Diagenetic evolution of lower Jurassic platform carbonates flanking the Tazoult salt wall (Central High Atlas, Morocco)

Platform carbonates diagenesis in salt basins could be complex due to potential alterations of fluids related and non‐related to diapirism. This paper presents the diagenetic history of the Hettangian to Pliensbachian platform carbonates from the Tazoult salt wall area (central High Atlas, Morocco)....

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Published in:Basin research 2020-06, Vol.32 (3), p.546-566
Main Authors: Moragas, Mar, Baqués, Vinyet, Travé, Anna, Martín‐Martín, Juan Diego, Saura, Eduard, Messager, Gregoire, Hunt, David, Vergés, Jaume
Format: Article
Language:English
Subjects:
Barriers
basin fluids
Basins
Brines
Calcite
Carbonates
Diagenesis
diapiric basins
Diapirism
Diapirs
Dolomite
Dolostone
Evolution
Fluids
Jurassic
Manganese
Orogeny
Outcrops
platform carbonates
Platforms
salt tectonics
Salts
Sediments
Slivers
Tectonics
Uplift
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Summary:Platform carbonates diagenesis in salt basins could be complex due to potential alterations of fluids related and non‐related to diapirism. This paper presents the diagenetic history of the Hettangian to Pliensbachian platform carbonates from the Tazoult salt wall area (central High Atlas, Morocco). Low structural relief and outcrop conditions allowed to define the entire diagenetic evolution occurred in the High Atlas diapiric basins since early stages of the diapiric activity up to their tectonic inversion. Precipitation of dolomite and calcite from both warmed marine‐derived and meteoric fluids characterised diagenetic stages during Pliensbachian, when the carbonate platforms were exposed and karstified. Burial diagenesis occurred from Toarcian to Middle Jurassic, due to changes of salt‐induced dynamic related to increase in siliciclastic input, fast diapir rise and rapid burial of Pliensbachian platforms. During this stage, the diapir acted as a physical barrier for fluid circulation between the core and the flanking sediments. In the carbonates and breccias flanking the structures, dolomite and calcite precipitated from basinal brines, whereas carbonate slivers located in the core of the structure, were affected by the circulation of Mn‐rich fluids. The final diagenetic event is characterised by the income of meteoric fluids into the system during uplift caused by Alpine orogeny. These results highlight the relevant influence of diapirism on the diagenetic modifications in salt‐related basins in terms of diagenetic events and involved fluids.
ISSN:0950-091X
1365-2117
DOI:10.1111/bre.12382