Deep weathering in the semi-arid Coastal Cordillera, Chile

Abstract The weathering front is the boundary beneath Earth’s surface where pristine rock is converted into weathered rock. It is the base of the “critical zone”, in which the lithosphere, biosphere, and atmosphere interact. Typically, this front is located no more than 20 m deep in granitoid rock i...

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Autores principales: Laura V. Krone, Ferdinand J. Hampl, Christopher Schwerdhelm, Casey Bryce, Lars Ganzert, Axel Kitte, Kirstin Übernickel, Armin Dielforder, Santiago Aldaz, Rómulo Oses-Pedraza, Jeffrey Paulo H. Perez, Pablo Sanchez-Alfaro, Dirk Wagner, Ute Weckmann, Friedhelm von Blanckenburg
Formato: article
Lenguaje:EN
Publicado: Nature Portfolio 2021
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Acceso en línea:https://doaj.org/article/127a87e9c54f4c688f95e83536c76b35
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