Typomorphic features of the quartz of various mineral paragenesis from the gold mineralization in Karakshatau Mountains (West Uzbekistan)

Svetlana KOLOSKOVA; Jakhongir MOVLANOV

doi:https://doi.org/10.19111/bulletinofmre.432046

Makale detayları

Typomorphic features of the quartz of various mineral paragenesis from the gold mineralization in Karakshatau Mountains (West Uzbekistan)

Yazarlar:

Svetlana KOLOSKOVA | Jakhongir MOVLANOV

Yayıncı:

Maden Tetkik Arama Genel Müdürlüğü

Ana Başlıklar:

Uygulamalı fizik

Dergi:

Bulletin of the Mineral Research and Exploration 2019 Vol.159 Issue 159, pp.117-127

Belge Tipi:

Makale

Yayın Tarihi:

8/2019

Belge Dili:

İngilizce

Document ID (Org No.):

2000519959

Sıklık:

Üç Yıllık

pISSN:

0026-4563

DOI:

https://doi.org/10.19111/bulletinofmre.432046

Özet:

 


As a result of complex studies -
geological-structural, morphostructural analytical, mineralogical mapping of
quartz 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 a
geological-genetic model of the gold-bearing ore-forming system in the collapse
zone. Favorable geological and structural conditions for the localization of
gold mineralization in the mountains of Karakchatau are associated with the
areas of long-term tectonic-magmatic activation in metalliferous sediments of
Є-О contrast lithological composition. The coincidence of manifestations of
gold mineralization to the blocks formed by transverse faults at the sites
where they intersected the Karakchatau crush zone was noted. To the
channel-localizing parts inside are blocky and unextended interblock tectonic
structures with positions in favorable “structural traps” in their azimuthal
curvatures of executed productive types of hydrothermal, sulfidizing quartz.
The results of mineralogical mapping of quartz formations along the Karakchatau
crush zone (Western Uzbekistan) are considered. Five genetic types of quartz
are distinguished. The most productive of them is hydrothermal quartz of types
3 and 4 associated with pyrite,arsenopyrite and gold, which forms vein fields
in areas of kinks and expansion of the zone of crushing. Identification of any
goods and services that can be used for commercial purposes, including in the
geological structure, other regions of Western Uzbekistan.

 


 

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Makale detayları

Typomorphic features of the quartz of various mineral paragenesis from the gold mineralization in Karakshatau Mountains (West Uzbekistan)

Yazarlar: Svetlana KOLOSKOVA | Jakhongir MOVLANOV

Yayıncı: Maden Tetkik Arama Genel Müdürlüğü

Ana Başlıklar: Uygulamalı fizik

Dergi: Bulletin of the Mineral Research and Exploration 2019 Vol.159 Issue 159, pp.117-127

Belge Tipi: Makale

Yayın Tarihi: 8/2019

Belge Dili: İngilizce

Document ID (Org No.): 2000519959

Sıklık: Üç Yıllık

pISSN: 0026-4563

DOI: https://doi.org/10.19111/bulletinofmre.432046

Sayı

Yazarlar:

Svetlana KOLOSKOVA | Jakhongir MOVLANOV

Yayıncı:

Maden Tetkik Arama Genel Müdürlüğü

Ana Başlıklar:

Uygulamalı fizik

Dergi:

Bulletin of the Mineral Research and Exploration 2019 Vol.159 Issue 159, pp.117-127

Belge Tipi:

Makale

Yayın Tarihi:

8/2019

Belge Dili:

İngilizce

Document ID (Org No.):

2000519959

Sıklık:

Üç Yıllık

pISSN:

0026-4563

DOI:

https://doi.org/10.19111/bulletinofmre.432046