[1] 李治兴，秦明宽，刘鑫扬，等. 黑色岩系多元素富集层特征、成因和研究意义[J]. 世界核地质科学，2022，39（1）：14-26.

Li Zhixing, Qin Mingkuan, Liu Xinyang, et al. Characteristics, genesis and research significances of multielements enrichment layer of black rock series[J]. World Nuclear Geoscience, 2022, 39(1): 14-26.
[2] 李有禹. 湖南下寒武统石煤中的镍钼铂族元素的地球化学特征[J]. 煤炭学报，1996，21（3）：261-264.

Li Youyu. Geochemistry characteristics of Ni-Mo-Pt group elements in the lower Cambrian bone coal in Hunan province[J]. Journal of China Coal Society, 1996, 21(3): 261-264.
[3] 范德廉，杨秀珍，王连芳，等. 某地下寒武统含镍钼多元素黑色岩系的岩石学及地球化学特点[J]. 地球化学，1973（3）：143-164.

Fan Delian, Yang Xiuzhen, Wang Lianfang, et al. Petrological and geochemical characteristics of a nickel- molybdenum- multe- element - bearing lower-Cambrian black shale from a certain district in South China[J]. Geochimica, 1973(3): 143-164.
[4] 温志亮，赵民，李普涛，等. 南秦岭北大巴山地区黑色岩系型钒钼矿床地质特征及成因[J]. 西北地质，2021，54（1）：100-108.

Wen Zhiliang, Zhao Min, Li Putao, et al. Geological features and genesis of vanadium molybdenum deposit of black rock series in northern Dabashan area of South Qinling[J]. Northwestern Geology, 2021, 54(1): 100-108.
[5] 施春华，曹剑，胡凯，等. 黑色岩系矿床成因及其海水、热水与生物有机成矿作用[J]. 地学前缘，2013，20（1）：19-31.

Shi Chunhua, Cao Jian, Hu Kai, et al. A review of origins of mineral deposits hosted in black rock series and the mineralizing functions of their sea water, hydrothermal fluid and bio-organics[J]. Earth Science Frontiers, 2013, 20(1): 19-31.
[6] 李胜荣，高振敏. 湘黔地区牛蹄塘组黑色岩系稀土特征：兼论海相热水沉积岩稀土模式[J]. 矿物学报，1995，15（2）：225-229.

Li Shengrong, Gao Zhenmin. REE characteristics of black rock series of the lower Cambrian Niutitang Formation in Hunan-Guizhou provinces, China, with a discussion on the REE patterns in marine hydrothermal sediments[J]. Acta Mineralogica Sinica, 1995, 15(2): 225-229.
[7] 陈先沛，高计元，陈多福，等. 热水沉积作用的概念和几个岩石学标志[J]. 沉积学报，1992，10（3）：124-132.

Chen Xianpei, Gao Jiyuan, Chen Duofu, et al. The concept of hydrothermal sedimentation and its petrological criteria[J]. Acta Sedimentologica Sinica, 1992, 10(3): 124-132.
[8] 薛春纪，祁思敬，郑明华，等. 热水沉积研究及相关科学问题[J]. 矿物岩石地球化学通报，2000，19（3）：155-163.

Xue Chunji, Qi Sijing, Zheng Minghua, et al. Hydrothermal sediment research and associated scientific problems[J]. Bulletin of Mineralogy, Petrology and Geochemistry, 2000, 19(3): 155-163.
[9] 杨瑞东，魏怀瑞，鲍淼，等. 贵州天柱上公塘—大河边寒武纪重晶石矿床海底热水喷流沉积结构、构造特征[J]. 地质论评，2007，53（5）：675-680.

Yang Ruidong, Wei Huairui, Bao Miao, et al. Submarine hydrothermal venting-flowing sedimentary characters of the Cambrian Shanggongtang and Dahebian barite deposits, Tianzhu county, Guizhou province[J]. Geological Review, 2007, 53(5): 675-680.
[10] 庞维华，丁孝忠，高林志，等. 湖南下寒武统层序地层特征与古环境演化变迁[J]. 中国地质，2011，38（3）：560-576.

