Gold producer in Mexico and investing in gold advantages: One of the major reasons for making any financial investment is that you consider it as a backup if in case you need it in future and gold is one of the most of the easy to liquidate the hard asset. In case you happen to be in need to use your gold to make your ends meet, you just have to sell it to the buyer you prefer. There are always buyers ready to buy the gold. But keep in mind the return rate is not exactly what you expect, instead, it is opposite especially in the case of physical gold, you get less than what you invest. Like we mentioned above, gold has a lot of significance in Indian culture but we are not talking of emotions here, in fact, financial investment is not a matter of heart but Mind and thus, let us take a look at all the practical reason that make gold a suitable investment medium over other options.
Starcore International Mining and El Creston Property development news: The Red Hill West Zone is located immediately adjacent to the western boundary of the Red Hill Zone. The zone refers to a 500 metre wide by 500 metre long zone of quartz vein stockwork, hosted by Creston Granite, in which appreciable, >100 ppm, values of molybdenum occur. The host rock is typically oxidized and variably sericitized. Chip sample results include 3 metres averaging 0.083% Mo and a 12 metre composite averaging 0.043% molybdenum. Copper values are negligible. The zone has not been drilled. Discover additional info at Gold producer.
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.
Discovered in 2012 this area has been found to host several veins 1 – 5m thick generally dipping 20 degrees to the east and striking north/south. It has been found within 50 meters of main in the footwall of San Martin structure in the footwall which was previously thought to be exclusively shales. To date at least 4 veins have been found above level 4 in the northeast of San Martin and possibly 2 veins above level 2 further south. Some of the veins are vertical and some are dipping around 40 degrees. In general most are striking parallel to San Martin breccia. See additional details on https://starcore.com/.
