TY - JOUR T1 - Typomorphic features of the quartz of various mineral paragenesis from the gold mineralization in Karakshatau Mountains (West Uzbekistan) AU - Movlanov, Jakhongir AU - Koloskova, Svetlana PY - 2019 DA - August DO - 10.19111/bulletinofmre.432046 JF - Bulletin of the Mineral Research and Exploration JO - Bull.Min.Res.Exp. PB - Maden Tetkik ve Arama Genel Müdürlüğü WT - DergiPark SN - 0026-4563 SP - 117 EP - 127 VL - 159 IS - 159 LA - en AB - As a result of complex studies -geological-structural, morphostructural analytical, mineralogical mapping ofquartz formations, detailed geochemical work and analysis of geochemical fields– forecasting prospecting features of gold ore taxon’s: ore zone; ore field;deposit and ore body. They are characterized by groups of criteria: morphostructural,stratigraphic-lithological, structural-tectonic, magmatic, geophysical,metasomatic, mineralogical, geochemical factors and attributes, and ageological-genetic model of the gold-bearing ore-forming system in the collapsezone. Favorable geological and structural conditions for the localization ofgold mineralization in the mountains of Karakchatau are associated with theareas of long-term tectonic-magmatic activation in metalliferous sediments ofЄ-О contrast lithological composition. The coincidence of manifestations ofgold mineralization to the blocks formed by transverse faults at the siteswhere they intersected the Karakchatau crush zone was noted. To thechannel-localizing parts inside are blocky and unextended interblock tectonicstructures with positions in favorable “structural traps” in their azimuthalcurvatures of executed productive types of hydrothermal, sulfidizing quartz.The results of mineralogical mapping of quartz formations along the Karakchataucrush zone (Western Uzbekistan) are considered. Five genetic types of quartzare distinguished. The most productive of them is hydrothermal quartz of types3 and 4 associated with pyrite,arsenopyrite and gold, which forms vein fieldsin areas of kinks and expansion of the zone of crushing. Identification of anygoods and services that can be used for commercial purposes, including in thegeological structure, other regions of Western Uzbekistan. KW - Gold KW - Mineralogical mapping KW - Typomorphism KW - Quartz KW - Karakchatau KW - Uzbekistan KW - Genetic type CR - Babaev, K.L. 1951. Genetic characteristics of quartz formations of the Nuratau range. Tr. Institute of Geology 6, Tashkent, ANUSSR, CR - Babaev, K.L. 1985. Genetic types of quartz // Zap.Uzb.otd. WMO. Issue. 38. Tashkent: Fan, 5-10. CR - Ivankin, P.F., Nazarova N.I. 2001. Deep fluidization of the earth’s crust and its role in petro-labor, salt and oil formation. Moscow, TsNIGRI, 206 p. CR - Koloskova, S.M. 2007. Geological and genetic model of the development of the gold-bearing ore-forming system in the Southnuratau zone of collapse. Geology and Mineral Resources 2, 44-49. CR - Koloskova, S.M. 2008. Ore-forming processes in the gold- bearing zones of the crushing of the cover-fold regions of Western Uzbekistan: the genesis and typomorphism of quartz formations // Problems of geology of ore deposits, mineralogy, petrology and geochemistry. Conference proceedings. - Moscow: IGEM RAS, 2008. p. 92-94 CR - Mikhailova, Yu.V., Mansurov, M.M. 2004. Polyformativity of gold ore deposits of the Kyzylkum-Nuratau region in connection with its geodynamic development. Problems of geology of the Phanerozoic Tien Shan. Conference proceedings. Issue 2, Tashkent, 95-102. CR - Petrovskaya, N.V. 1956. Some features of intrathoric metamorphism of gold-quartz formations on the example of deposits of the Yenisei Ridge. Tr. Institute “Nigrisoloto” 21, Moscow, 3-44. CR - Yurgenson, G.A. 1984. Typomorphism and ore-bearing property of veined quartz. Moscow, Nedra, 149 p. CR - Yanovsky, V.M. 1990. Ore-controlling structures of terrigenous miogeosyncline. Moscow, Nedra,–246 p. UR - https://doi.org/10.19111/bulletinofmre.432046 L1 - https://dergipark.org.tr/tr/download/article-file/486178 ER -