Publisher
Springer Science and Business Media LLC
Reference68 articles.
1. Acharyya, S. (2007). Evolution of the Himalayan Palaeogene foreland basins, influence of its litho-packet on the formation of thrust related domes and windows in the Eastern Himalayas—a review. Journal of Asian Earth Sciences, 31, 1–17. https://doi.org/10.1016/j.jseaes.2007.03.007
2. Agarwal, O. P. & Ghosh, N. C. (1986) Geology and Stratigraphy of Naga Ophiolite Belt between Meluri and Awankho, Phek District, Nagaland, India. Tectonic Context 105–130
3. Aier, I., Luirei, K., Bhakuni, S. S., Thong, G. T., & Kothyari, G. C. (2011). Geomorphic evolution of Medziphemainter montane basin and Quaternary deformation in the Schuppen Belt, Nagaland. NE India Zeitschrift fur Geomorphologie., 55(2), 247.
4. Allen, R., Najman, Y., Carter, A., Barfod, D., Bickle, M. J., Chapman, H. J., Garzanti, E., Vezzoli, G., Ando, S., & Parrish, R. R. (2008). Provenance of the Tertiary sedimentary rocks of the Indo-Burman Ranges, Burma: Burman arc or Himalayan derived? Journal of Geological Society of London., 165, 1045–1057. https://doi.org/10.1144/0016-76492007-143
5. Basu, A., Young, S. W., Suttner, L. J., James, W. C., & Mack, G. H. (1975). Re-evaluation of the use of undulatory extinction and poly-crystallinity in detrital quartz for provenance interpretation. Journal of Sedimentary Petrology., 45, 873–882. https://doi.org/10.1306/212F6E6F-2B24-11D7-8648000102C1865D