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Engineering professor solves the mystery of deep earthquakes

Engineering professor solves the mystery of deep earthquakes


Xanthippi Markenscoff, an engineering professor from the School of Engineering at the University of California, San Diego, has solved a mystery about the deep earthquakes that have puzzled the scientific community since they were first discovered in the 1920s. My findings are presented in the Journal of Mechanics and Physics of Solids.

Scientists in the 1920s discovered a mysterious phenomenon occurring far from the Earth’s crust: Earthquakes occur in areas that should not be possible, according to the latest scientific understanding.

Mysterious earthquakes arose between 400 and 700 kilometers (250-430 miles) below the Earth’s surface and were recorded on a scale of 8.3 on the Richter scale.

According to the term “deep-focus earthquake,” mysterious deep earthquakes – which originated in conditions of incredibly high pressure within the Earth’s mantle – were first discovered in 1929.

Scientists had previously assumed that the high-pressure environment deep below the Earth’s surface would cause an internal explosion, triggering deep earthquakes. However, they were unable to find enough evidence to support the theory.

The origin of highly concentrated earthquakes

In her new study, Markenscoff presents a novel solution to highly concentrated earthquakes, along with ample evidence presented through computer modeling.

A high-pressure environment extending 400-700 kilometers (250-430 miles) below the Earth’s surface is known to cause shale rocks to turn into a denser type of rock called spinel – a process somewhat similar to converting coal into diamonds below the Earth’s surface. . Under tremendous pressure.

The transformation from rock to spinel causes the rock size to decrease due to the high pressure environment. The so-called “scale collapse” is related to the transmutation defect, which is presented as the main cause of highly concentrated earthquakes in Markenskov’s paper.

Using mathematical models and simulations, Markensoff concluded that deep-focused earthquakes occur as a result of the effects of high pressure in conjunction with a shift in volume during a “volume collapse”.

When asked how she feels about her groundbreaking results, Markenscoff said, “I feel like I’m connected to nature. I’ve discovered the beauty of how nature works.”

“It’s the first time in my life,” she explained in a press release from the University of California, San Diego. “Before I took a small step on someone else’s footsteps. I felt this tremendous joy.”

The new research adds to a growing field of research into the effects, origins and impact of earthquakes run by computer simulations, including one operated by the world’s fastest supercomputer, Fugaku.

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