Extant anoxic basins form after dissolution of Messinian evaporites on the flanks of deep-sea rimmed depressions. Anoxia is due to brine density stratification which prevents bottom water ventilation. -from Authors
Extreme deep-sea environment of the eastern Mediterranean anoxic basins: the state of the art
Camerlenghi A.;
1991-01-01
Abstract
Extant anoxic basins form after dissolution of Messinian evaporites on the flanks of deep-sea rimmed depressions. Anoxia is due to brine density stratification which prevents bottom water ventilation. -from AuthorsFile in questo prodotto:
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