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10:59
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Originally posted by Furpo2
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Well the good news is what we largely knew already:The dilational nature of the shear has enabled Lady Jane Diorite (LJD) dykes to intrude on shear contacts and parallel to localised shear fabrics. Mineralisation is narrow and tightly constrained within the PSZ , which is consistent with a dominantly tensile or extensional-shear vein-controlled host structure. Gold mineralisation commonly extends along dilational structures that propagate from the diorites, particularly primary deformation event bedding parallel thrust faults.
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Thanks Furpo. Guess it buys them a bit more time to find better grades.
