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Volumn 475, Issue , 2012, Pages 281-293

Stable isotope and hydrochemical evolution of groundwater in the semi-arid Hamersley Basin of subtropical northwest Australia

Author keywords

2H and 18O; Alluvial and fractured aquifers; Br Cl ratio; Fortescue marsh; Hydrochemistry; Pilbara

Indexed keywords

ARID ZONES; AUSTRALIA; CHEMICAL COMPOSITIONS; FORTESCUE MARSH; FRACTURED AQUIFER; GROUND WATER RECHARGE; HAMERSLEY BASIN; HYDROCHEMICAL EVOLUTION; ISOTOPIC SIGNATURES; METEORIC WATERS; MINING ACTIVITIES; PILBARA; RAIN-OUT; RAINFALL EVENT; REGIONAL DEVELOPMENT; SALINE GROUNDWATER; SEMI ARID; STABLE ISOTOPES; SUSTAINABLE WATER MANAGEMENT; WATER ABSTRACTION;

EID: 84870235218     PISSN: 00221694     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.jhydrol.2012.10.004     Document Type: Article
Times cited : (153)

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