- Abstract:
-
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 study has analysed Li isotope (δ7Li) ratios from over 50 Ganges river waters and sediments, in order to trace silicate weathering processes. Sediments have δ7Li of ∼0‰, identical to bulk continental c...
Expand abstract - Publication status:
- Published
- Peer review status:
- Peer reviewed
- Version:
- Accepted manuscript
- Files:
-
-
(pdf, 1.5mb)
-
- Publisher copy:
- 10.1016/j.gca.2016.11.017
-
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- Publisher:
- Elsevier Publisher's website
- Journal:
- Geochimica et Cosmochimica Acta Journal website
- Volume:
- 198
- Pages:
- 17-31
- Publication date:
- 2016-11-16
- Acceptance date:
- 2016-11-09
- DOI:
- EISSN:
-
0016-7037
- ISSN:
-
0046-564X
- Pubs id:
-
pubs:660125
- URN:
-
uri:7ae66877-cf9b-4012-b4df-b61037468370
- UUID:
-
uuid:7ae66877-cf9b-4012-b4df-b61037468370
- Local pid:
- pubs:660125
- Copyright holder:
- Elsevier
- Copyright date:
- 2016
- Notes:
- © 2016 Elsevier Ltd. All rights reserved. This is the accepted manuscript version of the article. The final version is available online from Elsevier at: [10.1016/j.gca.2016.11.017].
Journal article
Lithium isotope behaviour during weathering in the Ganges alluvial plain
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