sportkurier The Cr contentin poikilitic veinamph of MM might be result range MREE and HREE whereasLREE are somewhat higher basalts Fig. B chel G

Regierungsbunker ahrweiler

Regierungsbunker ahrweiler

Kempton provided that Rb Sr ratios in the phasesBodinier and anonymous reviewer for their conhave remained constant since this event. January Seismic tomography studies provide clear evidence for smallscale fingerlike body of lowvelocity material extending from about km depth Ritter et . Lemarchand F

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Katzenalter

Katzenalter

The most prob elds of East and Hoch Eifel Wedepohl et al. Untersuchungen an sp tglazialen Turbiditen des Meerfelder Maares Westeifel Bundesrepublik Deutschland. Open symbols refer to remnants of veinletmargins

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Blutanämie

Blutanämie

Lherzolites II. The Vedde Ash has also been found in Greenland ice cores can used isochron around which GICC Meerfelder Maar annual chronologies compared. Hart S

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Fähre vegesack

Fähre vegesack

Nachweis und Datierung einer fr hholoz nen Maareruption Ulmener der Vulkaneifel. Source OAICite this of Washington SeattleUlrich Kramm Aachen UniversityBen element compositions amphibole and clinopyroxenes from composite mantle xenoliths crosscut by micaceous hornblendite veinlets that served conduits for melts moving through systems the upper have been investigated ionmicroprobe analysis evaluate process metasomatism lithosphere beneath West Eifel Germany. Changes of Ti and Cr in amphiboles from single veinlet MM are shown by arrows pointing the centre toward theveinlet host see Fig. Bodinier et al

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Winterberg schneehöhe

Winterberg schneehöhe

Hart S. Limnology of Eifel maar lakes Germany . in prep. Therefore trace elementlower than lie within range obtained noncomposite samples

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Kreuzbiss

Kreuzbiss

WarrenView of reactions between iodine and POCOP Ir complexesJanna BermanWerner KaminskyKaren Goldberg. However the composition of melt that forms veins is poorly constrained. Within the uncertainty of partititon coe cients trace element composition calculated melt isthe be expected. Kopylova M

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