materials Employed in the Construction Industry: A Systematic Review of Types, Properties, Applications, and Sustainability Performance. [PDF]

Materials (Basel)
Martínez Ángeles H, Navarro Rubio CA, Ríos Moreno JG, Gonzalez-Garcia I, Reyes Araiza JL, Garduño Aparicio M, Chavero-Navarrete E, Trejo Perea M.   +7 more
europepmc   +1 more source

Geometric phase sensing using seismic waves for comprehensive volcano monitoring at Kı̄lauea Hawaii. [PDF]

Nat Commun
Luo B, Beck S, Deymier P, Runge K, Kiser E, Moitra P, Huettmann F, Missoum S, Latypov M, Whitney E, Wang J, Schabib SS.   +11 more
europepmc   +1 more source

Numerical investigation on the seismically induced progressive failure of the 2017 Xinmo landslide in China. [PDF]

Sci Rep
Zhu L, Chen L, Wei T, Cui S, Sun P, Luo L, Liang Y.   +6 more
europepmc   +1 more source

Heterogeneous rupturing and barrier mechanism during the 2025 Mw7.7 Myanmar earthquake. [PDF]

Sci Rep
Gürboğa Ş, Çomut FC, Lyu S, Motagh M, Thu KS, Karadağlar M.   +5 more
europepmc   +1 more source

The olivine-ringwoodite transformation triggers deep slab seismicity and rheological weakening. [PDF]

Nat Commun
Honda R, Kubo T, Miyahara M, Iwasato T, Mori Y, Higo Y, Tsubokawa Y, Goto Y, Suzuki A, Shibazaki Y.   +9 more
europepmc   +1 more source

Some of the next articles are maybe not open access.

Related searches:

Co-seismic Deformation and Source Parameters of the Mw6.0 Düzce Earthquake by InSAR

2023
23 November, 2022 Mw 6.0 Düzce Earthquake occurred in the west of the North Anatolian Fault Zone (NAFZ) representing a nascent transform fault between the Eurasian Plate and Anatolian Plate. Well-documented seismic sequence along this fault zone started in the east with the 1939 M7.9 Erzincan Earthquake and migrated westward with M>7 ...
Tülay Kaya-Eken, Çağkan Serhun Zoroğlu, Emre Havazlı, Haluk Özener   +3 more
openaire   +1 more source

A Global Archive of Dinsar Co-Seismic Deformation MAPS from Sentinel-1 Data

IGARSS 2020 - 2020 IEEE International Geoscience and Remote Sensing Symposium, 2020
We present the implementation of a global archive of Differential Synthetic Aperture Radar Interferometry (DInSAR) co-seismic deformation maps. The archive has been generated by automatically processing all the Copernicus Sentinel-1 data spanning about 300 significant (at least Mw > 5.5) earthquakes all over the Earth.
MONTERROSO TOBAR , F., Ali, Z., Bonano, M., De Luca, C., De Novellis, V., Lanari, R., Manunta, M., Manzo, M., Onorato, G., Valerio, E., Zinno, I., Casu, F.   +11 more
openaire   +1 more source

Measuring co-seismic deformation of the Sichuan earthquake by satellite differential INSAR

SPIE Proceedings, 2008
The Sichuan Earthquake, occurred on May 12, 2008, is the strongest earthquake to hit China since the 1976 Tangshan earthquake. The earthquake had a magnitude of M 8.0, and caused surface deformation greater than 3 meters. This paper presents the research work of measuring the co-seismic deformations of the earthquake with satellite differential ...
Yonghong Zhang, Wenyu Gong, Jixian Zhang
openaire   +1 more source

Early preliminary results on co-seismic deformation of the island of Samos associated with co-seismic slip following the October 2020 Mw 6.9 Samos earthquake (Greece)

Arabian Journal of Geosciences, 2021
On 30 October 2020, an Mw 6.9 normal faulting earthquake to the north and offshore from the island of Samos, very close to the south west coast of Turkey, occurred at 14:51 local time (11:51:34.8 UTC). In this study, the stress change features of the rupture process and the co-seismic surface deformation of the island of Samos during this event are ...
Mustafa Toker, Erman Şentürk, Çağlar Bayık   +2 more
openaire   +4 more sources

Effect of Thickness of Sediment Layer on the Co‐seismic Deformation

ce/papers
AbstractModels with different thicknesses of sediment layer were developed based on the finite element method and equivalent‐bodyforce approach. Taking the fault information of the 2013 Lushan County Ms 7.0 earthquake as an example, the co‐seismic deformation of the surface under different thicknesses of sediment layer is comparatively analyzed. It was
Fang Zhang, Zhendong Shan
openaire   +1 more source