Groundwater flow system as an archive of palaeotemperature: Noble gas, radiocarbon, stable isotope and geochemical study in the Pannonian Basin, Hungary

Applied Geochemistry

Volumn 26, Issue 1, 2011, Pages 91-104

  Varsányi, Irén ^a   Palcsu, László ^b   Kovács, Lajos Ó ^c  

^a UNIVERSITY OF SZEGED   (Hungary)

^b INSTITUTE OF NUCLEAR RESEARCH ATOMKI   (Hungary)

^c Hungarian Office for Mining and Geology   (Hungary)

Author keywords

[No Author keywords available]

Indexed keywords

BATCH MODELLING; CARBONATE REACTION; CHEMICAL COMPONENT; CHEMICAL COMPOSITIONS; CHEMICAL PROCESS; DISPERSIVE TRANSPORT; FLOW PATH; FRACTIONATION PROCESS; GEOCHEMICAL MODELS; GLACIAL MAXIMA; GROUNDWATER FLOW SYSTEMS; HOLOCENES; HUNGARY; HYDRAULIC CONDITIONS; INFILTRATED WATER; INFILTRATION TEMPERATURES; ISOTOPE RATIO; ISOTOPIC COMPOSITION; MAIN PROCESS; MEAN RESIDENCE TIME; NOBLE GAS; NOBLE GAS TEMPERATURES; PANNONIAN BASIN; PANNONIAN BASIN , HUNGARY; PORE WATERS; QUATERNARY SEDIMENTS; RADIOCARBON AGE; RECHARGE AREA; STABLE ISOTOPES; STUDY AREAS; SUBBASINS; TEMPERATURE CONDITIONS; TEMPERATURE DEPENDENCE; TEMPERATURE DIFFERENCES; TIME SPAN; TRANSPORT MODELLING; WARM TEMPERATURES; WATER ROCK INTERACTIONS;

ALKALINITY; CARBONATE MINERALS; CARBONATION; DEIONIZED WATER; DISSOLUTION; EQUILIBRIUM CONSTANTS; GEOCHEMISTRY; GROUNDWATER; GROUNDWATER FLOW; ION EXCHANGE; ISOTOPES; SEEPAGE; SOIL MECHANICS;

INERT GASES;

CARBON ISOTOPE; DISPERSION; FLOW PATTERN; GROUNDWATER FLOW; HOLOCENE; HYDRAULIC CONDUCTIVITY; INFILTRATION; ISOTOPIC RATIO; LAST GLACIAL MAXIMUM; OXYGEN ISOTOPE; PALEOTEMPERATURE; POREWATER; RADIOCARBON DATING; RESIDENCE TIME; STABLE ISOTOPE; WATER-ROCK INTERACTION;

HUNGARY; PANNONIAN BASIN;

EID: 78650684463     PISSN: 08832927     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.apgeochem.2010.11.006     Document Type: Article

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