Assessing event magnitude and target water depth for marine-target impacts: Ocean resurge deposits in the Chicxulub M0077A drill core compared
Highlights Debris-laden ocean resurge crested Chicxulub's peak ring and was at least 450 m deep. Dominant sediment deposition occurred after a rapid drop in resurge transport energy. Relative distribution of melt and target clasts hints at provenance and flow dynamics. A method to estimate impa...
| Autores: | , , , , , |
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| Tipo de recurso: | artículo |
| Estado: | Versión publicada |
| Fecha de publicación: | 2021 |
| País: | España |
| Institución: | Instituto Nacional de Técnica Aeroespacial (INTA) |
| Repositorio: | DIGITAL.INTA Repositorio Digital del Instituto Nacional de Técnica Aeroespacial |
| OAI Identifier: | oai:digital.inta.es:20.500.12666/570 |
| Acceso en línea: | https://www.sciencedirect.com/science/article/pii/S0012821X21001746 http://hdl.handle.net/20.500.12666/570 |
| Access Level: | acceso abierto |
| Palabra clave: | Marine Target Crater Resurge Deposits Chicxulub Crater Site M0077 Suevite Melt Water Interaction |
| Sumario: | Highlights Debris-laden ocean resurge crested Chicxulub's peak ring and was at least 450 m deep. Dominant sediment deposition occurred after a rapid drop in resurge transport energy. Relative distribution of melt and target clasts hints at provenance and flow dynamics. A method to estimate impactor (thus indirectly, crater) size and/or paleobathymetry is proposed. Records of resurge depend on depositional setting within the marine-target crater. |
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