Figure 1From: Physicochemical conditions and timing of rodingite formation: evidence from rodingite-hosted fluid inclusions in the JM Asbestos mine, Asbestos, QuébecGeology of the Asbestos ophiolite in the area of the JM Asbestos mine, Asbestos, Québec (After maps by Johns-Manville Inc, Bédard et al. [18], Hébert [19]). The contact between the ophiolite and the Caldwell Group metasediments shows evidence of earlier thrusting and later normal faulting.Back to article page