[1] 王濡岳,丁文龙,龚大建,等. 渝东南—黔北地区下寒武统牛蹄塘组页岩裂缝发育特征与主控因素[J]. 石油学报,2016,37(7):832-845,877.

Wang Ruyue, Ding Wenlong, Gong Dajian, et al. Development characteristics and major controlling factors of shale fractures in the Lower Cambrian Niutitang Formation, southeastern Chongqing-northern Guizhou area[J]. Acta Petrolei Sinica, 2016, 37(7): 832-845, 877.
[2] 王濡岳,龚大建,冷济高,等. 黔北地区下寒武统牛蹄塘组页岩储层发育特征:以岑巩区块为例[J]. 地学前缘,2017,24(6):286-299.

Wang Ruyue, Gong Dajian, Leng Jigao, et al. Developmental characteristics of the Lower Cambrian Niutitang shale reservoir in northern Guizhou area: A case study in the Cengong block[J]. Earth Science Frontiers, 2017, 24(6): 286-299.
[3] 黄金亮,邹才能,李建忠,等. 川南下寒武统筇竹寺组页岩气形成条件及资源潜力[J]. 石油勘探与开发,2012,39(1):69-75.

Huang Jinliang, Zou Caineng, Li Jianzhong, et al. Shale gas generation and potential of the Lower Cambrian Qiongzhusi Formation in southern Sichuan Basin, China[J]. Petroleum Exploration and Development, 2012, 39(1): 69-75.
[4] 李延钧,赵圣贤,黄永斌,等. 四川盆地南部下寒武统筇竹寺组页岩沉积微相研究[J]. 地质学报,2013,87(8):1136-1148.

Li Yanjun, Zhao Shengxian, Huang Yongbin, et al. The sedimentary micro-facies study of the Lower Cambrian Qiongzhusi Formation in southern Sichuan Basin[J]. Acta Geologica Sinica, 2013, 87(8): 1136-1148.
[5] 黎彤. 化学元素的地球丰度[J]. 地球化学,1976(3):167-174.

Li Tong. Chemical element abundances in the earth and it's major shells[J]. Geochimica, 1976(3): 167-174.
[6] Boström K, Kraemer T, Gartner S. Provenance and accumulation rates of opaline silica, Al, Ti, Fe, Mn, Cu, Ni and Co in Pacific pelagic sediments[J]. Chemical Geology, 1973, 11(1/2): 123-148.
[7] Tyson R V, Pearson T H. Modern and ancient continental shelf anoxia: An overview[M]//Tyson R V, Pearson T H. Modern and ancient continental shelf anoxia. London: Geological Society, Special Publication, 1991, 58: 1-24.
[8] Jones B, Manning D A C. Comparison of geochemical indices used for the interpretation of palaeoredox conditions in ancient mudstones[J]. Chemical Geology, 1994, 111(1/2/3/4): 111-129.
[9] Wignall P B. Black shales[M]. Oxford: Clarendon Press, 1994: 1-127.
[10] Choi J H, Hariya Y. Geochemistry and depositional environment of Mn oxide deposits in the Tokoro Belt, Northeastern Hokkaido, Japan[J]. Economic Geology, 1992, 87(5): 1265-1274.
[11] 谢桂青,胡瑞忠,方维萱,等. 云南墨江金矿床硅质岩沉积环境的地球化学探讨[J]. 地球化学,2001,30(5):491-497.

Xie Guiqing, Hu Ruizhong, Fang Weixuan, et al. Geochemistry of depositional environment of siliceous rocks from Mojiang gold deposit in Yunnan province[J]. Geochimica, 2001, 30(5): 491-497.
[12] 夏菲,马东升,潘家永,等. 贵州天柱大河边和玉屏重晶石矿床热水沉积成因的锶同位素证据[J]. 科学通报,2004,49(24):2592-2595.

