Volume 32 Issue 5
Oct.  2026
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ZHOU S G,LONG T,JIANG S,et al.,2026. Research and application of a prospecting model for sedimentary manganese deposits in the Xialei–Longbang area, southwestern Guangxi[J]. Journal of Geomechanics,32(5):1265−1283 doi: 10.12090/j.issn.1006-6616.2026087
Citation: ZHOU S G,LONG T,JIANG S,et al.,2026. Research and application of a prospecting model for sedimentary manganese deposits in the Xialei–Longbang area, southwestern Guangxi[J]. Journal of Geomechanics,32(5):1265−1283 doi: 10.12090/j.issn.1006-6616.2026087

Research and application of a prospecting model for sedimentary manganese deposits in the Xialei–Longbang area, southwestern Guangxi

doi: 10.12090/j.issn.1006-6616.2026087
Funds:  This research was financially supported by the National Key Research and Development Program of China (Grant No. 2022YFC2903404), the Geological Comprehensive Research Project of China Metallurgical Geology Bureau (Grant No. [2023]CMGBDZYJ003), the National Routine Mineral Prospectivity Zoning (Grant No. DD2026021102), and the Guangxi Special Support Program for Talent Cultivation for the Marine-Oriented Economy (Grant No. 2025XHRC12).
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  • Author Bio:

    周尚国,正高级工程师。2025年荣获第十九次李四光地质科学奖野外奖。现任中国冶金地质总局首席专家,并担任自然资源部新一轮找矿突破战略行动专家指导组成员。深耕我国黑色金属找矿预测与勘查示范工作40余年,为实现国家找矿目标提供了关键支撑。作为计划项目负责人,部署开展全国锰矿勘查评价工作,解决了若干关键科学问题,有力推动了锰、铁、铜等重要矿产的找矿突破。主持了全国危机矿山专项首批试点“大冶铁矿深部勘查项目”,提出“多台阶”成矿新认识,实现了找矿突破,助力老矿山焕发新生机;针对“东平式”三叠系锰矿开展专项研究与勘查,推动该类型锰矿实现规模化开发与利用,填补了相关产业应用空白。出版专著5部,建立并提升了黑色金属的成矿理论与勘查技术体系;发表SCI/EI论文20篇;荣获省部级特等奖1项、一等奖4项、二等奖5项、三等奖1项;享受国务院政府特殊津贴

  • Received: 2026-07-03
  • Revised: 2026-09-20
  • Accepted: 2026-09-20
  • Available Online: 2026-09-22
  • Published: 2026-10-28
  •   Objective  The Xialei–Longbang area in southwestern Guangxi hosts a critical manganese ore concentration district in China. Current exploration is hindered by an incomplete understanding of the occurrence patterns of sedimentary manganese deposits and a lack of a sound basis for selecting effective exploration methods.  Methods  Based on an analysis of the metallogenic geological settings, this study compares the geological characteristics of typical deposits and the geochemical characteristics of manganese-bearing rock series, and evaluates the results of exploration tests using the multi-polarization magnetotelluric (MPMT) method in the ore concentration district.   Results  The study area can be divided into two secondary manganese-forming basins, namely the Xialei–Shangying Basin and the Longbang–Dizhou Basin. Three sedimentary microfacies types are identified in the Xialei–Shangying manganese-forming basin: calcareous siliceous rock, calcareous siliceous rock–siliceous limestone, and siliceous limestone–argillaceous banded limestone. Only the siliceous limestone–argillaceous banded limestone microfacies occurs in the Longbang–Dizhou manganese-forming basin. Among these microfacies, the calcareous siliceous rock microfacies is the most favorable for mineralization, followed by the calcareous siliceous rock–siliceous limestone microfacies, whereas the siliceous limestone–argillaceous banded limestone microfacies is the least favorable. Centers of manganese enrichment are distributed within a zone approximately 500–1000 m northwest of the Xialei–Lingma synsedimentary fault. The thickness and Mn grades of rhodochrosite ore beds vary considerably among different mining areas (segments). Outward from the Xialei Mining Area, the manganese ore beds gradually thin and their Mn grades decrease. Moreover, the thickness and Mn grade of ore beds II+III generally show positive correlations with those of ore bed I. The ore-forming fluids were dominated by submarine hydrothermal fluids, and the sedimentary metallogenic environment was weakly oxidizing to oxidizing. Compared with the overlying and underlying wall rocks, the manganese-bearing rock series are characterized by a combination of low resistivity and high magnetic susceptibility.   Conclusions  Based on these results, a comprehensive prospecting model for Devonian rhodochrosite deposits was established and validated through exploration tests in the Xialei–Longbang area. The model captures the key ore-controlling factors and prospecting criteria of sedimentary manganese deposits in the region.   Significance  The combination of MPMT and drilling is applicable to sedimentary manganese exploration in southwestern Guangxi and provides important guidance for deep and concealed ore prospecting.

