The Iberian Horseshoe

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The major source of terrigenous material feeding the HAP is the Sao Vicente canyon, which incises the Portuguese shelf, while minor sources are the surrounding seamounts. The elongate geometry of the abyssal plain with its single dominant source of sediments produced laterally continuous deposits from both large and small flows.

These covered the entire km length of the plain. Grain-size analysis of the four thickest turbidites H 2 , H 3 , H 8 , and H 9 demonstrates only slight downcurrent fining and vertical grading, expressed best in the ratio of coarse silt to fine silt plus clay. A small amount of sand is carried the length of the plain. The thicker units all show the same pattern of thickness, with a maximum in the middle of the plain around a topographic constriction and bend. This is most plausibly explained as due to reduction in flow speed of an initially supercritical flow causing enhanced deposition.

Some of the beds appear to have a double coarse layer in the base, which may indicate partial reflection of flows from the side of the basin. It is suggested by application of equations for flow behavior that both thick nearly equal 3 m and thin nearly equal 0. The stratigraphy is tied into the dated oceanic pelagic record by analysis of foraminifera in the pelagic layers above the turbidites and through recognition of two Heinrich layers H-1 and H-2, ages The resulting age framework shows higher turbidite frequency in the glacial 2.

This also gives higher mass flux during the glacial. Emplacement of turbidites cannot be clearly related to sea-level changes but may well be due to seismic activity. However, one of the largest earthquakes in human experience Lisbon in triggered only a thin turbidite, invalidating the term "seismite" for thick turbidites. Shibboleth Sign In.

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The Interesting Case of the Iberian Gene Pool

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Advanced Search. Article Navigation. Close mobile search navigation Article navigation. The resulting age framework shows higher turbidite frequency in the glacial 2. This also gives higher mass flux during the glacial. Emplacement of turbidites cannot be clearly related to sea-level changes but may well be due to seismic activity. However, one of the largest earthquakes in human experience Lisbon in triggered only a thin turbidite, invalidating the term "seismite" for thick turbidites.

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Close mobile search navigation Article navigation. Volume 67, Number 5. Previous Article Next Article. Other September 01, Lebreiro Susana M. Google Scholar. Nicholas McCave I.


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  • Nicholas McCave. Philip P. Weaver Philip P. Journal of Sedimentary Research 67 5 : ASK US …. Weight 0. Cancel reply Your email address will not be published. Similar Styles Weight Choose an option From to grs. From to grs. Weight Choose an option From 1,1 to 1,2 Kg. From 1,2 to 1,3 Kg. From 1,3 to 1,4 Kg. From 1,4 to 1,5 Kg. Weight Choose an option From to grs.

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