| Lat / long: | 24.98253, 105.74965 |
| Primary: | Gold |
| Ore: | Chalcopyrite, Gold, Pyrite |
| Operation type: | Unknown |
| Production size: | None |
| Development status: | Occurrence |
| Host rock: | Xinyuan Formation |
| Host type: | Shale |
| Structure: | At Southern End Of 30 Km-Long Lugong Anticline, Which Exposes Permian Rocks Along Crest; Axis Of Anticline Trends North-South, Approx. Parallel To Margin Of Yangtze Craton And To Strike Of Facies Changes, Large Northeast-Trending Reverse Faults Closely Related To Gold Distribution; Northwest-Trending Strike-Slip Faults Commonly Displace Northeast-Trending Faults |
| Tectonic: | Near Buried Southwestern Margin Of Precambrian Yangtze Craton |
| Alteration processes: | Silicification, Pyritization |
| MRDS | W700369 |
| DEP | 10084947 |
| 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. |