The lachlan belt of eastern Australia and Circum-Pacific tectonic evolution
There is considerable evidence that the Pacific Ocean basin has had a remarkable permanency at least throughout the Phanerozoic. The orogenic systems that have evolved around its margins are accretionary continental margin orogens and show little or no evidence of continental collisions in their evo...
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Veröffentlicht in: | Tectonophysics 1992-11, Vol.214 (1), p.1-25 |
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Format: | Artikel |
Sprache: | eng |
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