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Statements

Subject Item
dbr:Contourite
rdf:type
dbo:Library
rdfs:label
Conturiti Contourite 平流岩
rdfs:comment
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. 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。 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.
foaf:depiction
n14:Contourite_Distribution.jpg n14:Contourite_bedform_diagram_Stow2009.png n14:Contourite_bottom_water_flow_IODP_Gulf_of_Cadiz.png n14:Contourite_sheets_seismic_gulf_of_cadiz.png n14:Contourite_sparker_seismic_elongate_drift.png
dct:subject
dbc:Sedimentology
dbo:wikiPageID
24446547
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1107751757
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dbr:Faeroe_Islands dbr:Strait_of_Gibraltar dbr:Mya_(unit) dbr:Particle_size_(grain_size) dbr:Climate dbr:Sedimentation dbr:Surface_eddy_kinetic_energy dbr:Abyssal n9:Contourite_Distribution.jpg dbr:Erosion dbr:Bathymetric dbr:Lake dbr:Mud dbr:St._Croix dbr:Suspended_load dbr:Calcareous dbr:Ediacaran dbr:Sediment_transport dbr:Wave_base dbr:Sediment dbr:Tectonic_uplift dbr:Cenozoic dbr:Sediment_waves dbr:Chemistry dbr:Oceanic_basin dbr:Stream_channel dbr:Silt dbr:Compaction_(geology) dbr:Ocean_current dbr:Terrigenous dbr:Biology dbr:Continental_shelf dbr:Tide dbr:Hebrides dbr:Tectonics dbr:Biogenic dbr:Benthic dbr:Flow_conditions dbr:Carbonate_compensation_depth dbr:Contour_line dbr:Nova_Scotia dbr:Turbidite dbr:Benthic_storms dbr:Turbidity_current dbr:Ridges dbr:Continental_slope dbr:Sea_level dbr:Geomorphology dbr:Reflection_seismology dbr:Burrowing dbr:Continental_margin dbr:Nepheloid_layer dbr:Halifax_Regional_Municipality dbr:Storm dbr:Turbidites dbr:Bioturbation dbr:Continental_rise dbr:Coriolis_force dbc:Sedimentology dbr:Blake_Basin dbr:Density_gradient dbr:Thermohaline_circulation n9:Contourite_bedform_diagram_Stow2009.png n9:Contourite_bottom_water_flow_IODP_Gulf_of_Cadiz.png n9:Contourite_sheets_seismic_gulf_of_cadiz.png dbr:Volcanic n9:Contourite_sparker_seismic_elongate_drift.png dbr:Bathymetry dbr:Geostrophic_current
owl:sameAs
wikidata:Q3689394 freebase:m.080l_f8 dbpedia-it:Conturiti n16:3QQ8o dbpedia-zh:平流岩
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dbt:Legend2 dbt:Short_description dbt:Reflist dbt:Sediment_sidebar dbt:Clarify dbt:Where%3F dbt:Physical_oceanography
dbo:thumbnail
n14:Contourite_bottom_water_flow_IODP_Gulf_of_Cadiz.png?width=300
dbo:abstract
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。 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. 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.
gold:hypernym
dbr:Deposit
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wikipedia-en:Contourite?oldid=1107751757&ns=0
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20301
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wikipedia-en:Contourite