Pang Weihua, Ding Xiaozhong, Gao Linzhi, et al. Characteristics of sequence stratigraphy and plaeoenvironmental evolution of lower Cambrian strata in Hunan province[J]. Geology in China, 2011, 38(3): 560-576.
[11] 齐小兵，翟文建，章泽军. 慈利—保靖断裂带的性质及其演化[J]. 地质科技情报，2009，28（2）：54-59.

Qi Xiaobing, Zhai Wenjian, Zhang Zejun. Geological properties and evolution of Cili-Baojing fault zone[J]. Geological Science and Technology Information, 2009, 28(2): 54-59.
[12] 黄俨然，肖正辉，焦鹏，等. 湘西北牛蹄塘组探井页岩气富集要素的对比和启示[J]. 中南大学学报（自然科学版），2018，49（9）：2240-2248.

Huang Yanran, Xiao Zhenghui, Jiao Peng, et al. Comparison of factors for shale gas accumulation in Niutitang Formation wells in northwestern Hunan and its implications[J]. Journal of Central South University (Science and Technology), 2018, 49(9): 2240-2248.
[13] 李忠雄，陆永潮，王剑，等. 中扬子地区晚震旦世—早寒武世沉积特征及岩相古地理[J]. 古地理学报，2004，6（2）：151-162.

Li Zhongxiong, Lu Yongchao, Wang Jian, et al. Sedimentary characteristics and lithofacies palaeogeography of the Late Sinian and early Cambrian in middle Yangtze region[J]. Journal of Palaeogeography, 2004, 6(2): 151-162.
[14] 汪建国，陈代钊，严德天，等. 湘西地区前寒武纪—寒武纪转折期碳酸盐—硅泥质沉积体系的截然转换：地层—沉积样式，形成机理及意义[J]. 地质科学，2011，46（1）：27-41.

Wang Jianguo, Chen Daizhao, Yan Detian, et al. Sharp transition from carbonates to cherts across the platform margin in western Hunan, South China during Precambrian-Cambrian transition: Stratal-depositional patterns, mechanisms and implications[J]. Chinese Journal of Geology, 2011, 46(1): 27-41.
[15] 王约，黄再琴，陈洪德，等. 华南留茶坡组与灯影组的地层对比[J]. 吉林大学学报(地球科学版)，2012，42（增刊1）：328-335.

Wang Yue, Huang Zaiqin, Chen Hongde, et al. Stratigraphical correlation of the Liuchapo Formation with the Deng-ying Formation in South China[J]. Journal of Jilin University (Earth Science Edition), 2012, 42(Suppl. 1): 328-335.
[16] 李军，孙治雷，黄威，等. 现代海底热液过程及成矿[J]. 地球科学：中国地质大学学报，2014，39（3）：312-324.

Li Jun, Sun Zhilei, Huang Wei, et al. Modern seafloor hydrothermal processes and mineralization[J]. Earth Sciences: Journal of China University of Geosciences, 2014, 39(3): 312-324.
[17] Adachi M, Yamamoto K, Sugisaki R. Hydrothermal chert and associated siliceous rocks from the northern Pacific their geological significance as indication od ocean ridge activity[J]. Sedimentary Geology, 1986, 47(1/2): 125-148.
[18] 黄俨然，肖正辉，余烨，等. 湘西北下寒武统黑色岩系元素地球化学特征及地质意义[J]. 地球化学，2020，49（5）：516-527.

