Connecting slow earthquakes to huge earthquakes
K Obara, A Kato - Science, 2016 - science.org
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 …
radiation patterns that differ from those of traditional earthquakes. However, slow …
Developing, testing, and communicating earthquake forecasts: Current practices and future directions
L Mizrahi, I Dallo, NJ van der Elst… - Reviews of …, 2024 - Wiley Online Library
While deterministically predicting the time and location of earthquakes remains impossible,
earthquake forecasting models can provide estimates of the probabilities of earthquakes …
earthquake forecasting models can provide estimates of the probabilities of earthquakes …
Real-time discrimination of earthquake foreshocks and aftershocks
Immediately after a large earthquake, the main question asked by the public and decision-
makers is whether it was the mainshock or a foreshock to an even stronger event yet to …
makers is whether it was the mainshock or a foreshock to an even stronger event yet to …
The seismo-hydromechanical behavior during deep geothermal reservoir stimulations: open questions tackled in a decameter-scale in situ stimulation experiment
In this contribution, we present a review of scientific research results that address seismo-
hydromechanically coupled processes relevant for the development of a sustainable heat …
hydromechanically coupled processes relevant for the development of a sustainable heat …
B‐Positive: A Robust Estimator of Aftershock Magnitude Distribution in Transiently Incomplete Catalogs
NJ van der Elst - Journal of Geophysical Research: Solid Earth, 2021 - Wiley Online Library
The earthquake magnitude‐frequency distribution is characterized by the b‐value, which
describes the relative frequency of large versus small earthquakes. It has been suggested …
describes the relative frequency of large versus small earthquakes. It has been suggested …
Revealing the spatiotemporal complexity of the magnitude distribution and b-value during an earthquake sequence
Abstract The Magnitude–Frequency-Distribution (MFD) of earthquakes is typically modeled
with the (tapered) Gutenberg–Richter relation. The main parameter of this relation, the b …
with the (tapered) Gutenberg–Richter relation. The main parameter of this relation, the b …
[HTML][HTML] 2021年5月21日云南漾濞MS6.4地震序列发震构造
段梦乔, 赵翠萍, 周连庆, 赵策, 左可桢 - 地球物理学报, 2021 - html.rhhz.net
2021 年5 月21 日云南省大理州漾濞县发生MS 6.4 地震. 地震序列表现为" 前-主-余" 型,
余震频次较高. 为获得此次地震序列的活动特征和震源区潜在的发震构造, 本文首先计算2010 …
余震频次较高. 为获得此次地震序列的活动特征和震源区潜在的发震构造, 本文首先计算2010 …
[HTML][HTML] Subduction zone megathrust earthquakes
Subduction zone megathrust faults host Earth's largest earthquakes, along with multitudes of
smaller events that contribute to plate convergence. An understanding of the faulting …
smaller events that contribute to plate convergence. An understanding of the faulting …
A review on slow earthquakes in the Japan Trench
Slow earthquakes are episodic slow fault slips. They form a fundamental component of
interplate deformation processes, along with fast, regular earthquakes. Recent …
interplate deformation processes, along with fast, regular earthquakes. Recent …
A spatiotemporal clustering model for the third Uniform California Earthquake Rupture Forecast (UCERF3‐ETAS): Toward an operational earthquake forecast
EH Field, KR Milner, JL Hardebeck… - Bulletin of the …, 2017 - pubs.geoscienceworld.org
Abstract We, the ongoing Working Group on California Earthquake Probabilities, present a
spatiotemporal clustering model for the Third Uniform California Earthquake Rupture …
spatiotemporal clustering model for the Third Uniform California Earthquake Rupture …