Thermochronological constraints to late Cenozoic exhumation of the Barents Sea Shelf
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文摘

Selected cores from Loppa High have been analyzed with U–Th/He dating on apatite.

Thermal modelling indicates about 1000 m of denudation.

The last exhumation event started not later than the late Miocene-early Pliocene.

Exhumation is not related to glacial processes.

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