Xia Fei, Ma Dongsheng, Pan Jiayong, et al. Strontium isotopic signature of hydrothermal sedimentation from Early Cambrian barite deposits in east Guizhou, China[J]. Chinese Science Bulletin, 2004, 49(24): 2592-2595.
[13] Toth J R. Deposition of submarine crusts rich in manganese and iron[J]. GSA Bulletin, 1980, 91(1): 44-54.
[14] Sugisaki R, Yamamoto K, Adachi M. Triassic bedded cherts in central Japan are not pelagic[J]. Nature, 1982, 298(5875): 644-647.
[15] Murray R W, ten Brink M R B, Jones D L, et al. Rare earth elements as indicators of different marine depositional environments in chert and shale[J]. Geology, 1990, 18(3): 268-271.
[16] Murray R W. Chemical criteria to identify the depositional environment of chert: General principles and applications[J]. Sedimentary Geology, 1994, 90(3/4): 213-232.
[17] 韩吟文,马振东. 地球化学[M]. 北京:地质出版社,2003:190-192.

Han Yinwen, Ma Zhendong. Geochemistry[M]. Beijing: Geological Publishing House, 2003: 190-192.
[18] Wilde P, Quinby-Hunt M S, Erdtmann B D. The whole-rock cerium anomaly: A potential indicator of eustatic sea-level changes in shales of the anoxic facies[J]. Sedimentary Geology, 1996, 101(1/2): 43-53.
[19] Allegre C J, Minster J F. Quantitative models of trace element behavior in magmatic processes. Earth and Planetary Science Letters, 1978, 38(1): 1-25.
[20] Ganeshram R S, Pedersen T F, Calvert S E, et al. Large changes in oceanic nutrient inventories from glacial to interglacial periods[J]. Nature, 1995, 376(6543): 755-758.
[21] Kunzendorf H, Stoffers P, Gwozdz R. Regional variations of REE patterns in sediments from active plate boundaries[J]. Marine Geology, 1988, 84(3/4): 191-199.
[22] Wänk H, Dreibus G, Jagoutz E. Mantle Chemistry and accretion history of the earth[M]//Kröner A, Hanson G H, Goodwin A M. Archaean geochemistry: the origin and evolution of the archaean continental crust. Berlin: Springer-Verlag, 1984: 1-24.
[23] Taylor S R, McLennan S M. The continental crust: Its composition and evolution[M]. Oxford: Blackwell, 1985: 312.
[24] 侯东壮. 黔东地区黑色岩系地球化学特征及沉积环境研究[D]. 长沙:中南大学,2011.

Hou Dongzhuang. Research on geochemical characteristics and sedimentary environments of black shales in the eastern Guizhou[D]. Changsha: Central South University, 2011.
[25] Anderson R F, Fleisher M Q, LeHuray A P. Concentration, oxidation state, and particulate flux of uranium in the Black Sea[J]. Geochimica et Cosmochimica Acta, 1989, 53(9): 2215-2224.
[26] Cronan D S. Underwater minerals[M]. London: Academic Press, 1980: 362.
[27] Jacobs L, Emerson S, Skei I. Partitioning and transport of metals across the O2H2S interface in a permanently anoxic basin: Framvaren Fjord, Norway[J]. Geochimica et Cosmochimica Acta, 1985, 49(6): 1433-1444.
[28] Lewan M D, Maynard J B. Factors controlling enrichment of vanadium and nickel in the bitumen of organic sedimentary rocks[J]. Geochimica et Cosmochimica Acta, 1982, 46(12): 2547-2560.
[29] Dill H. Metallogenesis of early Paleozoic graptolite shales from the graefenthal horst (northern Bavaria-Federal republic of Germany)[J]. Economic Geology, 1986, 81(4): 889-903.
[30] 王奖臻,李泽琴,黄从俊. 康滇地轴元古代重大地质事件与拉拉IOCG矿床成矿响应[J]. 地球科学进展,2012,27(10):1074-1079.

Wang Jiangzhen, Li Zeqin, Huang Congjun. The main geological events of the Kangdian Proterozoic eon and response from to the La-La IOCG deposit[J]. Advances in Earth Science, 2012, 27(10): 1074-1079.
[31] 宋昊,倪师军,张成江,等. 康滇地轴基底IOCG铜铁矿床中岩浆岩的成矿及找矿指示意义[J]. 矿物学报,2015,35(增刊1):156-157.

