Pataz Gold 54

Producer in La Libertad, Peru with commodities Gold, Silver, Copper, Lead, Zinc, Antimony
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. Economic information about the deposit and operations
  13. Mining district
  14. Ownership information
  15. Production statistics
  16. Links to other databases
  17. Bibliographic references
  18. General comments
  19. Reporter information

Geologic information

Identification information

Deposit ID 10068888
MRDS ID W002160
Record type Site
Current site name Pataz Gold 54
Alternate or previous names San Francisco Vein, San Cayetano Level,, Pataz Group of Claims. With Delirio, Costa, Azoral, Constancia Veins, San Francisco Mine.

Geographic coordinates

Geographic coordinates: -77.59976, -7.77582 (WGS84)
Relative position THE PATAZ REGION IS CENTERED AROUND THE TOWN OF PATAZ AT THE NORTHERN END OF THE PATAZ PROVINCE GOLD BELT. THE REGION IS ABOUT 6 KM AIRLINE AND 15 KM BY TRAIL NE OF CHAGUAL ON THE RIO MARANON WHERE THE ROAD TO PARCOY AND BULDIBUYO CROSSES THE RIVER.

Site location context

Political divisions (FIPS codes)

La Libertad(province)

Peru(country)

South America(continent)

Land(continent)

Geographic areas

Country State
Peru La Libertad

Comments on the location information

  • NO. 54 ON METALLOGENIC MAPS OF PERU, 1969; EAST FLANK OF MARANON VALLEY.

Commodities

Commodity Importance
Gold Primary
Silver Primary
Copper Tertiary
Lead Tertiary
Zinc Critical Tertiary
Antimony Critical Tertiary

Comments on the commodity information

  • GANGUE MINERALS ARE QUARTZ, PYRITE, ARSENOPYRITE, PYRRHOTITE

Materials information

Materials Type of material
Chalcopyrite Ore
Electrum Ore
Galena Ore
Gold Ore
Pyrite Ore
Pyrrhotite Ore
Sphalerite Ore
Stibnite Ore
Calcite Gangue
Chlorite Gangue
Limonite Gangue
Quartz Gangue
Sericite Gangue
Siderite Gangue

Alteration

  • (Local) Veins Have Well Developed Alteration Selvages Of Muscovite And Quartz.

Host and associated rocks

  • Host or associated Associated
    Rock type Volcanic Rock (Aphanitic) > Intermediate Volcanic Rock > Andesite
    Stratigraphic age (youngest) Pleistocene
  • Host or associated Host
    Rock type Plutonic Rock > Mafic Intrusive Rock > Diorite
    Stratigraphic age (youngest) Carboniferous
    Chronological age 321
    Dating method Ar-Ar
    Type of media Biotite
  • Host or associated Host
    Rock type Metamorphic Rock > Metasedimentary Rock > Quartzite
  • Host or associated Host
    Rock type Metamorphic Rock > Gneiss
  • Host or associated Host
    Rock type Sedimentary Rock > Clastic Sedimentary Rock > Shale
  • Host or associated Host
    Rock type Sedimentary Rock > Clastic Sedimentary Rock > Sandstone
  • Host or associated Host
    Rock type Sedimentary Rock > Carbonate > Limestone

Nearby scientific data

(1) -77.59976, -7.77582

Economic information

Geologic structures

Type of structure Regional
Structure description Pataz Town Is At The Western Edge Of A Large Body Of Granodiorite Or Diorite That Extends 10-12 Km. To The Northwest And 12-15 Km To The Southeast.

Ore body information

  • Name SAN FRANCISCO VEIN
    Strike N
    Dip 15-60E
    Plunge NE
    Thickness 0.18M
    Length 750M
    Width 450M
    Depth to bottom 300M

Comments on the geologic information

  • SAN FRANCISCO HILL, TO THE SW OF PATAZ IS REPORTED TO CONSIST IN PART OF METAMORPHIC ROCKS AT THE BASE, OVERLAIN BY 200 M OR SO OF BLACK TO BLUE SHALE AND SANDSTONE THAT DIP 10 DEG-45 DEG E. THE BULK OF THE HILL CONSISTS OF GRANODIORITE. PRE-MINERAL DIKES A METER OR SO WIDE CUT THE SEDIMENTARY ROCKS. IN CONTACT WITH GRANODIORITE, THE SHALE IS CONVERTED LOCALLY TO A SILICEOUS SLATE OR SCHIST.

