Los Cerros Limited announced to update the market regarding recently received assays and additional porphyry-focussed drilling. The Chuscal target is part of the 100% owned Quinchia Gold Project in Colombia which includes the Tesorito near surface porphyry, and the Miraflores ~450koz Reserve all within a 3km radius, plus several undrilled high priority exploration targets. Drillhole CHDDH10 was the first hole designed to test the eastern or Guyacanes porphyry target established via vectoring information gained from previous drilling. Of most note, within a broader ~236m intercept of magmatic breccias, is a ~75m magmatic breccia sub zone from 75m downhole with greater density of porphyry vein textures, increased magnetite and elevated gold and porphyry pathfinders including an intercept of: The above-mentioned intercept and other clues extracted from spatial relationships of lithologies, particularly breccias, was the basis for commissioning CHDDH11 from the same drill pad as CHDDH10 but oriented to the NNW. CHDDH11 intercepted fine grained diorite dykes, being a new unit interpreted to be part of the target porphyry suite with elevated porphyry pathfinders. Vectoring information from CHDDH10 and CHDDH11 were inputs into the location of CHDDH12, located further south of CHDDH10 and collared at a lower elevation. Based on visual logs (assays pending), CHDDH12 has intercepted the same mineralised fine grained diorite intersected in CHDDH11 and intruded within that pulse is a 54m wide zone of an additional intrusion of porphyritic diorite from 89m downhole. This unit has not been previously logged and displays chlorite-sericite alteration overprinting weak potassic alteration. Also of great interest, in terms of gold mineralisation potential at depth, is a 164m wide zone of magmatic breccia (Photo 2) from 211m with classic porphyry pathfinder characteristics ­ such as pervasive secondary biotite, vein high magnetite plus elevated sulphides and vein density. This is the first occasion that diorite, interpreted to be part of the target causative porphyry intrusive suite, has been logged within the eastern target zone, which together with the characteristics of the 164m breccia zone, suggests are close to the porphyry target. Recent information, particularly the intercepts of porphyritic diorite surrounded by the fine grained diorite has provided insight into a potential geological model. The Montana Diorite, a diorite mapped extensively at surface, in artisanal adits and in drill core, is interpreted to be an early, pre-mineral, pulse from the porphyry suite. A series of magma pulses showing elevated pathfinders and encouraging alteration and textures have subsequently punched their way through the early Montana Diorite. The fine-grained diorite is one of these pulses. Like-wise, the porphyritic diorite logged in CHDDH12 is a later pulse punching through the previous pulses and possessing classic porphyry texture. The magmatic breccias, which often mark the boundaries between the pulses and contain transported material from deeper within the system, are enriched in pathfinders particularly the magmatic breccia logged in CHDDH12, which is very high in magnetite and elevated sulphides. The next drill hole (CHDDH13) will step 150m further south from pad CHDDH12 and, given the drop in pad elevation, will drill some 200m below the above-mentioned intersections to test for the presence of an underlying causative gold porphyry. The objectives of CHDDH09 (ASX release 7 December 2020) included testing depth potential of the near surface corporation epithermal vein corridor previously exploited by artisanal miners and gaining critical data to support the presence of a western causative porphyry intrusion accountable for local surface gold and molybdenum anomalism. With regard to the first objective, the hole crossed numerous epithermal veins overprinting the corporation Diorite including: 1.35m @ 10.57g/t Au & 89.77g/t Ag from 133m, 2.10m @ 37.94g/t Au & 18.64g/t Ag from 232.5m incl 0.8m @ 98.3g/t Au and 44.80g/t Ag from 233.8m. The shallow drilling program continues to discover numerous epithermal veins across the entire Chuscal area reporting narrow high grade gold and silver intersections of up to 98g/t and 90g/t respectively. The economic potential of these Au/Ag veins remains an ongoing investigation as the Company focusses on the hunt for large scale gold-copper porphyry style mineralisation. With regard to the second objective, after leaving the corporation Diorite at 332m, CHDDH09 entered an 18.3m dyke or `finger' of porphyritic diorite which is interpreted to be the upper portion of the western porphyry target with classic porphyry alteration and A-type veining. The porphyritic diorite is followed by 75m of associated magmatic breccia which comprised a dioritic matrix containing clasts or fragments of porphyritic diorite transported from its source. It is around this zone of diorite and breccia that gold mineralisation and elevated porphyry element pathfinders were encountered, such as 98m @ 0.6g/t Au, 92ppm Mo and 402p m Cu from 350m incl: 4m grading 0.27% Cu from 366m, and 43.70m @ 0.99g/t Au from 388m incl 12m grading 883ppm Cu and 195ppm Mo from 414m Hole CHDDH09 is the first occasion that porphyritic diorite, interpreted to be part of the causative porphyry intrusive suite, with associated magmatic breccia, has been logged in the western porphyry target. From 530m to 612.8m (end of hole) saw a moderate increase in molybdenum grades in monzonite with weak potassic alteration to levels suggesting this zone is also near to a causative porphyry source, with 82.8m at 20ppm Mo from 530m with increasing Mo grade at depth to 40.8m @ 29ppm Mo from 572m.