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La dépression nord-baléare (Espagne) 5
Auzende, Jean-marie; Olivet, Jean-louis; Mauffret, Alain; Pautet, Guy.
This document is a structural scheme of the northern Balearic depression based on continuous seismic-reflection profiles and on the results of the drilling cruise (n° 13) of the "Glomar Challenger" in the Mediterranean Sea. This scheme is linked, to a larger extent, to the hypothesis of the opening of the north-western Mediterranean Sea during the Oligocene epoch.
Tipo: Text Palavras-chave: Histoire Ifremer.
Ano: 1972 URL: http://archimer.ifremer.fr/doc/1972/publication-4903.pdf
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Les glissements sous-marins de la pente continentale niçoise et la rupture de câbles en mer Ligure (Méditerranée occidentale). 5
Gennesseaux, Maurice; Mauffret, Alain; Pautot, Guy.
On October 16, 1979, off the Bay of Nice, a turbidity current, generated by large submarine landslides. was channelled by submarine valleys down to the bathyal plain of the Ligurian Sea where it seriously damaged two submarine cables, at about 80 and 110 km from its starting-point. The measured mean speeds were 17 km/h, above the first cable, and 7 km/h between the two cables, but the speed may have reached 40 km/h on the upper slope. [NOT CONTROLLED OCR]
Tipo: Text Palavras-chave: Histoire Ifremer.
Ano: 1980 URL: http://archimer.ifremer.fr/doc/1980/publication-5314.pdf
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Upper miocene salt layer in the western mediterranean basin 5
Auzende, Jean-marie; Bonnin, Jean; Olivet, Jean-louis; Pautot, Guy; Mauffret, Alain.
"Flexotir" profiles in the Western Mediterranean Basin reveal a uniform salt layer, overlain by a sedimentary sequence affected by diapirism. The salt has been given an Upper Miocene age. [NOT CONTROLLED OCR]
Tipo: Text Palavras-chave: Histoire Ifremer.
Ano: 1971 URL: http://archimer.ifremer.fr/doc/1971/publication-4889.pdf
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Structural framework of selected regions of the western mediterranean 1. Valencia basin 5
Pautot, Guy; Auzende, Jean-marie; Olivet, Jean-louis; Mauffret, Alain.
The alignment of the Balearic Islands, stretching from the Spanish mainland towards the Corsican-Sardinian block, has long intrigued many geologists. Since Suess (1886), we know that the Balearic block (Ibiza, Formentera, and Majorca) is part of the Alpine system. Many authors (Kober, 1914; Staub, 1928; Kober, 1931) have subsequently attempted to comprehensively integrate the history of the Balearic block within the history of the Alpine chain. In this paper, we will use data from marine geology and geophysics to define the location of the Balearic Islands during the diverse phases of distension, shearing, and compression between the European and African plates, which created the present western Mediterranean and the Alpine chain. In particular, we will...
Tipo: Text Palavras-chave: Histoire Ifremer.
Ano: 1972 URL: http://archimer.ifremer.fr/doc/1972/publication-5035.pdf
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