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Current denudation rates in dolostone karst from central Spain: Implications for the formation of unroofed caves
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文摘

We perform a rock tablets experiment to measure subsurface weathering of carbonates.

Physical and chemical weathering account for denudation of karst regions.

Thermal and moisture cycles cause enhanced physical weathering of carbonate rocks.

Higher subsurface weathering of carbonates occurs during wet and cold periods.

In the studied region unroofed caves are unlikely to result from denudation.

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