Petrography, Major and Trace Element Geochemistry of the Discovery Seamounts

The Discovery Seamounts form a major bathymetric high in the South Atlantic southwestern of South Africa. Until now the seamounts were poorly explored: in two expeditions only five dredges could recover volcanic material from the seafloor. During the cruise MSM 19/3 with R/V Maria S. Merian in Decem...

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Main Author: Hoffmann, Paulina Ewa
Format: Thesis
Language:English
Published: 2012
Subjects:
Online Access:https://oceanrep.geomar.de/id/eprint/19931/
https://oceanrep.geomar.de/id/eprint/19931/1/HoffmannMasters1012.pdf
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spelling ftoceanrep:oai:oceanrep.geomar.de:19931 2024-09-15T18:36:29+00:00 Petrography, Major and Trace Element Geochemistry of the Discovery Seamounts Hoffmann, Paulina Ewa 2012 text https://oceanrep.geomar.de/id/eprint/19931/ https://oceanrep.geomar.de/id/eprint/19931/1/HoffmannMasters1012.pdf en eng https://oceanrep.geomar.de/id/eprint/19931/1/HoffmannMasters1012.pdf Hoffmann, P. E. (2012) Petrography, Major and Trace Element Geochemistry of the Discovery Seamounts. (Master thesis), Christian-Albrechts-Universität, Kiel, 66 pp. UrhG info:eu-repo/semantics/restrictedAccess Course of study: MSc Geoscience Thesis NonPeerReviewed 2012 ftoceanrep 2024-08-19T23:40:11Z The Discovery Seamounts form a major bathymetric high in the South Atlantic southwestern of South Africa. Until now the seamounts were poorly explored: in two expeditions only five dredges could recover volcanic material from the seafloor. During the cruise MSM 19/3 with R/V Maria S. Merian in December 2011 ten more dredges recovered volcanic material from the seamounts. These samples were petrographically examined and analyzed for major and trace element contents (XRF and ICP-MS). Due to advanced stages of alteration, some of the newly obtained samples are both richer in secondary volatile and P2O5 contents than the previously described samples. The most evolved lavas occur in the northeast (trachybasalts, basaltic trachyandesites, trachyandesites and trachytes), whereas the southwestern part of the Discovery Seamounts is dominated by more primitive lavas with basanitic/tephritic and basaltic compositions. The samples are all alkaline in character, were erupted in an intraplate setting and show a highly enriched OIB-like trace element pattern. Some trace elements even show higher values than other South Atlantic ocean island basalts. The Discovery Seamounts lie within the belt of the Dupal anomaly, whose origin is still a controversy. Different hypotheses on the origin of these anomalous enriched lavas have been published, including the presence of the Discovery Plume causing the enrichment of the magma source region. The enrichment in specific trace elements indicates that the EM1-mantle endmember as a possible source of the magma source region. The new data contribute to an improved understanding of the petrogenesis and geochemistry of the Discovery Seamounts. Thesis South Atlantic Ocean Ocean Island OceanRep (GEOMAR Helmholtz Centre für Ocean Research Kiel)
institution Open Polar
collection OceanRep (GEOMAR Helmholtz Centre für Ocean Research Kiel)
op_collection_id ftoceanrep
language English
topic Course of study: MSc Geoscience
spellingShingle Course of study: MSc Geoscience
Hoffmann, Paulina Ewa
Petrography, Major and Trace Element Geochemistry of the Discovery Seamounts
topic_facet Course of study: MSc Geoscience
description The Discovery Seamounts form a major bathymetric high in the South Atlantic southwestern of South Africa. Until now the seamounts were poorly explored: in two expeditions only five dredges could recover volcanic material from the seafloor. During the cruise MSM 19/3 with R/V Maria S. Merian in December 2011 ten more dredges recovered volcanic material from the seamounts. These samples were petrographically examined and analyzed for major and trace element contents (XRF and ICP-MS). Due to advanced stages of alteration, some of the newly obtained samples are both richer in secondary volatile and P2O5 contents than the previously described samples. The most evolved lavas occur in the northeast (trachybasalts, basaltic trachyandesites, trachyandesites and trachytes), whereas the southwestern part of the Discovery Seamounts is dominated by more primitive lavas with basanitic/tephritic and basaltic compositions. The samples are all alkaline in character, were erupted in an intraplate setting and show a highly enriched OIB-like trace element pattern. Some trace elements even show higher values than other South Atlantic ocean island basalts. The Discovery Seamounts lie within the belt of the Dupal anomaly, whose origin is still a controversy. Different hypotheses on the origin of these anomalous enriched lavas have been published, including the presence of the Discovery Plume causing the enrichment of the magma source region. The enrichment in specific trace elements indicates that the EM1-mantle endmember as a possible source of the magma source region. The new data contribute to an improved understanding of the petrogenesis and geochemistry of the Discovery Seamounts.
format Thesis
author Hoffmann, Paulina Ewa
author_facet Hoffmann, Paulina Ewa
author_sort Hoffmann, Paulina Ewa
title Petrography, Major and Trace Element Geochemistry of the Discovery Seamounts
title_short Petrography, Major and Trace Element Geochemistry of the Discovery Seamounts
title_full Petrography, Major and Trace Element Geochemistry of the Discovery Seamounts
title_fullStr Petrography, Major and Trace Element Geochemistry of the Discovery Seamounts
title_full_unstemmed Petrography, Major and Trace Element Geochemistry of the Discovery Seamounts
title_sort petrography, major and trace element geochemistry of the discovery seamounts
publishDate 2012
url https://oceanrep.geomar.de/id/eprint/19931/
https://oceanrep.geomar.de/id/eprint/19931/1/HoffmannMasters1012.pdf
genre South Atlantic Ocean
Ocean Island
genre_facet South Atlantic Ocean
Ocean Island
op_relation https://oceanrep.geomar.de/id/eprint/19931/1/HoffmannMasters1012.pdf
Hoffmann, P. E. (2012) Petrography, Major and Trace Element Geochemistry of the Discovery Seamounts. (Master thesis), Christian-Albrechts-Universität, Kiel, 66 pp.
op_rights UrhG
info:eu-repo/semantics/restrictedAccess
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