Kochbulak Deposit

Occurrence in Tajikistan with commodities Gold, Silver, Copper, Lead, Zinc, Iron, Antimony, Bismuth, Manganese, Tellurium
Sections on this page
  1. Identification information
  2. Geographic coordinates
  3. Site location context
  4. Geographic areas
  5. Commodities
  6. Materials information
  7. Alteration
  8. Host and associated rocks
  9. Nearby scientific data
  10. Geologic structures
  11. Ore body information
  12. Controls for ore emplacement
  13. Economic information about the deposit and operations
  14. Links to other databases
  15. Bibliographic references
  16. General comments
  17. Reporter information

Geologic information

Identification information

Deposit ID 10093894
MRDS ID W701771
Record type Site
Current site name Kochbulak Deposit

Geographic coordinates

Geographic coordinates: 70.50072, 40.99821 (WGS84)

Site location context

Political divisions (FIPS codes)

Tajikistan(country)

Geographic areas

Country
Tajikistan

Comments on the location information

  • WITHIN THE CHATKALA-KURAMINSK REGION.

Commodities

Commodity Importance
Gold Primary
Silver Secondary
Copper Secondary
Lead Secondary
Zinc Critical Secondary
Iron Secondary
Antimony Critical Secondary
Bismuth Critical Tertiary
Manganese Critical Tertiary
Tellurium Critical Tertiary

Materials information

Materials Type of material
Altaite Ore
Argentite Ore
Bismutite Ore
Bournonite Ore
Calaverite Ore
Chalcopyrite Ore
Galena Ore
Gold Ore
Hessite Ore
Huebnerite Ore
Jamesonite Ore
Marcasite Ore
Petzite Ore
Plagionite Ore
Pyrite Ore
Sphalerite Ore
Sylvanite Ore
Tennantite Ore
Tetradymite Ore
Tetrahedrite Ore
Barite Gangue
Calcite Gangue
Quartz Gangue
Sericite Gangue

Alteration

  • (Local) Silicification, Sericitization, Propylitization

Analytical data

Result GOLD PARTICLES RANGE FROM PREDOMINANTLY POWDERY TO .2 MM. FINENESS FROM 849-85. GOLD OCCURS AS DENDRITIC AND AMORPHOUS.

Host and associated rocks

  • Host or associated Associated
    Rock type Plutonic Rock > Mafic Intrusive Rock > Diorite
  • Host or associated Associated
    Rock type Volcanic Rock (Aphanitic) > Felsic Volcanic Rock > Dacite
  • Host or associated Host
    Rock type Volcanic Rock (Aphanitic) > Pyroclastic Rock > Volcanic Breccia (Agglomerate)
  • Host or associated Host
    Rock type Volcanic Rock (Aphanitic) > Felsic Volcanic Rock > Dacite
    Rock unit name Akcha Group
    Rock description Akcha Group

Nearby scientific data

(1) 70.50072, 40.99821

Economic information

Geologic structures

Type of structure Regional
Structure description Tyan'-Shan' Hercynian Fold System
Type of structure Local
Structure description Massif, Dikes, Autobreccia

Ore body information

  • Name FOURTH ZONE
    General form LENS
    Strike SUBLATITUDINAL}
    Dip 30-65 DEGREES NW}STEEPLY DIPPING JOINTS
    Thickness 10M
    Length 3000M
    Width 500M
  • Name LARGEST DISCORDANT ZONE
    General form LENS
    Strike SUBLATITUDINAL}
    Dip 30-65 DEGREES NW}STEEPLY DIPPING JOINTS
    Length 1000M

Controls for ore emplacement

  • Joints, Fractures, And Interformational Breaks

Comments on the geologic information

  • THE NEAR SURFACE DEPOSIT FORMED IN 2 STAGES. THE FIRST STAGE INCLUDES 3 PHASES 1) SILICIFICATION OF WALL ROCKS AND FORMATION OF SERICITE, CHLORITE, PYRITE, CARBONATE, AND ALBITE 2) GOLD-SULFIDE-QUARTZ; AND RESULTING HYPOGENE LEACHING OF HUEBNERITE 3) GOLD-SULFIDE-QUARTZ ASSOCIATED WITH PRECIPITATION OF MORE THAN 25 MINERAL SPECIES. THE SECOND STAGE INCLUDES THE FORMATION OF SULFIDE-BARITE, GALENA, CHALCOPYRITE AND QUARTZ-CARBONATE.

Economic information about the deposit and operations

Development status Occurrence
Commodity type Metallic
Deposit size Large
Significant No

Reference information

Bibliographic references

  • Deposit

    SMIRNOV, V.I., 1977, ORE DEPOSITS OF THE USSR, VIII, P. 18-19

General comments

Subject category Comment text
Deposit A SYSTEM OF BANDED TO COCKADE VEINS, VEINLETS, AND ZONES OF SILICIFICATION. ONE FRACTURE CONTROLLED MAJOR ORE ZONE, "THE FOURTH ZONE" (CONFORMABLE WITH STRATIFIED COUNTRY ROCKS) CONTAINS NINE ORE BODIES CONFINED TO JOINTS. THE LARGEST DISCORDANT ORE ZONE ( LOCATED IN THE WESTERN PART OF THE DEPOSIT) INCLUDES A SYSTEM OF STEEPLY DIPPING JOINTS FILLED WITH QUARTZ VEINS AND VEINLETS. STEEPLY DIPPING DISCORDANT BODIES ARE MORE ECONOMIC THAN THE GENTLY DIPPING DISCORDANT BODIES WHICH HAVE MORE COMPLICATED STRUCTURE AND UNEVENLY DISTRIBUTED GOLD.

Reporter information

Type Date Name Affiliation Comment
Reporter 01-JUL-1990 Paidakovich, Matthew E. U.S. Geological Survey
Updater 01-JUL-1993 Moyer, Lorre A. U.S. Geological Survey

Beyond USGS

Supplemental information added by qvyshift.com. Not part of the original USGS MRDS record.