Tectonic Processes in the Midcontinent Rift System

Summary

The Midcontinent Rift System represents a failed continental rift that began forming ca 1.1 billion years ago as Laurentia underwent regional extension and plume-related upwelling of the mantle. Initial rift inception was marked by widespread flood basalts and mafic intrusions fed by decompression melting beneath thinned lithosphere. Rift propagation produced dual arms diverging from the Lake Superior region, with asymmetric magma volumes reflecting variations in lithospheric strength and plate motion. Although extension did not progress to continental break-up, the rift accumulated kilometres of volcanic and sedimentary strata in fluvial, lacustrine and aeolian environments. Following magmatism, the system experienced inversion during the Grenvillian Orogeny, reactivating thrusts such as the Keweenaw fault and folding overlying sequences. Modern geophysical imaging and high-precision geochronology have elucidated crustal underplating, lithospheric thinning, and timing of inversion, while sedimentological studies refine depositional models. The Midcontinent Rift provides a natural laboratory for understanding plume–lithosphere interaction, intra-plate tectonics and the controls on failed rifting, with implications for mineralisation, basin evolution and global large igneous province dynamics.

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Tectonic Processes in the Midcontinent Rift System publication trend

The graph below shows the total number of articles in tectonic processes in the midcontinent rift system across all publications each year (not limited to Nature Index journals).

Technical terms

Continental rift: A linear zone where continental crust is being pulled apart, potentially leading to the formation of a new ocean basin.

Magmatic underplating: The accumulation of magma at the base of the crust, which can thicken lower crustal levels and modify thermal structure.

Lithospheric thinning: Reduction in thickness of the rigid outer shell of Earth, often due to extension and thermal erosion.

Geochronology: The science of determining the age and history of geological materials through radiometric dating methods.

Plume: A column of hot, buoyant mantle material that ascends towards the surface, potentially triggering uplift and magmatism.

References

  1. Variations in Mid‐Continent Rift magma volumes consistent with microplate evolution. Geophysical Research Letters (2013).
  2. Final inversion of the Midcontinent Rift during the Rigolet Phase of the Grenvillian Orogeny. Geology (2022).
  3. Temporal evolution of mantle temperature and lithospheric thickness beneath the ∼1.1 Ga Midcontinent Rift, North America: Implications for rapid motion of Laurentia. Earth and Planetary Science Letters (2022).
  4. Seismic Imaging of the North American Midcontinent Rift Using S‐to‐P Receiver Functions. Journal of Geophysical Research: Solid Earth (2018).
  5. Facies analysis and depositional model of the Midcontinent Rift System in Kansas, USA. The Depositional Record (2024).

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