     

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  • [1]
    BAU M, DULSKI P, 1999. Comparing yttrium and rare earths in hydrothermal fluids from the Mid-Atlantic Ridge: implications for Y and REE behaviour during near-vent mixing and for the Y/Ho ratio of Proterozoic seawater[J]. Chemical Geology, 155(1-2): 77-90. doi: 10.1016/S0009-2541(98)00142-9
    [2]
    BECKER R T, KÖNIGSHOF P, BRETT C E, 2016. Devonian climate, sea level and evolutionary events: an introduction[J]. Geological Society, London, Special Publications, 423(1): 1-10. doi: 10.1144/sp423.15
    [3]
    BOSTROM K, 1983. Hydrothermal processes at seafloor spreading centers: application of basalt-seawater experimental results[M]. New York: Plenum Press.
    [4]
    CALVERT S E, PEDERSEN T F, 1996. Sedimentary geochemistry of manganese; implications for the environment of formation of manganiferous black shales[J]. Economic Geology, 91(1): 36-47. doi: 10.2113/gsecongeo.91.1.36
    [5]
    CHANG H J, CHU X L, FENG L J, et al., 2009. Redox sensitive trace elements as paleoenvironments proxies[J]. Geological Review, 55(1): 91-99. (in Chinese with English abstract)
    [6]
    CHEN F G, PUFAHL P K, WANG Q F, et al, 2022. A new model for the genesis of Carboniferous Mn ores, Longtou deposit, South China block[J]. Economic Geology, 117(1): 107-125. doi: 10.5382/econgeo.4855
    [7]
    CHEN F G, WANG Q F, PUFAHL P K, et al., 2023. Carbonate-hosted manganese deposits and ocean anoxia[J]. Earth and Planetary Science Letters, 622: 118385. doi: 10.1016/j.epsl.2023.118385
    [8]
    CHEN H D, ZENG Y F, 1990. Nature and evolution of the Youjiang Basin[J]. Sedimentary Geology and Tethyan Geology(1): 28-37. (in Chinese)
    [9]
    CHEN J H, TIAN Y M, JIANG S, et al., 2026. Application of manganese metallogenic model and effective exploration methods in the prospecting process: a case study of the Xialei manganese deposit[J]. Acta Geologica Sinica, 100(2): 679-692. (in Chinese with English abstract)
    [10]
    CHEN X, TIAN Y M, GAO B L, et al., 2026. Biochemical mineralization of manganese in the Nanhua System[J]. Acta Geologica Sinica, 100(2): 484-509. (in Chinese with English abstract)
    [11]
    CONG Y, DONG Q J, XIAO K Y, et al., 2018. Characteristics and predicted potential of Mn resources in China[J]. Earth Science Frontiers, 25(3): 118-137. (in Chinese with English abstract)
    [12]
    DONG J H, LIU H, JIANG S, et al., 2025. Two-dimensional mineral exploration prediction based on random forest: a case study of sedimentary manganese deposit in Xialei-Tuhu area[J]. Mineral Deposits, 44(1): 143-158. (in Chinese with English abstract)
    [13]
    DONG Z G, ZHANG L C, WANG C L, et al., 2020. Progress and problems in understanding sedimentary manganese carbonate metallogenesis[J]. Mineral Deposits, 39(2): 237-255. (in Chinese with English abstract)
    [14]
    DONG Z G, PENG Z D, ROBBINS L J, et al., 2023. Episodic ventilation of euxinic bottom waters triggers the formation of black shale-hosted Mn carbonate deposits[J]. Geochimica et Cosmochimica Acta, 341: 132-149. doi: 10.1016/j.gca.2022.11.027
    [15]
