Thermodynamic Efficiency of Brittle Frictional Mountain Building
An active fold-and-thrust belt in unchanging tectonic and climatic conditions attains a dynamic steady-state in which the influx of accreted material at the toe is balanced by the erosive efflux off the top. The overall balance of energy in such a steady-state fold-and-thrust belt is described by th...
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Veröffentlicht in: | Science (American Association for the Advancement of Science) 1988-11, Vol.242 (4879), p.749-752 |
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Format: | Artikel |
Sprache: | eng |
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