Links Between Faulting, Topography, and Sediment Production During Continental Rifting: Insights From Coupled Surface Process, Thermomechanical Modeling
نویسندگان
چکیده
Continental rifts form by extension, and their subsequent evolution depends on the tectonic climatic boundary conditions. We investigate how faulting, topography, of sediment flux during rifting are affected these conditions, in particular whether it is possible to correlate activity, long timescales (40 Myr). use a thermomechanical model coupled with landscape present series 14 models, testing sensitivity models crustal strength, extension rate, fluvial erodibility. The degree strain localization drives structural modeled rifts: slow high efficient surface processes promote localization, resulting fewer active faults larger offset. Overall, magnitude production correlates localization. In case unchanged erosional power similar amount systems slower produce more owing stronger positive feedback between erosion fault observe characteristic sequence events, reflecting morpho-tectonic highest rock uplift rates observed before maximum elevation, postdates peak elevation. Our results indicate that for natural systems, good proxy time lag 2–5 Myr peaks main activity can exist.
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ژورنال
عنوان ژورنال: Journal Of Geophysical Research: Solid Earth
سال: 2022
ISSN: ['2169-9356', '2169-9313']
DOI: https://doi.org/10.1029/2021jb023490