Lopari-Sibosnica

Occurrence in Bosnia and Herzegovina with commodity Boron-Borates
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. Mining district
  11. Links to other databases
  12. Bibliographic references
  13. General comments
  14. Reporter information

Geologic information

Identification information

Deposit ID 10055368
MRDS ID RL10038
Record type Site
Current site name Lopari-Sibosnica
Alternate or previous names Lopare, Sibosica

Geographic coordinates

Geographic coordinates: 18.84472, 44.63649 (WGS84)

Site location context

Political divisions (FIPS codes)

Bosnia and Herzegovina(country)

Geographic areas

Country
Bosnia and Herzegovina

Comments on the location information

  • LOCATION IS UNCERTAIN, LAT-LONG IS FOR THE TOWN OF LOPARE.
  • EAST OF BARSTOW (WITHIN TERTIARY BARSTOW BASIN).

Commodities

Commodity Importance
Boron-Borates Primary

Comments on the commodity information

  • SUBTYPE: BORIC ACID

Materials information

Materials Type of material
Searlesite Ore

Host and associated rocks

  • Host or associated Associated
    Rock type Sedimentary Rock > Clastic Sedimentary Rock > Sandstone
    Stratigraphic age (youngest) Miocene
  • Host or associated Associated
    Rock type Volcanic Rock (Aphanitic) > Pyroclastic Rock > Tuff
  • Host or associated Host
    Rock type Sedimentary Rock > Clastic Sedimentary Rock > Shale

Nearby scientific data

(1) 18.84472, 44.63649

Economic information

Comments on the geologic information

  • BORATES OCCUR WITHIN GREEN-GREY SHALES INTERBEDDED WITH YELLOW-TAN LIMESTONES. THERMAL SPRING ACTIVITY ASSOCIATED WITH NUMEROUS FAULTS IN THE AREA PROVIDED SOURCE OF BORON. BORATES DEPOSITED CYCLIC SEQUENCE IN SHALLOW-DEEP LACUSTRINE ENVIRONMENTS (PLAYA) COVERED POSSIBLY AN AREA OF 15 KM X 100-150 KM. THE BARSTOW-BRISTOL VOLCANIC-TECTONIC TROUGH PROBABLY DEVELOPED AS A BROAD SYNCLINAL DOWNWARP. POST DEPOSITIONAL FAULTING UPLIFTED AND FOLDED B-BEARING SEQUENCE INTO 'TIGHT FOLDS'. B-BEARING BEDS GENERALLY OCCUR IN THE NE LIMB OF THE BARSTOW SYNCLINE. VOLCANIC AGGLOMERATE OVERLY THE BARSTOW FM.

Economic information about the deposit and operations

Development status Occurrence
Commodity type Non-metallic
Deposit size Small
Significant No

Mining district

District name Balkans

Comments on the production information

  • REGION VALUED AS AN ESTIMATE $9 MILL COLEMANITE.

Comments on the workings information

  • SEVERAL OPERATING MINES ON AREA; B-SHALE MINED FOR BORIC ACID; SMALL SCALE PLANT EST. IN EARLY 1900'S INCLUDING 122 M INCLINED SHAFT.

Comments on development

  • LEADING BORATE DEPOSIT IN US IN 1907; OLD BORATE MINE FIRST MAJOR MINE IN AREA.

Reference information

Bibliographic references

  • Deposit

    LYDAY, P.A., 1992, HISTORY OF BORON PRODUCTION AND PROCESSING: INDUSTRIAL MINERALS, NO. 303, P. 19-37

General comments

Subject category Comment text
Deposit ELLIPSOIDAL LUMPS OF SEARLESITE OCCUR IN SHALE-MARLS INTERBEDDED WITH TUFF AND TUFFACEOUS SANDSTONE.
Deposit FIVE BORATEEDS EXPOSED AT SURFACE 0.6-4.6 M THICK. PODS OF BORATES (10-20 CM) OCCUR BELOW B HORIZONS IN B-RICH SHALES/LST. NUMEROUS DEPOSITS MINED IN AREA INCLUDING THE CENTINIAL MINE, OLD BORATE MINE (LARGEST MINE IN US TILL 1907).

Reporter information

Type Date Name Affiliation Comment
Reporter 01-SEP-1993 Langford, R.P. BHP Utah Industries

Beyond USGS

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