Fig. 5


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(A) Detail picture of the Figure 4B W-As-Bi-Au bearing quartz vein crosscutting leucogranitic dykes (La Borie vein, outcrops B in Fig. 3). (B) Fault plane seen on Figure 5A with high angle pitch striation. (C) Cm-sized mineralized quartz veins network crosscutting the leucogranitic dyke (the Rode vein, outcrops C on Fig. 3). (D) Focus on the fault plane in the mineralized vein of the Figure 5C showing a normal kinematics.

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