Results 111 to 120 of about 942,715 (203)

Observational Evidence of a Very‐Low‐Frequency Earthquake (Mw 3.8) Leading to an Earthquake (Mw 4.2): Minto Flats Strike‐Slip Fault Zone, Central Alaska

Geophysical Research Letters
The physical conditions governing earthquake initiation are largely unknown, particularly in the minutes to seconds preceding rupture. While there is geodetic and seismic evidence of precursory activity in the hours to weeks prior to large earthquakes ...
A. M. McPherson, C. Tape, Y. Kaneko
doaj   +1 more source

Advances in Deep Learning Applications for Slow Earthquake Research

Applied Sciences
Slow earthquakes represent an important mode of fault slip transitional between stable creep and dynamic rupture. Their occurrence is jointly controlled by mineral composition, pore-fluid pressure, effective normal stress, system stiffness, and ...
Shimin Liu, Huiru Lei, Wenhao Dai, Zekang Yang   +3 more
doaj   +1 more source

Connecting slow earthquakes to huge earthquakes

Connecting slow earthquakes to huge earthquakes
Slow earthquakes are characterized by a wide spectrum of fault slip behaviors and seismic radiation patterns that differ from those of traditional earthquakes. However, slow earthquakes and huge megathrust earthquakes can have common slip mechanisms and are located in neighboring regions of the seismogenic zone.
openaire   +1 more source

Mechanical models of slow source processes

, 1984
The occurrence of slow slip episodes on seismogenic faults is examined and its role in the earthquake mechanism is ...
Bonafede, Maurizio, Dragoni, Michele, Boschi, Enzo   +2 more
core   +1 more source

Simulation of 2009, Mw=4 Tehran earthquake using a hybrid method of modal summation and finite difference

, 2012
The Greater Tehran area is the most important city of Iran and hosts about 20% of the country population. Despite the presence of major faults and the occurrence of historical earthquakes, nowadays the seismicity is relatively quite low and this enhances
Ghayamghamian, M. R., Magrin, A., Gholami, V., VACCARI, FRANCO, Hanzehloo, H., PANZA, GIULIANO   +5 more
core  

Spatial and temporal variations of the 3-year earthquake swarm activities leading up to the M7.6 Noto Peninsula earthquake and interpretations of their activities

Earth, Planets and Space
The seismic swarm activity that began and expanded in four separate regions in the northern Noto Peninsula at the end of 2020 was followed by the M6.5 earthquake in May 2023, which cascaded into the M7.6 earthquake on New Year’s Day 2024.
Takao Kumazawa, Yosihiko Ogata
doaj   +1 more source

EXTENDED FRAMEWORK FOR EARTHQUAKE AND TSUNAMI RISK ASSESSMENT: PADANG CITY A CASE STUDY [PDF]

, 2013
The Great Sumatra earthquake and resulting devastating tsunami in 2004 have highlighted the significance of earthquake risk assessment that can effectively include all main associated hazards, such as tsunami.
Mulyani, Rini
core  

Development of a Slow Earthquake Database

Development of a Slow Earthquake Database
identifier:oai:t2r2.star.titech.ac.jp ...
openaire   +1 more source

Structural barriers control the spatial extent of slow earthquake slip. [PDF]

Nat Commun
Akuhara T, Shiraishi K, Tsuji T, Yamashita Y, Sugioka H, Farazi AH, Ohyanagi S, Ito Y, Arai R, Araki E, Fujie G, Nakamura Y, Tonegawa T, Azuma R, Hino R, Mochizuki K, Takemura S, Yamada T, Shinohara M.   +18 more
europepmc   +1 more source

Development of Slow Earthquake Database

Development of Slow Earthquake Database
identifier:oai:t2r2.star.titech.ac.jp ...
openaire   +1 more source