Contourite (original) (raw)

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A contourite is a sedimentary deposit commonly formed on continental rise to lower slope settings, although they may occur anywhere that is below storm wave base. Countourites are produced by thermohaline-induced deepwater bottom currents and may be influenced by wind or tidal forces. The geomorphology of contourite deposits is mainly influenced by the deepwater bottom-current velocity, sediment supply, and seafloor topography.

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dbo:abstract A contourite is a sedimentary deposit commonly formed on continental rise to lower slope settings, although they may occur anywhere that is below storm wave base. Countourites are produced by thermohaline-induced deepwater bottom currents and may be influenced by wind or tidal forces. The geomorphology of contourite deposits is mainly influenced by the deepwater bottom-current velocity, sediment supply, and seafloor topography. (en) Le conturiti, sono depositi di mare profondo guidate dalle . Trovandosi alla base della scarpata continentale, proprio dove la corrente le trasporta, queste vanno ad erodere su un lato, formando i , e depositano sul lato opposto, formando i Drift. Esistono poi drift di vario tipo, a seconda di come scorre la corrente e come viene depositato il sedimento. Le forme caratteristiche delle conturiti sono i Sediment wave, vale a dire delle ondulazioni del fondo marino, dovute sia al movimento costante delle conturiti (e la loro relativa corrente), sia al movimento degli che muovono in continuazione il sedimento. Le conturiti possono essere sabbiose o fangose; le prime sono le più rare, le seconde sono le più comuni. (it) 平流岩(英語:Contourite),又称等深岩,是由平流沉积物或经平流改造的原有沉积物所形成的沉积岩,常产于复理石等深水相层系中,这一地質名詞最先由Hollister和Heezen於1972年提出。 (zh)
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rdfs:comment A contourite is a sedimentary deposit commonly formed on continental rise to lower slope settings, although they may occur anywhere that is below storm wave base. Countourites are produced by thermohaline-induced deepwater bottom currents and may be influenced by wind or tidal forces. The geomorphology of contourite deposits is mainly influenced by the deepwater bottom-current velocity, sediment supply, and seafloor topography. (en) Le conturiti, sono depositi di mare profondo guidate dalle . Trovandosi alla base della scarpata continentale, proprio dove la corrente le trasporta, queste vanno ad erodere su un lato, formando i , e depositano sul lato opposto, formando i Drift. Esistono poi drift di vario tipo, a seconda di come scorre la corrente e come viene depositato il sedimento. Le forme caratteristiche delle conturiti sono i Sediment wave, vale a dire delle ondulazioni del fondo marino, dovute sia al movimento costante delle conturiti (e la loro relativa corrente), sia al movimento degli che muovono in continuazione il sedimento. Le conturiti possono essere sabbiose o fangose; le prime sono le più rare, le seconde sono le più comuni. (it) 平流岩(英語:Contourite),又称等深岩,是由平流沉积物或经平流改造的原有沉积物所形成的沉积岩,常产于复理石等深水相层系中,这一地質名詞最先由Hollister和Heezen於1972年提出。 (zh)
rdfs:label Contourite (en) Conturiti (it) 平流岩 (zh)
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