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Fig. 13
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Depth variation of secondary minerals in F1 and Glc1 wells from XRD and Mössbauer data (dashed lines) and temperature change with depth in the well (black line). Secondary minerals: Sm: smectite; Cc: calcite; Qz: quartz; Ch: chlorite; Ep: epidote; Py: pyrite; Mgt: magnetite; Ze: zeolite.
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