Huang Yanran, Xiao Zhenghui, Yu Ye, et al. Geological significance of the elemental geochemistry of lower Cambrian black shales from northwestern Hunan[J]. Geochimica, 2020, 49(5): 516-527.
[19] Marchig V, Gundlach H, Möller P, et al. Some geochemical indicators for discrimination between diagenetic and hydrothermal metalliferous sediments[J]. Marine Geology, 1982, 50(3): 241-256.
[20] Douville E, Bienvenu P, Charlou J L, et al. Yttrium and rare earth elements in fluids from various deep-sea hydrothermal systems[J]. Geochimica et Cosmochimica Acta, 1999, 63(5): 627-643.
[21] Peter J M, Scott S D. Mineralogy, Composition, and fluid-inclusion microthermometry of sea-floor hydrothermal deposits in the southern trough of Guaymas Basin, gulf of California[J]. The Canadian Mineralogist, 1988, 26(3): 567-587.
[22] 夏威，于炳松，孙梦迪. 渝东南YK1井下寒武统牛蹄塘组底部黑色页岩沉积环境及有机质富集机制[J]. 矿物岩石，2015，35（2）：70-80.

Xia Wei, Yu Bingsong, Sun Mengdi. Depositional setting and enrichment mechanism of organic matter of the black shales of Niutitang Formation at the bottom of lower Cambrian, in well Yuke1, southeast Chongqing[J]. Journal of Mineralogy and Petrology, 2015, 35(2): 70-80.
[23] Michard A, Albarède F. The REE content of some hydrothermal fluids[J]. Chemical Geology, 1986, 55(1/2): 51-60.
[24] 李晓彪，罗远良，罗泰义，等. 重庆城口地区早前寒武系黑色岩系研究：（2）早寒武世硅质岩的沉积环境研究[J]. 矿物学报，2007，27（3/4）：302-314.

Li Xiaobiao, Luo Yuanliang, Luo Taiyi, et al. Pre-Early Cambrian black rock series in Chengkou district, Chongqing: (2) sedimentary environment study of chert in lower Cambrian Bashan Formation[J]. Acta Mineralogica Sinica, 2007, 27(3/4): 302-314.
[25] 张沛，郑建平，张瑞生，等. 塔里木盆地塔北隆起奥陶系—侏罗系泥岩稀土元素地球化学特征[J]. 沉积学报，2005，23（4）：740-746.

Zhang Pei, Zheng Jianping, Zhang Ruisheng, et al. Rare earth elemental characteristics of Ordovician-Jurassic mudstone in Tabei uplift, Tarim Basin[J]. Acta Sedimentologica Sinica, 2005, 23(4): 740-746.
[26] Alexander B W, Bau M, Andersson P, et al. Continentally-derived solutes in shallow Archean seawater: Rare earth element and Nd isotope evidence in iron formation from the 2.9 Ga Pongola Supergroup, South Africa[J]. Geochimica et Cosmochimica Acta, 2008, 72(2): 378-394.
[27] 王登，周豹，冷双梁，等. 鄂西咸丰地区五峰组—龙马溪组硅质岩地球化学特征及地质意义[J]. 岩性油气藏，2022，34（1）：52-62.

Wang Deng, Zhou Bao, Leng Shuangliang, et al. Geochemical characteristics and geological significance of siliceous rocks of Wufeng-Longmaxi Formation in Xianfeng area, western Hubei[J]. Lithologic Reservoirs, 2022, 34(1): 52-62.
[28] 李有禹. 湘西北下寒武统黑色页岩伴生元素研究新进展[J]. 矿床地质，1995，14（4）：346-354.

Li Youyu. New advances in the study of associated elements in lower Cambrian black shale of northwestern Hunan[J]. Mineral Deposits, 1995, 14(4): 346-354.
[29] 杨瑞东，鲍淼，魏怀瑞，等. 贵州天柱寒武系底部重晶石矿床中热水生物群的发现及意义[J]. 自然科学进展，2007，17（9）：1304-1309.

Yang Ruidong, Bao Miao, Wei Huairui, et al. The discovery and its significance of hydrothermal biota in the bottom of Cambrian barite deposits, Tianzhu county, Guizhou province[J]. Progress in Natural Science, 2007, 17(9): 1304-1309.
[30] 孙泽航，胡凯，韩善楚，等. 湘黔新晃—天柱重晶石矿床微量稀土元素和硫同位素研究[J]. 高校地质学报，2015，21（4）：701-710.

