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Analysing lava flows that solidified and then broke apart over a massive crack in the Earth's crust in Turkey has brought new insights into how continents move over time, improving our understanding ...
and he has made multiple animated maps based from his research. For more animations from Scotese about tectonic plate motions — past and present — and Earth history, check out his YouTube page.
Tibetan uplift was mainly caused by post-collisional mantle dynamics, not ongoing India-Asia convergence. The study ...
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