    DONG Z G, ZHANG B L, ZHANG L C, et al., 2025. Unravelling the mechanisms underlying marine redox shifts during sedimentary manganese metallogenesis: insights from the Carboniferous Muhu deposit, China[J]. Mineralium Deposita, 60(7): 1367-1396. doi: 10.1007/s00126-024-01343-7
    [16]
    DU Y S, YU W C, ZHOU Q, et al., 2023. Discussion about the coupling relationship between the breakup of supercontinent and the large-scale manganese accumulation in China[J]. Journal of Palaeogeography (Chinese Edition), 25(6): 1211-1234. (in Chinese with English abstract)
    [17]
    FU Y, XU Z G, PEI H X, et al., 2014. Study on metallogenic regularity of manganese ore deposits in China[J]. Acta Geologica Sinica, 88(12): 2192-2207. (in Chinese with English abstract)
    [18]
    GAN L, YANG C C, WANG L, et al., 2026. Tectonic controls and redox dynamics: a comprehensive review of sedimentary manganese mineralization in the Devonian-Triassic Youjiang Basin, South China[J]. Earth-Science Reviews, 281: 105638. doi: 10.1016/j.earscirev.2026.105638
    [19]
    GUO N N, GAO Z F, JIA J L, et al., 2026. Geological and geochemical characteristics of the Xialei manganese deposit in Guangxi and their constraints on different manganese mineralization mechanisms[J]. Acta Geologica Sinica, 100(2): 537-552. (in Chinese with English abstract)
    [20]
    GUO X L, CAI W M, LU Y G, et al., 2026. Resource attributes, geological characteristics, and utilization of manganese metal[J]. Acta Geologica Sinica, 100(2): 633-656. (in Chinese with English abstract)
    [21]
    HE H X, XIAO J F, YANG H Y, et al., 2024. Redox conditions of Datangpo-type manganese ores constrained by statistical analysis of pyrite framboids and iron isotopes[J]. Sedimentary Geology, 463: 106606. doi: 10.1016/j.sedgeo.2024.106606
    [22]
    HEIN J R, SCHULZ M S, DUNHAM R E, et al., 2008. Diffuse flow hydrothermal manganese mineralization along the active Mariana and southern Izu-Bonin arc system, Western Pacific[J]. Journal of Geophysical Research: Solid Earth, 113(B8): B08S14. doi: 10.1029/2007jb005432
    [23]
    HOU Z L, XUE Y Z, HUANG J S, et al. , 1997. Manganese deposits around the Yangtze platform[M]. Beijing: Metallurgical Industry Press. (in Chinese)
    [24]
    HOUSE M R, 2002. Strength, timing, setting and cause of mid-Palaeozoic extinctions[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 181(1-3): 5-25. doi: 10.1016/S0031-0182(01)00471-0
    [25]
    HUANG Q, PI D H, JIANG S Y, et al, 2022. The dual role of microbes in the formation of the Malkantu manganese carbonate deposit, NW China: petrographic, geochemical, and experimental evidence[J]. Chemical Geology, 606: 120992. doi: 10.1016/j.chemgeo.2022.120992
    [26]
    JEWELL P W, STALLARD R F, 1991. Geochemistry and paleoceanographic setting of central Nevada bedded barites[J]. The Journal of Geology, 99(2): 151-170. doi: 10.1086/629482
    [27]
    JOACHIMSKI M M, OSTERTAG-HENNING C, PANCOST R D, et al., 2001. Water column anoxia, enhanced productivity and concomitant changes in δ13C and δ34S across the Frasnian–Famennian boundary (Kowala — Holy Cross Mountains/Poland)[J]. Chemical Geology, 2001, 175(1-2): 109-131.
