Corrego Baixio

Past Producer in Minas Gerais, Brazil with commodity Mica
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. Economic information about the deposit and operations
  10. Links to other databases
  11. Bibliographic references
  12. General comments
  13. Reporter information

Geologic information

Identification information

Deposit ID 10099601
MRDS ID TC42510
Record type Site
Current site name Corrego Baixio
Alternate or previous names Baixio

Geographic coordinates

Geographic coordinates: -40.72279, -18.56585 (WGS84)
Location accuracy 10000(meters)

Site location context

Political divisions (FIPS codes)

Minas Gerais(province)

Brazil(country)

South America(continent)

Land(continent)

Geographic areas

Country State
Brazil Minas Gerais

Comments on the location information

  • PLACERS ARE ON THE EAST FLANK OF THE LOST BASIN RANGE.

Commodities

Commodity Importance
Mica Primary

Materials information

Materials Type of material
Muscovite Ore

Host and associated rocks

  • Host or associated Host
    Rock type Plutonic Rock > Pegmatite
    Stratigraphic age (youngest) Neoproterozoic

Nearby scientific data

(1) -40.72279, -18.56585

Economic information

Economic information about the deposit and operations

Development status Past Producer
Commodity type Non-metallic
Significant No

Comments on the workings information

  • DEPOSIT WORKED BY DRY WASHING, POWER SHOVELS.

Reference information

Bibliographic references

  • Deposit

    PECORA, W.T., KLEPPER, M.R., LARRABEE, D.M., BARBOSA, A.L.M., AND FRAYHA, RESK, 1950, MICA DEPOSITS IN MINAS GERAIS, BRAZIL: U.S. GEOLOGICAL SURVEY BULLETIN 964-C, P. 205-305

  • Other Database

    CIMRI

General comments

Subject category Comment text
Deposit AU-BEARING GRAVELS WERE LESS THAN 2 FT THICK AND RESTED ON CEMENTED GRAVELS. NUGGETS WERE COMMONLY UP TO 0.75 OZ IN SIZE; ONE WAS REPORTED TO BE 4 OZS IN SIZE. THE SOURCE OF THE GOLD IS BELIEVED TO BE AU-QUARTZ-CARBONATE-SULFIDE VEINS IN PRECAMBRIAN ROCKS. GOLD IS RELATIVELY COARSE.

Reporter information

Type Date Name Affiliation Comment
Reporter 01-DEC-1994 Page, Norman J. U.S. Geological Survey

Beyond USGS

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