Articles tagged with Seismology
A novel convolutional neural network, FMNet, was developed to determine the source focal mechanism of earthquakes rapidly using full waveforms. The method proves effective in calculating parameters within one second with minimal computing resources.
Researchers analyzed data from dense seismic, geodetic and tsunami networks to understand the 2011 quake. The study found that a large coseismic fault slip ruptured into a shallow part of the Japan Trench's megathrust fault.
The 2021 SSA Annual Meeting will showcase the latest seismological research globally, with sessions on recent earthquakes and new technologies for monitoring glacier change. Journalists can register for free access to technical presentations and events.
Researchers use fin whale songs to probe Earth's crust at seafloor, producing lower-resolution results than traditional air-gun signals. The method complements conventional techniques and avoids harming ocean life caused by powerful blasts.
A new study reveals common seismological equipment is vulnerable to cyberattacks, posing risks to data collection and processing. Seismic networks may be exposed to security breaches if devices use non-encrypted data, insecure protocols, and poor user authentication mechanisms.
A new framework predicts likelihood and impact of earthquakes over an entire region by simulating hundreds of thousands of years of seismic history in California. The results compare well with historical earthquakes and display a realistic distribution of earthquake probabilities.
A new study highlights the impact of socioeconomic factors on eyewitness accounts of earthquake shaking reported through online systems like DYFI. The research found complex trends in California and India, with differences in self-reported reports based on neighborhood income levels and literacy rates.
The Gulf of Mexico holds vast untapped offshore oil deposits, thanks to a remarkable geologic past that began 200 million years ago. A unique combination of fine- and coarse-grained sediments, salt layers, and seals has made the basin a formidable petroleum resource.
The study provides a detailed understanding of the crustal deformation mechanism in the western Qilian Mountains, northeastern margin of the Tibetan Plateau. The researchers discovered a decoupled crustal deformation with intra-crustal decollement layers, which reveals the Asian lithospheric mantle being underthrust beneath the region.
Researchers developed a state-of-the-art model that revealed high complexity in rupture processes even in simple oceanic faults. The study used seismic data from around the world to build a model of the 2020 Caribbean earthquake, finding variations in rupture speed and direction.
Researchers provide a 4D image of an active linkage zone between two major faults, offering insights into fault behavior and implications for seismic hazard assessment. The study highlights the importance of reevaluating 'silent' seismogenic sources in assessing earthquake risk.
Researchers at Tohoku University have discovered a mantle plume beneath central Greenland that melts the ice from below, bolstering understanding of volcanic activities and global sea-level rising.
Research suggests that some parts of the Alpine Fault, particularly around Hokitika and Greymouth, may experience strong ground shaking more often than previously thought. The study found evidence of a 19th-century earthquake along the fault's northeastern end, indicating that smaller earthquakes could occur between large rupture events.
Al-phase D mineral discovered to transport and host water up to 1200 km in lower mantle, improving stability against pressure and temperature. Researchers measured sound velocities and density of Al-phase D using synchrotron X-ray techniques, providing clear understanding of seismic velocities of hydrous rocks.
Researchers have used powerful seismic imaging techniques to study the Alaska coastline's volcanic activity, revealing unexpected details about tectonic plates and volcano distribution. The new research highlights complexities in subduction zones and how they control volcano formation.
A new study has created the first high-resolution seismic images of a rocky tectonic plate within Earth's mantle transition zone. The research provides evidence that the slab hasn't completely mixed with the surrounding mantle, shedding light on the processes that shaped Earth's surface over billions of years.
A team of researchers has discovered more about the grain-scale fluid connectivity beneath the earth's surface, shedding new light on fluid circulation and seismic velocity anomalies in subduction zones. The study found that fluids with minor components, such as CO2 and NaCl, can have a significant impact on the dihedral angle between ...
A new model has been developed to predict earthquake propagation speeds, resolving a long-standing inconsistency between theory and observations. The 3D model overcomes the limitations of previous 2D models and accounts for oblique sliding, making it more accurate in predicting seismic wave behavior.
Researchers measured rocks formed by seismic slips in central Japan's subduction zone to identify conditions leading to earthquake faulting. This study provides insights into the thermal fracturing process, which could contribute to generating frictional melt and accelerating seismic slip.
The Hayabusa2 mission's artificial impact crater on asteroid Ryugu revealed significant boulder movements and seismic shaking, up to 40m from the center. The study provides valuable insights into asteroids' resurfacing processes and can be used as a benchmark for numerical simulations.
Researchers have found that the Earth's mantle has a different composition to its upper layer, contradicting long-held assumptions. Lab experiments and seismic wave analysis suggest that silicon is present in the lower mantle, not the core.
