Calcite fracture fillings as indicators of paleohydrology at Laxemar at the Äspö Hard Rock Laboratory, southern Sweden

Author:

Wallin Bill,Peterman Zell

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Pollution,Environmental Chemistry

Reference32 articles.

1. Large scale intrusion of shallow water into a vertical fracture zone in crystalline bedrock: Initial hydrochemical perturbation during tunnel construction at the Äspö Hard Rock Laboratory, south-eastern Sweden;Banwart;Water Resour. Res.,1994

2. Blyth, A., Frape, S., Blomqvist, R., Nissinen, R., McNutt, R., 1998. An isotopic and fluid inclusion study of fracture calcite from borehole OL-KR1 at the Olkiluoto site, Finland: Posiva 98–04

3. Hydrogeological essay;Borevski,1984

4. The isotope geochemistry of fracture calcites from the chalk River Area, Ontario, Canada;Bottomley;Appl. Geochem.,1987

5. The nature of groundwater flow in fractured rock: Evidence from the isotopic and chemical evolution of recrystallized fracture calcites from the Canadian Precambrian Shield;Bottomley;Geochim. Cosmochim. Acta,1992

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