Elemental interactions between pore water and lake sediments with their environmental significance: a case as Holocene sediments in Guozha Co, northwestern Tibetan Plateau-Reference-Cited by-同舟云学术

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Elemental interactions between pore water and lake sediments with their environmental significance: a case as Holocene sediments in Guozha Co, northwestern Tibetan Plateau

Published:2024-01-30 Issue:3 Volume:83 Page:
ISSN:1866-6280
Container-title:Environmental Earth Sciences
language:en
Short-container-title:Environ Earth Sci

Author:

Li Minghui,Zhu Liping,Wang Junbo,Ju Jianting,Wang Xiaoxiao,Liu Chong,Ma Qingfeng,Xu Teng,Qiao Baojin

Publisher

Springer Science and Business Media LLC

Link

https://link.springer.com/content/pdf/10.1007/s12665-024-11429-0.pdf

Reference35 articles.

1. Andrews E, Pogge von Strandmann PAE, Fantle MS (2020) Exploring the importance of authigenic clay formation in the global Li cycle. Geochim Cosmochim Acta 289:47–68

2. Berner (1980) Early diagenesis: a theoretical approach. Princeton Press, Princeton

3. Brown GE Jr (2001) How minerals react with water. Science. https://doi.org/10.1126/science.1063544

4. Bureau of Geology and Mineral resources of Xizang Autonomous Regions (1993) Regional Geology of Xingzang (Tibet) Autonomous Region. Geological Publishing House, Beijing (in Chinese)

5. Chen H, Zhu LP, Ju JT, Wang JB, Ma QF (2019) Temporal variability of 14C reservoir effects and sedimentological chronology analysis in lake sediments from Chibuzhang Co, North Tibet (China). Quat Geochronol 52:88–102

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