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Hadaean to Palaeoarchaean stagnant-lid tectonics revealed by zircon magnetism - Nature

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Hadaean to Palaeoarchaean stagnant-lid tectonics revealed by zircon magnetism - Nature

Plate tectonics is a fundamental factor in the sustained habitability of Earth, but its time of onset is unknown, with ages ranging from the Hadaean to Proterozoic eons1–3. Plate motion is a key diagnostic to distinguish between plate and stagnant-lid tectonics, but palaeomagnetic tests have been thwarted because the planet's oldest extant rocks have been metamorphosed and/or deformed4.

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Hadaean to Palaeoarchaean stagnant-lid tectonics revealed by zircon magnetism - Nature

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Hadaean to Palaeoarchaean stagnant-lid tectonics revealed by zircon magnetism - Nature

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