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Therole of Metasomatic Breeds in Ore Bodies Forecasting to Depth (Beshkuduk)
Shermuhamedov T.Z.1, Janibekov B.O.2, N.Sh.Tulyaganova3, N.T.Rakhmatullayeva4

1Shermukhamedov Tulkin Zakirovich*, Assistant professor, Department of Geology, Mineralogy and Petrography, Tashkent State Technical University, PhD University Street, Tashkent, Uzbekistan.
2Janibekov Bobir Omonovich, Assistant professor, Department of Geology, Mineralogy and Petrography, Tashkent state technical university, PhD University Street, Tashkent, Uzbekistan.
3Tulyaganova Nargiza Shermatovna, Head of Department of Geology, Mineralogy and Petrography, Tashkent State Technical University, University Street, Tashkent, Uzbekistan.
4Rahmatullayeva Nargiza Tulkunovna, Senior lecturer Department of Ecology and Environmental Protection, Tashkent State Technical University Street, Tashkent, Uzbekistan.

Manuscript received on November 11, 2019. | Revised Manuscript received on 22 November, 2019. | Manuscript published on December 10, 2019. | PP: 2828-2830 | Volume-9 Issue-2, December 2019. | Retrieval Number: B7199129219/2019©BEIESP | DOI: 10.35940/ijitee.B7199.129219
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© The Authors. Blue Eyes Intelligence Engineering and Sciences Publication (BEIESP). This is an open access article under the CC-BY-NC-ND license (http://creativecommons.org/licenses/by-nc-nd/4.0/)

Abstract: Hydrothermal mineralization in the deposit has a wide development. It occurs itself in three stages: pre-ore, ore and post-ore. In the pre-ore phase, quartz-albite-sericite chlorite metasomatitesoccurred. In the ore stage, two stages are distinguished: the earlier quartz-pyrite-arsenopyrite stage with gold and quartz – the bleachers association. The minerals of these stages are confined to tectonic troublesome zones, zones of vein silicification, quartz and shale breccias. In the placement of products of hydrothermal metasomatism, a certain horizontal zonality is detected. There is a consistent sequential change of zones with distance from the quartz veins and faults. 
Keywords:  Metasomatic, Biotite, Quartz, Slbite, Sericite, Chlorite, Main Mineral, Associated Mineral, Pyrite, Arsenopyrite, Postmagmatic, New Formations.
Scope of the Article: Petroleum and Mineral Resources Engineering