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Алания Шота Николаевич .8 905 744 78 29 #
New data about the Hokrila-Achapara Gold Ore-Mineralization
The Hokrila-Achapara gold ore-manifestation was found in the western mountainous part of Georgia – Svaneti. Svaneti is one of the most beautiful region, which is situated on the Southern slope of the Greater Caucasus and is facing the Black sea.
The Greater Caucasus is the farthest northern segment of the Eastern Mediterranean orogenic system, which is spread out at about 1200 km, between the Black and Caspian seas. It is collision-accretionary formation and in it construction Pre-Alpine crystalline basement and Alpine cover are conspicuous.
The information about gold ore is mentioned already in the Greek and Roman historical sources. According to Strabon (the first century Greek historian) it was gold that stipulated Greek Argonauts visit to Kolkheti Kingdom (the ancient Georgia) to gain "The Golden Fleece".
Not only historical sources, bit high composition of this metal in Enguri river sand (the main water collection) has information about the existence of gold-bearing rocks in Svaneti. Quartz veins of Lower Jurassic schist were regarded as the main source of gold in Svaneti. And that's why gold was looked for only in schist and without much result. At the beginning the nineties gold was found in the Hercynian crystalline basement of the Greater Caucasus and was separated qurtz-lessersulfidic-hidrothermic genetic type Hocrila-Achapara gold ore-manifestation.
It is considered that Greater Caucasian crystalline basement is poor in mineral resources. Bat as a result of the field work, we have revealed three interesting ore manifestations: Thviberi, Szgimazuki and Hokrila-Achapara. Hokrila-Achapara is the most significant among them, which we will describe in detal. Besides, some areas of investigated granitoids represent very good building and facing material. Among them should be mentioned plagiogranits of the Szgimazuki massiff, of the gabbro-plagiogranite series. They are situated in the upper level of the mentioned massif, wich are outcrop compriess 5 km2. They are white-milk color finegrained massif rocks and represent good fasing material, because look like white marble, but different from which are resistant as to chemical as mechanic factors.
Tviberi ore-mineralization. It is outcroppes in the upper river Tviberi (river Enguri right tributary) and was formed in Lower Jurassic sediments, which are localized as tectonic scale among granitoids of plagiogranite-granite series. In the 1991 the left cornice of the river Tviberi fell down and a massife ore-mineralization zone was outcropped, which is of 100-150 m thickness and lies along 700 m. The ore is represented by quartz-pirite-pirotine associations where the gold composition does not exceed 1 g/t. Notwithstanding this fact, the detailed study of the zone is nessesary because dimension of ore-mineralization is high.
Szgimazuki ore mineralization. It is developes on the Lakchkhilda mountion range, near the Southern contact of Szgimazuki plagiogranite massif in the Lower Jurassic sediments. The ore-mineralization outcrop is of 12-15 m thickness and lies along 60 m and other part is covered with deluvion sediments. The ore-mineralization is represented by massif pirite-pirotine ore, where gold consentration ranges between 1.7-2.5 g/t, as to silver composition reaches 50-55 g/t. As we can see this ore-mineralization is of great interest and needs further investigation.
At the beginning of the ninetes last century in the crystalline basement of the Greater Caucasus was separated quartz-gold lesser sulfidic hydrothermic genetic type the Hokrila-Achapara ore-mineralization zone. It is situated in the crystalline basement of the Greater Caucasus and structurally is related to the regional fault general Greater Caucasian direction (SE-NW), co called Alibek, along which granite-migmati
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