Geochemistry and dose rate of terraces sediments close to the Chenab river

DOI

Sediment depth = depth from top of unit. Measurements for OSL were performed at the Wadia Institute (Dehradun, India). SAR protocol on 30 aliquots is used to estimate mean palaeodose (Murray and Wintle, 2000). All the aliquots showing recycle ratio within 10% are considered. Water content is assumed to be 10 ± 5% by weight for all samples. Least consists the least 20% (JK samples) and 30% (DAG samples) of the palaeodoses.

Identifier
DOI https://doi.org/10.1594/PANGAEA.836905
Related Identifier https://doi.org/10.1594/PANGAEA.836910
Metadata Access https://ws.pangaea.de/oai/provider?verb=GetRecord&metadataPrefix=datacite4&identifier=oai:pangaea.de:doi:10.1594/PANGAEA.836905
Provenance
Creator Vignon, Violaine; Srivastava, Pradeep; Vassallo, Riccardo; Mugnier, Jean-Louis; Carcaillet, Julien
Publisher PANGAEA
Publication Year 2014
Rights Creative Commons Attribution 3.0 Unported; https://creativecommons.org/licenses/by/3.0/
OpenAccess true
Representation
Resource Type Dataset
Format text/tab-separated-values
Size 192 data points
Discipline Earth System Research
Spatial Coverage (74.511W, 33.007S, 74.843E, 33.386N); Himalaya