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earthquakes

Diagram of subduction interface
Posted inEditors' Highlights

Subduction Zone Earthquakes: Fast and Slow, Weak and Strong

by T. Parsons 13 September 202118 January 2022

What causes slow earthquakes in subduction zones? New insights from numerical models suggest that a mixture of strong and weak rocks might be the cause.

Series of six figures showing recovered fault geometry and slip models, from early to late stages in the inversion procedure.
Posted inEditors' Highlights

New Inversion Method Improves Earthquake Source Imaging

by Cécile Lasserre 30 August 20218 December 2022

A new method uses Bayesian inference to jointly invert for non-planar fault geometry and spatially variable slip (with associated uncertainties) in earthquake source modeling, based on geodetic data.

Navakanesh M Batmanathan mapped faults in Sabah, Malaysia.
Posted inFeatures

Navakanesh M Batmanathan: Customizing Hazard Outreach

by Jack Lee 24 August 202123 March 2023

Geologist contributes to community-focused outreach in Southeast Asia.

Dead tree trunks and stumps stand along a shoreline
Posted inScience Updates

Swipe Left on the “Big One”: Better Dates for Cascadia Quakes

by J. K. Pearl and L. Staisch 20 August 202114 March 2024

Improving our understanding of hazards posed by future large earthquakes on the Cascadia Subduction Zone requires advancements in the methods and sampling used to date and characterize past events.

Police tape in front of the National Cathedral.
Posted inFeatures

Ten Years on from the Quake That Shook the Nation’s Capital

by T. L. Pratt, M. C. Chapman, A. Shah, J. W. Horton Jr. and O. Boyd 20 August 202128 September 2021

A decade of study into the Virginia earthquake that damaged D.C. and reverberated up and down the Atlantic coast in 2011 has shed light on rare, but risk-laden, seismicity in eastern North America.

Kominato Beach and Kopepe Beach, part of the Ogasawara Islands located in Japan
Posted inResearch Spotlights

First Report of Seismicity That Initiated in the Lower Mantle

by Jack Lee 19 August 20214 August 2023

A 4D back-projection method revealed that aftershocks of the 2015 earthquake beneath the Ogasawara (Bonin) Islands occurred as deep as about 750 kilometers.

Sketch showing induced seismicity on critically stressed faults as a consequence of changes in pore pressure and related changes in stress due to anthropogenic activities
Posted inEditors' Vox

Understanding and Anticipating Induced Seismicity

by B. Müller, M.-L. Doan, T. H. Goebel, Yajing Liu, Patricia Martínez-Garzón, T. Mitchell and I. Zaliapin 30 July 20218 February 2023

A new special collection in JGR: Solid Earth and Earth and Space Science seeks papers from across disciplines that provide insights into induced seismicity at different spatial and temporal scales.

Diagram of megathrust earthquakes resulting from different material contrast scenarios
Posted inEditors' Highlights

The Highs and the Lows of Megathrust Earthquakes

by T. Parsons 21 July 20212 December 2022

Why does low-frequency energy come from the shallow part of ruptures, and the high frequencies from deep?

The San Andreas Fault near Juniper Hills, Calif.
Posted inResearch Spotlights

A New Method Produces Improved Surface Strain Rate Maps

by Jack Lee 19 July 20215 December 2022

The transdimensional Bayesian approach handles GPS data limitations better than existing methods and may assist future seismic hazard assessment studies.

In the center of a cross-polarized image, a purple-pink grain of muscovite with dark asymmetric kink bands lies within a matrix of much finer grained, rainbow-colored micas, as well as small black, white, and gray feldspar and quartz grains.
Posted inNews

Tiny Kinks Record Ancient Quakes

by Alka Tripathy-Lang 19 July 202114 September 2022

As Earth ruptures, micas kink. These kink bands hide in rocks millions of years old, preserving evidence of past quakes.

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Over a dark blue-green square appear the words Special Report: The State of the Science 1 Year On.

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