| Lat / long: | 30.95852, -102.65878 |
| Primary: | Zinc, Lead |
| Ore: | Galena |
| Gangue: | Calcite, Dolomite, Pyrite |
| Discovery year: | 1949 |
| Operation type: | Unknown |
| Deposit type: | Stratabound |
| Production size: | None |
| Development status: | Occurrence |
| Host type: | Dolomite |
| Associated type: | Shale,Limestone |
| Structure: | Paleoshelf Edge, Reef Complex |
| Tectonic: | Interior Basin |
| Alteration processes: | Dolomite Replaces Lower Leonardian Shelf-Margin Reef And Bio-Grainstones. Perhaps An Early (Shallow Burial) Phase Of Fine-To-Medium Crystalline Dolomite And A Late, But Pre-Mineral, (Deep Burial) Phase Of Coarse Crystalline Dolomite And Formation Of Secondary Porosity. A Late (Pre, Syn, And Post Mineral) Phase Of Dolomite And Calcite Cement. |
| MRDS | TC40067 |
| DEP | 10065070 |
| Reference | {Deposit:: MAZULLO, S.J., 1986, MISSISSIPPI VALLEY-TYPE SULFIDES IN LOWER PERMIAN DOLOMITES, DELAWARE BASIN, TEXAS: IMPLICATIONS FOR BASIN EVOLUTION: AAPG BULLETIN, V. 70, P. 943-952}{Other Database:: CIMRI} |
| Reporter | Long, Keith R. |