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A localized dehydration zone, Söndrum stone quarry, Halmstad, SW Sweden, consists of a central, 1 m wide granitic pegmatoid dyke, on either side of which extends a 2·5–3 m wide dehydration zone (650–700°C; 800 MPa; orthopyroxene–clinopyroxene–biotite–amphibole–garnet) overprinting a local migmatized granitic gneiss (amphibole–biotite–garnet). Whole-rock chemistry indicates that dehydration of the ...

The Role of Advective Fluid Flow and Diffusion during Localized, Solid-State Dehydration: Söndrum Stenhuggeriet, Halmstad, SW Sweden