2019
DOI: 10.1016/j.oregeorev.2019.102987
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Ore-forming fluids and ore genesis of the large Bayanbaolege Ag polymetallic deposit, Southern Great Xing’an Range, NE China

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Cited by 9 publications
(8 citation statements)
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“…Regional magmatism includes Hercynian plutons (321-250 Ma), including quartz diorite, tonalite, granodiorite, monzogranite, gabbro, quartz monzonite, biotite granite, and K-feldspar granite [11][12][13][14][15]. Indosinian granitoids (250-225 Ma) consist of two-mica granite, granite porphyry [16,17], and granodiorite porphyry and Yanshanian intrusions (182-125 Ma) [1,4,9,[16][17][18]. In addition, the W, Sn, Pb, Zn, Cu, and Ag deposits in the region are all closely related to Indosinian and Yanshanian granites, including granodiorite, quartz syenite, K-feldspar granite, hornblende monzonite, and monzogranite [2,6,14,16,19,20].…”
Section: Geological Settingmentioning
confidence: 99%
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“…Regional magmatism includes Hercynian plutons (321-250 Ma), including quartz diorite, tonalite, granodiorite, monzogranite, gabbro, quartz monzonite, biotite granite, and K-feldspar granite [11][12][13][14][15]. Indosinian granitoids (250-225 Ma) consist of two-mica granite, granite porphyry [16,17], and granodiorite porphyry and Yanshanian intrusions (182-125 Ma) [1,4,9,[16][17][18]. In addition, the W, Sn, Pb, Zn, Cu, and Ag deposits in the region are all closely related to Indosinian and Yanshanian granites, including granodiorite, quartz syenite, K-feldspar granite, hornblende monzonite, and monzogranite [2,6,14,16,19,20].…”
Section: Geological Settingmentioning
confidence: 99%
“…Two periods of magmatic activity have been identified in the ore district (Figures 2 and 3). The earlier period is represented by the granodiorite porphyry, which is spatial-temporal and genetically closely related to the polymetallic mineralization (Figure 4a,b) [4], and the latter is represented by diorite porphyrite (Figure 4c,d), which broke down the integrity of the ore body (Figure 4c).…”
Section: Deposit Geologymentioning
confidence: 99%
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