A magnitude 4.9 earthquake triggered by hydraulic fracturing in a Chinese shale gas field occurred along a fault about one kilometer deep. The event challenges current understanding of seismic risk for shallow faults, highlighting the need to reassess evaluation strategies.
The study found that long-period buildings experienced the most amplification of shaking from the Ridgecrest earthquake, with maximum amplification occurring in the western part of the L.A. basin and the south-central San Fernando Valley. This could result in high-rise buildings in those areas experiencing shaking four times larger tha...
A Stanford-developed model shows that fluids ascending by fits and starts weaken the fault, propelling the boundary or locking depth upward. This process can trigger earthquake swarms, strings of quakes clustered in a local area, often too subtle to notice but sometimes strong enough to rattle cities.
New seismic data gathered by Stanford University researchers provides the first west-to-east view of the subsurface where India and Asia collide. The study suggests two competing processes are operating beneath the collision zone: movement of one tectonic plate under another, as well as thinning and collapse of the crust.
Researchers at ETH Zurich propose an alternative theory for the formation of the Alps, suggesting that the mountains were uplifted by the subduction of the Eurasian plate beneath the Adriatic microplate. This new model simulates the processes leading to the formation of the Alps and explains the observed seismicity in the region.
A recent study used OBS data to clarify the formation mechanism of the Double-peak seamount in the Northwest Sub-basin (NWSB) of the South China Sea (SCS). The survey revealed a high velocity layer at the bottom of the crust, indicating possible in-situ mantle serpentinization or lower crust magma underplating. The study enriches the d...
A magnitude 5 earthquake near Le Teil in southern France revealed unexpected surface rupture and ground displacement, reactivating the ancient La Rouvière fault. The event raised concerns about seismic risk in France and Western Europe, with potential for other faults producing similar surface ruptures.
A team of scientists installed an optical seismometer on La Soufrière de Guadeloupe volcano's summit to monitor gas and steam eruptions. The instrument collects data that will be combined with other observations to better understand the volcano's explosive potential.
Researchers have matched seismic signals with aurora displays in Alaska, offering a new way to study magnetic fluctuations. By combining data from all-sky cameras and seismometers, scientists can better understand the link between solar winds and the Earth's magnetic field.
The study reveals an 'inchworm-like' slip evolution of supershear rupture along the Palu-Koro fault, showcasing the effect of complex fault geometry on rupture propagation. This phenomenon may have significant implications for assessing future earthquake impacts and related disasters.
A recent study found that COVID-19 lockdowns led to a 50% global reduction in human-caused seismic noise, with the most pronounced effects seen in densely populated areas. This 'anthropause' phenomenon has provided a unique opportunity for researchers to better distinguish between human and natural seismic noise.
Researchers found a significant link between well depth and seismic probability, suggesting that deeper wells are more likely to trigger earthquakes. The study also revealed that the type of fluid used in hydraulic fracturing, including gel vs. slickwater operations, may affect seismic activity.
Researchers have discovered ancient volcanic activity and subtle, unusual movements in the Earth's surface in the Eifel region of Germany, suggesting a greater risk to northwestern Europe. The study suggests that the region is an active volcanic system with significant seismic activity.
Researchers at Kyushu University analyzed data from NASA's InSight lander to determine the sources of different types and frequencies of Martian microtremors. The study found that low-frequency P-waves were related to changes in wind and solar irradiation, while higher-frequency ambient noises were dominated by lander vibration.
A typhoon-induced event altered the frequency and location of earthquakes in Taiwan by changing crustal stress levels. This study suggests that surface processes can trigger seismicity, highlighting a new connection between tectonics and external factors in earthquake hazard assessment.
A new study maps over 22,000 tremors to recreate the complex three-dimensional structure of a fault zone in southern California. The research reveals that dynamic pressure changes from natural fluid injections controlled the evolution of an earthquake swarm in the region.
A four-year-long earthquake swarm near Cahuilla, California was driven by a naturally occurring injection of underground fluids, revealing complex conditions for fluid flow within the fault zone. The study provides new insights into seismic processes and brings closer concrete explanations for how earthquake swarms start and terminate.
A team of geoscientists used seismic anisotropy to create high-resolution, 3D images of mantle flows in a subduction region. The images revealed fragmented tectonic plates and complex mantle flow patterns.
Researchers have created a new map revealing the Earth's mantle at a depth of 3,000 kilometers by analyzing thousands of seismic waves collected over 30 years. The map shows hot and dense regions below Hawaii and French Polynesia.
