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Fig.4a).
Fig. 2. The Revsund granitoids in county Ja¨mtland consist of the northern Fja¨llsjo¨ Massif and the Southern Massif, which is dividedinto a western (investigated here) and an eastern part
Fig. 3. Geological map of the western part of the Southern Massif in Fig. 2 showing the shear zones described in the paper (modifiedafter Lundega˚rdh et al., 1984; Lundqvist, 1996; Lundqvist and Korja, 1997; Sturkell et al., 1998), (1), dextral, west-side-up shearzone at the boundary between metasedimentary rocks and the Revsund granitoid; (2), discontinuous mylonite zone; (3), Forsaa˚nzone; and (4) a belt of anastomosing deformations zones dominated by L�S-mylonites.
Fig. 4. (A) The undeformed, coarsely porphyritic granitoid sampled for U–Pb TIMS titanite analyses
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