Occurrence of kaolinite and mixed-layer kaolinite/smectite in hydrothermal sediments of Grimsey Graben, Tjornes Fracture Zone (north of Iceland)
The sediments at a site situated among high-temperature vents in the Grimsey Graben (Tjornes Fracture Zone, north of Iceland) exhibit features of strong hydrothermal alteration: (1) almost total dissolution of the volcaniclastic material composing the background sediment; (2) sulfate and sulfide pre...
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2005
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Online Access: | https://oceanrep.geomar.de/id/eprint/16046/ https://oceanrep.geomar.de/id/eprint/16046/1/Dekov.pdf https://doi.org/10.1016/j.margeo.2004.12.004 |
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ftoceanrep:oai:oceanrep.geomar.de:16046 2023-05-15T16:31:13+02:00 Occurrence of kaolinite and mixed-layer kaolinite/smectite in hydrothermal sediments of Grimsey Graben, Tjornes Fracture Zone (north of Iceland) Dekov, V. M. Scholten, J. Botz, R. Garbe-Schönberg, C. D. Thiry, M. Stoffers, Peter Schmidt, Mark 2005 text https://oceanrep.geomar.de/id/eprint/16046/ https://oceanrep.geomar.de/id/eprint/16046/1/Dekov.pdf https://doi.org/10.1016/j.margeo.2004.12.004 en eng Elsevier https://oceanrep.geomar.de/id/eprint/16046/1/Dekov.pdf Dekov, V. M., Scholten, J., Botz, R., Garbe-Schönberg, C. D., Thiry, M., Stoffers, P. and Schmidt, M. (2005) Occurrence of kaolinite and mixed-layer kaolinite/smectite in hydrothermal sediments of Grimsey Graben, Tjornes Fracture Zone (north of Iceland). Marine Geology, 215 (3-4). pp. 159-170. DOI 10.1016/j.margeo.2004.12.004 <https://doi.org/10.1016/j.margeo.2004.12.004>. doi:10.1016/j.margeo.2004.12.004 info:eu-repo/semantics/restrictedAccess Article PeerReviewed 2005 ftoceanrep https://doi.org/10.1016/j.margeo.2004.12.004 2023-04-07T15:05:35Z The sediments at a site situated among high-temperature vents in the Grimsey Graben (Tjornes Fracture Zone, north of Iceland) exhibit features of strong hydrothermal alteration: (1) almost total dissolution of the volcaniclastic material composing the background sediment; (2) sulfate and sulfide precipitation; (3) kaolinitisation. Smectite, precipitated in the shallowest sediment, is gradually replaced downward by mixed-layer kaolinite/smectite and pure, well-crystallised kaolinite. The kaolinite/smectite is interstratified with up to 10% swelling smectitic layers. According to the oxygen isotope composition kaolinite/smectite mixed-layer mineral most likely formed at temperatures near 160 degrees C. The vertical sequence kaolinite -> kaolinite/smectite -> smectite as well as the distinct zonation across the kaolinitic veins (almost pure kaolinite in the central zone and kaolinite/smectite along the rim) suggest hydrothermal transformation of initially formed smectite -> kaolinite/smectite -> kaolinite. Most probably this conversion occurred in an evolving (from alkaline to slightly acidic) hydrothermal environment. (c) 2004 Elsevier B.V. All rights reserved. Article in Journal/Newspaper Grimsey Iceland OceanRep (GEOMAR Helmholtz Centre für Ocean Research Kiel) Marine Geology 215 3-4 159 170 |
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Open Polar |
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OceanRep (GEOMAR Helmholtz Centre für Ocean Research Kiel) |
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ftoceanrep |
language |
English |
description |
