Abstract：Liba gold deposit in Lixian, Gansu Province, belonging to altered fracture zone type, is hosted in Devonian epi-metamorphic fine clastic rocks. The ore bodies are strictly controlled by faults. The ore-forming matters are derived mainly from deep strata. The ore-forming fluid is a mixture of meteoric water, metamorphic water and magmatic water. The Zhongchuan granite serves as the heating dynamics for metallization.
张印飞. 甘肃省礼县李坝金矿床地质特征及成因探讨[J]. 地质与资源, 2005, 14(4): 265-267,271.
ZHANG Yin-fei. DISCUSSION ON THE GEOLOGY AND GENESIS OF LIBA GOLD DEPOSIT IN LIXIAN, GANSU PROVINCE. GEOLOGY AND RESOURCES, 2005, 14(4): 265-267,271.
2005, Vol. 14 
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