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Facies architecture related to sea-level changes of the Upper Cretaceous (Santonian) Taneichi Formation, northeast Japan: evidence of actual sea-level fluctuation during the Late Cretaceous
Well-exposed transgressive and regressive sequence of the Santonian Taneichi Formation occurs along the Pacific Coast of northeastern Honshu, Japan. Although the studied sequence is of only 60 m thickness, the outcrops show various sedimentary facies accompanied with two disconformities, suggesting...
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| Formato: | Online Artículo Texto |
| Lenguaje: | English |
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The Japan Academy
2004
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| Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8157910/ |