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- W4386611577 abstract "The paper describes the status of the post-Mesozoic global regression, across the resulting Cretaceous-Paleogene (K-Pg) boundary, which is observed at the stratigraphic contact between Maastrichtian and Danian rocks. In the Indus Basin of Pakistan, the intensity of the regression/erosion decreases from northeast to the southwest. In the northeastern plateau, the contact of the Maastrichtian laterite and the Danian clastics is recognized in a few outcrops and many oil wells in Potwar. Along the ranges, the Danian rocks, have an erosional contact with the Maastrichtian sandstone. Further southwest, in the southern Kirthar fold belt, transgressive facies of Korara Shale was deposited. The Indus Basin carries a unique stratigraphic framework below the Danian rocks, a disconformable contact with the laterite in the northeastern plateau, an erosional disconformable contact along the ranges, to the presence of a transgressive facies in the far southwest. The boundary is represented by simple geological contacts having minor evidence of erosional surfaces, without any specific clay marker enriched with radioactive minerals or a meteorite impact ejecta. In the case of Korara Shale, the K-Pg boundary could not be identified in the field and was established by biostratigraphic studies, which is confirmed by the presence of faunal composition of the global framework. The paper has updated the species taxonomy of the previous authors and has brought the existing literature into a single version, including our field observations." @default.
- W4386611577 created "2023-09-12" @default.
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- W4386611577 date "2023-01-01" @default.
- W4386611577 modified "2023-09-30" @default.
- W4386611577 title "The Cretaceous-Paleogene boundary (K-Pg) in Pakistan stratigraphy" @default.
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- W4386611577 doi "https://doi.org/10.1016/bs.sats.2023.08.004" @default.
- W4386611577 hasPublicationYear "2023" @default.
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