Economic information about the deposit and operations

Development status Producer
Commodity type Metallic
Significant No
Discovery year 1675
Discoverer Worked During Colonial Period.
Year of first production 1924

Mining district

District name Pataz District

Ownership information

  • Type Operator
    Owner Northern Peru Mining And Smelting Co.
    First year 1924

Production statistics

  • Year 1942
    Period 1927 - 1942
    Material AU
    Accuracy Accurate
    Description Cp_Grade: ^16 - 31 G Au/T
    Importance Item Commodity Group Amount recovered Grade Recovery percentage
    Major Gold Gold 24g/mt

Comments on the production information

  • ORE AMOUNT BASED ON AVERAGE GOLD CONTENT OF 24 G/TON AU; DEPOSITS WORKED FROM LATE 1600'S TO 1800 ACTIVE DEVELOPED PRODUCER.

Comments on the reserve resource information

  • INSUFFICIENT DATA 3/74 TO MAKE ESTIMATE. METALLOGENIC MAPS OF PERU INDICATE A DEPOSIT CONTAINING BETWEEN 100,000 AND ONE MILLION TONS OF ORE. MILL HEADS AVERAGED 0.772 OUNCE (= 24 GRAMS) GOLD AND 1.741 OUNCES (= 54 GRAMS) SILVER PER TON (1930) AND THE LOWEST WAS 0.511 OUNCES (= 16 GRAMS) GOLD PER TON (1937).

Comments on the workings information

  • SAN FRANCISCO VEIN WAS DEVELOPED ON 16 LEVELS OR SUBLEVELS OVER A TOTAL HORIZONTAL DISTANCE OF ABOUT 750M THROUGH A VERTICAL INTERVAL OF MORE THAN 300M & DOWN THE DIP WITH A RAKE TO THE NE FOR MORE THAN 450M.

Comments on development

  • SOME PLACER MINING IN 1770; 1924-1928 CONCENTRATED BY FLOTATION, IN 1929 PUT IN 180 T/D CYANIDE PLANT, MINE USED CUT AND FILL STOPING

Reference information

Bibliographic references

General comments

Subject category Comment text
Deposit AVERAGE WIDTH 100 CM. THE VEINS ARE ZONES OF CRUSHED AND SHEETED ROCK REPLACED BY WHITE AND SMOKY QUARTZ WITH STREAKS, VEINLETS, AND DISSEMINATIONS OF SULFIDE MINERALS, MAINLY PYRITE (95%) AND ATTAIN A LENGTH OF MORE THAN 750 M AND VERTICAL EXTENTS IN EXCESS OF 300 M. THEIR THICKNESS RANGES FROM A FEW CENTIMETERS TO 200 CM AND AVERAGES PERHAPS 60-80 CM. GOLD OCCURS FREE IN QUARTZ AND PYRITE AND IS REPORTED TO BE ASSOCIATED WITH BOTH CHALCOPYRITE AND ARSENOPYRITE ALTHOUGH IT IS NOT FOUND AS INCLUSIONS IN CHALCOPYRITE. THE VEINS SEEM TO BE MOST PRODUCTIVE IN SHALE... THE PRINCIPAL VEIN OF THE PATAZ REGION IS THE SAN FRANCISCO, THE ONLY VEIN WORKED ON A LARGE SCALE IN THE PERIOD 1924-1942. THE VEIN STRIKES NORTH, DIPS 15-60 DEG E (AVERAGE 35 DEG). WIDTH RANGED FROM 25 TO 180CM & AVERAGED ABOUT 100CM. THE VEIN LIES APPROX. ALONG THE CONTACT BETWEEN GRANODIORITE & SHALE LOCALLY CONVERTED TO HORNFELS.
Deposit First Production Year: 1924-FIRST YEAR OF LARGE-SCALE MINING
Deposit Discovery Year: LATE 1600'S

Reporter information

Type Date Name Affiliation Comment
Reporter 01-DEC-1973 Shaffer, Glenn L. U.S. Geological Survey
Updater 01-DEC-1993 Page, Norman J. U.S. Geological Survey

Beyond USGS

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