    [28]
    LI X P, CHEN Z B, WEI J W, et al., 2019. Petrogenesis and geological significance of mafic rock in De′e area of the western Guangxi[J]. Journal of Guilin University of Technology, 39(2): 270-281. (in Chinese with English abstract)
    [29]
    LI Z L, LIU X J, XU J F, et al., 2015. Geochemical evolution characteristics and regional tectonic significance of mafic rocks from Youjiang Basin[J]. Journal of Guilin University of Technology, 35(4): 727-735. (in Chinese with English abstract)
    [30]
    MA Z X, LIU X T, YU W C, et al., 2019. Redox conditions and manganese metallogenesis in the Cryogenian Nanhua Basin: Insight from the basal Datangpo Formation of South China[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 529: 39-52. doi: 10.1016/j.palaeo.2019.05.031
    [31]
    MAYNARD J B, 2010. The chemistry of manganese ores through time: a signal of increasing diversity of earth-surface environments[J]. Economic Geology, 105(3): 535-552. doi: 10.2113/gsecongeo.105.3.535
    [32]
    OU L H, 2013. Research on depositional feature and mineralization mechanism of the Upper Devonian manganese deposit in Southwestern Guangxi area[D]. Chengdu: Chengdu University of Technology. (in Chinese with English abstract)
    [33]
    QIN Y K, ZHANG H C, YAO J Q, 2010a. Geochemical Characteristics and Geological Implication of the Xialei Manganese Depost, Daxin County, Guangxi[J]. Geological Review, 56(5): 664-672. (in Chinese with English abstract)
    [34]
    QIN Y K, XU B A, YAO J Q, 2010b. Depth of ancient sea related with formation of the Upper Devonian Mn-bearing rock series in Southwestern Guangxi Province[J]. Geology and Exploration, 46(2): 277-284. (in Chinese with English abstract)
    [35]
    RACKA M, MARYNOWSKI L, FILIPIAK P, et al., 2010. Anoxic annulata events in the Late Famennian of the Holy Cross Mountains (Southern Poland): Geochemical and palaeontological record[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 297(3-4): 549-575. doi: 10.1016/j.palaeo.2010.08.028
    [36]
    RONA P A, 1978. Criteria for recognition of hydrothermal mineral deposits in oceanic crust[J]. Economic Geology, 73(2): 135-160. doi: 10.2113/gsecongeo.73.2.135
    [37]
    ROY S, 2006. Sedimentary manganese metallogenesis in response to the evolution of the earth system[J]. Earth-Science Reviews, 77(4): 273-305. doi: 10.1016/j.earscirev.2006.03.004
    [38]
    RU T Q, WEI L D, SHU G, 1992. Manganese ore geology of Guangxi[M]. Beijing: Geological Publishing House. (in Chinese)
    [39]
    ŞAŞMAZ A, TÜRKYILMAZ B, ÖZTÜRK N, et al., 2014. Geology and geochemistry of Middle Eocene maden complex ferromanganese deposits from the Elazığ–Malatya region, Eastern Turkey[J]. Ore Geology Reviews, 56: 352-372. doi: 10.1016/j.oregeorev.2013.06.012
    [40]
    TAYLOR S R, MCLENNAN S M, 1985. The continental crust: Its composition and evolution[M]. Oxford: Blackwell Scientific Publications.
    [41]
    TOTH J R, 1980. Deposition of submarine crusts rich in manganese and iron[J]. GSA Bulletin, 91(1): 44-54.
    [42]
    TRIBOVILLARD N, ALGEO T J, BAUDIN F, et al. , 2012. Analysis of marine environmental conditions based onmolybdenum–uranium covariation—Applications to Mesozoic paleoceanography[J]. Chemical Geology, 324-325: 46-58.
