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Statements

Subject Item
dbr:Hemipelagic_sediment
rdfs:label
Hemipelagic sediment 半遠洋性沉積物
rdfs:comment
Hemipelagic sediment, or hemipelagite, is a type of marine sediment that consists of clay and silt-sized grains that are terrigenous and some biogenic material derived from the landmass nearest the deposits or from organisms living in the water. Hemipelagic sediments are deposited on continental shelves and continental rises, and differ from pelagic sediment compositionally. Pelagic sediment is composed of primarily biogenic material from organisms living in the water column or on the seafloor and contains little to no terrigenous material. Terrigenous material includes minerals from the lithosphere like feldspar or quartz. Volcanism on land, wind blown sediments as well as particulates discharged from rivers can contribute to Hemipelagic deposits. These deposits can be used to qualify cli 半遠洋性沉積物或半深海沉積物是遠海沉積物的一種，是由紋路細膩的生物和陸源物質所組成，不同之處在於遠海沉積物主要是由幾乎不含路原物質的生物物質所組成。 半遠洋性沉積物的沉積速度相較於遠海沉積物之下是相對快速的，但依舊很緩慢。　半遠洋性沉積物主要沉積在大陸棚和大陸基，而且通常因為沉積過快導致無法與海水產生化學反應，因此在大多數情況下，每一顆粒子都保留了它們形成區域所賦予它們的特徵。
dcterms:subject
dbc:Sediments
dbo:wikiPageID
27500004
dbo:wikiPageRevisionID
1000075015
dbo:wikiPageWikiLink
dbr:Biogenic dbr:Fluvial dbr:Continental_rise dbr:Feldspar dbr:Tuffaceous dbr:Interglacial dbr:Lithosphere dbc:Sediments dbr:Glacial dbr:Detritus dbr:Quartz dbr:Turbidity_currents dbr:Turbidite dbr:Hydrothermal dbr:Radiolarians dbr:Continental_shelves dbr:Chert dbr:Argillite dbr:Terrigenous dbr:Diatoms dbr:Marine_sediment dbr:Volcanism dbr:Pelagic_sediment dbr:Sedimentary_rock
owl:sameAs
wikidata:Q5711878 dbpedia-vi:Trầm_tích_nửa_biển_khơi dbpedia-az:Hemipelagik_çöküntülər n14:4masj dbpedia-zh:半遠洋性沉積物
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dbo:abstract
半遠洋性沉積物或半深海沉積物是遠海沉積物的一種，是由紋路細膩的生物和陸源物質所組成，不同之處在於遠海沉積物主要是由幾乎不含路原物質的生物物質所組成。 半遠洋性沉積物的沉積速度相較於遠海沉積物之下是相對快速的，但依舊很緩慢。　半遠洋性沉積物主要沉積在大陸棚和大陸基，而且通常因為沉積過快導致無法與海水產生化學反應，因此在大多數情況下，每一顆粒子都保留了它們形成區域所賦予它們的特徵。 Hemipelagic sediment, or hemipelagite, is a type of marine sediment that consists of clay and silt-sized grains that are terrigenous and some biogenic material derived from the landmass nearest the deposits or from organisms living in the water. Hemipelagic sediments are deposited on continental shelves and continental rises, and differ from pelagic sediment compositionally. Pelagic sediment is composed of primarily biogenic material from organisms living in the water column or on the seafloor and contains little to no terrigenous material. Terrigenous material includes minerals from the lithosphere like feldspar or quartz. Volcanism on land, wind blown sediments as well as particulates discharged from rivers can contribute to Hemipelagic deposits. These deposits can be used to qualify climatic changes and identify changes in sediment provenances.
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wikipedia-en:Hemipelagic_sediment?oldid=1000075015&ns=0
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8149
foaf:isPrimaryTopicOf
wikipedia-en:Hemipelagic_sediment