Coupling Crustal‐Scale Rift Architecture With Passive Margin Salt Tectonics: A Geodynamic Modeling Approach

Continental rifted margins are often associated with widespread, thick evaporite (i.e., salt) deposits and pronounced salt tectonics. The majority of salt basins formed during the latest stages of rifting, prior to continental breakup. We use 2D thermo‐mechanical finite element modeling of lithosphe...

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Bibliographic Details
Published in:Journal of geophysical research. Solid earth 2022-11, Vol.127 (11), p.n/a
Main Authors: Pichel, Leonardo M., Huismans, Ritske S., Gawthorpe, Robert, Faleide, Jan Inge, Theunissen, Thomas
Format: Article
Language:eng ; nor
Subjects:
Architecture
Basins
Complexity
Continental margins
Deformation
Deposition
Diapirism
Diapirs
Dynamics
Evaporites
Expulsion
Finite element method
Geological structures
Geophysics
Lithosphere
Mathematical analysis
Mathematical models
minibasins
Modelling
Oceanic crust
Overburden
Passive margins
Plate tectonics
Progradation
rifted margins
Rifting
Salt deposition
salt nappes
salt tectonics
Salts
Tectonics
Temporal distribution
Translation
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Summary:Continental rifted margins are often associated with widespread, thick evaporite (i.e., salt) deposits and pronounced salt tectonics. The majority of salt basins formed during the latest stages of rifting, prior to continental breakup. We use 2D thermo‐mechanical finite element modeling of lithospheric extension to investigate the interplay between rifted margin architecture, late syn‐rift salt deposition, and post‐rift salt tectonics. We focus on four different types of continental margins: (a) narrow, (b) intermediate, (c) wide, and (d) ultra‐wide margins. We evaluate the: (a) interplay between laterally variable syn‐rift extension, salt deposition and salt tectonics, (b) influence of syn‐rift basin architecture on post‐rift salt flow, (c) spatial and temporal distribution of salt‐related structural domains, and (d) contrasting styles of salt tectonics for different margin types. Narrow and intermediate margins form partially isolated salt basins associated with prominent base‐salt relief, limited translation but significant diapirism, and minibasin development. Wide and ultra‐wide margins form wide salt basins with subtle base‐salt relief that results in significant seaward salt expulsion and overburden translation. These wide margins demonstrate significant updip extension with the development of post‐rift normal faults and rollovers, mid‐margin translation associated with complex diapirism and downdip diapir shortening. All margins contain a distal salt nappe that varies in width and complexity. We also test the effect of different salt viscosities, relative post‐salt progradation rates, and pre‐salt sediment thicknesses. The results are comparable to several examples of salt‐bearing rifted margins and improve our understanding of their dynamics and on the controls on their salt tectonics variability. Plain Language Summary Rifting of the continental lithosphere can lead to continental breakup and formation of continental margins, which are often associated with widespread, thick salt basins that deform in a ductile fashion and produce complex geological structures. Most of these basins formed during the latest stages of rifting, prior to continental breakup. We use 2D thermo‐mechanical numerical modeling of lithospheric extension to investigate the interplay between rifted margin architecture, late‐syn‐rift salt and post‐rift salt tectonics for four different types of margins: (a) narrow, (b) intermediate, (c) wide, and (d) ultra‐wide. We evaluate th
ISSN:2169-9313
2169-9356
DOI:10.1029/2022JB025177