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- W182990781 abstract "The Boltysh meteorite crater (diameter ≈ 23 km) on the Ukrainian shield was formed in Precambrian (~ 2.1 Ga) granites and has a classical complex structure with a central uplift (average diameter ~ 4 km). The annular trough around the uplift is filled with predominantly glassy impactites (impact melt rocks = tagamites) that are up to 230 m thick. The crater lake sediments overlie impactites and are represented by laminated siltstones, sandstones, claystones. These sediments have a maximum thickness of nearly 400 m in the center of the crater. Previous data about the geological age of the lowermost crater-fill sediments were contradictory (K1-P2), as weere the K-Ar whole rock ages of the tagamites ( 177-56 Ma)." @default.
- W182990781 created "2016-06-24" @default.
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- W182990781 date "2003-01-01" @default.
- W182990781 modified "2023-09-27" @default.
- W182990781 title "Biostratigraphic Indications of the Age of the Boltysh Impact Crater, Ukraine" @default.
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- W182990781 doi "https://doi.org/10.1007/978-3-642-55463-6_7" @default.
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