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2021 Vol. 45, No. 6
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PANG Wen-Jing, CHEN Bei-Bei, ZHOU Tao, HUANG Rou-Rui, ZHOU Yun-Yun, GUO Fu-Sheng, WU Zhi-Chun, XIE Cai-Fu. 2021. A comparative study on polymetallic metallogenic characteristics of Xiangshan and Lengshuikeng ore fields. Geophysical and Geochemical Exploration, 45(6): 1416-1424. doi: 10.11720/wtyht.2021.0362
Citation: PANG Wen-Jing, CHEN Bei-Bei, ZHOU Tao, HUANG Rou-Rui, ZHOU Yun-Yun, GUO Fu-Sheng, WU Zhi-Chun, XIE Cai-Fu. 2021. A comparative study on polymetallic metallogenic characteristics of Xiangshan and Lengshuikeng ore fields. Geophysical and Geochemical Exploration, 45(6): 1416-1424. doi: 10.11720/wtyht.2021.0362

A comparative study on polymetallic metallogenic characteristics of Xiangshan and Lengshuikeng ore fields

  • More than 20 uranium deposits and polymetallic mineralization have been discovered in the Xiangshan ore field at present. However, breakthroughs in polymetallic prospecting are yet to be made in the ore field.This paper compared the Xiangshan ore field with the Lengshuikeng lead-zircon-silver polymetallic ore field at a high exploration level in terms of regional geological setting, strata, magmatic rocks, ore body characteristics, and wall-rock alteration. Based on this, it is found that the Xiangshan and Lengshuikeng ore fields are similar in geological conditions, the geochemical characteristics of rare earth elements (REEs) and trace elements, and the characteristics of ore bodies and alternation. Regarding lithology, both are mainly composed of volcanic rock series of the Cretaceous Ehuling and Daguding formations, which are present as high high-K calc-alkaline basalts and possess quasi-aluminous-weakly peraluminous characteristics. The REE-distribution patterns and trace element spider diagrams of the two ore fields are notably rightward, indicating the enrichment of light REEs, low content of Ba and Sr, and obvious Eu depletion. Therefore, the sediments in the two ore fields mainly originate from the crust. Meanwhile, the magmatic rocks feature a high crystallization differentiation degree, and the wall-rock alteration is dominated by chloritization, sericitization, silicification, and carbonation.By referring to the metallogenic model of the Lengshuikeng ore field, it is considered that the future polymetallic prospecting in the Xiangshan ore field should focus on the porphyry-type polymetallic ore in small rock masses and strata-bound, superimposed polymetallic ore at the K1d1 horizon. In this manner, breakthroughs are expected to be made in polymetallic prospecting in the Xiangshan ore field.
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  • [1] 聂江涛, 李子颖, 王健, 等. 江西相山矿田多金属成矿流体特征与成矿作用[J]. 地质通报, 2015, 34(2/3):535-547.

    Google Scholar

    [2] Nie J T, Li Z Y, Wang J, et al. Characteristics of polymetallic ore-forming fluid and metallogenesis of the Xiangshan ore field in Jiangxi[J]. Geological Bulletin of China, 2015, 34(2/3):535-547.

    Google Scholar

    [3] 杨庆坤, 黄强太, 罗勇, 等. 江西相山铀矿田深部铅锌矿成矿流体演化特征[J]. 科学技术与工程, 2017, 17(5):132-141.

    Google Scholar

    [4] Yang Q K, Huang Q T, Luo Y, et al. The characteristics of metallogenic fluid evolution of lead zinc polymetallic in Xiangshan ore field,Jiangxi Province[J]. Science Technology and Engineering, 2017, 17(5):132-141.

    Google Scholar

    [5] 王健, 聂江涛, 郭建, 等. 江西相山矿田深部多金属矿化特征[J]. 地质与勘探, 2016, 52(1):47-59.

    Google Scholar

    [6] Wang J, Nie J T, Guo J, et al. Characteristics of deep polymetallic mineralization in the Xiangshan uranium ore field of Jiangxi Province[J]. Geology and Exploration, 2016, 52(1):47-59.

    Google Scholar

    [7] 肖茂章, 狄永军, 明小泉, 等. 冷水坑矿田层状富铅锌矿赋矿围岩——铁锰碳酸岩角砾岩物质来源及成因分析[J]. 中国地质, 2014, 41(2):589-601.

    Google Scholar

    [8] Xiao M Z, Di Y J, Ming X Q, et al. Material sources and genetic analysis of the iron-manganese carbonatite breccia host rock of the stratiform Pb-Zn-rich orebodies in the Lengshuikeng orefield[J]. Geology in China, 2014, 41(2):589-601.

    Google Scholar

    [9] 左力艳, 侯增谦, 宋玉财, 等. 冷水坑斑岩型银铅锌矿床成矿流体特征研究[J]. 地球学报, 2009, 30(5):616-626.

    Google Scholar

    [10] Zuo L Y, Hou Z Q, Song Y C, et al. A study of the ore-forming fuid in the Lengshuikeng Ag-Pb-Zn porphyry deposit[J]. Acta Geoscientica Sinica, 2009, 30(5):616-626.

    Google Scholar

    [11] 肖克炎, 邢树文, 丁建华, 等. 全国重要固体矿产重点成矿区带划分与资源潜力特征[J]. 地质学报, 2016, 90(7):1269-1280.