Song Hao, Ni Shijun, Zhang Chengjiang, et al. Mineralization and mineralization indication of magmatic rocks in IOCG copper and iron ore deposit in the basement of Kangdian axial[J]. Acta Mineralogica Sinica, 2015, 35(Suppl.1): 156-157.
[32] 刘军平,孙柏东,王晓峰,等. 滇中禄丰地区中元古代早期球颗玄武岩的锆石U-Pb年龄、地球化学特征及其大地构造意义[J]. 地质论评,2020,66(1):35-51.

Liu Junping, Sun Baidong, Wang Xiaofeng, et al. The zircon U-Pb age, geochemical characteristics and tectonic significance of the spherical basalt in the early Mesoproterozoic in Lufeng area central Yunnan[J]. Geological Review, 2020, 66(1): 35-51.
[33] 李胜荣,高振敏. 湘黔寒武系底部黑色岩系贵金属元素来源示踪[J]. 中国科学(D辑):地球科学,2000,30(2):169-174.

Li Shengrong, Gao Zhenmin. Source tracing of noble metal elements in Lower Cambrian black rock series of Guizhou-Hunan provinces, China[J]. Science China (Seri. D): Earth Sciences, 2000, 30(2): 169-174.
[34] 彭军,田景春,伊海生,等. 扬子板块东南大陆边缘晚前寒武纪热水沉积作用[J]. 沉积学报,2000,18(1):107-113.

Peng Jun, Tian Jingchun, Yi Haisheng, et al. The Late Precambrian hot water sedimentation of the southeast Yangtze Plate continental margin[J]. Acta Sedimentologica Sinica, 2000, 18(1): 107-113.
[35] 周明忠,罗泰义,李正祥,等. 遵义牛蹄塘组底部凝灰岩锆石SHRIMP U-Pb年龄及其地质意义[J]. 科学通报,2008,53(1):104-110.

Zhou Mingzhong, Luo Taiyi, Li Zhengxiang, et al. SHRIMP U-Pb zircon age of tuff at the bottom of the Lower Cambrian Niutitang Formation, Zunyi, South China[J]. Chinese Science Bulletin, 2008, 53(1): 104-110.
[36] 卓皆文,汪正江,王剑,等. 铜仁坝黄震旦系老堡组顶部晶屑凝灰岩SHRIMP锆石U-Pb年龄及其地质意义[J]. 地质论评,2009,55(5):639-646.

Zhuo Jiewen, Wang Zhengjiang, Wang Jian, et al. SHRIMP Zircon U-Pb age of crystal tuffs on the top of Sinian Laobao Formation at Bahuang, Tongren area, and its geological implications[J]. Geological Review, 2009, 55(5): 639-646.
[37] 汪泽成,姜华,王铜山,等. 四川盆地桐湾期古地貌特征及成藏意义[J]. 石油勘探与开发,2014,41(3):305-312.

Wang Zecheng, Jiang Hua, Wang Tongshan, et al. Paleogeomorphology formed during Tongwan tectonization in Sichuan Basin and its significance for hydrocarbon accumulation[J]. Petroleum Exploration and Development, 2014, 41(3): 305-312.
[38] 章乐彤. 重庆地区富有机质页岩地球化学特征及地质意义[D]. 北京:中国地质大学(北京),2019:23-30.

Zhang Letong. Geochemical characteristics and geological significance of rignic-rich shale in Chongqing area[D]. Beijing: China University of Geoscience (Beijing), 2019: 23-30.
[39] 吴朝东,杨承运,陈其英. 湘西黑色岩系地球化学特征和成因意义[J]. 岩石矿物学杂志,1999,18(1):26-39.

Wu Chaodong, Yang Chengyun, Chen Qiying. The origin and geochemical characteristics of Upper Sinain_Lower Cambrian black shales in western Hunan[J]. Acta Petrologica et Mineralogica, 1999, 18(1): 26-39.