Melange production and the importance of shale diapirism in accretionary terrains
Although melanges are widely believed to form in subduction zones, there is little agreement as to the mechanism by which the characteristic chaotic aspect of a melange develops 1,2 . Debate centres on the relative effects of gravity sliding down the inner trench slope and shearing along thrust faul...
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Veröffentlicht in: | Nature (London) 1984-01, Vol.309 (5964), p.145-146 |
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Format: | Artikel |
Sprache: | eng |
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