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Phase transitions in olivine may be the cause of a deep seismic fault
Left: the retrieved sample. The red police lines represent errors. Center: The rift is filled with nanocrystalline olives and wadslite. Right: Close-up view of the error in error. The iron-rich particles (product of partial fusion of olive: green) are distributed along the grain boundaries of the nanocrystalline peridot. Credit: Tomohiro Ohuchi, Ehime University
Earthquakes that occur hundreds of kilometers deep in the mantle are called “deep focus earthquakes”. Such earthquakes sometimes lead to serious disasters such as the 1994 Bolivia earthquake, which occurred at a depth of 638 km with a magnitude of 8.3.
However, the cause of high-focal earthquakes has been a mystery, because earthquakes occur with rapid fault slip, which is difficult under large deep mantle stresses. Attempts have been made to understand the mechanism of occurrence of hyperfocal earthquakes based on laboratory deformation experiments, but experiments under deep mantle conditions have not been performed due to technological limitations.
The team, for the first time, performed deformation experiments on natural olivine, the main mineral in the mantle and oceanic lithosphere (slate), by means of a modern, large-scale deformation apparatus in combination with a synchrotron. X-ray notes. They observed significant abnormalities in the sample by X-ray imaging under deep mantle conditions and ‘seismicity’ associated with ultrasonic acoustic emission measurements.
After careful analyzes of the retrieved sample, they found that the cause of the crack was the growth of “new” olivine with ultrafine grains of tens of nanometers at the phase transformation of the “old” olive, which acted as a lubricant for the rapid slip of the fault. They also found evidence that the sample melted locally along the fault due to the very high temperature generated by the rapid slip. Their model, based on these laboratory experiments, explains the distribution of deep-focus earthquakes, which increases with depths from ~400 km to ~600 km, where metastatic “old” olivine is expected to form “new” ultrafine grains. olivine.
The research has been published in the journal Nature Communications.
Left: Forming lenticular bundles filled with nanocrystalline peridot/Wadslite. Right: localization of the shear on the weak layer formed by the fusion of lenticular bundles. This results in shear heating followed by deeply focused faulting earthquakes. Credit: Tomohiro Ohuchi, Ehime University This study indicates that highly concentrated earthquakes are preferentially distributed around the surface of the spreading olefin wedge, which forms the central portion of the sliding plate. Credit: Tomohiro Ohuchi, University of Ehime’s Possible Olivine Mechanism for Boron Transfer to the Earth’s Deep Mantle More information: Tomohiro Ohuchi et al, In situ X-ray and acoustic observations of deep seismic fault on phase transitions in olivine, Nature Communications (2022). DOI: 10.1038 / s41467-022-32923-8
Presented by Ehime University
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