    Google Scholar

    [12] Xiao K Y, Xing S W, Ding J H, et al. Division of major mineralization belts of China's key solid mineral resources and their mineral resource potential[J]. Acta Geologica Sinica, 2016, 90(7):1269-1280.

    Google Scholar

    [13] 朱裕生, 肖克炎, 马玉波, 等. 中国成矿区带划分的历史与现状[J]. 地质学刊, 2013, 37(3):349-357.

    Google Scholar

    [14] Zhu Y S, Xiao K Y, Ma Y B, et al. Review and status of mineralization belt study in China[J]. Journal of Geology, 2013, 37(3):349-357.

    Google Scholar

    [15] 林锦荣, 胡志华, 王勇剑, 等. 相山铀矿田铀多金属成矿时代与成矿热历史[J]. 岩石学报, 2019, 35(9):2801-2816.

    Google Scholar

    [16] Lin J R, Hu Z H, Wang Y J, et al. Ore-forming age and thermal history of uranium-polymetallic mineralization in Xiangshan uranium orefield[J]. Acta Petrologica Sinica, 2019, 35(9):2801-2816.

    Google Scholar

    [17] 肖茂章, 漆光明. 江西冷水坑铅锌银矿田成矿系统与成矿模式[J]. 地质与勘探, 2014, 50(2):311-320.

    Google Scholar

    [18] Xiao M Z, Qi G M. The metallogenic system and metallogenic model of the Lengshuikeng Pb-Zn-Ag orefield, Jiangxi province[J]. Geology and Exploration, 2014, 50(2):311-320.

    Google Scholar

    [19] 孟祥金, 侯增谦, 董光裕, 等. 江西冷水坑斑岩型铅锌银矿床地质特征、热液蚀变与成矿时限[J]. 地质学报, 2009, 83(12):1951-1967.

    Google Scholar

    [20] eng X J, Hou Z Q, Dong G Y, et al. Geological characteristics and mineralization timing of the Lengshuikeng porphyry Pb-Zn-Ag deposit, Jiangxi Province[J]. Acta Geoscientica Sinica, 2009, 83(12):1951-1967.

    Google Scholar

    [21] 郭福生, 杨庆坤, 孟祥金, 等. 江西相山酸性火山—侵入杂岩体地球化学特征与岩石成因[J]. 地质学报, 2016, 90(4):769-784.

    Google Scholar

    [22] Guo F S, Yang Q K, Meng X J, et al. Geochemical characteristics and petrogenesis of the acidic volcan-intrusive complexes, Xiangshan, Jiangxi[J]. Acta Geoscientica Sinica, 2016, 90(4):769-784.

    Google Scholar

    [23] 张春茂. 江西省冷水坑银铅锌矿床矿石特征及成矿条件[D]. 成都:成都理工大学, 2013.

    Google Scholar

    [24] Zhang C M. Ore Characters and metallogenic conditions of the Lengshuikeng Ag-Pb-Zn deposit, Jiangxi Province[D]. Chengdu: Chengdu University of Technology, 2013.

    Google Scholar

    [25] 左利艳, 孟祥金, 杨竹森. 冷水坑斑岩型银铅锌矿床含矿岩系岩石地球化学及 Sr、Nd 同位素研究[J]. 矿床地质, 2008, 27(3):367-382.

    Google Scholar

    [26] Zuo L Y, Meng X J, Yang Z S. Petrochemistry and Sr, Nd isotopes of intrusive in Lengshuikeng porphyry type Ag-Pb-Zn deposit[J]. Mineral Deposits, 2008, 27(3):367-382.

    Google Scholar

    [27] 龚雪婧, 曾建辉, 曹殿华. 江西冷水坑矿床含矿花岗斑岩的Sr-Nd及锆石Hf-O同位素研究[J]. 中国地质, 2019, 46(4):818-831.

    Google Scholar

    [28] Gong X J, Zeng J H, Cao D H. Sr-Nd and zircon Hf-O isotopic constraints on the petrogenesis of the orebearing granitic porphyry at Lengshuikeng, Jiangxi Province[J]. Geology in China, 2019, 46(4):818-831.

    Google Scholar

    [29] 徐贻赣, 吴淦国, 王长明, 等. 江西冷水坑银铅锌矿田闪锌矿铷-锶测年及地质意义[J]. 地质学报, 2013, 87(5):621-633.

    Google Scholar

    [30] Xu Y G, Wu G G, Wang C M, et al. Rb-Sr dating of sphalerites from the Lengshuikeng Ag-Pb-Zn deposit, Jiangxi, and its geological significances[J]. Acta Geologica Sinica, 2013, 87(5):621-633.

    Google Scholar

    [31] 骆学全, 张雪辉, 徐贻赣, 等. 江西冷水坑银铅锌矿床层状矿体的成矿模式及深部勘查方向[J]. 地质与勘探, 2013, 49(6):1078-1087.

    Google Scholar

    [32] Luo X Q, Zhang X H, Xu Y G, et al. A metallogenic model for bedded orebodies in the Lengshuikeng Ag-Pb-Zn deposit, Jiangxi and deep exploration direction[J]. Geology and Exploration, 2013, 49(6):1078-1087.

    Google Scholar

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