Rainfall-recharge relationships within a karstic terrain in the Eastern Mediterranean semi-arid region, Israel: δ 18O and δD characteristics

Author:

Ayalon Avner,Bar-Matthews Miryam,Sass Eytan

Publisher

Elsevier BV

Subject

Water Science and Technology

Reference35 articles.

1. Stable isotope variations in recharge to a karst aquifer. Yorkshire Dales, Preliminary work;Atkinson;Ann. Soc. Geol. Belg.,1985

2. Rainfall-recharge relationships in the Eastern Mediterranean semi-arid regime;Ayalon,1997

3. Carbon and oxygen isotope study of the active water-carbonate system in a karstic Mediterranean cave: implications for paleoclimate research in semiarid regions;Bar-Matthews;Geochim. Cosmochim. Acta,1996

4. Late Quaternary paleoclimate in the eastern Mediterranean region from stable isotope analysis of speleothems at Soreq Cave. Israel;Bar-Matthews;Quaternary Research,1997

5. Paleoclimate evolution in the eastern Mediterranean region during the last 58,000 yr as derived from stable isotopes of speleothems (Soreq Cave, Israel);Bar-Matthews,1997

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