| Lat / long: | 24.93254, 105.64965 |
| Primary: | Gold |
| Ore: | Chalcopyrite, Gold, Marcasite, Pyrite, Realgar, Sphalerite, Stibnite |
| Gangue: | Ankerite, Quartz |
| Operation type: | Unknown |
| Production size: | None |
| Development status: | Occurrence |
| Host rock: | Xinyuan Formation |
| Host type: | Shale,Sandstone,Arkose,Limestone |
| Structure: | Gentle To Locally Moderately Tight Folds, Sometimes With High-Angle Faults, Trend Generally East-West, East-West Trending Anticline With Subsidiary Anticlines, Synclines, And East-West Trending Faults Subparallel To Trend Of Fold Axes |
| Tectonic: | Near Buried Southwestern Margin Of Precambrian Yangtze Craton |
| Alteration processes: | Intense Silicification, Minerals Predominantly Hydrothermal Illite And Kaolinite |
| MRDS | W700366 |
| DEP | 10084944 |
| Reference | CUNNINGHAM, C. G., ASHLEY, R. P., CHOU, I-M., HUANG, Z., WAN, C., AND LI, W., 1988, THE NEWLY DISCOVERED SEDIMENTARY-ROCK HOSTED DISSEMINATED GOLD DEPOSITS IN THE PEOPL* REPUBLIC OF CHINA: U. S. GEOLOGICAL SURVEY OPEN-FILE REPORT 88-220, 15 P |
| Reporter | Paidakovich, Matthew E. |