    [43]
    WANG C S, HU X M, LI X H, 1999. Dissolved oxygen in palaeo-ocean: anoxic events and high-oxic problems[J]. Marine Geology & Quaternary Geology, 19(3): 39-48. (in Chinese with English abstract)
    [44]
    WANG H Q, JIANG S, CHEN J H, et al., 2026. Advances in manganese ore exploration in China[J]. Acta Geologica Sinica, 100(2): 598-613. (in Chinese with English abstract)
    [45]
    WANG Y L, WANG D H, ZHANG C Q, et al., 2011. LA-ICP-MS zircon U-Pb dating of the Qinjia granite in Guangxi Province and its geologic significance[J]. Acta Geologica Sinica, 85(4): 475-481. (in Chinese with English abstract)
    [46]
    WU X K, LIANG G K, LI Y K, et al., 2023. Zircon U-Pb age and Hf isotopic composition of Bama basic rocks in western Guangxi: genetic relationship with Emeishan large igneous province[J]. Journal of Guilin University of Technology, 43(1): 14-29. (in Chinese with English abstract)
    [47]
    XUE Y Z, YAO J Q, HUANG J S, et al., 2019. A review of the metallogenic theory of endogenous origin and exogenous mineralization of manganese ores[J]. Geology and Exploration, 55(4): 891-898. (in Chinese with English abstract)
    [48]
    YAN H, PI D H, JIANG S Y, et al., 2022. Mineral paragenesis in Paleozoic manganese ore deposits: Depositional versus post-depositional formation processes[J]. Geochimica et Cosmochimica Acta, 325: 65-86. doi: 10.1016/j.gca.2022.03.030
    [49]
    YAN Z, HE P X, FU C L, et al., 2026. Study on the manganese ore-forming environment in western Guangxi[J]. Acta Geologica Sinica, 100(2): 363-386. (in Chinese with English abstract)
    [50]
    YANG R D, GAO J B, XU H, et al., 2022. Ore-forming source analysis of huge manganese deposits in the Neoproterozoic Datangpo stage, Guizhou Province, China[J]. Acta Geologica Sinica, 96(5): 1815-1826. (in Chinese with English abstract)
    [51]
    YIN J N, XIAO K Y, 2014. Resources potential analysis and metallogenic prospect of Mn resources in China[J]. Geology in China, 41(5): 1424-1437. (in Chinese with English abstract)
    [52]
    YU W C, ALGEO T J, DU Y S, et al, 2016. Genesis of Cryogenian Datangpo manganese deposit: hydrothermal influence and episodic post-glacial ventilation of Nanhua Basin, South China[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 459: 321-337. doi: 10.1016/j.palaeo.2016.05.023
    [53]
    YU W C, POLGÁRI M, ZHOU Q, et al., 2025. Geobiological perspective for the formation of manganiferous deposit: principle, evidence, and model[J]. Earth Science, 50(3): 1142-1161. (in Chinese with English abstract)
    [54]
    ZHANG T G, TRELA W, JIANG S Y, et al., 2011. Major oceanic redox condition change correlated with the rebound of marine animal diversity during the Late Ordovician[J]. Geology, 39(7): 675-678. doi: 10.1130/G32020.1
    [55]
    ZHANG X S, OVER D J, MA K Y, et al., 2019. Upper Devonian conodont zonation, sea-level changes and bio-events in offshore carbonate facies Lali section, South China[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 531: 109219. doi: 10.1016/j.palaeo.2019.05.041
    [56]
    ZHAO L Q, ZHOU S G, YI H S, et al., 2016. Geochemical characteristics and sedimentary environment of the Xialei manganese deposit in Southwest Guangxi[J]. Geology and Exploration, 52(1): 25-39. (in Chinese with English abstract)
    [57]
    ZHAO Y Q, YANG C C, XU H, et al., 2026. Late Devonian Mn mineralization as a result of volcanism-and orbital-forced palaeoceanographic changes[J]. Scientia Sinica Terrae, 56(5): 1912-1923. (in Chinese) doi: 10.1360/N072025-0463
    [58]
    ZHOU C M, JIANG S Y, 2009. Palaeoceanographic redox environments for the Lower Cambrian Hetang Formation in South China: Evidence from pyrite framboids, redox sensitive trace elements, and sponge biota occurrence[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 271(3-4): 279-286. doi: 10.1016/j.palaeo.2008.10.024
    [59]
    ZHOU H Y, PI D H, HUANG Q, et al., 2024. Geology, geochemistry and genesis of the Dongping manganese deposit, Guangxi Province, China[J]. Earth Science, 49(2): 656-668. (in Chinese with English abstract)
    [60]
    ZHOU Q, 2008. Geological and geochemical characteristics of cold seep carbonates of Neoproterozoic Nanhua Period and their significance for manganese ore deposits in East Guizhou[D]. Wuhan: China University of Geosciences. (in Chinese with English abstract)
    [61]
    ZHU Q K, ZHOU H Y, 2021. Reviews and prospects of submarine metalliferous sediments of hydrothermal origin[J]. Marine Sciences, 45(8): 69-80. (in Chinese with English abstract)
    [62]
    常华进, 储雪蕾, 冯连君, 等, 2009. 氧化还原敏感微量元素对古海洋沉积环境的指示意义[J]. 地质论评, 55(1): 91-99. doi: 10.16509/j.georeview.2009.01.014
    [63]
    陈洪德, 曾允孚, 1990. 右江沉积盆地的性质及演化讨论[J]. 岩相古地理(1): 28-37.
