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Table S6. Past Himalayan erosion from Bengal Fan: Sr-Nd and 10Be data from river sediment used for the fG and K(t) computation

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Main Authors:	Lenard, Sebastien Jean Paul, Lavé, Jérôme, France-Lanord, Christian, Aumaître, Georges, Bourlès, Didier L, Keddadouche, Karim
Format:	Dataset Open Access
Language:	en
Published:	PANGAEA 2020
Subjects:	10Be; Area; Bangladesh; Bengal Fan; Beryllium-10; Beryllium-10, production rate per year; Beryllium-10, uncertainty; Cenozoic; climate; cosmogenic nuclides; erosion; Erosion rate; Erosion rate, uncertainty; Event label; Ganga_Harding_bridge; glaciations; Himalaya; India; Indian Ocean; Indo-Burman range; Integrated Ocean Drilling Program / International Ocean Discovery Program; IODP; Location; Lower Meghna; Namche Barwa; Nd; Neodymium; Neodymium, uncertainty; Pleistocene; provenance study; Quaternary; River; Sediment; Shillong; Sr; Strontium; Strontium, uncertainty; Strontium-87/Strontium-86 ratio; Strontium-87/Strontium-86 ratio, uncertainty; turbidites; ε-Neodymium; ε-Neodymium, uncertainty
Online Access:	Acceder al recurso
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author	Lenard, Sebastien Jean Paul Lavé, Jérôme France-Lanord, Christian Aumaître, Georges Bourlès, Didier L Keddadouche, Karim
author_facet	Lenard, Sebastien Jean Paul Lavé, Jérôme France-Lanord, Christian Aumaître, Georges Bourlès, Didier L Keddadouche, Karim
collection	Datos científicos de ciencias marinas y ambientales
contents	Bulk silicate Sr-Nd data, extracted from bank and bedload, are from Galy and France-Lanord (2001) (URI:https://doi.org/10.1130/0091-7613(2001)029<0023:HERITH>2.0.CO;2), Singh and France-Lanord (2002) (URI:https://doi.org/10.1016/S0012-821X(02)00822-1), Singh et al. (2008) (URI:https://doi.org/10.1029/2007JF000909). 10Be data are averaged from Lupker et al. (2012, 2017) (URI:https://doi.org/10.1016/j.epsl.2012.04.020) (URI:https://doi.org/10.5194/esurf-5-429-2017). The production rates were computed using Basinga (Charreau et al., 2019) (URI:https://doi.org/10.1002/esp.4649) with the Lal-Stone / ERA40 atmosphere configuration using a sea-level high latitude production rate of 4.18 atom/g/y (Martin et al., 2017) (URI:https://doi.org/10.1016/j.quageo.2016.11.006), factors for different particle production rates of 0.9886 for spallation, 0.0027 for slow muons, 0.0087 for fast muons and attenuation lengths of 260 g/cm2 for slow muons and 510 g/cm2 for fast muons (Braucher et al., 2011) (URI:https://doi.org/10.1016/j.epsl.2011.06.036), and the basins defined in the Methods of the article associated to the dataset.
format	Dataset Open Access
id	pangaea_https___doi_org_10_1594_PANGAEA_912109
institution	PANGAEA
language	en
publishDate	2020
publisher	PANGAEA
record_format	pangaea
spellingShingle	Table S6. Past Himalayan erosion from Bengal Fan: Sr-Nd and 10Be data from river sediment used for the fG and K(t) computation Lenard, Sebastien Jean Paul Lavé, Jérôme France-Lanord, Christian Aumaître, Georges Bourlès, Didier L Keddadouche, Karim 10Be; Area; Bangladesh; Bengal Fan; Beryllium-10; Beryllium-10, production rate per year; Beryllium-10, uncertainty; Cenozoic; climate; cosmogenic nuclides; erosion; Erosion rate; Erosion rate, uncertainty; Event label; Ganga_Harding_bridge; glaciations; Himalaya; India; Indian Ocean; Indo-Burman range; Integrated Ocean Drilling Program / International Ocean Discovery Program; IODP; Location; Lower Meghna; Namche Barwa; Nd; Neodymium; Neodymium, uncertainty; Pleistocene; provenance study; Quaternary; River; Sediment; Shillong; Sr; Strontium; Strontium, uncertainty; Strontium-87/Strontium-86 ratio; Strontium-87/Strontium-86 ratio, uncertainty; turbidites; ε-Neodymium; ε-Neodymium, uncertainty Bulk silicate Sr-Nd data, extracted from bank and bedload, are from Galy and France-Lanord (2001) (URI:https://doi.org/10.1130/0091-7613(2001)029<0023:HERITH>2.0.CO;2), Singh and France-Lanord (2002) (URI:https://doi.org/10.1016/S0012-821X(02)00822-1), Singh et al. (2008) (URI:https://doi.org/10.1029/2007JF000909). 10Be data are averaged from Lupker et al. (2012, 2017) (URI:https://doi.org/10.1016/j.epsl.2012.04.020) (URI:https://doi.org/10.5194/esurf-5-429-2017). The production rates were computed using Basinga (Charreau et al., 2019) (URI:https://doi.org/10.1002/esp.4649) with the Lal-Stone / ERA40 atmosphere configuration using a sea-level high latitude production rate of 4.18 atom/g/y (Martin et al., 2017) (URI:https://doi.org/10.1016/j.quageo.2016.11.006), factors for different particle production rates of 0.9886 for spallation, 0.0027 for slow muons, 0.0087 for fast muons and attenuation lengths of 260 g/cm2 for slow muons and 510 g/cm2 for fast muons (Braucher et al., 2011) (URI:https://doi.org/10.1016/j.epsl.2011.06.036), and the basins defined in the Methods of the article associated to the dataset.
title	Table S6. Past Himalayan erosion from Bengal Fan: Sr-Nd and 10Be data from river sediment used for the fG and K(t) computation
topic	10Be; Area; Bangladesh; Bengal Fan; Beryllium-10; Beryllium-10, production rate per year; Beryllium-10, uncertainty; Cenozoic; climate; cosmogenic nuclides; erosion; Erosion rate; Erosion rate, uncertainty; Event label; Ganga_Harding_bridge; glaciations; Himalaya; India; Indian Ocean; Indo-Burman range; Integrated Ocean Drilling Program / International Ocean Discovery Program; IODP; Location; Lower Meghna; Namche Barwa; Nd; Neodymium; Neodymium, uncertainty; Pleistocene; provenance study; Quaternary; River; Sediment; Shillong; Sr; Strontium; Strontium, uncertainty; Strontium-87/Strontium-86 ratio; Strontium-87/Strontium-86 ratio, uncertainty; turbidites; ε-Neodymium; ε-Neodymium, uncertainty
url	https://doi.org/10.1594/PANGAEA.912109