EGU25-15268, updated on 15 Mar 2025
https://doi.org/10.5194/egusphere-egu25-15268
EGU General Assembly 2025
© Author(s) 2025. This work is distributed under the Creative Commons Attribution 4.0 License.
Evidence of oblique collision between the Aravalli Delhi Mobile Belt and Marwar Craton along the Phulad – Ranakpur paleo-suture zone: Implication for the partition transpression style deformation during the Grenville-age orogeny
1,2,3,4- 1Department of Civil Engineering, National Institute of Technology Karnataka, Surathkal, Mangalore, India
- 2Department of Geology, University of Delhi, North Campus, Delhi, India
- 3Earth and Planetary Systems Science Program, Graduate School of Advanced Science and Engineering, Hiroshima University, Hiroshima, Japan
- 4Department of Earth and Planetary Systems Science, Hiroshima Institute of Plate Convergence Region Research, Hiroshima, Japan
How to cite: Hatui, K., Chattopadhyay, A., and Das, K.: Evidence of oblique collision between the Aravalli Delhi Mobile Belt and Marwar Craton along the Phulad – Ranakpur paleo-suture zone: Implication for the partition transpression style deformation during the Grenville-age orogeny, EGU General Assembly 2025, Vienna, Austria, 27 Apr–2 May 2025, EGU25-15268, https://doi.org/10.5194/egusphere-egu25-15268, 2025.