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- W4317103734 endingPage "106992" @default.
- W4317103734 startingPage "106992" @default.
- W4317103734 abstract "The present work studies the Harhoura coastal deposits located immediately southwest of Rabat, Morocco. The base of this sequence has been previously dated by 14C as 9900 ± 150 BP. These deposits exhibit a thick record potentially related to the footprint of a high-energy storm. They are primarily characterized by coarse-grained dark shelly/gravelly units bearing highly fragmented shells inherited from shallow water platform. A high amount of organic matter was also observed. The provenance signature using modal analysis of detrital grains, and major and trace elements indicates two main phases. The first sedimentation is a marine within the shallow platform, followed by a coastal phase belonging to the littoral zone. The first source to sink pathway indicate that platform was supplied by sediments from felsic magmatic source, low-grade and medium metamorphic rocks belonging to the fold and thrust belt of the Sehoul Block, with a minor contribution from mafic source rocks. The second pathway indicates their subsequent remobilization and deposition on the calcarenite coastal plain by mean of high-energy storm(s). The provenance relationship of the latter phase was corroborated by the geochemical signature using major, trace and rare earth elements, assigning their latest source to a coastal-marine origin." @default.
- W4317103734 created "2023-01-18" @default.
- W4317103734 creator A5015272017 @default.
- W4317103734 creator A5018710511 @default.
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- W4317103734 creator A5058339922 @default.
- W4317103734 creator A5068207125 @default.
- W4317103734 creator A5090261408 @default.
- W4317103734 date "2023-03-01" @default.
- W4317103734 modified "2023-10-18" @default.
- W4317103734 title "Provenance and sedimentary processes on Pleistocene storm deposits in Harhoura (Northern Coastal Atlantic, Morocco): New constraints from a source to sink perspective" @default.
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