Mesozonal orogenic gold deposit, related to the Linglong granite. The ore bodies are hosted in a second-order fault zone which strikes 30-60° NE and dips 50-80° SE. They are of disseminated, stockwork and quartz-vein-style, up to 3130 m long and up to 5 m wide.
References
- Chen Guangyuan, Sun Daisheng, Huang Shaofeng et al. (1995): Genetic mineralogy of Lingshangou gold deposit in Jiaodong region. China University of Geosciences Press (Wuhan), pp. 150 (in Chinese with English abstract).
- Yumin Qiu, Groves, D.I., McNaughton, N.J., Lianggen Wang, and Taihe Zhou (2002): Nature, age, and tectonic setting of granitoid-hosted, orogenic gold deposits of the Jiaodong Peninsula, eastern North China craton, China. Mineralium Deposita 37, 283-305.
- Yanjing Chen, Pirajno, F., and Jinping Qi (2005): Origin of Gold Metallogeny and Sources of Ore-Forming Fluids, Jiaodong Province, Eastern China. International Geology Review 47(5), 530-549.
Mineral List
12 entries listed. 9 valid minerals.
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