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Seismic study sheds light on factors leading to supershear rupture in Myanmar in 2025
Measurements of slip and width of the coseismic damage zone associated with the earthquake. Credit: Science (2025). doi: 10.1126/science.adz2101
Recently, the journal Science published an article detailing new research on the Myanmar earthquake that occurred on March 28, 2025. In one such study, Shengji Wei and his colleagues analyzed data about the event and provide insight into the multiple factors that lead to these rare and devastating supershear ruptures. Their research was published this week.
Widespread destruction in Myanmar
The Myanmar earthquake was one of the longest and fastest ruptures ever recorded on Earth, causing widespread devastation along the Sagaing Fault. The magnitude of the moment was reported to be 7.7 to 7.8, resulting in at least 5,352 deaths and extensive structural damage. Its effects reached as far as Bangkok, Thailand, 1,000 kilometers away.
The earthquake produced a surface rupture more than 450 km long, extending north-south through major cities, such as Mandalay and Naypyidaw. The surface rupture superseded the shear velocities, meaning that the rupture traveled faster than the local shear wave speed. This is similar to what happens when a supersonic aircraft travels faster than the speed of sound.
Better understanding for better future results
While studies on this type of massive earthquake cannot prevent them from occurring, they can help at-risk communities understand the level of risk and prepare accordingly. The results of these studies can inform risk analysis of other major strike-slip faults with similar characteristics, such as the San Andreas Fault or the North Anatolia Fault.
The Myanmar event has provided a unique opportunity for researchers to study how fault zones affect rupture dynamics in order to gain a deeper understanding of how these events occur. Wei and his team took this opportunity to analyze rupture dynamics through a multifaceted lens, consisting of satellite-based and seismic techniques, including 3D surface deformation mapping, strong motion records, and receiver function analysis. They also used remote sensing, seismic data, and local seismic arrays to resolve rupture dynamics and fault structure.
Unraveling the dynamics of supershear
Faults that experience supershear events, such as the San Andreas, North Anatolia, and Sagaing faults, have some common features. For example, they are all simple, straight faults, which tend to allow energy to be concentrated rather than dispersed. This leads to weakening of the crust along the fault and further damage during earthquakes.
The researchers say in the study that the rupture began at partial shear speeds and then quickly turned to supershear. Their results show speeds of up to 5.3 km/s.
“The rupture started as binary subshear and transitioned to supershear (~5.3 km/s) about 100 km south of the epicenter, maintaining this velocity for over 200 km. The supershear portion is aligned with a low-velocity fault zone about 2 km thick and shows a reduction in shear wave velocity of ~45%. We propose that the thick fault zone, aided by fault geometry and basin structure, enabled prolonged propagating supershear,” explain the study authors.
They note that the simple fault geometry and wide fault zone likely provide the most important conditions behind the long-distance supershear and supershear-to-supershear transition, due to fault stress perturbations leading to the development of a supershear rupture front.
“As rupture propagated on the western rift, smooth fault geometry provided a 'highway' to help maintain supershear rupture, similar to what might happen for other supershear events. The relatively thick sedimentary basin (about 2 to 3 km) along the southern rift segment is another favorable condition for maintaining supershear rupture, as reflected waves from the basin floor can increase shear stress on the fault and promote rupture propagation.” The study authors say.
Insights into the features that lead to higher potential for superrupture velocities can help improve seismic hazard models for regions with known thick fault zones and simple fault geometries, especially for cities near major strike-slip faults. However, there is still work to be done. More comprehensive models that include detailed fault zone structures may be useful for more detailed seismic hazard assessment.
Written for you by our author Crystal Casal, edited by Gabe Clark, fact-checked and reviewed by Robert Egan – this article is the result of careful human work. We depend on readers like you to keep independent science journalism alive. If this report is important to you, please consider making a donation (especially monthly). You'll get an ad-free account as a thank you.
More information: Shengji Wei et al, Supershear rupture induced through a thick fault zone in the 2025Mw7.8 Mandalay earthquake, Science (2025). doi: 10.1126/science.adz2101
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Citation: Seismic study sheds light on factors leading to 2025 Myanmar supershear rupture (2025, November 1) Retrieved November 1, 2025 from https://phys.org/news/2025-10-seismic-factors-myanmar-supershear-rupture.html
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