Kincora Copper Ltd V.KCC

So we have almost 350m of

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Quartz monzonite or adamellite is an intrusive, felsic, igneous rock that has an approximately equal proportion of orthoclase and plagioclase feldspars. It is typically a light colored phaneritic (coarse-grained) to porphyritic granitic rock. The plagioclase is typically intermediate to sodic in composition, andesine to oligoclase. Quartz is present in significant amounts. Biotite and/or hornblende constitute the dark minerals. Because of its coloring, it is often confused with granite, but whereas granite contains more than 20% quartz, quartz monzonite is only 5–20% quartz. Rock with less than five percent quartz is classified as monzonite. A rock with more alkali feldspar is a syenite whereas one with more plagioclase is a quartz diorite.^[1] The fine grained volcanic rock equivalent of quartz monzonite is quartz latite.^[1]

Quartz monzonite porphyry is often associated with copper mineralization in the porphyry copper ore deposits.^[2]

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Below shallow skarn alteration, TRDD022 intersected a thick interval of equi-crystaline monzodiorite from 376m to 723m depth, which was expected from the geological model (Figures 4, 5 and 6). Notable and positive indicators include: Multiple felsic intrusions, with: (1) an early monzodiorite, cut by (2) quartz-monzodiorite and in turn by (3) later aplite dykes – see