2020 Vol. 26, No. 3

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Chief Editor’s Address
2020, 26(3): .
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Cover Page
2020, 26(3): .
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Inside Cover
2020, 26(3): 封三-封三.
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Contents
2020, 26(3): .
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Inside Cover
2020, 26(3): 封二-封二.
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Development process of fault structure and formation and evolution of ore-controlling structure: A case study of the Zoujiashan uranium deposit
CHEN Bailin
2020, 26(3): 285-298. doi: 10.12090/j.issn.1006-6616.2020.26.03.027
Abstract (729) HTML (517) PDF (29998KB)(79)
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Hydrothermal lode deposit is mainly controlled by fault structure. The ore-bearing or ore-hosting structures controlling the emplacement of ore-body and ore vein are often minor second-order faults or fractures,while the major faults are generally considered as passage-ways for ore fluids; however,t...
Ore-forming fluid fracturing treatment of ore-bearing fractures and the characteristics of the related veins in porphyry deposits
ZHAO Maochun, WU Baoqian, YU Haijun, HE Yun, TANG Qiong, YANG Jinsong, LI Jiacheng, ZHANG Sishan, WANG Guanglong
2020, 26(3): 299-315. doi: 10.12090/j.issn.1006-6616.2020.26.03.028
Abstract (619) HTML (173) PDF (19747KB)(38)
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Veins in porphyry deposits are well developed and their crosscutting relationship is complex. The initial fractures,where the veins fill in,are connected in varying degrees. Mineralization is a process of migration,filling and precipitation of ore-bearing fluid in the existing fractures. During the ...
Physical simulation analysis of the Cenozoic fault activities and structural deformation mechanism of the Youjiang area
NIE Guanjun, YU Hongmei, HE Sheng, LI Bingsu, PAN Lili
2020, 26(3): 316-328. doi: 10.12090/j.issn.1006-6616.2020.26.03.029
Abstract (551) HTML (180) PDF (37295KB)(67)
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The NW-trending faults in the Youjiang area originated from synsedimentary faults developed in the Youjiang Basin of Late Paleozoic. In Cenozoic these equidistantly spaced faults have undergone multiple left-lateral strike-slip activities,which then led to a simple-shear deformation of the Youjiang ...
Characteristics of ore-controlling structures and ore-prospecting of the Xitieshan lead-zinc deposit, northern edge of the Qaidam basin, NW China
FENG Zhixing, CHEN Zhengle, LI Zhengming, ZHAN Weilu, SHI Yonghong, CHEN Bailin, JIANG Wan, LIU Bo, LI Jilin, TAN Renwen
2020, 26(3): 329-344. doi: 10.12090/j.issn.1006-6616.2020.26.03.030
Abstract (516) HTML (121) PDF (48836KB)(51)
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The Xitieshan deposit,one of the large-size lead-zinc deposits located at the northern edge of the Qaidam basin in western China,is related to marine Volcanic-Sedimentary Hosted Massive Sulfur deposit (VSHMS). Most prior researches are focused on the mineralization age,the nature of ore-forming flui...
Structural analysis and ore-controlling model of the Xiaohe lead-zinc deposit in ore-concentrated area, northeastern Yunnan, China
ZHAO Dong, HAN Runsheng, WANG Jiasheng, ZHANG Xiaopei, CUI Junhao, LI Ziteng
2020, 26(3): 345-362. doi: 10.12090/j.issn.1006-6616.2020.26.03.031
Abstract (483) HTML (100) PDF (51394KB)(54)
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The Xiaohe lead-zinc deposit is one of the few typical lead-zinc deposits controlled by NW-trending major faults in the ore-concentrated area in northeastern Yunnan,China. The spatial distribution of mineralization and alteration is strictly controlled by structures. In order to ascertain the charac...
Analysis of ore-controlling structure in the Changgou gold deposit of the northern Hanyin gold orefield, southern Qinling Mountains
ZHANG Kang, YANG Xingke, YU Hengbin, GUO Runping, WANG Jiawei
2020, 26(3): 363-375. doi: 10.12090/j.issn.1006-6616.2020.26.03.032
Abstract (530) HTML (122) PDF (40991KB)(58)
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The ore-bearing rock series in the northern Hanyin gold orefield of the southern Qinling mountains mainly consists of the shallow metamorphic rocks in the Silurian Meiziya formation,which underwent complex tectonic deformation in Mesozoic,and the brittle-ductile shear zone is a good place for the en...
