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PubMed
Article by Tian L
Article by Sun F
Article by Wang L
Article by Liu J
Article by Wu Q
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1. ���ִ�ѧ�����ѧѧԺ, ���� 130061;
2. �й����ʵ�����������ʵ�������, ���� 110034
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Characteristics of fluid inclusions and genesis of Huanggoushan Pb-Zn deposit in Linjiang area, Jilin
TIAN Li-dan1, SUN Feng-yue1, WANG Li1, LIU Jin-long2, WU Qiong1
1. College of Earth Sciences, Jilin University, Changchun 130061, China;
2. Shenyang Center of Geological Survey, CGS, Shenyang 110034, China
Abstract: In order to determine the ore-forming fluid and metallogenic mechanism of the Huanggoushan Pb-Zn deposit in Linjiang area, the authors undertook petrography, micro-thermometry and C-H-O-S-Pb stable isotope analysis of fluid inclusions in lead-zinc ores from the main metallogenic stage(polymetallic sulfide stage). The results show that the inclusions are gas-liquid two-phrase belonging to NaCl-H2O system. The main metallogenic stage's fluid is characterized by medium temperature(209��~276��), medium salinity(1.98~16.34wt%) and low density(0.79~0.96 g/cm3).Themetallogenic pressure ranges approximately from 16.8 to 33.0 MPa with depth mainly in 1.68~3.30 km. The hydrogen and oxygen isotope analysis indicate that the ��18OH2O and ��D values are 3.3×10-3~9.9×10-3 and -115×10-3~-74.8×10-3. Combining with the ��18O-��13C diagram of carbon and oxygen isotopes, it can be concluded that the metallogenic fluids are mainly from mantle-derived fluids and may have mixed with the meteoric water. The ��34S values of sulfur isotopes range from 2.6×10-3 to 18.9×10-3, representing the enrichment of heavy sulfur. The 206Pb/204Pb, 207Pb/204Pb and 208Pb/204Pb ratios of lead isotopes vary from 15.43 to 15.57,15.25 to 15.33 and 34.88 to 35.07, respectively, indicating that the metallogenic materials were derived from Zhenzhumen Formation, but does not rule out the mixing of materials from deep source. Combining with the regional geology, the deposit belongs to mesothermal vein-type lead-zinc deposit formed in the subduction background of the Paleo-Pacific Plate to the North China Plate, and the metallogenic age is the Late Yanshanian.
Keywords: fluid inclusion   metallogenic fluid   metallogenic material   ore genesis   Huanggoushan Pb-Zn deposit   Linjiang area  
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DOI: 10.3969/j.issn.1004-5589.2017.03.017
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