Results 101 to 110 of about 8,225 (218)

Spaceborne and spaceborn: Physiological aspects of pregnancy and birth during interplanetary flight

open access: yesExperimental Physiology, Volume 111, Issue 9, Page 4015-4040, 1 September 2026.
Abstract Crewed interplanetary return missions that are on the planning horizon will take years, more than enough time for initiation and completion of a pregnancy. Pregnancy is viewed as a sequence of processes – fertilization, blastocyst formation, implantation, gastrulation, placentation, organogenesis, gross morphogenesis, birth and neonatal ...
Arun V. Holden
wiley   +1 more source

Description of earthquake aftershock sequences using prototype point patterns [PDF]

open access: yes, 2007
We introduce the use of prototype point patterns to characterize the behavior of a typical aftershock sequence from the global Harvard earthquake catalog.
Schoenberg, Frederic P   +3 more
core   +1 more source

Deep Seismic Tremors in the 2025 Santorini Seismo‐Volcanic Crisis Highlight Magmatic Feeding From a Mid‐Crustal Reservoir

open access: yesGeophysical Research Letters, Volume 53, Issue 16, 28 August 2026.
Abstract An intense seismic swarm started on 27 January 2025 in the Santorini‐Amorgos region and lasted for approximately 45 days. A widely observed seismic tremor on 14 February 2025 suggested a volcanic origin for the 2025 Santorini crisis. Here we present an in‐depth combined seismological analysis of the earthquakes and tremors that occurred during
Jean Soubestre   +5 more
wiley   +1 more source

On the adaptive daily forecasting of seismic aftershock hazard

open access: yes, 2013
Seismic aftershock-hazard analysis is one of the first steps toward establishing an integrated risk-based decision-making support framework for emergency management in the event of an ongoing aftershock sequence.
PROTA, ANDREA   +6 more
core  

Regional variations in the diffusion of triggered seismicity [PDF]

open access: yes, 2005
We determine the spatiotemporal characteristics of interearthquake triggering in the International Seismological Centre catalogue on regional and global scales. We pose a null hypothesis of spatially clustered, temporally random seismicity, and determine
Ian G. Main   +3 more
core   +1 more source

An Inflating Upper Mantle Magma Reservoir Beneath the Tip of the Condor Seamount, Azores Revealed by Rapid‐Response Ocean‐Bottom‐Seismometer Data

open access: yesGeophysical Research Letters, Volume 53, Issue 16, 28 August 2026.
Abstract Condor Seamount is among the most seismically active regions on the Azores Plateau. In December 2019, an earthquake crisis occurred at the tip of the seamount, which was strongly felt on nearby islands. Two months after the peak of the crisis, we deployed a local network of five ocean‐bottom seismometers around the seamount, recording ...
Yingchen Liu   +3 more
wiley   +1 more source

Updip and along-strike aftershock migration model driven by afterslip : application to the 2011 Tohoku-Oki aftershock sequence

open access: yes, 2019
We present an analytical model based on the idea that afterslip drives seismicity: aftershocks occur when a given level of afterslip is reached in their vicinity.
Marsan, D.   +3 more
core  

Properties of the Aftershock Sequence of the 1999 M_w 7.1 Hector Mine Earthquake: Implications for Aftershock Hazard [PDF]

open access: yes, 2002
We investigate the spatial and temporal seismicity parameters and the related probabilistic aftershock hazard for the aftershock sequence of the 1999 M_w 7.1 Hector Mine mainshock and compare it with the neighboring 1992 M_w 7.3 Landers sequence. Using a
Hauksson, Egill   +2 more
core  

Aftershock Activity in the Vicinity of Kyoto [PDF]

open access: yes, 1970
During the period from 1964 to 1968 about 50 earthquakes with a magnitude of 3.0 or greater occurred in the vicinity of Kyoto. These earthquakes are studied on their aftershock activity.
OKANO, Kennosuke
core  

Maximum inelastic displacement of mainshock-damaged structures under succeeding aftershock

open access: yes, 2020
To facilitate the rapid, though, reliable assessment of mainshock-damaged structures against the succeeding aftershock excitations, the γ-index is introduced, defined as the ratio of the residual displacement of a structure under the mainshock excitation
Ji, Duofa   +3 more
core   +1 more source

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