Comquimbo Mn Mines

Producer in Chile with commodity Manganese
Sections on this page
  1. Identification information
  2. Geographic coordinates
  3. Site location context
  4. Geographic areas
  5. Commodities
  6. Materials information
  7. Host and associated rocks
  8. Nearby scientific data
  9. Geologic structures
  10. Ore body information
  11. Controls for ore emplacement
  12. Economic information about the deposit and operations
  13. Mining district
  14. Production statistics
  15. Links to other databases
  16. Bibliographic references
  17. General comments
  18. Reporter information

Geologic information

Identification information

Deposit ID 10068744
MRDS ID W001985
Record type Site
Current site name Comquimbo Mn Mines

Geographic coordinates

Geographic coordinates: -70.99953, -29.99745 (WGS84)
Elevation 1000
Relative position ABOUT 35 KM NE., E., & SE. OF LA SERENA

Site location context

Political divisions (FIPS codes)

Chile(country)

South America(continent)

Land(continent)

Geographic areas

Country
Chile

Comments on the location information

  • COORDINATES INDICATE APPROXIMATE CENTER OF MN-PRODUCING AREA OF COQUINBO PROVINCE. NOTE - INCLUDES FOLLOWING MINES; LAT. S. AND LONG. W. IN DEGREES, MINUTES AND SECONDS: ARRAYANES, 29-48-30, 70-56-06; LEONCITO, 29-48-48, 71-01-48; ESCONDIDA, 29-50-42, 71-06-06; TALCUNA, 29-53-42, 70-55-42; ALTA, 29-54-06, 70-55-06; ROMERO, 29-55-54, 70-54; LA LIGA, 30-07, 70-57-30; ARRAYAN, 30-11-06, 70-56-18; PORVENIR, 30-14-30, 70-58-12; CORAL QUEMADO, 30-15, 70-56-54; FRAGUA, 30-20, 71-00-12

Commodities

Commodity Importance
Manganese Critical Primary

Materials information

Materials Type of material
Braunite Ore
Hausmanite Ore
Manganite Ore
Psilomelane Ore
Pyrolusite Ore

Host and associated rocks

  • Host or associated Associated
    Rock type Plutonic Rock > Mafic Intrusive Rock > Diorite
    Rock unit name Andean Diorite Complex Intrusive
    Rock description Andean Diorite Complex Intrusive
    Stratigraphic age (youngest) Late Cretaceous
    Stratigraphic age (youngest) Early Cretaceous
  • Host or associated Host
    Rock type Sedimentary Rock > Clastic Sedimentary Rock
  • Host or associated Host
    Rock type Sedimentary Rock > Carbonate > Limestone
  • Host or associated Host
    Rock type Volcanic Rock (Aphanitic) > Intermediate Volcanic Rock > Andesite

Nearby scientific data

(1) -70.99953, -29.99745

Economic information

Geologic structures

Type of structure Regional
Structure description North-Trending Broad Open Folds, Faults Of Varying Lengths And Displacements, And Plutonic Masses
Type of structure Local
Structure description North-Trending Anticline And Adjacent Synclines To E And W

Ore body information

  • Thickness 3M

Controls for ore emplacement

  • Coarse Clastic Material And Andesitic Lava Flows Were Deposited In A Shallow-Water Marine Environment. Evidence Indicates Mn Associated With Volcanic Activity. Accumulation Of Sediments And Lava Flows In Basin Left Isolated Shallow Troughs Of Mn-Saturated Water From Which Mn Minerals Were Ppecipitated

Comments on the geologic information

  • BOTH FMS CONSTITUTE A N-S TRENDING BELT 25 KM WIDE IN WEST-CENTRAL PART OF PROVINCE

Economic information about the deposit and operations

Development status Producer
Commodity type Metallic
Significant No
Year of first production 1884

Mining district

District name See Note In Location Comments.

Production statistics

  • Year 1963
    Period 1884 - 1963
    Material MN
    Accuracy Accurate
    Description Cp_Grade: ^46 %
    Importance Item Commodity Group Amount recovered Grade Recovery percentage
    Manganese Manganese 46wt-pct

Comments on the production information

  • 87% OF MN PRODUCTION COMES FROM COQUIMBO PROVINCE AGUIRRE 1964, REF.

Comments on the workings information

  • MANTOS STRIKE GENERALLY N. 10-40 DEG. W. DIPS VARY FROM SUBHORIZONTAL TO STEEP.

Comments on development

  • ECON.COM: GRADE OF LOWER CYCLE MN DEPOSITS IS 31-51%; MIDDLE CYCLE IS 45%

Reference information

Bibliographic references

General comments

Subject category Comment text
Deposit MN OCCURS IN 3 DIFFERENT STRATIGRAPHIC HORIZONS IN THE 2 FMS AND PROBABLY ACCUMULATED DURING 3 HETEROCHRONOUS EPISODES OF SEDIMENTATION REFERRED TO AS LOWER, MIDDLE AND UPPER DEPOSITIONAL CYCLES. DEPOSITION IN LOCAL TROUGHS THAT BECAME SEPARATED AND ISOLATED DETERMINED VARIATION IN THICKNESS OF MINERALIZED BEDS. ABSENCE OF MN-BEARING BEDS IN SAME STRATIGRAPHIC SEQUENCE OF DIFFERENT AREAS PROBABLY IS THE RESULT OF NON-DEPOSITION OR CHANNEL SCOURING

Reporter information

Type Date Name Affiliation Comment
Reporter 01-MAY-1973 Davidson, Claire B. U.S. Geological Survey

Beyond USGS

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