Mineralogical study of two sites in the abyssal plains of Madeira and Nares (North Atlantic Ocean) ESOPE cruise

Mineraiogical analyses (bulk sediment and <2μum clay fraction) were carried out on the sediment deposits from the abyssal plains of Madeira (NE Atlantic) and Nares (NW Atlantic) these deposits were sampled during the ESOPE océanographie cruise organised by IFREMER. In spite of the depth of the ba...

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Main Authors: Latouche, Claude, Maillet, Noèle, Auffret, Gérard
Format: Article in Journal/Newspaper
Language:English
Published: Strasbourg : Institut de Géologie – Université Louis-Pasteur 1990
Subjects:
Online Access:https://www.persee.fr/doc/sgeol_0302-2684_1990_act_88_1_2171
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spelling ftpersee:oai:persee:article/sgeol_0302-2684_1990_act_88_1_2171 2023-05-15T17:31:23+02:00 Mineralogical study of two sites in the abyssal plains of Madeira and Nares (North Atlantic Ocean) ESOPE cruise Latouche, Claude Maillet, Noèle Auffret, Gérard pp. 73-81 1990 https://www.persee.fr/doc/sgeol_0302-2684_1990_act_88_1_2171 eng eng Strasbourg : Institut de Géologie – Université Louis-Pasteur PERSÉE : Université de Lyon, CNRS & ENS de Lyon article 1990 ftpersee 2018-12-23T20:55:42Z Mineraiogical analyses (bulk sediment and <2μum clay fraction) were carried out on the sediment deposits from the abyssal plains of Madeira (NE Atlantic) and Nares (NW Atlantic) these deposits were sampled during the ESOPE océanographie cruise organised by IFREMER. In spite of the depth of the basin (5376 m), deposits in the Madeira plain are highly carbonated (40-60%) nannofossil ooze and calcareous mud whereas in the Nares plain (57 95 m deep) sediments are mainly composed by silty clayey muds and silty muds with a unique carbonate episode. Clay phases are in both cases made up of a mixture of illite, smectite, chlorite and kaolinite. Non clay minerals associated with the clay fraction are recorded in the East (very fine-grained quartz) and in the West (amphiboles, feldspars and some quartz). After comparison of the results obtained with those from studies from adjacent marine and continentai environments, it is suggested that settling was particularly marked by gravity flows originated from the continental slopes (mainly for the Madeira Basin) and by advective transport processes over long distances (for the Nares Basin). A small part of deposits might be the result of wind-borne transport. Latouche Claude, Maillet Noèle, Auffret Gérard. Mineralogical study of two sites in the abyssal plains of Madeira and Nares (North Atlantic Ocean) ESOPE cruise. In: Proceedings of the 9th international Clay Conference, Strasbourg, 1989. Vol IV : Clays in sediments. Diagenesis and hydrothermalism. Strasbourg : Institut de Géologie – Université Louis-Pasteur, 1990. pp. 73-81. (Sciences Géologiques. Mémoire, 88) Article in Journal/Newspaper North Atlantic Persée: Portail de revues scientifiques en sciences humaines et sociales Nares ENVELOPE(158.167,158.167,-81.450,-81.450) Pasteur ENVELOPE(140.099,140.099,-66.625,-66.625)
institution Open Polar
collection Persée: Portail de revues scientifiques en sciences humaines et sociales
op_collection_id ftpersee
language English
description Mineraiogical analyses (bulk sediment and <2μum clay fraction) were carried out on the sediment deposits from the abyssal plains of Madeira (NE Atlantic) and Nares (NW Atlantic) these deposits were sampled during the ESOPE océanographie cruise organised by IFREMER. In spite of the depth of the basin (5376 m), deposits in the Madeira plain are highly carbonated (40-60%) nannofossil ooze and calcareous mud whereas in the Nares plain (57 95 m deep) sediments are mainly composed by silty clayey muds and silty muds with a unique carbonate episode. Clay phases are in both cases made up of a mixture of illite, smectite, chlorite and kaolinite. Non clay minerals associated with the clay fraction are recorded in the East (very fine-grained quartz) and in the West (amphiboles, feldspars and some quartz). After comparison of the results obtained with those from studies from adjacent marine and continentai environments, it is suggested that settling was particularly marked by gravity flows originated from the continental slopes (mainly for the Madeira Basin) and by advective transport processes over long distances (for the Nares Basin). A small part of deposits might be the result of wind-borne transport. Latouche Claude, Maillet Noèle, Auffret Gérard. Mineralogical study of two sites in the abyssal plains of Madeira and Nares (North Atlantic Ocean) ESOPE cruise. In: Proceedings of the 9th international Clay Conference, Strasbourg, 1989. Vol IV : Clays in sediments. Diagenesis and hydrothermalism. Strasbourg : Institut de Géologie – Université Louis-Pasteur, 1990. pp. 73-81. (Sciences Géologiques. Mémoire, 88)
format Article in Journal/Newspaper
author Latouche, Claude
Maillet, Noèle
Auffret, Gérard
spellingShingle Latouche, Claude
Maillet, Noèle
Auffret, Gérard
Mineralogical study of two sites in the abyssal plains of Madeira and Nares (North Atlantic Ocean) ESOPE cruise
author_facet Latouche, Claude
Maillet, Noèle
Auffret, Gérard
author_sort Latouche, Claude
title Mineralogical study of two sites in the abyssal plains of Madeira and Nares (North Atlantic Ocean) ESOPE cruise
title_short Mineralogical study of two sites in the abyssal plains of Madeira and Nares (North Atlantic Ocean) ESOPE cruise
title_full Mineralogical study of two sites in the abyssal plains of Madeira and Nares (North Atlantic Ocean) ESOPE cruise
title_fullStr Mineralogical study of two sites in the abyssal plains of Madeira and Nares (North Atlantic Ocean) ESOPE cruise
title_full_unstemmed Mineralogical study of two sites in the abyssal plains of Madeira and Nares (North Atlantic Ocean) ESOPE cruise
title_sort mineralogical study of two sites in the abyssal plains of madeira and nares (north atlantic ocean) esope cruise
publisher Strasbourg : Institut de Géologie – Université Louis-Pasteur
publishDate 1990
url https://www.persee.fr/doc/sgeol_0302-2684_1990_act_88_1_2171
op_coverage pp. 73-81
long_lat ENVELOPE(158.167,158.167,-81.450,-81.450)
ENVELOPE(140.099,140.099,-66.625,-66.625)
geographic Nares
Pasteur
geographic_facet Nares
Pasteur
genre North Atlantic
genre_facet North Atlantic
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