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Andean margin

Benedetto, J.L. (1998) Early Paleozoic brachiopods and associated shelly faunas from western Gondwana their bearing on the geodynamic history of the pre-Andean margin. Geological Society, London, Special Publications, 142, 57-83. [Pg.311]

Figure SJ4 The La/Yb-Sc/Ni discriminadon diagram for andesites (after Bailey, 1981) showing the fields of Andean-type (active continental margin), continental island-arc, low-K oceanic island-arc and other oceanic island-arc andesites. Figure SJ4 The La/Yb-Sc/Ni discriminadon diagram for andesites (after Bailey, 1981) showing the fields of Andean-type (active continental margin), continental island-arc, low-K oceanic island-arc and other oceanic island-arc andesites.
Active continental margin — Andean- pe basins developed on or adjacent to thick continental margins. Strike-slip basins also develop in this environment... [Pg.206]


See other pages where Andean margin is mentioned: [Pg.165]    [Pg.165]    [Pg.88]    [Pg.1798]    [Pg.19]    [Pg.201]    [Pg.161]    [Pg.190]    [Pg.409]   
See also in sourсe #XX -- [ Pg.19 ]




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Marginalization

Margining

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