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- j.epsl.2008.07.009 accessDate "2013-04-22".
- j.epsl.2008.07.009 date "2008-09-15".
- j.epsl.2008.07.009 doi "10.1016/j.epsl.2008.07.009".
- j.epsl.2008.07.009 first1 "Michael S.".
- j.epsl.2008.07.009 first2 "S. Akhter".
- j.epsl.2008.07.009 first3 "Leonardo".
- j.epsl.2008.07.009 isCitedBy Ganges_Delta.
- j.epsl.2008.07.009 issue "3–4".
- j.epsl.2008.07.009 journal "Earth & Planetary Science Letters".
- j.epsl.2008.07.009 last1 "Steckler".
- j.epsl.2008.07.009 last2 "Humayun".
- j.epsl.2008.07.009 last3 "Seeber".
- j.epsl.2008.07.009 publisher "Elsevier".
- j.epsl.2008.07.009 quote "The edge of the pre-delta Eocene paleoshelf is marked by the shallow-water Sylhet Limestone, which runs NNE from near Calcutta to the edge of the Shillong Plateau ... The Sylhet Limestone drops ... indicating the presence of thick continental crust [NW of the edge]. East of the [the edge] the great thickness of sediments indicates that the crust is greatly thinned or oceanic ... The enormous supply of sediments provided by the Himalayan collision fed the [Ganges-Brahmaputra Delta ] and has produced ~400 km of progradation of the shelf edge since the Eocene ... Total sediment thickness beneath the GBD southeast of the hinge zone exceeds 16 km.".
- j.epsl.2008.07.009 title "Collision of the Ganges-Brahmaputra Delta with the Burma Arc".
- j.epsl.2008.07.009 url Collision_of_the_Ganges-Brahmaputra_Delta_with_the_Burma_Arc.
- j.epsl.2008.07.009 volume "273".