Stable isotope study of cave percolation waters in subtropical Brazil: Implications for paleoclimate inferences from speleothems-Reference-Cited by-同舟云学术

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Stable isotope study of cave percolation waters in subtropical Brazil: Implications for paleoclimate inferences from speleothems

Published:2005-08 Issue:3-4 Volume:220 Page:245-262
ISSN:0009-2541
Container-title:Chemical Geology
language:en
Short-container-title:Chemical Geology

Author:

Cruz Francisco W.,Karmann Ivo,Viana Oduvaldo,Burns Stephen J.,Ferrari José A.,Vuille Mathias,Sial Alcides N.,Moreira Marcelo Z.

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference43 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. Non-linearities in drip water hydrology: an example from Stump Cross Caverns, Yorkshire;Baker;J. Hydrol.,2003

3. Late Quaternary paleoclimate in the Eastern Mediterranean Region from stable isotope analysis of speleothems at Soreq Cave, Israel;Bar-Matthews;Quat. Res.,1997

4. Paradox of groundwater age: correction;Bethke;Geology,2002

5. A high-resolution proxy record of rainfall and ENSO since AD 1550 from layering in stalagmites from Anjohibe cave Madagascar;Brook;Holocene,1999

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