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The Luanling gold telluride deposit in the Xiong'ershan region is located in the southern margin of the North China Craton. The deposit formed in four stages, that is, an early pyrite-quartz stage (I), a pyritemolybdenite stage (II), a sulfide-telluride-gold stage (III), and a late carbonate stage (IV). Six species of telluride in stage (III) are recognized, including hessite, altaite, petzite, unidentified Au-Ag-Te mineral, empressite, and unidentified Ag-Te-S mineral. Gold occurs mostly as native gold and electrum along the microfractures of sulfides or the contact between sulfide and telluride. The mineralization temperature of stage I and stage III ranges from 296 to 377 C and 241 to 324 C, respectively. Tellurides in stage III precipitate at the logƒ S2 from −14.3 to −7.3 and logƒ Te2 from −17.4 to −9.4. The ores were formed in an oxidizing environment. The Re-Os model ages of molybdenite are 162-164 Ma, which indicate that the main ore formation stage was in the Late Jurassic. The Re contents of five molybdenite samples from the Luanling deposit have a range of 36.32-81.95 ppm, except for one large value of 220 ppm, which indicates that the ore-forming materials are mainly derived from a crustal-dominated source. The δ 34 S values of sulfides range from −17.6 to −6.2‰, whereas those of sulfates are from 6.8 to 11.5‰. The δ 34 S ΣS value of the ore-forming system is 0.0-3.7‰, indicating that the sulfur of the Luanling deposit derived from a deep igneous source. Mineral association and isotope data of the Luanling deposit, together with its geodynamic setting, imply that this deposit belongs to a part of the metallogenic system of the Nannihu-Sandaozhuang, Shangfangou porphyry molybdenum deposits, and the Late Jurassic granitic intrusions.

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