Saidu Wali Deposits

Occurrence in Pakistan with commodity Gypsum-Anhydrite
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. Ore body information
  10. Economic information about the deposit and operations
  11. Links to other databases
  12. Bibliographic references
  13. General comments
  14. Reporter information

Geologic information

Identification information

Deposit ID 10023309
MRDS ID I000161
Record type Site
Current site name Saidu Wali Deposits

Geographic coordinates

Geographic coordinates: 71.83394, 32.08203 (WGS84)
Location accuracy 10000(meters)

Site location context

Political divisions (FIPS codes)

Pakistan(country)

Asia(continent)

Land(continent)

Geographic areas

Country
Pakistan

Comments on the location information

  • DEPOSIT IS IN THE DERA GHAZI KHAN HILLS WHICH ARE PART OF THE SULAIMAN RANGES.

Commodities

Commodity Importance
Gypsum-Anhydrite Primary

Materials information

Materials Type of material
Gypsum Ore

Host and associated rocks

  • Host or associated Host
    Rock type Sedimentary Rock > Chemical Sediment > Evaporite

Nearby scientific data

(1) 71.83394, 32.08203

Economic information

Ore body information

  • Thickness 7.62M

Economic information about the deposit and operations

Development status Occurrence
Commodity type Non-metallic
Significant No

Comments on the reserve resource information

  • ESTIMATE OF RESERVES IS A MINIMUM.

Reference information

General comments

Subject category Comment text
Deposit THICK LAYERS OF GYPSUM ARE UP TO 25 FT THICK AND SEVERAL MILES LONG. THESE DEPOSITS ARE PART OF A 45 TO 500 FT THICK GYPSUM-BEARING SEDIMENTARY SEQUENCE. THE DEPOSITS ARE SAID TO BE "HIGH-GRADE".

Reporter information

Type Date Name Affiliation Comment
Reporter 01-FEB-90 Orris, Greta J. U.S. Geological Survey

Beyond USGS

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