Titlebook: Weathering and the Riverine Denudation of Continents; Pedro José Depetris,Andrea Inés Pasquini,Karina Le Book 2014 The Author(s) 2014 Diss

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The Wearing Away of Continents, wearing down, of which it is a chief agent. Tectonic uplift stimulates fluvial erosion, on contact with the water cycled by solar energy and clustered in surface channels by catchment processes. Progressive sediment transfers occur between upper and lower catchments, and subsequently between lower

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只看該作者 · 發(fā)表于 2025-3-30 21:14:36

Conclusion,aining fraction by dissolved solids. Aeolian dust and ice-rafted rock fragments contribute a less-known proportion. This material transfer does not necessarily reflect the intensity and rate of weathering occurring on the continents because a significant fraction is supplied by outcropping sedimenta

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