Ishdа Kеlеnchаk-Tоshsоy mа’dаnli mаydоnidаgi rutil bilаn nоаn’аnаviy nоdir mеtаlli, hаmdа siyrаk elеmеntliminеrаllаnish ko’rib chiqilgаn vа ulаrning аsоsiy ko’rsаtkichlаri umumlаshtirilgаn. Pеgamаtitlаrning аktsеssоrliminеrаltаrkibi, hаmdа endоgеn-mаъdаndоrlikni grаnitоidli mаgmаtizm bilаn minеrаl-gеоhimik bоg’liqligi kеltirilgаn.Jumlаdаn, аl’bit mаъdаn vа jinslarni shаkllаntiruvchi аsоsiy minеrаl ekаnligi аniqlаngan.
Tayanch iboralar: Kеlеnchаk-Tоshsоy, rutil, mа’dаnli mаydоn, minеrаllаnish, mаgmаtizm, siyrаk yer elеmеntlari,аktsеssоrli-minеrаl tаrkib, аl’bit, grаnit, grаnitоid, аl’bitit, formasia, kimyoviy tarkib, endоgеn-mаъdаndоrlik.
The paper considers the rutile content and unconventional rare metal - and rare earth mineralization of theKelenchok-Tashsay ore field and generalizes their main indicators. The accessory-mineral composition of pegmatites,as well as mineralogical and geochemical indicators of the connection between endogenous mineralization andgranitoid magmatism, are given. The results of the chemical composition of rocks granite (alaskite) - leucograniteformation P1 and albitites of Kelenchek are given. It has been established that albite is the main ore-bearing and rockformingmineral in rare-earth and rare-earth albitites.
Key words: Kelenchok-Tashsai, rutilonost, ore field, mineralization, magmatism, rare earth, accessory-mineralcomposition, albite, granite, granitoid, albitite, formation, chemical composition, endogenic mineralization.