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- W1980641477 abstract "The arid zone of Rajasthan has a humid past. The present communication records provide evidence of paleo-humidity from the Ajmer district in Rajasthan manifested as channel conglomerates and karst development in the marble rocks within the arid landscape, which suggests that a humid phase existed in the Luni Basin during the Quaternary period in Rajasthan. The present find of Quaternary signatures of paleo-humidity suggests that the humid phase in the Thar Desert extended beyond the Saraswati drainage basin up to the Luni basin, covering the entire Trans-Aravalli region." @default.
- W1980641477 created "2016-06-24" @default.
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- W1980641477 date "2000-06-01" @default.
- W1980641477 modified "2023-09-27" @default.
- W1980641477 title "Quaternary signatures of paleo-humidity in arid zone, Rajasthan, India" @default.
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- W1980641477 doi "https://doi.org/10.1006/jare.1999.0629" @default.
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