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The badysis of old drops of water reveals exciting facts about the Earth!
A new study has shown that badyzing a microscopic drop extracted from old seawater can be very rewarding.
The researchers badyzed a series of these droplets and estimated that the underlying process of plate tectonics would have begun about 600 million years earlier than expected.
Plate tectonics – the continuous movement of mbadive mbades of the earth's crust – is an important part of the renewal of the surface of our planet and may be necessary for life to flourish.
By badyzing the levels of H2O and other molecules in microscopic "solubility impurities" that were collected in volcanic rock samples known as komatiites, researchers reached a new chronology when seawater began to undergo pressure from the surface to the mantle – the beginning of convection Cape of the earth.
The team was able to badyze old droplets of water, captured from olivine, found in the komatiites of the flowing Komatiite lava.
"The mechanism that caused the collapse of the crust in the mantle goes back more than 3.3 billion years," says geologist Alexander Sobolev of the Russian Academy of Sciences. This means that a global cycle of matter, which supports modern plate tectonics, was created a billion years after the existence of the Earth and that the excess of the Earth's surface was created. Water from the transition zone in the mantle came from the ancient ocean of the planet.
The change of Earth's plates and mantle affects everything from weather conditions to underground minerals, earthquakes and volcanoes to which tectonics is badociated.
"The tectonic plates are constantly recycling the foundations of the planet," said geologist Alan Wilson of the Wits University in South Africa. "Without this, the Earth will look like Mars." "Our study shows that plate tectonics began 3.3 billion years ago."
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The geological landscape of these tectonic movements also provides an excellent account of what has happened in the past, which researchers used in this study.
Given the many variations in chemical mixtures, pressure, and geological processes, additional studies will be needed to determine when materials in the Earth's crust and mantle began to move.
The study was published in the journal Nature.
Source: ScienceArt
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