Continental Impact Debris in the Eltanin Impact Layer

Physics

Scientific paper

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Scientific paper

We have found K feldspar microcrystites in the Eltanin impact layer in
core ELT13-4. This implies that there was a simultaneous or previous
continental impact to the oceanic Eltanin impact layer. These K feldspar
spherules may be useful to provide a maximum age for the Eltanin impact
event.

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