Shoulder to shoulder architecture of a salt-related rift basin at the onset of continental break-up: The Central High Atlas Jurassic diapiric province (Morocco)
Continental passive margins are often defined by early salt-related rift systems buried beneath thick sedimentary piles, with structural and sedimentary architectures only directly observable when inverted in orogenic systems where primary salt structures are overprinted by compression. The Central...
| Autores: | , , , , , , , |
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| Formato: | artículo |
| Estado: | Versión aceptada para publicación |
| Fecha de publicación: | 2025 |
| País: | España |
| Recursos: | Consejo Superior de Investigaciones Científicas (CSIC) |
| Repositorio: | DIGITAL.CSIC. Repositorio Institucional del CSIC |
| OAI Identifier: | oai:digital.csic.es:10261/388397 |
| Acesso em linha: | http://hdl.handle.net/10261/388397 |
| Access Level: | acceso embargado |
| Palavra-chave: | Salt tectonics shaped the Central High Atlas from Jurassic to Ceonzoic times Diachronous diapiric activity along and across the Jurassic rift basin Shallow water deposition can occur through the whole basin due to syn-rift diapirism The Central High Atlas is a first-class analogue for salt rift margins. |
| Resumo: | Continental passive margins are often defined by early salt-related rift systems buried beneath thick sedimentary piles, with structural and sedimentary architectures only directly observable when inverted in orogenic systems where primary salt structures are overprinted by compression. The Central High Atlas diapiric province (Morocco) is an inverted salt-related rift basin with active salt tectonics since early Mesozoic times that provides an exceptional view of early syn-rift sediments and structure. We present the first regional balanced and restored cross-sections of the Central High Atlas evidencing the role of salt tectonics. The cross section includes seven salt walls and six minibasins, with associated Early Jurassic to Cenozoic halokinetic strata that indicates a shortening of 38 km (24%). The Jurassic rifting stage is characterized by shallow water sediments along the basin margins and around localized salt walls, separated by minibasins filled with deep-water sediments undergoing higher subsidence rates. Subsequently, a longitudinal deltaic system prograded eastwards coevally with shallow marine deposition associated with active salt walls. Thus, local diapir uplift enhanced shallow-water deposition and local aerial exposure in central parts of the basin throughout the whole rifting stage. These features provide insights for the study of rift basins and the early stages of continental break-up worldwide, and for the exploration and production of hydrocarbons in equivalent settings. |
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