How Plate Tectonics Shapes Long-Term Climate Through Silicate Weathering and Carbon Sequestration

板块构造如何通过硅酸盐风化与碳封存塑造长期气候

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Mountain building from continental collisions exposes fresh silicate rock to atmospheric CO₂ and rainfall, initiating chemical weathering that draws down greenhouse gases over millions of years.
The reaction converts CO₂ into bicarbonate ions, which rivers carry to oceans where marine organisms precipitate carbonate shells—locking carbon into sediments.

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