D/H ratios of fluid inclusions of Soreq cave (Israel) speleothems as a guide to the Eastern Mediterranean Meteoric Line relationships in the last 120 ky-Reference-Cited by-同舟云学术

D/H ratios of fluid inclusions of Soreq cave (Israel) speleothems as a guide to the Eastern Mediterranean Meteoric Line relationships in the last 120 ky

Published:2000-05 Issue:3-4 Volume:166 Page:183-191
ISSN:0009-2541
Container-title:Chemical Geology
language:en
Short-container-title:Chemical Geology

Author:

Matthews Alan,Ayalon Avner,Bar-Matthews Miryam

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference29 articles.

1. Rainfall–recharge relationships within a karstic terrain in the Eastern Mediterranean semi-arid region, Israel: δ18O and δD characteristics;Ayalon;J. Hydrol.,1998

2. Petrography, trace elements (Ba, Sr, Mg and U) and isotope geochemistry of strontium and uranium in speleothems as paleoclimate proxies: Soreq cave, Israel;Ayalon;Holocene,1999

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;Quat. Res.,1997

5. Bar-Matthews, M., Ayalon, A., Kaufman, A., 1998. Middle to Late Holocene (6500 yr period) paleoclimate in the Eastern Mediterranean region from stable isotopic composition of speleothems from Soreq cave, Israel. In: Issar, A.S., Brown, N. (Eds.), Water, Environment and Society in the Time of Climate Change. Kluwer Academic Publishers, the Netherlands, pp. 203–214.

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