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- W2943595953 abstract "The JOIDES drillings, positioned on the Floridian Shelf and on the Blake Plateau, were examined in order to try to find the nature and the origin of the fine non calcareous particles. During a long time span, from the Paleocene to the Oligocene, the fine terrigenous imput remained remarkably constant on the shelf and on the deeper Blake Plateau. It comprised quartz and montmorillonite brought by the Gulf Stream from the Gulf of Mexico. With the Miocene, the shelf emerged and was transformed in lagoons. There, the detritals and the dissolved elements washed from the continent were deposited as marl oozes comprising attapulgite, phosphates and dolomitic aggregates. During the same period, the Blake Plateau still received Gulf Stream imput. Finally during the Pleistocene regressions a general revorking of the superficial deposits occured on the shelf." @default.
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- W2943595953 date "1971-01-01" @default.
- W2943595953 modified "2023-10-17" @default.
- W2943595953 title "Les apports terrigènes fins dans les dépôts du précontinent américain au large de la Floride (projet Joides)" @default.
- W2943595953 doi "https://doi.org/10.3406/bulmi.1971.6590" @default.
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