The sediments at a site situated among high-temperature vents in the Grimsey Graben (Tjornes Fracture Zone, north of Iceland) exhibit features of strong hydrothermal alteration: (1) almost total dissolution of the volcaniclastic material composing the background sediment; (2) sulfate and sulfide precipitation; (3) kaolinitisation. Smectite, precipitated in the shallowest sediment, is gradually replaced downward by mixed-layer kaolinite/smectite and pure, well-crystallised kaolinite. The kaolinite/smectite is interstratified with up to 10% swelling smectitic layers. According to the oxygen isotope composition kaolinite/smectite mixed-layer mineral most likely formed at temperatures near 160 degrees C. The vertical sequence kaolinite -> kaolinite/smectite -> smectite as well as the distinct zonation across the kaolinitic veins (almost pure kaolinite in the central zone and kaolinite/smectite along the rim) suggest hydrothermal transformation of initially formed smectite -> kaolinite/smectite -> kaolinite. Most probably this conversion occurred in an evolving (from alkaline to slightly acidic) hydrothermal environment. (c) 2004 Elsevier B.V. All rights reserved. |
format |
Article in Journal/Newspaper |
author |
Dekov, V. M. Scholten, J. Botz, R. Garbe-Schönberg, C. D. Thiry, M. Stoffers, Peter Schmidt, Mark |
spellingShingle |
Dekov, V. M. Scholten, J. Botz, R. Garbe-Schönberg, C. D. Thiry, M. Stoffers, Peter Schmidt, Mark Occurrence of kaolinite and mixed-layer kaolinite/smectite in hydrothermal sediments of Grimsey Graben, Tjornes Fracture Zone (north of Iceland) |
author_facet |
Dekov, V. M. Scholten, J. Botz, R. Garbe-Schönberg, C. D. Thiry, M. Stoffers, Peter Schmidt, Mark |
author_sort |
Dekov, V. M. |
title |
Occurrence of kaolinite and mixed-layer kaolinite/smectite in hydrothermal sediments of Grimsey Graben, Tjornes Fracture Zone (north of Iceland) |
title_short |
Occurrence of kaolinite and mixed-layer kaolinite/smectite in hydrothermal sediments of Grimsey Graben, Tjornes Fracture Zone (north of Iceland) |
title_full |
Occurrence of kaolinite and mixed-layer kaolinite/smectite in hydrothermal sediments of Grimsey Graben, Tjornes Fracture Zone (north of Iceland) |
title_fullStr |
Occurrence of kaolinite and mixed-layer kaolinite/smectite in hydrothermal sediments of Grimsey Graben, Tjornes Fracture Zone (north of Iceland) |
title_full_unstemmed |
Occurrence of kaolinite and mixed-layer kaolinite/smectite in hydrothermal sediments of Grimsey Graben, Tjornes Fracture Zone (north of Iceland) |
title_sort |
occurrence of kaolinite and mixed-layer kaolinite/smectite in hydrothermal sediments of grimsey graben, tjornes fracture zone (north of iceland) |
publisher |
Elsevier |
publishDate |
2005 |
url |
https://oceanrep.geomar.de/id/eprint/16046/ https://oceanrep.geomar.de/id/eprint/16046/1/Dekov.pdf https://doi.org/10.1016/j.margeo.2004.12.004 |
genre |
Grimsey Iceland |
genre_facet |
Grimsey Iceland |
op_relation |
https://oceanrep.geomar.de/id/eprint/16046/1/Dekov.pdf Dekov, V. M., Scholten, J., Botz, R., Garbe-Schönberg, C. D., Thiry, M., Stoffers, P. and Schmidt, M. (2005) Occurrence of kaolinite and mixed-layer kaolinite/smectite in hydrothermal sediments of Grimsey Graben, Tjornes Fracture Zone (north of Iceland). Marine Geology, 215 (3-4). pp. 159-170. DOI 10.1016/j.margeo.2004.12.004 <https://doi.org/10.1016/j.margeo.2004.12.004>. doi:10.1016/j.margeo.2004.12.004 |
op_rights |
info:eu-repo/semantics/restrictedAccess |
op_doi |
https://doi.org/10.1016/j.margeo.2004.12.004 |
container_title |
Marine Geology |
container_volume |
215 |
container_issue |
3-4 |
container_start_page |
159 |
op_container_end_page |
170 |
_version_ |
1766020988618670080 |