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Multistage lithospheric drips control active basin formation within an uplifting orogenic plateau.

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Area of Science:

  • Geophysics
  • Tectonics
  • Geodynamics

Background:

  • The Konya Basin in Central Anatolia exhibits rapid subsidence contrasting with its uplifting orogenic plateau.
  • Geophysical data indicate a thickened crust, a fast seismic wave speed anomaly in the mantle, and a significant residual topographic depression over the basin.

Purpose of the Study:

  • To investigate the geodynamic mechanisms responsible for the formation of the Konya Basin and its relationship with regional plateau uplift.
  • To explain the localized subsidence within the context of broader tectonic processes.

Main Methods:

  • Utilizing scaled laboratory (analogue) experiments to simulate geological processes.
  • Integrating geophysical data (GNSS/INSAR, seismic wave speeds, gravity-topography) with experimental results.

Main Results:

  • Laboratory experiments demonstrate that mantle lithospheric drip can cause localized, circular surface subsidence, consistent with the Konya Basin's features.
  • The basin's formation is attributed to a secondary mantle lithospheric drip pulse.
  • This secondary drip is contemporaneous with a larger-scale lithospheric drip responsible for Miocene plateau uplift.

Conclusions:

  • Basin evolution and plateau uplift are interconnected, driven by multistage lithospheric removal.
  • Episodic development of orogenic systems can involve linked processes of basin formation and regional uplift.
  • Mantle dynamics play a crucial role in shaping surface topography and tectonic structures in regions like Central Anatolia.