Unveiling the contourite depositional system in the Vema Fracture Zone (Central Atlantic)
Unveiling the contourite depositional system in the Vema Fracture Zone (Central Atlantic)
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Publisher
London: Nature Publishing Group UK
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English
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London: Nature Publishing Group UK
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A combination of a high sediment input and intense bottom currents often leads to the formation of contourites (sediments deposited or significantly reworked by bottom currents). Both of these components are present in the Vema Fracture Zone valley which is the most important passageway for the distribution of the Antarctic Bottom Water from the We...
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Full title
Unveiling the contourite depositional system in the Vema Fracture Zone (Central Atlantic)
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TN_cdi_doaj_primary_oai_doaj_org_article_80ff27800aac484980ed244f1fca81b7
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https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_doaj_primary_oai_doaj_org_article_80ff27800aac484980ed244f1fca81b7
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ISSN
2045-2322
E-ISSN
2045-2322
DOI
10.1038/s41598-023-40401-4
