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10.1016/J.MARGEO.2021.106603

The Bengal Fan is world famous for its developed turbiditic system.

Frequency of deep-sea turbidity as an important component of the response of a source-to-sink system to climate: A case study in the eastern middle Bengal Fan since 32 ka

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10.14379/IODP.PROC.362.205.2021

The composition of the Nicobar Fan is similar to the Bengal Fan and is sourced mainly from the Himalayan-derived Ganges-Brahmaputra river system and the Indo-Burman range/West Burma (McNeill et al.

Data report: electrical resistivity of sediments from Site U1480, IODP Expedition 362, Sumatra subduction zone

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10.1016/j.marpetgeo.2020.104874

Previous U–Pb zircon studies of the Nicobar and Bengal fans indicate the Himalaya as the dominate sediment source, making these fans a major Cenozoic sink for uplifted Himalayan sediment.

Sedimentary provenance of the Plio-Pleistocene Nicobar Fan: Complex sourcing revealed through Raman spectroscopy heavy mineral analysis

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10.1007/s12517-019-4378-0

The Bengal Fan has attracted extensive attention from the oil industry because of its hydrocarbon reservoir potential.

Architectural elements and stratigraphy of a deepwater fan: a case study of the Bengal Fan, Rakhine Basin, offshore Myanmar

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10.1029/2018GC007860

The divergence of the record in the Bay of Bengal since ~8 ka to lower ƐNd-values is coincident with a major increase in the strength of the rain-bearing southwest monsoon, and a high sediment load from the GangaBrahmaputra Rivers to the Bengal Fan that reflects major impacts from the intensified monsoon.

A 16-kyr Record of Ocean Circulation and Monsoon Intensification From the Central Bay of Bengal

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10.1016/J.QUASCIREV.2019.04.008

The Bengal Fan, as the largest submarine fan in the world, receives a large amount of sediments discharged from the Himalayas through the Ganges-Brahmaputra (G-B) river system.

Staged fine-grained sediment supply from the Himalayas to the Bengal Fan in response to climate change over the past 50,000 years

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10.3390/min9100640

The accurate quantitative characterization of different size fractions of Bengal shelf sediments represents an essential step to allow comparison of compositional signatures characterizing different segments of this huge source-to-sink system, from fluvial and deltaic sediments of the Himalayan foreland basin and Bengal shelf to the Bengal Fan.

Provenance of Bengal Shelf Sediments: 1. Mineralogy and Geochemistry of Silt

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10.1016/j.jseaes.2019.104000

The Bengal Fan, the largest submarine fan in the world, receives a large amount of terrestrial material from the Himalayas and the Indian Peninsula, making it an ideal area for studying land-sea interactions in different time scales.

Major and trace element compositions of surface sediments from the lower Bengal Fan: Implications for provenance discrimination and sedimentary environment

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10.1073/pnas.1913714116

Significance The Bengal Fan is the largest sedimentary deposit in the world and has previously been shown to represent a major sink of carbon that may have contributed to the Cenozoic cooling trend.

Sustained wood burial in the Bengal Fan over the last 19 My

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10.1017/S0016756818000018

Turtleback mud diapirs mainly occur in the southern segment of the accretionary wedge of the Andaman Sea Basin, which is far from the Bengal Fan and characterized by low deposition rate and strong compression tectonic setting.

Structural features and formation conditions of mud diapirs in the Andaman Sea Basin

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10.1016/j.jseaes.2019.104008

Previously published geochemical and mineralogical data have revealed conflicting views on the provenance of the deep-sea sediments in the Bengal Fan.

Evidence for provenance change in deep sea sediments of the Bengal Fan: A 7 million year record from IODP U1444A

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What is/are Bengal Fan?

Bengal Fan - The Bengal Fan is world famous for its developed turbiditic system. [1] The composition of the Nicobar Fan is similar to the Bengal Fan and is sourced mainly from the Himalayan-derived Ganges-Brahmaputra river system and the Indo-Burman range/West Burma (McNeill et al. [2] Previous U–Pb zircon studies of the Nicobar and Bengal fans indicate the Himalaya as the dominate sediment source, making these fans a major Cenozoic sink for uplifted Himalayan sediment. [3] The Bengal Fan has attracted extensive attention from the oil industry because of its hydrocarbon reservoir potential. [4] The divergence of the record in the Bay of Bengal since ~8 ka to lower ƐNd-values is coincident with a major increase in the strength of the rain-bearing southwest monsoon, and a high sediment load from the GangaBrahmaputra Rivers to the Bengal Fan that reflects major impacts from the intensified monsoon. [5] The Bengal Fan, as the largest submarine fan in the world, receives a large amount of sediments discharged from the Himalayas through the Ganges-Brahmaputra (G-B) river system. [6] The accurate quantitative characterization of different size fractions of Bengal shelf sediments represents an essential step to allow comparison of compositional signatures characterizing different segments of this huge source-to-sink system, from fluvial and deltaic sediments of the Himalayan foreland basin and Bengal shelf to the Bengal Fan. [7] The Bengal Fan, the largest submarine fan in the world, receives a large amount of terrestrial material from the Himalayas and the Indian Peninsula, making it an ideal area for studying land-sea interactions in different time scales. [8] Significance The Bengal Fan is the largest sedimentary deposit in the world and has previously been shown to represent a major sink of carbon that may have contributed to the Cenozoic cooling trend. [9] Turtleback mud diapirs mainly occur in the southern segment of the accretionary wedge of the Andaman Sea Basin, which is far from the Bengal Fan and characterized by low deposition rate and strong compression tectonic setting. [10] Previously published geochemical and mineralogical data have revealed conflicting views on the provenance of the deep-sea sediments in the Bengal Fan. [11]