Clay minerals as indicators of late Quaternary sedimentation constraints in the Mendeleev Rise, Amerasian Basin, Arctic Ocean
The results of study of six cores taken from different morphostructural zones in the Mendeleev Ridge area are discussed. Average contents of minerals of the illite group, chlorite, kaolinite, and smectite are about 60, 21, 12, and 5%, respectively. It was found that fluctuations of minerals along th...
Published in: | Lithology and Mineral Resources |
---|---|
Main Authors: | , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Springer
2014
|
Subjects: | |
Online Access: | https://oceanrep.geomar.de/id/eprint/28022/ https://oceanrep.geomar.de/id/eprint/28022/1/2014_Krylov-etal-Clay_LithMinRes-49.pdf https://doi.org/10.1134/S0024490213060059 |
id |
ftoceanrep:oai:oceanrep.geomar.de:28022 |
---|---|
record_format |
openpolar |
spelling |
ftoceanrep:oai:oceanrep.geomar.de:28022 2024-02-04T09:56:40+01:00 Clay minerals as indicators of late Quaternary sedimentation constraints in the Mendeleev Rise, Amerasian Basin, Arctic Ocean Krylov, A. A. Stein, Rüdiger Ermakova, L. A. 2014 text https://oceanrep.geomar.de/id/eprint/28022/ https://oceanrep.geomar.de/id/eprint/28022/1/2014_Krylov-etal-Clay_LithMinRes-49.pdf https://doi.org/10.1134/S0024490213060059 en eng Springer https://oceanrep.geomar.de/id/eprint/28022/1/2014_Krylov-etal-Clay_LithMinRes-49.pdf Krylov, A. A., Stein, R. and Ermakova, L. A. (2014) Clay minerals as indicators of late Quaternary sedimentation constraints in the Mendeleev Rise, Amerasian Basin, Arctic Ocean. Open Access Lithology and Mineral Resources, 49 (1). pp. 103-116. DOI 10.1134/S0024490213060059 <https://doi.org/10.1134/S0024490213060059>. doi:10.1134/S0024490213060059 cc_by_nc info:eu-repo/semantics/openAccess Article PeerReviewed 2014 ftoceanrep https://doi.org/10.1134/S0024490213060059 2024-01-08T00:22:41Z The results of study of six cores taken from different morphostructural zones in the Mendeleev Ridge area are discussed. Average contents of minerals of the illite group, chlorite, kaolinite, and smectite are about 60, 21, 12, and 5%, respectively. It was found that fluctuations of minerals along the section correlate with variations in sedimentation constraints in the Late Quaternary. Peaks of kaolinite usually coincide with increased contents of the sand fraction, probably, due to its delivery by icebergs. In contrast, illite shows good correlation with the pelite fraction, testifying to its transport mainly by ices and currents. Minerals of the chlorite and smectite groups in the studied cores are less informative. Article in Journal/Newspaper Arctic Arctic Arctic Ocean Iceberg* OceanRep (GEOMAR Helmholtz Centre für Ocean Research Kiel) Arctic Arctic Ocean Mendeleev Rise ENVELOPE(-177.250,-177.250,80.250,80.250) Lithology and Mineral Resources 49 1 103 116 |
institution |
Open Polar |
collection |
OceanRep (GEOMAR Helmholtz Centre für Ocean Research Kiel) |
op_collection_id |
ftoceanrep |
language |
English |
description |
The results of study of six cores taken from different morphostructural zones in the Mendeleev Ridge area are discussed. Average contents of minerals of the illite group, chlorite, kaolinite, and smectite are about 60, 21, 12, and 5%, respectively. It was found that fluctuations of minerals along the section correlate with variations in sedimentation constraints in the Late Quaternary. Peaks of kaolinite usually coincide with increased contents of the sand fraction, probably, due to its delivery by icebergs. In contrast, illite shows good correlation with the pelite fraction, testifying to its transport mainly by ices and currents. Minerals of the chlorite and smectite groups in the studied cores are less informative. |
format |
Article in Journal/Newspaper |
author |
Krylov, A. A. Stein, Rüdiger Ermakova, L. A. |
spellingShingle |
Krylov, A. A. Stein, Rüdiger Ermakova, L. A. Clay minerals as indicators of late Quaternary sedimentation constraints in the Mendeleev Rise, Amerasian Basin, Arctic Ocean |
author_facet |
Krylov, A. A. Stein, Rüdiger Ermakova, L. A. |
author_sort |
Krylov, A. A. |
title |
Clay minerals as indicators of late Quaternary sedimentation constraints in the Mendeleev Rise, Amerasian Basin, Arctic Ocean |
title_short |
Clay minerals as indicators of late Quaternary sedimentation constraints in the Mendeleev Rise, Amerasian Basin, Arctic Ocean |
title_full |
Clay minerals as indicators of late Quaternary sedimentation constraints in the Mendeleev Rise, Amerasian Basin, Arctic Ocean |
title_fullStr |
Clay minerals as indicators of late Quaternary sedimentation constraints in the Mendeleev Rise, Amerasian Basin, Arctic Ocean |
title_full_unstemmed |
Clay minerals as indicators of late Quaternary sedimentation constraints in the Mendeleev Rise, Amerasian Basin, Arctic Ocean |
title_sort |
clay minerals as indicators of late quaternary sedimentation constraints in the mendeleev rise, amerasian basin, arctic ocean |
publisher |
Springer |
publishDate |
2014 |
url |
https://oceanrep.geomar.de/id/eprint/28022/ https://oceanrep.geomar.de/id/eprint/28022/1/2014_Krylov-etal-Clay_LithMinRes-49.pdf https://doi.org/10.1134/S0024490213060059 |
long_lat |
ENVELOPE(-177.250,-177.250,80.250,80.250) |
geographic |
Arctic Arctic Ocean Mendeleev Rise |
geographic_facet |
Arctic Arctic Ocean Mendeleev Rise |
genre |
Arctic Arctic Arctic Ocean Iceberg* |
genre_facet |
Arctic Arctic Arctic Ocean Iceberg* |
op_relation |
https://oceanrep.geomar.de/id/eprint/28022/1/2014_Krylov-etal-Clay_LithMinRes-49.pdf Krylov, A. A., Stein, R. and Ermakova, L. A. (2014) Clay minerals as indicators of late Quaternary sedimentation constraints in the Mendeleev Rise, Amerasian Basin, Arctic Ocean. Open Access Lithology and Mineral Resources, 49 (1). pp. 103-116. DOI 10.1134/S0024490213060059 <https://doi.org/10.1134/S0024490213060059>. doi:10.1134/S0024490213060059 |
op_rights |
cc_by_nc info:eu-repo/semantics/openAccess |
op_doi |
https://doi.org/10.1134/S0024490213060059 |
container_title |
Lithology and Mineral Resources |
container_volume |
49 |
container_issue |
1 |
container_start_page |
103 |
op_container_end_page |
116 |
_version_ |
1789961075245973504 |