Zobrazeno 1 - 5
of 5
pro vyhledávání: '"Anwesa Banerjee"'
Publikováno v:
Lithosphere, Vol 2022, Iss Special 8 (2022)
AbstractThe Great Indian Proterozoic Fold Belt (GIPFOB) is a curviplanar highly-tectonized zone of Precambrian crystalline rocks. In the GIPFOB, the N/NNE-striking western arm (the Aravalli Delhi Fold Belt, ADFB) and the E-striking southern arm consi
Externí odkaz:
https://doaj.org/article/d79b345dc9f0470bae750fed360c2291
Publikováno v:
Lithos
Lithos, 2022, pp.106715. ⟨10.1016/j.lithos.2022.106715⟩
Lithos, 2022, pp.106715. ⟨10.1016/j.lithos.2022.106715⟩
International audience; The Godhra-Chhota Udepur (GC) sector (west-central India) is the zone of convergence between two crustal-scale accretion zones, i.e. the N/NNE-striking Aravalli Delhi Fold Belt (ADFB) against the E-striking Central Indian Tect
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::2fdfe9282f9c861d7805513b89cb42c1
https://insu.hal.science/insu-03658496/file/banerjee-2022.pdf
https://insu.hal.science/insu-03658496/file/banerjee-2022.pdf
Publikováno v:
Lithos
Lithos, 2022, 422-423, pp.106740. ⟨10.1016/j.lithos.2022.106740⟩
Lithos, 2022, 422-423, pp.106740. ⟨10.1016/j.lithos.2022.106740⟩
International audience; The N/NNE-striking Aravalli Delhi Fold Belt (ADFB) and the E-striking Central Indian Tectonic Zone (CITZ) converge at the Godhra-Chhota Udepur (GC) sector, west-central India. Analyses of mesoscale deformation structures and m
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::1d0f0451fbda835c8de044e020edb6ff
https://insu.hal.science/insu-03677906
https://insu.hal.science/insu-03677906
Publikováno v:
Geological Society of America Abstracts with Programs.
Publikováno v:
Earth-Science Reviews. 221:103758
The Greater India Proterozoic Fold Belt (GIPFOB) is a curved highly tectonized zone dominated by Early Paleoproterozoic to Early Neoproterozoic magmatic and metamorphic rocks extending from NW India (Aravalli Delhi Fold Belt, ADFB) through central In