Gold in Mexico with Starcore? Gold is a precious metal and we all know that. As we have mentioned earlier, gold holds a special place in any Indian household and is considered a wealth of the family, for example, the gold jewels are passed on from one generation to the other as a legacy and a symbol of family wealth. Have you ever tried to invest in real estate or tried to make any financial investment? If yes, then you must know that buying gold is much easier than real estate or anything else. It is safe for the people who are trying to start doing investments as very less risk is involved with the gold purchase.
Unlike paper currency, coins or other assets, gold has maintained its value throughout the ages. People see gold as a way to pass on and preserve their wealth from one generation to the next. Since ancient times, people have valued the unique properties of the precious metal. Gold doesn’t corrode and can be melted over a common flame, making it easy to work with and stamp as a coin. Moreover, gold has a unique and beautiful color, unlike other elements. The atoms in gold are heavier and the electrons move faster, creating absorption of some light; a process which took Einstein’s theory of relativity to figure out.
Starcore International Mining and El Creston Property development news: The Copper Anomaly Zone is a 1000 metre long x up to 250 metre wide copper in rock anomaly as defined by the >0.05% Cu contour. The anomaly is underlain by mafic metamorphic complex rocks and diorite that locally have been variably fractured, argillic and chloritic altered. Within the zone, anomalous copper and silver values occur. Molybdenum values are low throughout. Chip sample results include composites of 18 and 27 metres respectfully averaging 0.210% Cu, 3.9 ppm Ag and 0.23% Cu with 4.7 ppm Ag. The Copper Anomaly Zone has not been drilled. Find extra info on gold company.
The Ajax Property occurs along the western margin of the Stikinia Terrane of the North America Cordillera, immediately adjacent to the eastern margin of the Coast Plutonic Complex. The property is underlain by Jurassic Hazelton Group rocks consisting primarily of argillaceous sediments and minor interbedded andesite tuffs that locally has been intruded by four closely spaced stocks of quartz monzonite porphyry. The Ajax deposit occupies a rectangular area approximately 650 m x 600 m that ranges in elevation from 425 masl to 1050 masl. The mineralization is predominantly pyrrhotite and lesser molybdenite that typically comprises less than 2% of the rock by volume. Molybdenite is typically associated with quartz and occurs in pyrrhotite-bearing veinlets, in thin stringers and on fracture and shear surfaces. Areas of elevated molybdenite grades (>0.060% Mo) are characterized by a high fracture density where quartz vein stockwork is well developed. Lower grade material (0.030 to 0.060 % Mo), is found in areas of weaker fracturing and forms a broad halo around the higher grade zones, especially below the 762 m elevation contour.
Mineralization is generally made up of breccia that commonly is concordant with a limestone/shale contact (in the San Martin and San Jose areas) which forms the relatively steeply dipping tronco deposits, these troncos contact the younger volcanic flows (dacite and ignimbrite) where they have formed the more horizontal manto portions of the deposit. The mineralized economic breccia grades from 30 g Ag/t to 250 g Ag/t. Exploration has been concentrated along the NE trending breccia zone however evidence of a northerly trend in area 30 leads us to suspect possible other structures together with 2.0 g Au/t to 30 g Au/t over widths that vary from 1.0 to 17.0 m but average 4.0 m. Read additional info on here.
