hdl:10013/epic.30765
Clay minerals as indicator of deposition of upper Quaternary sediments within the St. Anna Trough (Kara Sea)
Krylov, A. A., Weiel, D., Sapega, V. F., Ivanov, G. I., Stein, Rüdiger 
ORCID: https://orcid.org/0000-0002-4453-9564, Vogt, C. and Rys'kova, E. O.
;
ORCID: https://orcid.org/0000-0002-4453-9564, Vogt, C. and Rys'kova, E. O.
;
Contact
Ruediger.Stein [ at ] awi.de
Abstract
Item Type
Article
Authors
Krylov, A. A., Weiel, D., Sapega, V. F., Ivanov, G. I., Stein, Rüdiger ORCID: https://orcid.org/0000-0002-4453-9564, Vogt, C. and Rys'kova, E. O.
;
ORCID: https://orcid.org/0000-0002-4453-9564, Vogt, C. and Rys'kova, E. O.
;
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Programs
Helmholtz Research Programs > MARCOPOLI (2004-2008) > POL-MARCOPOLI
Helmholtz Research Programs > MARCOPOLI (2004-2008) > POL6-Earth climate variability since the Pliocene
Helmholtz Research Programs > MARCOPOLI (2004-2008) > POL6-Earth climate variability since the Pliocene
Publication Status
Published
Eprint ID
19009
Cite as
Krylov, A. A.
,
Weiel, D.
,
Sapega, V. F.
,
Ivanov, G. I.
,
Stein, R.
,
Vogt, C.
and
Rys'kova, E. O.
(2008):
Clay minerals as indicator of deposition of upper Quaternary sediments within the St. Anna Trough (Kara Sea)
,
Oceanology,
48
(1),
pp. 85-93
.
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