Eduardo Garzanti, Sergio Andò, Christian France‐Lanord, P. Censi et al.
Eduardo Garzanti, Sergio Andò, Christian France‐Lanord, Giovanni Vezzoli et al.
Yani Najman, Eduardo Garzanti
The latest Paleocene-middle Eocene Subathu Formation and the Oligocene-Miocene Dagshai and Kasauli Formations of the Indian foreland basin record the early evolution of the Himalayan fold-thrust belt. Sandstone petrography of the Subathu Formation shows a predominantly recycled sedimentary source, w...
Yani Najman, M. J. Bickle, Marcelle K. BouDagher‐Fadel, Andrew Carter et al.
Yani Najman, R. Allen, E. Willett, Andrew Carter et al.
Abstract The Cenozoic sedimentary succession of Bangladesh provides an archive of Himalayan erosion. However, its potential as an archive is currently hampered by a poor lithostratigaphic framework with limited age control. We focus on the Hatia Trough of the Bengal Basin and the adjacent fold belt ...
Eduardo Garzanti, Giovanni Vezzoli, Sergio Andò, Mara Limonta et al.
The Bangladesh lowlands are traversed by the largest sediment flux on the planet. Detritus generated mostly in Himalayan highlands and conveyed through the Ganga–Brahmaputra rivers and Meghna estuary reaches the Bay of Bengal, where it forms a composite deltaic system. This study integrates the vast...
Yani Najman, Eduardo Garzanti
Research Article| March 01, 2000 Reconstructing early Himalayan tectonic evolution and paleogeography from Tertiary foreland basin sedimentary rocks, northern India Yani Najman; Yani Najman 1Department of Earth Sciences, Cambridge University, Downing Street, Cambridge CB2 3EQ, United Kingdom, and De...
Laura Bracciali, Yani Najman, Randall Parrish, S. H. Akhter et al.
Fluvial drainages impact on, and are impacted by, surface uplift, exhumation and strain, and thus an investigation of their evolution provides a key to understanding crustal deformation processes and erosion-tectonic-climate interactions.
Eduardo Garzanti, Sergio Andò, Christian France‐Lanord, Giovanni Vezzoli et al.
This study investigates the natural processes that control concentration of detrital minerals and consequently chemical elements in river sand. The novelty of our approach consists in the systematic integration of detailed textural, petrographical, mineralogical and chemical data, and in the quantit...
Yani Najman, R. Allen, M. J. Bickle, Marcelle K. BouDagher‐Fadel et al.
DOI = 10.3126/hjs.v5i7.1288 Himalayan Journal of Sciences Vol.5(7) (Special Issue) 2008 p.94
Yani Najman, Edward R. Sobel, Ian Millar, Daniel F. Stöckli et al.
The Indo-Burman Ranges (IBR) are a mountain range comprised of Mesozoic-Cenozoic rocks which run the length of Western Myanmar, extending into India and Bangladesh; to the west lies the Indian Ocean, and to the east lies the Central Myanmar Basin (CMB) along which the Irrawaddy River flows. The IBR ...
Yani Najman, R. Allen, E. Willett, Andrew Carter et al.
The Cenozoic sedimentary succession of Bangladesh provides an archive of Himalayan erosion. However, its potential as an archive is currently hampered by a poor lithostratigaphic framework with limited age control. We focus on the Hatia Trough of the Bengal Basin and the adjacent fold belt of the Ch...
Yani Najman, S. H. Akhter, R. Allen, Sergio Andò et al.
R. C. Allen, Yani Najman, A. Carter, E. Willett et al.