!! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! !! ! !! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! !! ! ! ! ! ! ! ! ! ! ! ! ! A A A' B B' 350 400 300 450 500 250 350 350 350 300 350 450 350 300 300 400 300 300 350 300 450 300 300 450 450 300 300 300 300 300 400 300 300 300 400 300 400 300 300 400 300 300 300 300 300 300 300 300 400 300 Sc SSf SLTs(1) SLTr CGL SLTs(2) Igb LAT SSs REJ SLTg TRS Scss Id BXsed Bxhem 646000 646000 646250 646250 646500 646500 646750 646750 647000 647000 647250 647250 647500 647500 647750 647750 648000 648000 648250 648250 648500 648500 648750 648750 649000 649000 649250 649250 9340750 9340750 9341000 9341000 9341250 9341250 9341500 9341500 9341750 9341750 9342000 9342000 9342250 9342250 9342500 9342500 9342750 9342750 9343000 9343000 9343250 9343250 9343500 9343500 9343750 9343750 9344000 9344000 0 500 1,000 250 m Geological Map of Serra Pelada 20° stratigraphic Column of the Serra Pelada Project 1:10,000 Serra Pelada Project - Geological Map Date:January 2013 1:10,000 Scale: Geologist: Graham Long Paulo Mauricio Lopes Gilberto Luiz Silva Carlos José Evangelista Silva Datum: UTM - South America 1969 Legend Elefante Target Auger Drilling ! Phase 1 ! Phase 2 850425/1990 813687/1969 - 700ha 850424/1990 Topography Lines 50m Topography Lines 10m Old Pit Serra Pelada/ Lake Structural Structure Axe Fold # # # Inverse Fault # # # Inverse Fault inferred Normal Fault Red Siltsone: Pink red colored siltstone with alternating layer of silt and fine grained quartz, locay rich in manganese and iron oxide. Friable Sandstone: Pure sandstone, friable, locally with sandy-silt layers, locally contains varying amounts of manganese. manganese. These sandstones are interpreted as the product of decalcification of dolomitic sandstones. Siliceous Sandstone: Sandstones eventually poorly selected microcrystalline silica, associated with ferruginous sandstones. Occur associated with ferruginous and manganesíferas breccias and might be associated with dolomitic rocks. Sandy Siltstone: Sand siltstone, pink to red, sometimes laminated with sand levels, silt levels rich in manganese or iron oxides. SLTg - Siltstone: Grey to black colors with minor to moderate carbon content, contains alternating levels of silt and clay. (SLTcb - Carbon Up Grade Hydrothermal in Siltstone) Diorite: Intrusive coarse-grained rock, green colored and reddish when altered. Composed mainly of feldspar, pyroxene and minor quartz. Weathers to clay. Conglomerates: Matrix-supported conglomerates and locally clast-supported conglomerates intercalated . It has fragments of quartz and iron formation locally in sandy matrix with large concentrations of hematite. Neoarchean Rio Fresco Group Archean Rio Novo Complex Hematite Breccia: Rock with rhythmic banding of between silt and sand. The sand matrix is rich in Fe, and dark brown Soil with many fragments smaller than 10 cm specularite Gabbro: A green course grained basic igneous rock, consisting of plagioclase feldspar, clinopyroxene and orthopyroxene. Schist: Chlorite talc schist, chlorite schist, with abundant biotite. with strong metamorphic foliation and tight micro folds. Quartzite: Metamorphic rock composed mainly of microcrystaline quartz grains and locally contains an iron stained matrix. Sedimentary Breccia: A rock composed of broken fragments of minerals or rock cemented together by a fine-grained matrix, that can be either similar to or different from the composition of the fragments Serra Pelada Lithologies Red soil Laterite,that locally displays an iron laterite crust. Material deposited by human activity Tranported silt sand soil. Red, yellow or cream colored. Early Jurasssic Quaternary REJ LAT TRS Id Bxhem BXsed CGL SSs SLTs(2) SLTs(1) SLTr SSf Neoarchean Igb Sc Scss SLTg !! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! . ! . ! . ! . ! . ! . ! . ! . ! . ! . ! . ! . ! . ! . ! . ! . ! . ! . ! . ! . ! . ! . ! . ! . ! . ! . ! . ! . ! . ! . ! . ! . ! . ! . ! . ! . ! . ! . ! . ! . ! . ! . ! . ! . ! . ! . ! . ! . ! . ! . ! . ! . ! . ! . ! . ! . ! . ! . ! . ! . ! . ! . ! . ! . ! . ! . ! . ! . ! . ! . ! . ! . ! . ! . ! . ! . ! . ! . ! . ! . ! . ! . ! . ! . ! . ! . ! . ! . ! . ! . ! . ! . ! . ! . ! . ! . ! . ! . ! . ! . ! . ! . ! . ! . ! . X Y X Y Ç Ç 311 312 307 309 308 310 306 305 304 303 302 301 300 313 314 299 315 298 297 316 296 317 295 318 298 296 298 297 297 299 295 295 ELD-002 ELD-001 EL-12-004 EL-12-003 EL-12-002 EL-12-001 0.9 2.76 0.58 3.23 2.285 0.883 0.977 1.498 5.923 1.877 0.596 0.045 0.218 1.318 1.352 5.005 1.813 5.661 2.717 6.093 1.291 0.578 2.978 1.749 0.915 4.119 19.25 1.348 1.387 0.3502 0.1787 0.2883 0.6163 0.6162 0.2582 0.8746 1.6623 0.5254 0.5696 1.0879 0.6331 1.2621 0.6385 0.3025 0.5599 0.2747 1.0146 0.6276 0.7035 1.4829 0.5658 2.3007 1.1698 9.6479 5.6417 0.3574 0.2087 0.6128 0.3858 0.2984 0.4277 0.7447 0.2255 0.4727 0.5308 0.7623 1.2439 2.9405 7.0711 0.1775 0.2728 0.4362 0.2973 0.7439 1.3904 0.1165 0.6733 0.3245 0.4445 0.6097 2.5577 0.3549 0.2142 0.2589 1.1256 0.2378 5.7898 0.0844 0.0873 0.0757 0.0244 3.3337 9.3978 1.4028 0.6915 9.4765 18.6513 2.41261 24.917999 480.98099 20.639999 017 016 SLTs(1) Sc SLTg 648900 648900 648950 648950 649000 649000 649050 649050 649100 649100 649150 649150 649200 649200 9341350 9341350 9341400 9341400 9341450 9341450 9341500 9341500 Holes with anomalies in saprolite/transition zone Auger Phase Phase 1 Phase 2 ! . ! . SPTRD-016 X SPTRD-017 X Elefante Drilling Elefante drill holes priority ! . Trace hole (surface Iso-contour Au+Pt+Pd (g/tonne) > 1 1 - 20 20 - 50 > 50 Topographic contour Ç Old Garimpeiro Shafts Shafts Lengend of Elefante Target 5 meters spacing 1 meters spacing 0 25 50 75 100 12.5 Meters 1:1,000 ± ± Elefante Target - Inset 1 Inset 1 Legend ! Diamont Drilling