GEOLOGICAL CHARACTERISTICS AND METALLOGENIC AGE OF THE LARGE SILVER-LEAD-ZINC DEPOSIT IN HALASHENG OF MANZHOULI AREA, INNER MONGOLIA
WANG Jing-xin1, XU Jia2, YU He3, SHU Guang-long2, FENG De-sheng4, SHI Jian-min2, SUN Zhen-jiang4
1. College of Earth Sciences, Guilin University of Technology, Guilin 541004, Guangxi Autonomous Region, China; 2. Shenyang Center of Geological Survey, CGS, Shenyang 110034, China; 3. Hezhou College, Hezhou 542899, Guangxi Autonomous Region, China; 4. No. 706 Team of Heilongjiang Geological Survey for Nonferrous Metals, Qiqihar 161031, Heilongjiang Province, China
Abstract:This Ag-Pb-Zn deposit is occurred in the Halasheng volcanic dome, with mineralization closely related to volcano-magmatism. The drilling and high-precision magnetic data show that the volcanic basement is the Ergunahe Formation, with subvolcanic body as the core of the dome and the volcanic-sedimentary cap rocks of Tamulangou and Manketouebo formations as ore-host rocks. The delineated 11 orebodies in the northeast of the dome are controlled by the N-S-trending extensional fault/fracture with steep occurrence. The four main orebodies are 500-1400 m long with an average thickness of 1-3 m and general depths of 500-900 m. The geochemical anomaly element assemblages from the rock body to surrounding rocks are in the order of Bi(-Pb-Ag-As-Mo)→Ag-Pb-Mo-Cu→Pb-Zn-As→Ag-Pb-Zn-Sb→Ag-Pb-Zn-Sb. The mineralized element associations are Cu (-Mo-Pb-Zn)→Pb-Zn-Ag→Pb-Ag in sequence. The wallrock alterations from inside to outside of the rock body are silicification→potash feldspathization→quartz sericitization→skarnization→chalcedonization→epidotization→chloritization→ carbonation successively. The zircon U-Pb isotopic age of 3 magmatic rock samples is 161-142 Ma. Combined with the research of regional typical deposits, it is believed that the diagenesis and mineralization occurred in Late Jurassic to Early Cretaceous with a metallogenic age of 142 Ma.
王景昕, 胥嘉, 余何, 舒广龙, 冯德胜, 时建民, 孙振江. 内蒙古满洲里地区哈拉胜大型银铅锌矿床地质特征及成矿时代[J]. 地质与资源, 2019, 28(1): 18-24,97.
WANG Jing-xin, XU Jia, YU He, SHU Guang-long, FENG De-sheng, SHI Jian-min, SUN Zhen-jiang. GEOLOGICAL CHARACTERISTICS AND METALLOGENIC AGE OF THE LARGE SILVER-LEAD-ZINC DEPOSIT IN HALASHENG OF MANZHOULI AREA, INNER MONGOLIA. GEOLOGY AND RESOURCES, 2019, 28(1): 18-24,97.
Li T G, Wu G, Liu J, et al. Geochronology, fluid inclusions and isotopic characteristics of the Jiawula Pb-Zn-Ag deposit, Inner Mongolia, China[J]. Journal of Asian Earth Scionce, 2015,103:305-320.
Wu G, Chen Y C, Chen Y J, et al. Zircon U-Pb ages of the metamorphic supracrustal rocks of the Xinghuadukou Group and granitc complexes in the Argun massif of the northern Great Hinggan Range, NE China, and their tectonic implications[J]. Journal of Asian Earth Sciences, 2012,49:214-233.
Wu G, Sen F Y, Zhao C S, et al. Discovery of the Early Paleozonic post-collisional granites in the northern margin of the Erguna massif and its geological significance[J]. Chinese Science Bulletin,2005,50(23):2733-2743.
HU Shao-kang, YAN Hong-quan, YE Mao, et al. Metallogenic focus-area and superlarge mineral deposits in bordering zones between China, Russia and Mongolia[J]. Science China:Series D (Earth Sciences),1998(s1):28-36.
WANG Fei, ZHOU Xin-hua, ZHANG Lian-chang, et al. late Mesozonic volcanism in the Great Xing'an Range (NE China):Timing and implications for the dynamic setting of NE Asia[J]. Earth and Planeary Science Letters, 2006,251(4):179-198.