Clay minerals as paleo-climate proxy in Quaternary Dun sediments, NW Himalaya, India
Author:
Publisher
Springer Science and Business Media LLC
Subject
Stratigraphy,Earth-Surface Processes
Link
https://link.springer.com/content/pdf/10.1007/s11368-023-03671-z.pdf
Reference95 articles.
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2. Alizai A, Hillier S, Clift PD et al (2012) Clay mineral variations in Holocene terrestrial sediments from the Indus Basin. Quat Res 77:368–381. https://doi.org/10.1016/J.YQRES.2012.01.008
3. Andrade GRP, Cuadros J, Partiti CSM et al (2018) Sequential mineral transformation from kaolinite to Fe-illite in two Brazilian mangrove soils. Geoderma 309:84–99. https://doi.org/10.1016/j.geoderma.2017.08.042
4. Andrade GRP, de Azevedo AC, Cuadros J et al (2014) Transformation of kaolinite into smectite and iron-illite in Brazilian mangrove soils. Soil Sci Soc Amer J 78:655–672. https://doi.org/10.2136/SSSAJ2013.09.0381
5. Aoki S, Kohyama N, Ishizuka T (1991) Sedimentary history and chemical characteristics of clay minerals in cores from the distal part of the Bengal Fan (ODP 116). Mar Geol 99:175–185. https://doi.org/10.1016/0025-3227(91)90090-Q
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