hdl:10013/epic.45406

Clay minerals as indicators of late Quaternary sedimentation constraints in the Mendeleev Ridge, Amerasian Basin, Arctic Ocean.


Krylov, A. A., Stein, Rüdiger ORCID: https://orcid.org/0000-0002-4453-9564 and Ermakova, L.A. ;
Contact
akrylow [ at ] gmail.com

Abstract


Item Type
Article
Authors
Krylov, A. A., Stein, Rüdiger ORCID: https://orcid.org/0000-0002-4453-9564 and Ermakova, L.A. ;
Divisions
AWI Organizations > Geosciences > Marine Geology and Paleontology
Primary Division
Organizations > AWI Organizations > Geosciences > Marine Geology and Paleontology
Programs
Helmholtz Research Programs > PACES II (2014-2020) > TOPIC 3: The earth system from a polar perspective > WP 3.1: Circumpolar climate variability and global teleconnections at seasonal to orbital time scales
Primary Topic
Helmholtz Programs > Helmholtz Research Programs > PACES II (2014-2020) > TOPIC 3: The earth system from a polar perspective > WP 3.1: Circumpolar climate variability and global teleconnections at seasonal to orbital time scales
Publication Status
Published
Eprint ID
37817
Cite as
Krylov, A. A. , Stein, R. and Ermakova, L. (2014): Clay minerals as indicators of late Quaternary sedimentation constraints in the Mendeleev Ridge, Amerasian Basin, Arctic Ocean. , Lithology and Mineral Resources, 49 , pp. 103-116 .


Share
Add to AnyAdd to TwitterAdd to FacebookAdd to LinkedinAdd to PinterestAdd to Email

Geographical region
Arctic Ocean

Research Platforms
N/A

Campaigns
N/A


Actions
Edit Item Edit Item