Lithium isotope behaviour during weathering in the Ganges alluvial plain
The Ganges river system is responsible for the transportation of a large flux of dissolved materials derived from Himalayan weathering to the oceans. Silicate weathering-driven cooling resulting from uplift of the Himalayas has been proposed to be a key player in Cenozoic climate variation. This stu...
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Format: | Journal article |
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Elsevier
2016
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