    [64]
    陈家浩, 田郁溟, 江沙, 等, 2026. 锰矿成矿模型与有效勘查方法在找矿过程中的应用: 以下雷锰矿床为例[J]. 地质学报, 100(2): 679-692. doi: 10.19762/j.cnki.dizhixuebao.2025475
    [65]
    陈旭, 田郁溟, 高宝龙, 等, 2026. 南华系锰的生物化学成矿作用[J]. 地质学报, 100(2): 484-509. doi: 10.19762/j.cnki.dizhixuebao.2025474
    [66]
    丛源, 董庆吉, 肖克炎, 等, 2018. 中国锰矿资源特征及潜力预测[J]. 地学前缘, 25(3): 118-137. doi: 10.13745/j.esf.2018.03.010
    [67]
    董建辉, 刘欢, 江沙, 等, 2025. 基于随机森林的二维找矿预测: 以下雷-土湖地区沉积型锰矿为例[J]. 矿床地质, 44(1): 143-158. doi: 10.16111/j.0258-7106.2025.01.009
    [68]
    董志国, 张连昌, 王长乐, 等, 2020. 沉积碳酸锰矿床研究进展及有待深入探讨的若干问题[J]. 矿床地质, 39(2): 237-255. doi: 10.16111/j.0258-7106.2020.02.003
    [69]
    杜远生, 余文超, 周琦, 等, 2023. 超大陆裂解与中国大规模成锰作用的耦合关系探讨[J]. 古地理学报, 25(6): 1211-1234. doi: 10.7605/gdlxb.2023.06.093
    [70]
    付勇, 徐志刚, 裴浩翔, 等, 2014. 中国锰矿成矿规律初探[J]. 地质学报, 88(12): 2192-2207. doi: 10.19762/j.cnki.dizhixuebao.2014.12.004
    [71]
    郭宁宁, 高兆富, 贾建亮, 等, 2026. 广西下雷锰矿的地质、地球化学特征及其对不同锰矿化机制的约束[J]. 地质学报, 100(2): 537-552. doi: 10.19762/j.cnki.dizhixuebao.2025249
    [72]
    郭馨莲, 蔡为民, 卢宜冠, 等, 2026. 锰金属的资源属性、地质特征及其利用[J]. 地质学报, 100(2): 633-656. doi: 10.19762/j.cnki.dizhixuebao.2025232
    [73]
    侯宗林, 薛友智, 黄金水, 等, 1997. 扬子地台周边锰矿[M]. 北京: 冶金工业出版社.
    [74]
    李兴鹏, 陈忠斌, 韦剑玮, 等, 2019. 桂西德峨地区基性岩的岩石成因及地质意义[J]. 桂林理工大学学报, 39(2): 270-281. doi: 10.3969/j.issn.1674-9057.2019.02.003
    [75]
    李政林, 刘希军, 许继峰, 等, 2015. 右江盆地基性岩的地球化学演化特征及其区域构造意义[J]. 桂林理工大学学报, 35(4): 727-735. doi: 10.3969/j.issn.1674-9057.2015.04.010
    [76]
    欧莉华, 2013. 桂西南地区上泥盆统锰矿沉积特征与成矿机理研究[D]. 成都: 成都理工大学.
