Six duplicates of various granulometric fractions (col. 6-7) for the Bengal Fan samples and one for the Lower Meghna were measured for 10Be. The results are presented in a similar way than for Table S1 (https://doi.org/10.1594/PANGAEA.912098). The col. 22 presents the relative difference with the results of the same samples presented Table S1
A holistic view of the Bengal-Nicobar Fan system requires sampling the full sedimentary section of t...
The Bengal Fan provides a Neogene record of Eastern and Central Himalaya exhumation. We provide the ...
International audienceIn Himalaya, the monsoon precipitations exert a primary control on erosion. Fr...
Samples from the Bengal Fan and Lower Meghna River were measured. Each line gives the 10Be measureme...
For the Bengal Fan samples, the measurements of major and trace elements were performed at SARM (Nan...
Bulk silicate Sr-Nd data, extracted from bank and bedload, are from Galy and France-Lanord (2001) (U...
Ganga, Brahmaputra and Lower Meghna sample data are presented. Al/Si and Fe/Si ratios are from Lupke...
International audienceGlobal records of erosion have led to conjecture that the Quaternary climatic ...
International audienceSediment accumulation rates and thermal trackers suggest a substantial and glo...
International audienceIODP Expedition 354 in the Bengal fan [1] generated a comprehensive record of ...
Western Bhutan provides an ideal setting to understand the interplay between uplift, erosion, and fl...
Western Bhutan provides an ideal setting to understand the interplay between uplift, erosion, and fl...
International audienceRecent IODP Expedition 354 in the Bengal fan [1] generated a comprehensive rec...
International audienceIn Himalaya, the monsoon precipitations and tectonic exert a primary control o...
International audienceThe Indian monsoon and tectonic both control the Himalayan erosion. Tectonic g...
A holistic view of the Bengal-Nicobar Fan system requires sampling the full sedimentary section of t...
The Bengal Fan provides a Neogene record of Eastern and Central Himalaya exhumation. We provide the ...
International audienceIn Himalaya, the monsoon precipitations exert a primary control on erosion. Fr...
Samples from the Bengal Fan and Lower Meghna River were measured. Each line gives the 10Be measureme...
For the Bengal Fan samples, the measurements of major and trace elements were performed at SARM (Nan...
Bulk silicate Sr-Nd data, extracted from bank and bedload, are from Galy and France-Lanord (2001) (U...
Ganga, Brahmaputra and Lower Meghna sample data are presented. Al/Si and Fe/Si ratios are from Lupke...
International audienceGlobal records of erosion have led to conjecture that the Quaternary climatic ...
International audienceSediment accumulation rates and thermal trackers suggest a substantial and glo...
International audienceIODP Expedition 354 in the Bengal fan [1] generated a comprehensive record of ...
Western Bhutan provides an ideal setting to understand the interplay between uplift, erosion, and fl...
Western Bhutan provides an ideal setting to understand the interplay between uplift, erosion, and fl...
International audienceRecent IODP Expedition 354 in the Bengal fan [1] generated a comprehensive rec...
International audienceIn Himalaya, the monsoon precipitations and tectonic exert a primary control o...
International audienceThe Indian monsoon and tectonic both control the Himalayan erosion. Tectonic g...
A holistic view of the Bengal-Nicobar Fan system requires sampling the full sedimentary section of t...
The Bengal Fan provides a Neogene record of Eastern and Central Himalaya exhumation. We provide the ...
International audienceIn Himalaya, the monsoon precipitations exert a primary control on erosion. Fr...