By G. Morizot (auth.), Alexander G. Tvalchrelidze, Georges Morizot (eds.)
The NATO complex learn Workshop “Mineral source Base of the Southern Caucasus and structures for its administration within the XXI Century” was once held in Tbilisi on April 3-6, 2001. The workshop was once financed by way of the NATO technology Programme and financially supported by means of the Open Society – Georgia starting place. by way of the tip of the XX century the recent states of the Southern Caucasus (Azerbaijan, Armenia and Georgia) came across themselves within the lowest part of a critical structural challenge. Belonging to an identical geopolitical house and having the typical monetary heritage through the XIX and XX centuries, those international locations may be in a position to triumph over this obstacle and to combine into the area neighborhood basically step by step, exploiting their source bases and constructing aggressive branches of industries. in addition, in our opinion, such notion is the one substitute to the spontaneous most economical chaos. resolution of this challenge seems most unlikely with out shut overseas collaboration. From this standpoint, the assumption of local alliances the place neighborhood actors will be associated via a common, non-contradictory macroeconomic version appears to be like the single danger for sustainable improvement. production of The Southern Caucasus Alliance (SCA) the place Georgia, Azerbaijan, Armenia and Turkey may locate their position will be attainable in simple terms in case if the commercial fact and financial pursuits could crush nationalistic doctrines of political isolationism.
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Additional resources for Mineral Resource Base of the Southern Caucasus and Systems for its Management in the XXI Century
Geologically gumbrine represent a product of autigene marine (halmirolysis) alteration of the andesitic ash. This conception, first forwarded by Tvalchrelidze (1941), was afterward proven by Machabeli [32, 33]. Among numerous manifestations of gumbrine the better technologic properties are characteristic of the Gumbri and the Askana group deposits (Early Alpine mineralization of the Dzirula subterrane). Reserves are equal to about 11 millions tons of this precious raw material. 3. Talc Bulk current talc reserves of the Chorchana group deposits amount to 1,900,000 tons.
In the AdjaraTrialeti subterrane a typical porphyry copper system as well as iron skarn deposits were related to quartz-monzonite-diorite intrusive bodies. Simultaneous postvolcanic processes resulted in agate formation. In shallow subsequent fresh-water lakes and bogs, correspondingly, diatomites and carboniferous strata were deposited. In the SomkhitoKarabakh terrane last volcanic paroxysms and a postvolcanic activity produced perlite, obsidian and agate deposits. Quaternary epoch was governed by climatic conditions of the Greater and the Lesser Caucasus as well as by features of their relief.
Siderite strata alternate with coal seams here. 9 m. Magnetite placers of the Black Sea coast are 50 km long, but they are extremely rich near the influx of the river Supsa (Supsa-Natanebi deposit). Here content of magnetite and titanomagnetite fractions is 3% with reserves of 45,000,000 tons (15,400,000 tons of iron). From the XIX century Georgia has been known as having important reserves of manganese oxide and carbonate ores. All commercial deposits and mines are due to the Middle Alpine mineralization epoch.