Gypsum Area
Total Area Size: 52 hectares
Area Status : Under Claim
Pyrite Area
Total Area Size: 50 Hectares
Area Status : Under Claim
Copper Area/Molybdenum Area
Total Area Size: 5 x 20 Hectares = 100 hectares
Area Status : With Small Scale Mining Permit
Cu Grade: LOw and High Grade Copper Ore
Manganese Area
Total Area Size: 10 Hectares
Area Status : In Application Stage
Mn Grade: Above 45% Mn content
Dolomitic Limestone Area
Total Area Size: 1500 hectares
Area Status: Under Claim
Dolomite Grade: not less than 18% magnesia
Calcium: more than 30%
Black Sand Area
Total Area Size: Approximately 10 Hectares with 1 meter thick Black Sand
Area Status : Under Claim
Silica Area
Total Area Size: 100 Hectares
Area Status: under claim
Silica Grade: above 98% SiO2 content(granulated sand), above 99%(washed granulated sand)
Silica Area 2
Total Area Size: 749 Hectares
Area Status: With Lease Agreement/Mine Operation Permit
Silica Grade: above 97% SiO2 content(fine sand), Above 97% SiO2 content(quartz rock)
Copper/Gold/Molybdenum/Iron Area
Total Area Size: 6,917 hectares
Area Status: With Mineral Production Sharing Agreement (MPSA)
Geologic Reserve
Molybdenum: 10.5 Billion Metric Tons x 40.42% Mo = 4.23 Billion Metric Tons Mo
Copper: 10.5 Billion Metric Tons x 14.66% Cu average = 1.54 Billions Tons Cu
Gold: 10.5 Billions Metric Tons x 7.35grams/Ton Au = 77,175 Tons Au
Iron: 2 Billions Tons of Iron Ore averaging 53.26%(50% to 63%)in 400 hectares portion of the total area
Mineralization
The area evaluated is mainly underlain by medium to coarse grained diorite occuring as the xenolithic bodies
intercalated sequence of metamorphosed volcanics. The mapped sediment is on the southern section of the mineral
claim.
The intersection of NNW trending fault in the area are the most possible pasage of mineralized solutions that
that form veins, fracture filling and disseminated type of sulfide mineralization.
The volcanic sequence was noted in various metamorphic zoning. This rock unit is apparently closer to the intusive,
while the sediments patterns seems further because it is partly responded and the reaction of this unit is mainly
on the lower temperature scale.The metamorphic zoning is the best possible and favorable depositional site of the
massive sulfide metal.
Gold Portion Area
The gold area is largely underlain by thick sequence of clastic rocks, overlain locally by the trangresive
pyroclastic young volcanic units, chiefly conglomerates, with sometimes associated with basic to intermediate
flows. These arkosic and quartzitic clastic locally intruded by the diorite.
Megascopic identification of rock samples in this area showed a mineralized pyroclastic volcanic with
abundant malachite, azurite, bornite with fine grained pyrite, chalcopyrite exposed 35 meters width.
Portion Area A (Copper Deposit)
In the vicinity of the area, a widespread metamorphic sequence of volcanic and sedimentary unit were
intruded by the hornblende diorite and underlain unconformable by the young volcanic sequence and sediments.
Both type of sulfide mineral are superficially manifested by the widespread and thick malachite, azurite stains.
This type of mineral is noted by highly magnetic attraction of rocks.
Megascopic identification revealed a highly mineralized volcanics (pyc),oxidixed,massive sulfides.
Portion Area B (Molybdenum, Copper, Iron Deposits)
The area mapped noted for molybdenum, iron, and copper minerals. It is perfectly bedded,
moderately contorted, both football and hanging wall also noted the disseminated of sulfide
minerals, and enriched of copper stains are dominant oxidation. These may be the reaction of
cupriferous sulfides in the area.
Megascopic identification indicated a silicified pyroclastic abundant fine grained pyrite
and chalco pyrite, and with strong magnetic attraction.
Portion Area C (Copper Deposit)
The area survey noted is a widely scattered highly mineralized outcrops and boulders of
of massive sulfide with chalcocite, pyrite, chalcopyrite and malachite, azurites stains.
Hydrothermal solutions emanating from the intrusive diorite magma occur during the later phase
of intrusions. These units partially replaced the younger volcanic. Pyritization, silification,
epidotization, and chloritization are common in rock alteration along the mineralized zones.
Malachite, azurite,chalcocite are dominant oxidation product of cupriferous sulfides.
Megascopic identification in this type of deposit is a silicified diorite phorphyritec
textures with pyrite, chalcopyrite and magnetite.
