The Tieluping deposit is controlled by the NE-trending Tieluping fault and hosted by plagioclase-amphibolite gneisses, amphibolites and biotite-plagioclase gneisses of the Taihua Supergroup. The ore bodies are associated with subsidiary, parallel fractures on the west side of the Tieluping fault, and hosted by strongly altered tectonic breccias.
Ref.:
- Sui Yinghui, Wang Haihua, Gao Xiuli et al. (2000): Ore fluid of the Tieluping silver deposit of Henan Province and its illustration of the tectonic model for collisional petrogenesis, metallogenesis and fluidization. Science in China, Series D (Earth Sciences), 43(s), 108-112．
- Yanjing Chen, Pirajno, F., and Yinghui Sui (2004): Isotope geochemistry of the Tieluping silver-lead deposit, Henan, China: A case study of orogenic silver-dominated deposits and related tectonic setting. Mineralium Deposita 39(5/6), 560-575.
- Yanjing Chen, Pirajno, F., and Yinghui Sui (2005): Geology and D-O-C Isotope Systematics of the Tieluping Silver Deposit, Henan, China: Implications for Ore Genesis. Acta Geologica Sinica 79(1), 106-119.
- Zhengyou Chen (2005): Geochemical characteristics of Tieluping silver deposit, Henan province. Mineral Resources and Geology 19(6), 715-722 (in Chinese with English abstract).
Mineral List:19 entries listed. 15 valid minerals.
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