Which is the better proxy for paleo‐current strength: Sortable‐silt mean size () or sortable‐silt mean grain diameter (d SS )? A case study from the N ordic S eas-Reference-Cited by-同舟云学术

Which is the better proxy for paleo‐current strength: Sortable‐silt mean size () or sortable‐silt mean grain diameter (d SS )? A case study from the N ordic S eas

Published:2015-10 Issue:10 Volume:16 Page:3456-3471
ISSN:1525-2027
Container-title:Geochemistry, Geophysics, Geosystems
language:en
Short-container-title:Geochem. Geophys. Geosyst.

Author:

Tegzes Andrea D.¹,Jansen Eystein²,Telford Richard J.³

Affiliation:

1. UNI Research and Bjerknes Centre for Climate ResearchBergen Norway

2. Department of Earth Science and Bjerknes Centre for Climate ResearchUniversity of BergenBergen Norway

3. Department of Biology and Bjerknes Centre for Climate ResearchUniversity of BergenBergen Norway

Funder

Research Council of Norway

Bjerknes Centre for Climate Research

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1002/2014GC005655

Reference41 articles.

1. Measurement of the sortable silt current speed proxy using the Sedigraph 5100 and Coulter Multisizer IIe: precision and accuracy

2. SediGraph technique

3. Predicting erosion resistance of muds

4. Sedimentary environment and glacial history during the last 40 ka of the Vøring continental margin, mid-Norway

5. Surface and Deep Ocean Interactions During the Cold Climate Event 8200 Years Ago

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