Raw X-ray fluorescence (XRF) scannings and radiocarbon age of sediment cores GeoB8323-2, and GeoB8331-4
Variations in the sediment input to the Namaqualand mudbelt during the Holocene are assessed using an integrative terrestrial to marine, source to sink approach. Geochemical and Sr and Nd isotopic signatures are used to distinguish fluvial sediment source areas. Relative to the sediments of the Olif...
Main Authors: | , , , , , , , |
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Format: | Other/Unknown Material |
Language: | English |
Published: |
PANGAEA
2016
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Subjects: | |
Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.863961 https://doi.org/10.1594/PANGAEA.863961 |