    [77]
    秦元奎, 张华成, 姚敬劬, 2010a. 广西大新县下雷锰矿床的地球化学特征及其意义[J]. 地质论评, 56(5): 664-672. doi: 10.16509/j.georeview.2010.05.014
    [78]
    秦元奎, 徐柏安, 姚敬劬, 2010b. 桂西南上泥盆统含锰岩系形成古海水深度条件分析[J]. 地质与勘探, 46(2): 277-284.
    [79]
    茹廷锵, 韦灵敦, 树皋, 1992. 广西锰矿地质[M]. 北京: 地质出版社.
    [80]
    王成善, 胡修棉, 李祥辉, 1999. 古海洋溶解氧与缺氧和富氧问题研究[J]. 海洋地质与第四纪地质, 19(3): 39-48. doi: 10.16562/j.cnki.0256-1492.1999.03.006
    [81]
    王华青, 江沙, 陈家浩, 等, 2026. 中国锰矿勘查进展[J]. 地质学报, 100(2): 598-613. doi: 10.19762/j.cnki.dizhixuebao.2025491
    [82]
    王永磊, 王登红, 张长青, 等, 2011. 广西钦甲花岗岩体单颗粒锆石LA-ICP-MS U-Pb定年及其地质意义[J]. 地质学报, 85(4): 475-481.
    [83]
    吴祥珂, 梁国科, 李玉坤, 等, 2023. 桂西巴马基性岩锆石U-Pb年龄和Hf同位素特征: 与峨眉山大火成岩省的成因联系[J]. 桂林理工大学学报, 43(1): 14-29. doi: 10.3969/j.issn.1674-9057.2023.01.002
    [84]
    薛友智, 姚敬劬, 黄金水, 等, 2019. 再论锰的“内源外生”成矿说[J]. 地质与勘探, 55(4): 891-898. doi: 10.12134/j.dzykt.2019.04.001
    [85]
    闫臻, 和平贤, 付长垒, 等, 2026. 桂西锰矿成矿环境研究[J]. 地质学报, 100(2): 363-386.
    [86]
    杨瑞东, 高军波, 徐海, 等, 2022. 贵州新元古代大塘坡期巨量锰矿成矿物质来源分析[J]. 地质学报, 96(5): 1815-1826.
    [87]
    阴江宁, 肖克炎, 2014. 中国锰矿资源潜力分析及成矿预测[J]. 中国地质, 41(5): 1424-1437. doi: 10.3969/j.issn.1000-3657.2014.05.002
    [88]
    余文超, POLGÁRI M, 周琦, 等, 2025. 地球生物学视角下的富锰沉积形成过程: 原理、证据与模式[J]. 地球科学, 50(3): 1142-1161. doi: 10.3799/dqkx.2025.002
    [89]
    赵立群, 周尚国, 伊海生, 等, 2016. 桂西南下雷锰矿床地球化学特征及沉积环境分析[J]. 地质与勘探, 52(1): 25-39.
    [90]
    赵银强, 杨晨晨, 徐海, 等, 2026. 火山活动与轨道周期协同驱动下的晚泥盆世锰成矿响应[J]. 中国科学: 地球科学, 56(5): 1912-1923.
    [91]
    周皓宇, 皮道会, 黄钦, 等, 2024. 广西东平锰矿床地质地球化学特征及矿床成因[J]. 地球科学, 49(2): 656-668. doi: 10.3799/dqkx.2022.159
    [92]
    周琦, 2008. 黔东新元古代南华纪早期冷泉碳酸盐岩地质地球化学特征及其对锰矿的控矿意义[D]. 武汉: 中国地质大学.
    [93]
    朱启宽, 周怀阳, 2021. 海底热液成因含金属沉积物的研究现状及展望[J]. 海洋科学, 45(8): 69-80. doi: 10.11759/hykx20191221001
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