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A team of geologists has uncovered that a remnant of the ancient Neotethys oceanic plate is plunging into the mantle beneath the Zagros Mountains in Iraq, causing significant geological changes in the region. The study, published in the journal Solid Earth, reveals that as this plate descends, it is also tearing apart beneath the mountains, relieving some pressure from the overlying crust, according to lead researcher Renas Koshnaw from Göttingen University.
The Neotethys ocean existed approximately 195 million years ago when Pangaea split into two supercontinents. Its crust had significant impacts on the formation of the Zagros Mountains, causing a depression filled with sediment between 3,000 to 4,000 meters deep. The research indicates that the unique sediment thickness cannot solely be explained by the weight of the mountains, suggesting that the dynamics between the mantle and crust play a crucial role in shaping the area's topography. Understanding these processes, researchers noted, could also aid in locating natural resources and assessing geological hazards in the region.