Location: | Guizhou [Kweichow], China, Asia |
Lat / long: | 24.98253, 105.74965 |
dep_id: | 10084947 |
mrds_id: | W700369 |
Commodity type: | metallic |
Major mineral: | Gold |
Operation type: | Unknown |
Production size: | No production occurred |
Development status: | Occurrence |
ore: | Chalcopyrite, Gold, Pyrite |
model: | 172: Carbonate-hosted Au-Ag |
alteration: | Silicification, Pyritization |
ore_ctrl: | Orebodies In Silicified And Pyritized Zone At Intersection Of Arkosic Shales And Northeast-Trending Faults |
Reporter: | Paidakovich, Matthew E. |
hrock_unit: | Xinyuan Formation |
hrock_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 |
References: |
- 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
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