Uranium Deposit Report

Deposit :

Dzhidely  

Country :

Kazakhstan  

General Information

Geological District

North Betpakdala  

Geological Region

Pribalkhash  

Political/Geographical Province

Karaganda Region  

Last Data Update

2005-01-01  

Owner(s)

Kazatomprom  

Operator

Kyrgyzstan Government  

Technical Information

Tonnage Range (t U)Initial U amount in the deposit (Global Resource)

2,500 - 5,000  

Grade Range (% U)Initial U Grade in the deposit

0.20 - 0.50  

Deposit StatusCurrent status of the deposit

Depleted  

Current Processing PlantCurrent processing mill of the U from the deposit, if any

 

Cumulative Production (t U) Total U production from the deposit

4000  

Production PeriodU production period

1966-1978  

Produced Grade (% U) Grade of the produced U

0.3  

General Remarks

 

Geological Information

Deposit Type

Volcanic  

Geological Setting

Lithology: Three suites of Middle to Upper Devonian volcanics contain U mineralization (from top to bottom): plagioclase porphyry, tuff-sandstone, and volcanic breccia; two horizons of welded felsite tuff, up to 170 m thick (principal host rocks); and plagioclase quartz porphyry, tuff, ignimbrite, and lava-breccia, up to 350 m thick. NW-SE and W-E striking diabase and diabase porphyry dikes dissect this volcanic suite. Tectonics: Principal structures are the NW-SE and NE-SW trending Northern, Southern and Dzhideli faults. Alteration: Host rock alterations produced pre-ore chlorite-albite, ore related pyrite-ankerite, and post ore quartz-calcite-sulfide. Hostrock Age: Middle to Upper Devonian  

Age of Mineralization

Primary mineralization is dated at 360±8 m.y., and redistributed mineralization at 210-100 m.y..  

Mineralization

Ore Mineralogy: Mineralization is of polymetallic nature dominated by uranium-molybdenum associated with As, Bi, Co, Ga, Pb, Sb, and Zn. Two ore types are distinguished: femolite-pitchblende and pitchblende-sooty pitchblende. Uranophane, beta-uranotile, autunite, etc are Mineralization Description: Ore bodies #1, 2, 5, 6, and 8 have a lenticular shape and occur in fault zones within welded felsite tuff at depths from 30 to 180 m. Ore bodies #1, #2 and #5 contain 95 % of the Dzhideli resources. Ore body #1 is 400 m long, 0.5 to 35 m (av.10 m) thick, Ore Controls: Lithological and structural control: Middle to Upper Devonian acid tuffs cutted by the NW-SE and NE-SW trending faults.  

MetallogenicAspects

 

Age of Mineralization

Primary mineralization is dated at 360±8 m.y., and redistributed mineralization at 210-100 m.y..  

DepositShape

 

DepositDimensions

Deposit Width: 200 to 500 m Deposit Length: 1200 m Deposit Depth Top: 30 m Deposit Depth Bottom: 180 m  

GeologicalRemarks

 

Metallogenic Aspects

 














Uranium Deposit Report

Deposit :

Dzhidely  

Country :

Kazakhstan  

General Information

Geological District

North Betpakdala  

Geological Region

Pribalkhash  

Political/Geographical Province

Karaganda Region  

Last Data Update

2005-01-01  

Owner(s)

Kazatomprom  

Operator

Kyrgyzstan Government  

Technical Information

Tonnage Range (t U)Initial U amount in the deposit (Global Resource)

2,500 - 5,000  

Grade Range (% U)Initial U Grade in the deposit

0.20 - 0.50  

Deposit StatusCurrent status of the deposit

Depleted  

Current Processing PlantCurrent processing mill of the U from the deposit, if any

 

Cumulative Production (t U) Total U production from the deposit

4000  

Production PeriodU production period

1966-1978  

Produced Grade (% U) Grade of the produced U

0.3  

General Remarks

 















Uranium Deposit Report

Deposit :

Dzhidely  

Country :

Kazakhstan  

Geological Information

Deposit Type

Volcanic  

Lithology

Three suites of Middle to Upper Devonian volcanics contain U mineralization (from top to bottom): plagioclase porphyry, tuff-sandstone, and volcanic breccia; two horizons of welded felsite tuff, up to 170 m thick (principal host rocks); and plagioclase quartz porphyry, tuff, ignimbrite, and lava-breccia, up to 350 m thick. NW-SE and W-E striking diabase and diabase porphyry dikes dissect this volcanic suite.  

Tectonics

Principal structures are the NW-SE and NE-SW trending Northern, Southern and Dzhideli faults.  

Alteration

Host rock alterations produced pre-ore chlorite-albite, ore related pyrite-ankerite, and post ore quartz-calcite-sulfide.  

Host Rock Age

Middle to Upper Devonian  

Age of Mineralization

Primary mineralization is dated at 360±8 m.y., and redistributed mineralization at 210-100 m.y..  

Ore Mineralogy

Mineralization is of polymetallic nature dominated by uranium-molybdenum associated with As, Bi, Co, Ga, Pb, Sb, and Zn. Two ore types are distinguished: femolite-pitchblende and pitchblende-sooty pitchblende. Uranophane, beta-uranotile, autunite, etc are  

Mineralization Description

Ore bodies #1, 2, 5, 6, and 8 have a lenticular shape and occur in fault zones within welded felsite tuff at depths from 30 to 180 m. Ore bodies #1, #2 and #5 contain 95 % of the Dzhideli resources. Ore body #1 is 400 m long, 0.5 to 35 m (av.10 m) thick,  

Ore Controls

Lithological and structural control: Middle to Upper Devonian acid tuffs cutted by the NW-SE and NE-SW trending faults.  

Metallogenic Aspects

 

Deposit Shape

 

Deposit Width

200 to 500 m  

Deposit Length

1200 m  

Deposit Thickness

 

Deposit Depth

Top = 30 m  ; Bottom = 180 m  

Geological Remarks