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Application of the authigenic 10Be/9Be dating method to Late Miocene-Pliocene sequences in the northern Danube Basin (Pannonian Basin System): Confirmation of heterochronous evolution of sedimentary environments
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文摘

First application of the 10Be/9Be dating in the Alpine orogenic realm

Relative biochronology validated by absolute 10Be/9Be authigenic ages

Effective application to lacustrine and floodplain samples from outcrops and boreholes

Progradation of deltaic systems across the Danube Basin lasted from 11.0 to 9.4 Ma

Heterochronous onset of alluvial sedimentation from 10.5 to 8.7 Ma in NW-SE direction

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