Coastal evolution, changes in sea level and molluscan fauna in northeastern Argentina during the Late Quaternary
The northern Argentine shoreline underwent a remarkable progradation during the last 6890 years, equivalent to about 4000 km 2. The shoreline moved approximately 30 km seaward on the average. Two types of accretionary shorelines were formed. High energy environments produced barrier islands and barr...
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Veröffentlicht in: | Marine geology 1993-02, Vol.110 (1), p.163-175 |
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Format: | Artikel |
Sprache: | eng |
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