УДК: 553.411

Структурные позиции и геодинамические условия формирования золоторудных проявлений в Ауминзатау-Бельтауском рудном районе

Авторы: Турапов М.К. || Жанибеков Б.О. || Умматов Н.Ф. || Умаралиев А.У. || Суяров Ш. ||

Рубрика: Геология || Выпуск: №3 (Июль-Сентябрь), 2017 год. || Скачать

Maqolada Auminzatov-Beltov rayonining oltin konlari va ma'dan namoyonlarining geologik-strukturaviy pozitsiyalarini o'rganilganlik natijalari, iindan lashqari geodinamik sharoit ostida rivojlangan ma'dan ob'ektlarini rasshifrovkasi keltirilgan. Aniqlandiki, o'rganilayotgan rayonda oltin namoyon bo'lishi keng spektrli uzilmali buzilmalar ostida rivojlangan. Ularni maydon bo'yicha birikmasi etti xil stmktura pozitsiyalarida shakllanishi oldindan aniqlangan. Aniqlangan Auminzatov-Beltov struktura pozitsiyalarinio'yxshashligiga qaramav ularni minerallashuv jarayoni ostida ta'sirlari turlicha. Geodinamik va tektonik jihatdan farqlanadigan, tektonik bloklarga aloqador bo'lmagan Auminzatov va Beltovni alohida ko'rib chiqish uchun yo'l qo'yib beradi. ShSh va ShF uzilmali buzilmalar profillanadigan strukturalar, Auminzatov va Beltov oltin hosil bo'lish struktura pozitsiyalaridagi elementlardagi farqlanish hisoblanadi.

Tayanch iboralar: foydali qazilmalar, region, oltin, strukturaviy pozitsiyalar, tektonika, geodinamika, darzliklar, tektonik bloklar, oltin m a’danlashuvini joilashishi.

The article rejlects the results o f studying the geological and structural positions o f gold deposits and ore occurrences in the Auminzatau-Beltau region, as well as the decoding o f the geodynamic environments under which ore objects were formed. It is shown that manifestations o f gold were form ed in the investigated area under the influence of a wide spectrum o f breaking disruptions. Their combinations in space predetermined the formation of seven types o f structural positions. Despite the similarities between the revealed structural positions o f Auminzatau and Beltau, their influence on the process o f ore formation is different. Differences in the elements o f the structural position o f the manifestations of gold in Beltau and Auminzatau, where the structural structures are SW and NW breaking, allow Beltau and Auminzatau to be considered as separate, interconnected tectonic blocks that differ in tectonics and geodynamics.

Key words: minerals, region, gold, structural positions, tectonics, geodynamics, faults, tectonic blocks, gold mineralization locations.

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Библиографический список

1. Королев В.А. Структурные типы рудных полей и месторождений Средней Азии. Москва, «Недра», 1983, С.- 216.

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