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Water samples were collected from cold and warm karst springs for stable isotopes (δ18O and δD) and 3H from SE of Kashmir valley (western Himalayas) to distinguish the sources of recharge and infer their recharge areas. The spring water samples were most depleted in heavier isotopes in May (average δ18O: −8.87‰ and δD: −50.3‰) and enriched in September (average δ18O: −7.58‰ and δD: −48.1‰). The depleted...
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