Dataset 6043

Dataset record

Type

title in English

Global contourite distribution database, version 2

Description in English

More info http://www.marineregions.org/sources.php#contourite

Abstract in English

This product offers a global overview of contourite distribution. Contourites are sedimentary units which are deposited or substantially reworked by alongslope bottom currents. They refer to the lithological unit and the terminology reflects the grain size of the sediment. Drifts refer to the same sedimentary unit as a contourite, but the word 'drift' reflects the morphological appearance of the sedimentary unit. The product was elaborated digitizing the information from several hundred published scientific papers.

Contactpoint

Email: info@marineregions.org

License

https://spdx.org/licenses/CC-BY-NC-SA-4.0.html

bibliographicCitation

Flanders Marine Institute; Renard Centre of Marine Geology - Ugent (2018). Global contourite distribution database, version 2. Available online at https://www.marineregions.org

Release date

Oct 12 2018 12:00AM

Publication references

related reference: Used in this dataset /id/publication/302334; Used in this dataset /id/publication/302379; Used in this dataset /id/publication/302422; Used in this dataset /id/publication/302381; Used in this dataset /id/publication/302386; Used in this dataset /id/publication/302336; Used in this dataset /id/publication/302085; Used in this dataset /id/publication/302385; Used in this dataset /id/publication/240590; Used in this dataset /id/publication/240718; Used in this dataset /id/publication/302302; Used in this dataset /id/publication/302248; Used in this dataset /id/publication/199043; Used in this dataset /id/publication/302089; Used in this dataset /id/publication/302387; Used in this dataset /id/publication/302244; Used in this dataset /id/publication/302238; Used in this dataset /id/publication/302242; Used in this dataset /id/publication/302328; Used in this dataset /id/publication/199095; Used in this dataset /id/publication/302330; Used in this dataset /id/publication/302088; Used in this dataset /id/publication/302093; Used in this dataset /id/publication/302395; Used in this dataset /id/publication/240711; Used in this dataset /id/publication/302232; Used in this dataset /id/publication/302096; Used in this dataset /id/publication/240724; Used in this dataset /id/publication/302090; Used in this dataset /id/publication/302245; Used in this dataset /id/publication/302251; Used in this dataset /id/publication/201194; Used in this dataset /id/publication/201191; Used in this dataset /id/publication/201179; Used in this dataset /id/publication/199913; Used in this dataset /id/publication/201192; Used in this dataset /id/publication/302326; Used in this dataset /id/publication/201187; Used in this dataset /id/publication/302074; Used in this dataset /id/publication/302230; Used in this dataset /id/publication/302234; Used in this dataset /id/publication/302299; Used in this dataset /id/publication/302083; Used in this dataset /id/publication/302229; Used in this dataset /id/publication/302082; Used in this dataset /id/publication/302249; Used in this dataset /id/publication/302081; Used in this dataset /id/publication/302378; Used in this dataset /id/publication/302308; Used in this dataset /id/publication/302087; Used in this dataset /id/publication/302627; Used in this dataset /id/publication/302078; Used in this dataset /id/publication/143477; Used in this dataset /id/publication/302428

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