Location: | Moore County, North Carolina, United States, North America |
Lat / long: | 35.50454, -79.43087 |
dep_id: | 10055252 |
mrds_id: | RE00539 |
Commodity type: | nonmetallic |
Major mineral: | Talc-Soapstone |
Minor mineral: | Mica |
Operation type: | Unknown |
Production size: | Medium ammount of material produced |
Development status: | Past Producer |
ore: | Pyrophyllite |
gangue: | Chloritoid, Quartz |
orebody_fm: | TABULAR AND LENSES |
work_type: | Surface/Underground |
model: | 154: Epithermal quartz-alunite Au |
alteration: | Pyrophyllite Appears To Be Controlled By A Fracture System That Predates The Last Movement On The Glendon Fault. |
conc_proc: | Extreme Leaching From High-Acid Hydrothermal Fluids. |
ore_ctrl: | Ne-Trending Fracture |
Reporter: | Klein, T.L. |
hrock_type: | Tuff |
arock_type: | Rhyolite |
Structure: | Deposit Deformed By The Glendon Fault. Regional Folds Ne-Trending, Overturned To The East (West-Dipping Limbs)., Overturned And Attenuated Fold From Reverse Faulting Along The Glendon Fault. |
yfp_ba: | < |
Year first produced: | 1903 |
yr_lst_prd: | 1990 |
dy_ba: | < |
disc_yr: | 1902 |
References: |
- Deposit:: STUCKEY, J.L., 1967, PYROPHYLLITE DEPOSITS IN NORTH CAROLINA: NORTH CAROLINA DEPARTMENT OF CONSERVATION AND DEVELOPMENT, DIVISION OF MINERAL RESOURCES BULLETIN 80
- Deposit:: KLEIN, T.L., SITE VISITS, 1980-1986
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