Researchers at University of Alaska Fairbanks found that seismic surveys can cause long-lasting scars on the tundra, affecting its hydrology and habitat. The study emphasizes the need for more data on seismic exploration impacts and better weather records to minimize damage in the Arctic Refuge.
A new method for creating digital replicas of rock samples is being developed by geoscience researchers at the University of Texas at Austin. This technique allows scientists to learn about rock samples without touching them and can be used to calculate important rock properties such as permeability and electrical conductivity.
A new study proposes a model for the formation of diamond-bearing kimberlites in Northern Alberta, which was caused by the movement of an ancient slab of oceanic rocks. The research combines geophysical imaging, geochronological dating and plate motion calculation to explain how diamonds came to Earth's surface.
Researchers discovered new variants of feldspar stable under extreme pressure conditions, potentially altering seismologic signatures and plate dynamics. The high-pressure polymorphs were formed through severe geometrical distortions in the tetrahedral framework.
Researchers from Los Alamos National Laboratory have developed a new technique that separates industrial noise from natural seismic signals using cloud computing. The approach allows for large-scale seismic analysis ten times faster than traditional methods and has the potential to transform the field of seismology.
Scientists have measured the velocity of seismic waves in iron-sulfur alloys thought to comprise Mars' core, providing crucial information about the planet's internal structure. This study simulates the Martian core's composition and origin, helping researchers compare observations with Martian space probes.
A recent study used fiber optic cables to capture seismic signatures of the Rose Parade, capturing the vibrations of marching bands and floats. The technique, called distributed acoustic sensing (DAS), revealed distinct signals from the parade, including harmonic frequencies corresponding to even-stepping marching bands.
NASA scientists have developed a new seismometer system called SUBLIME to measure moonquakes and map the Moon's interior. The system will alert astronauts to seismic events and provide an early-warning system, with the long-term goal of establishing a network of seismic stations.
The Stanford study develops a calculation of the risk that shaking triggered by a given project will be felt in surrounding communities. The authors propose setting yellow-light thresholds approximately two magnitude units below the red light to reduce nuisance-level shaking.
The study presents a comprehensive view of tectonic stresses acting on North America, offering regional clues about subsurface behavior. The findings have implications for understanding and mitigating induced seismicity, particularly in areas targeted for energy exploration.
Researchers have found that fault segments connected at depth can influence earthquake risk and magnitude. A study suggests that a rapid decay in slip at the edge of a fault segment indicates a connection below the surface.
Researchers propose that rocks colliding inside a fault zone during an earthquake produce high-frequency vibrations, which could help explain puzzling seismic patterns and predict quake damage. The new explanation suggests smoother faults with rounded internal structures may produce less damaging quakes.
Researchers at MIT have developed a machine learning method to fill in the missing low-frequency seismic waves in human-generated seismic data, allowing for more accurate mapping of underground structures. The technique was trained on simulated earthquakes and used to infer missing frequencies from new input data.
Researchers analyzed Marsquakes from InSight mission, finding moderate seismic activity intermediate between Earth and the Moon. The data revealed geological layers within the planet and identified areas of high geological activity, guiding future missions searching for potential life.
Seismologists have recovered nearly 40-year-old seismic data tapes from the 1980 Mount St. Helens eruption, providing a near-continuous sequence of activity leading up to the May 18th event. The data analysis suggests no significant change in seismic signals that would have hinted at an imminent major eruption.
A high-resolution catalog of earthquakes from the 2019 Ridgecrest sequence reveals complex rupturing and crosscutting fault structures. The catalog helps researchers understand the triggering and evolution of the sequence, shedding light on the physics and processes involved.
Researchers at Kazan University are developing advanced aerial drones with devices such as detectors and special cameras to enhance geological surveys. The goal is to analyze upper strata of rocks, evaluate hydrocarbon potential, and improve forest planning and soil analysis.
A new study has recalculated the magnitude of the Great Lisbon Earthquake from 8.5 to 9.0 to 7.7 using macroseismic data from Portugal, Spain, and Morocco. The analysis suggests that the earthquake's epicenter was offshore the southwestern Iberian Peninsula and may have involved faulting onshore.
Researchers at BP partner with ORNL to tackle the challenge of managing large seismic datasets, which can reach half a petabyte in size. The Adaptable I/O System (ADIOS) provides a flexible way to describe data, allowing for efficient compression and processing.
Researchers propose a new theory that iron particles fall from the molten outer core and accumulate on the inner core, creating piles up to 200 miles thick. This phenomenon could help explain seismic wave anomalies and provide insights into the Earth's interior composition and behavior.