Sun Zehang, Hu Kai, Han Shanchu, et al. Trace and rare earth elements and sulfur isotope analysis of barite deposits in west Hunan and east Guizhou[J]. Geological Journal of China Universities, 2015, 21(4): 701-710.
[31] Ray E, Paul D. Major and trace element characteristics of the average Indian Post-Archean Shale: Implications for provenance, weathering, and depositional environment[J]. ACS Earth and Space Chemistry, 2021, 5(5): 1114-1129.
[32] 王健, 漆富成, 王文全，等. 湘西北含铀多金属黑色岩系矿化元素组合划分及矿物赋存特征[J].铀矿地质, 2021, 37(6): 1049-1056.

Wang Jian, Qi Fucheng, Wang Wenquan, et al. Association type of mineralization elements and mineral occurrence of uranium polymetallic-bearing black-rock series in northwestern Hunan[J]. Uranium Geology, 2021, 37(6): 1049-1056.
[33] 樊秋爽，夏国清，李高杰，等. 古海洋氧化还原条件分析方法与研究进展[J]. 沉积学报，2022，40（5）：1151-1171.

Fan Qiushuang, Xia Guoqing, Li Gaojie, et al. Analytical methods and research progress of redox conditions in the paleo-ocean[J]. Acta Sedimentologica Sinica, 2022, 40(5): 1151-1171.
[34] 常华进，储雪蕾，冯连君，等. 氧化还原敏感微量元素对古海洋沉积环境的指示意义[J]. 地质评论，2009，55（1）：91-99.

Chang Huajin, Chu Xuelei, Feng Lianjun, et al. Redox sensitive trace elements as paleoenvironments proxies[J]. Geological Review, 2009, 55(1): 91-99.
[35] 王璞珺，王东坡，常平，等. 油页岩中生物及有机质与金属元素富集的关系及机理探讨[J]. 长春地质学院学报，1996，26（1）：47-53.

Wang Pujun, Wang Dongpo, Chang Ping, et al. Metallic biomineralization of continental black shales[J]. Journal of Changchun University of Earth Sciences, 1996, 26(1): 47-53.
[36] Tribovillard N, Algeo T J, Lyons T, et al. Trace metals as paleoredox and paleoproductivity proxies: An update[J]. Chemical Geology, 2006, 232(1/2): 12-32.
[37] Dong L, Huang Y R, Li W B, et al. Understanding hydrothermal activity and organic matter enrichment with the geochemical characteristics of black shales in lower Cambrian, northwestern Hunan, South China[J].Lithosphere, 2022, Special 12: 2241381.
[38] 董宏坤，万世明，刘喜停. 海洋沉积物早期成岩作用研究进展[J]. 沉积学报，2022，40（5）：1172-1187.

Dong Hongkun, Wan Shiming, Liu Xiting. Research progress on geochemical behavior of minerals and elements in early diagenesis of marine sediments[J]. Acta Sedimentologica Sinica, 2022, 40(5): 1172-1187.
[39] 孙省利，陈践发，刘文汇，等. 海底热水活动与海相富有机质层形成的关系：以华北新元古界青白口系下马岭组为例[J]. 地质评论，2003，49（6）：588-595.

Sun Shengli, Chen Jianfa, Liu Wenhui, et al. Hydrothermal venting on the seafloor and formation of organic-rich sediments: Evidence from the Neoproterozoic Xiamaling Formation, North China[J]. Geological Review, 2003, 49(6): 588-595.
[40] 付伟，周永章，杨志军，等. 现代海底热水活动的系统性研究及其科学意义[J]. 地球科学进展，2005，20（1）：81-88.

Fu Wei, Zhou Yongzhang, Yang Zhijun, et al. Modern seafloor hydrothermal system and its scientific implications[J]. Advances in Earth Science, 2005, 20(1): 81-88.
[41] 刘焱光，曹东林，张德玉，等. 冲绳海槽北部的全新世火山碎屑沉积[J]. 海洋科学进展，2007，25（1）：34-45.

Liu Yanguang, Cao Donglin, Zhang Deyu, et al. Holocene tephra deposits in the northern Okinawa Trough[J]. Advances in Marine Science, 2007, 25(1): 34-45.