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| Name：GabrielUnliz | 03, Feb, 2026 23:06:27 | |
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it is shown how contrasting styles of crustal relamination and magmatism in continental collision zones are controlled by slab steepening which itself is mainly a function of the subducting continental crust's buoyancy. We drank a lot together. We laughed a lot together. We were there for each other | |
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