Tectonic evolution of the Aravalli orogen (NW India): an inverted Proterozoic rift basin?

@article{Verma1995TectonicEO,
  title={Tectonic evolution of the Aravalli orogen (NW India): an inverted Proterozoic rift basin?},
  author={P. K. Verma and Reinhard O. Greiling},
  journal={Geologische Rundschau},
  year={1995},
  volume={84},
  pages={683-696}
}
The Aravalli mountain range (AMR) in the northwestern part of the Indian Peninsula consists of two main Proterozoic metasedimentary and metaigneous sequences, the Aravalli and Delhi Supergroups, respectively, which rest over the Archaean gneissic basement. A synthesis and reinterpretation of the available geological, geochronological and geophysical data, including results of own field work and geophysical interpretations pertaining to the AMR, indicate its origin as an inverted basin: rifting… 

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