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U-Th-Ra disequilibria in basalts from the Mid-Atlantic Ridge 6-11 S: Constraints on melting, mixing and time-scales of magmatic processes

Description: Das Projekt "U-Th-Ra disequilibria in basalts from the Mid-Atlantic Ridge 6-11 S: Constraints on melting, mixing and time-scales of magmatic processes" wird vom Umweltbundesamt gefördert und von Universität Erlangen-Nürnberg, Geowissenschaftliches Zentrum Nordbayern, Lehrstuhl für Endogene Geodynamik durchgeführt. We propose to study the U, Th, and Ra isotopic compositions of zero-age MORB samples from the slow-spreading Mid-Atlantic Ridge between 6 and 11 degree S. This part of the spreading axis shows large variations in axial depth, crustal thickness and samples melts with significant variations in major and trace element geochemistry as well as Sr, Nd, and Pb isotopic composition. The existing data indicates a complex interplay of variations in mantle sources, binary mixing and degree of magma differentiation during melt ascent. In the first year wie suggest to determine U, Th and Ra isotope compositions of fresh young samples along the axis and from young ( 200.000 years) near- axis seamounts to evalute the depth and extent of melting, the mantle composition, porosity and upwelling rate and the mixing processes along a propagating ridge segment. In the second year wie propose to investigate the timing of magma evolution and eruption processes on this spreading axis on the basis of U series isotope data and stratigraphic mapping and sampling of selected volcanic structures of the working area.

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Origin: /Bund/UBA/UFORDAT

Tags: Geochemie ? Gebäude ? Kartographie ? Spurenelement ? Basalt ? Daten ? Evolution ? Isotop ? Studie ? Lebensalter ? Schmelzen ? Arbeit ? Änderung ? Differenzierung ? Mischen ? Null ? Porosität ? Probe ? Schmelzbad ? Verarbeiten ? ausgewählt ? bestehend ? gemischt ? neu ? vorschlagen ?

Region: Bayern

Bounding box: 12.53381° .. 12.53381° x 47.795° .. 47.795°

License: cc-by-nc-nd/4.0

Language: Deutsch

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Time ranges: 2004-01-01 - 2007-12-31

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