Gold investment advantages and Starcore gold mining company: Gold retains its value not only in times of financial uncertainty, but in times of geopolitical uncertainty. It is often called the “crisis commodity,” because people flee to its relative safety when world tensions rise; during such times, it often outperforms other investments. For example, gold prices experienced some major price movements this year in response to the crisis occurring in the European Union. Its price often rises the most when confidence in governments is low.
Speaking of gold, it is easily the oldest form of currency in use on earth. It was used by our ancestors centuries ago and is still used today, its mention can even be found in the epics of Hindu mythology which highlights the position that gold holds in the Indian and especially Hindu culture. It is considered as a carrier of good luck and thus is gifted to the new brides and other important milestones of life as well. Therefore, one of the tools which are popular for this purpose is the financial investment which allows a person to multiply his savings by investing it into one of the multiple options available like mutual funds, real estate, gold etc.
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. Discover extra info at gold investment.
High grade mineralization was discovered at San Martin in the 18th Century, and is reported to have been mined over a period of 40 years; however, no production records exist. Between 1900 and 1924, an estimated 250,000 tonnes grading 15 g Au/t and 100 g Ag/t was reportedly mined. Mineralization occurs in Upper Cretaceous black limestone and calcareous shales of the Soyatal Mexcala Formation as electrum, and silver selenide minerals principally associated with quartz and to a lesser degree with calcite. The deposit is an epithermal, probably high sulphidation precious metal (Ag-Au) type (metal ratio Au:Ag at 1:10), related to a Tertiary dacitic/andesitic intrusive dome.
Starcore International Mining and El Creston Property development news: The Creston Deposit is largely underlain by foliated Proterozoic Creston Granite and Laramide granitic porphyry and hydrothermal breccia. At the deposit molybdenum +/- copper mineralization are hosted in both hydrothermal breccias and the surrounding quartz vein stockwork. In addition, a supergene copper blanket consisting largely of chalcocite has been identified occurring primarily on the west and south sides of the deposit. The alteration pattern within the deposit is complex resulting from multiple intrusions and overlapping alteration. Low-angle normal faults divide the El Creston deposit in to three main tectonic slices causing sliding towards N-NNE In profile the El Creston deposit can be imaged as a series of tectonic slices, having their root in the footwall of the Creston Fault. Read more details at https://starcore.com/.