Steady incision of Grand Canyon at the million year timeframe: A case for mantle-driven differential uplift
The Grand Canyon region provides an excellent laboratory to examine the interplay between river incision, magmatism, and the geomorphic and tectonic processes that shape landscapes. Here we apply U-series, Ar–Ar, and cosmogenic burial dating of river terraces to examine spatial variations in incisio...
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Veröffentlicht in: | Earth and planetary science letters 2014-07, Vol.397, p.159-173 |
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