Dissertation (Metadaten)
Titel:Magma genesis and mantle sources at the Mid-Atlantic Ridge East of Ascension Island
 
Autor:Helge Möller
 
URN:NBN:urn:nbn:de:gbv:8-diss-5971
 
Fakultät:Mathematisch-Naturwissenschaftliche Fakultät
DDC Sachgebiet:550 Geowissenschaften
 
Datum der mdl. Prüfung:06.06.2002
 
Referent(in):Prof. Dr. P. Stoffers
Korreferent(en) Korreferentin:Prof. Dr. C.W. Devey
 
Beschreibung:Results from the Meteor 41-2 cruise to the Mid-Atlantic Ridge (MAR) between 6° and 11°S, are reported. Six spreading segments, which are bounded by non-transform offsets were discovered and numbered from north to south. Anomalously shallow segments (Segment 4 and 5) occur between ~9°S and 11°S, pointing to an excess volcanism in this area. For detailed geochemical and petrological investigations samples (mostly glasses) were taken every 5-10 km. The cause of the melting anomaly beneath Segments 4 & 5 could be either a hot mantle plume or a cold mantle heterogeneity. A mantle plume with a low excess temperature of about 50° C (Minshull et al., 1998) is unlikely, instead melting of a H2O enriched, fertile mantle is proposed. Higher H2O and incompatible element concentrations are known to lower the mantle solidus significantly. HREE depletion mainly in Segment 5 lavas suggest initial melting in the garnet peridotite stability field.
 
Schlagworte:Ascension ; Mid-Atlantic Ridge , Melting anomaly, Mantle heterogeneity
Mittelatlantischer Rücken ; MORB ; Geochemie ; Gesteinskunde
 
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