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Lower Eocene red-clay sedimentation on the George Bligh/Rockall Channel (1984)

Ferragne, A. ; Latouche, C. ; Parra, M.

Springer

Geo-marine letters 4 (1984), S. 77-82

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ISSN: 1432-1157

Source: Springer Online Journal Archives 1860-2000

Topics: Geosciences

Notes: Abstract Core 7710, recovered on the George Bligh/Rockall Channel, is composed of fine grained ocher-colored sediments rich in ferriferous smectite (montmorillonite, beidellite). These sediments were deposited during early Eocene in a shallow marine environment. Their mineralogic, chemical and isotopic constituents indicate subaerial weathering of lower Eocene intermediate igneous rocks (ferrodiorite, marscoiite) eroded from the still-emergent George Bligh and Rockall Banks. Lack of any post Eocene Sediments may be due to major morphologic and hydrologic changes forming sedimentation gaps.

Type of Medium: Electronic Resource

URL: http://dx.doi.org/10.1007/BF02277076

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