T. R. Weaver

发表

Distinguishing groundwater flow paths in different fractured-rock aquifers using groundwater chemistry: Dandenong Ranges, southeast Australia

S. Tweed, I. Cartwright, T. R. Weaver, 2005 .

Geochemical Evolution in the Cambrian‐Ordovician Sandstone Aquifer, Eastern Wisconsin: 2. Correlation Between Flow Paths and Ground‐Water Chemistry

J. Bahr, T. R. Weaver, T. Weaver, 1991 .

Constraining groundwater flow, residence times, inter-aquifer mixing, and aquifer properties using environmental isotopes in the southeast Murray Basin, Australia

S. Tweed, L. Fifield, I. Cartwright, 2012 .

Environmental isotopes as indicators of inter-aquifer mixing, Wimmera region, Murray Basin, Southeast Australia

I. Cartwright, D. Cendón, T. R. Weaver, 2010 .

Constraining modern and historical recharge from bore hydrographs, 3H, 14C, and chloride concentrations: Applications to dual-porosity aquifers in dryland salinity areas, Murray Basin, Australia

I. Cartwright, M. Reid, T. R. Weaver, 2007 .

Cl/Br ratios and environmental isotopes as indicators of recharge variability and groundwater flow: An example from the southeast Murray Basin, Australia

L. Fifield, I. Cartwright, T. R. Weaver, 2006 .

Physical hydrogeology and environmental isotopes to constrain the age, origins, and stability of a low-salinity groundwater lens formed by periodic river recharge: Murray Basin, Australia

C. Lawrence, C. Simmons, L. Fifield, 2010 .

Stable isotope geochemistry of cold CO2-bearing mineral spring waters, Daylesford, Victoria, Australia: sources of gas and water and links with waning volcanism

S. Tweed, M. Cooper, I. Cartwright, 2002 .