Model of tectonite-lithofacies zoning in ore-controlling faults of the Qingshan lead-zinc deposit in northwestern Guizhou
SONG Danhui, HAN Runsheng, WANG Mingzhi, ZHANG Yan, ZHOU Wei
2020, 26(3): 376-390. doi: 10.12090/j.issn.1006-6616.2020.26.03.033
Abstract (334) HTML (99) PDF (40580KB)(50)
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The Qingshan lead-zinc deposit is one of the typical deposits in the Weining-Shuicheng metallogenic subzone in the northwestern Guizhou ore concentration area, and orebodies are strictly controlled by both tectonic and lithologic factors. The tectonites in the ore-bearing fault zone with remarkable ...
Ore-controlling rules of fault structures in the Wangjiaping gold deposit in Shanyang County, Shaanxi Province
XUE Yushan, WANG Ruiting, WANG Chao, MEN Wenhui, LIU Xinwei, HU Xishun, NING Jiangchao, GU Yuming, SONG Shuguang
2020, 26(3): 391-404. doi: 10.12090/j.issn.1006-6616.2020.26.03.034
Abstract (911) HTML (326) PDF (21976KB)(37)
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The Wangjiaping gold deposit in Shanyang County, Shaanxi province, is a newly discovered carlin-type gold deposit in the southern Qinling orogeny, characterized by obvious ore-controlling structure and developed mineralization and alteration. The mining area is located in the north wing of the Longt...
Model of rock and ore controlling structures in the Baoshan Cu-Pb-Zn polymetallic deposit, southern Hunan province, China
CHEN Pengyuan, WU Peng, HAN Runsheng, ZHOU Mengxiang, LI Maoping, ZHAO Dong, JIANG Longyan
2020, 26(3): 405-418. doi: 10.12090/j.issn.1006-6616.2020.26.03.035
Abstract (522) HTML (150) PDF (24581KB)(50)
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The Baoshan Cu-Pb-Zn polymetallic deposit, located in the overlapped part of the Nanling EW-trending tectonic belt and the Leiyang-Linwu SN-trending tectonic belt, is a typical large and super-large mineral deposit in this area. The deposit and ore-bodies are spatially closely related to the early Y...
Element association anomaly of tectonites and prediction of concealed deposit in the Xiaozhuqing exploration area on the periphery of Huize lead-zinc mine area, northeastern Yunnan Province
GONG Hongsheng, HAN Runsheng, LI Ziteng, REN Tao, LI Wenyao, WANG Jiasheng, CHEN Gang
2020, 26(3): 419-431. doi: 10.12090/j.issn.1006-6616.2020.26.03.036
Abstract (541) HTML (237) PDF (20755KB)(33)
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The Huize super-large Ge-rich Pb-Zn deposit in Yunnan is located on the southwestern margin of the Yangtze block and east of the Xiaojiang deep fault in Sichuan-Yunnan-Guizhou lead-zinc metallogenic areas, and it is controlled by the NE-trending thrust-fold structures. Although the Huize Pb-Zn depos...
Methods of ASTER remote sensing data used in extracting mineralization and alteration information in the Hutouya mining area of the Qimantag metallogenic belt, Qinghai Province
CHENG Sanyou, YANG Xingke, YU Hengbin, LIU Wei
2020, 26(3): 432-442. doi: 10.12090/j.issn.1006-6616.2020.26.03.037
Abstract (882) HTML (208) PDF (29185KB)(62)
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Using ASTER remote sensing images as the data source, the extraction of mineralization and alteration anomaly in the Hutouya mining area of the Qimantag metallogenic belt in Qinghai Province is studied through two methods. One method is using the minimum noise component (MNF) transform, pixel purity...
Geochemical characteristics of gold-bearing minerals and its geological significance in the Ashawayi gold deposit in the southwestern Tianshan Orogen
ZHANG Tao, CHEN Zhengle, HUANG Hongye, ZHANG Wengao, ZHANG Qing, PAN Jiayong, ZHOU Zhenju, ZOU Mingliang, FENG Hongye, WANG Xiaohu, HAN Fengbin, SUN Yue, HUO Hailong, MA Ji, YANG Bin
2020, 26(3): 443-458. doi: 10.12090/j.issn.1006-6616.2020.26.03.038
Abstract (600) HTML (157) PDF (35957KB)(54)
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Ashawayi gold deposit, the second largest gold deposit in the southwestern Tianshan Orogen, NW China, is located at the southern margin of the Central Asian Orogenic Belt of the "Asian Golden Belt". Detailed field observations showed that the regional area experienced two tectonic processes from ear...