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Thermal history of deep-sea sediments as a record of recent changes in the deep circulation of the eastern Mediterranean ArchiMer
Della Vedova, B; Pellis, G; Camerlenghi, A; Foucher, Jean-paul; Harmegnies, Francois.
[1] During three cruises of the MEDRIFF project in 1993 and 1994, 154 geothermal heat flow measurements and seven CTD profiles in the water column have been collected along a 300 km SW-NE oriented transect traversing the Mediterranean Ridge accretionary complex. The original goal of the measurements was to identify areas of anomalous heat flow that could be interpreted as possible sites for fluid outflow. Contrary to expectations, the upper few meters of the temperature profiles in the sediments showed decreasing temperature from the seafloor down to 3 to 6 m depth indicating consistently transient temperature regimes. The only exception ( positive heat flow) was found in the Sirte abyssal plain. Measurements collected in the same area at different times...
Tipo: Text Palavras-chave: Eastern Mediterranean; Aegean waters; Sediment warming; Heat flow measurements; Thermal modeling; Thermal history.
Ano: 2003 URL:
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