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Simulating 800,000 years of California earthquake history to pinpoint risks

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.

SourceUniversity of Texas at Austin, Texas Advanced Computing Center·JournalBulletin of the Seismological Society of America·DateJan 25, 2021

The revelation of the crustal geometry of the western Qilian Mountains, NE Tibetan Plateau

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.

SourceScience China Press·JournalScience China Earth Sciences·DateJan 6, 2021

Seismic activity of New Zealand's alpine fault more complex than suspected

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.

SourceSeismological Society of America·JournalBulletin of the Seismological Society of America·DateDec 1, 2020

Transportation of water into the deep Earth by Al-phase D

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.

SourceEhime University·JournalGeophysical Research Letters·DateNov 30, 2020

The connectivity of multicomponent fluids in subduction zones

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 ...

SourceTohoku University·JournalEarth and Planetary Science Letters·DateNov 12, 2020

Asteroid Ryugu shaken by Hayabusa2's impactor

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.

A new way of looking at the Earth's interior

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.

SourceETH Zurich·JournalProceedings of the National Academy of Sciences·DateOct 21, 2020

Network reveals large variations in shaking in LA basin after Ridgecrest earthquake

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...

SourceSeismological Society of America·JournalSeismological Research Letters·DateSep 30, 2020

How earthquake swarms arise

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.

SourceStanford University·JournalNature Communications·DateSep 24, 2020

Seismic data explains continental collision beneath Tibet

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.

SourceStanford University·JournalProceedings of the National Academy of Sciences·DateSep 22, 2020

Detaching and uplifting, not bulldozing

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.

SourceETH Zurich·JournalGeophysical Research Letters·DateSep 17, 2020

OBS deep seismic survey uncovered crustal structure mystery of NW sub-basin of the SCS

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...

SourceScience China Press·JournalScience China Earth Sciences·DateSep 15, 2020

Research team builds better rock models

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.

What's Mars made of?

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.

SourceUniversity of Tokyo·JournalNature Communications·DateMay 13, 2020