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Seismologists are taking advantage of Martian earthquakes to map the internal structure of the planet, as seismic energy resonates through the crust in two types of waves, and scientists measure the subtle differences in the motion of the two waves and calculate the starting point of the core of the planet, its mantle, its crust and the end of each section, and these data also give them information about the components of These layers.
Earth’s continental crust is divided into sub-layers of different types of rock, and Justin Filiberto, a planetary geologist at the Texas Lunar and Planetary Institute, said the researchers speculated that the layers of Mars’ crust looked like layers of the Earth’s crust, but new data sent by Insight shows that the Mars crust has two or three layers, and the crustal thickness and layers can vary by region.
Julia Simbrich, a planet specialist at the Open University in the UK, told Nature that the new data better explains Martian geochemical models and meteorites, and that scientists are awaiting further data from the depth of Mars to the future, and possibly new information about the Red Planet’s core and mantle, and future studies will help researchers find out how Mars formed and evolved over time.
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Source: “The seventh day”
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