Question
Asked 11 February 2020
Sole marks in Late Paleozoic Ice Age deposits. What do you think about these ones?
I'm looking for help about this sole marks. These structures are described in the interface between sandstones with scoured base and sandy matrix diamictites with granule up to boulder clasts. These rocks are from the Itararé Group, record of the Late Paleozoic Ice Age in Paraná Basin Brazil, so they can be glacial-influenced.
What do you think about this structures?
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