[1] Kelling G, Mullin P R. Graded limestones and limestone-quartzite couplets: Possible storm-deposits from the Moroccan Carboniferous[J]. Sedimentary Geology, 1975, 13(3): 161-190.
[2] Kumar N, Sanders J E. Characteristics of shoreface storm deposits: Modern and ancient examples[J]. Journal of Sedimentary Research, 1976, 46(1): 145-162.
[3] Aigner T. Schill-tmlpestite im oberen muschelkalk (Trias, SW-Deutschland)[J]. Neues Jahrbuch für Geologie und Paläontologie-Abhandlungen, 1979, 156: 285-304.
[4] 孟祥化,乔秀夫,葛铭. 华北古浅海碳酸盐风暴沉积和丁家滩相序模式[J]. 沉积学报,1986,4(2):1-18.

Meng Xianghua, Qiao Xiufu, Ge Ming. Study on ancient shallow sea carbonate storm deposits (tempestite) in North China and Dingjiatan model of facies sequences[J]. Acta Sedimentologica Sinica, 1986, 4(2): 1-18.
[5] 刘宝珺,张继庆,许效松. 四川兴文四龙下二叠统碳酸盐风暴岩[J]. 地质学报,1986,60(1):55-67.

Liu Baojun, Zhang Jiqing, Xu Xiaosong. On the calcareous tempestites in the Lower Permian of Silong, Xingwen, Sichuan[J]. Acta Geologica Sinica, 1986, 60(1): 55-67.
[6] 张继庆,冯纯江,杜德勋,等. 四川盆地早二叠世碳酸盐沉积相及风暴沉积作用[M]. 重庆:重庆出版社,1986:11-74.

Zhang Jiqing, Feng Chunjiang, Du Dexun, et al. Carbonate deposition and storm deposition in Early Permian in Sichuan Basin[M]. Chongqing: Chongqing Publishing House, 1986: 11-74.
[7] 黄程,沈宇葳,文馨. 四川广元清风峡剖面上泥盆统风暴沉积特征及其古环境意义[J]. 古地理学报,2021,23(6):1094-1109.

Huang Cheng, Shen Yuwei, Wen Xin. Sedimentary characteristics and its palaeoenvironmental significance of the Upper Devonian storm deposits at Qingfengxia section in Guangyuan city, Sichuan province[J]. Journal of Palaeogeography, 2021, 23(6): 1094-1109.
[8] 金鑫,宋金民,刘树根,等. 四川盆地周缘灯影组风暴沉积特征及其地质意义[J]. 天然气工业,2021,41(10):39-49.

Jin Xin, Song Jinmin, Liu Shugen, et al. Characteristics and geological implications of Dengying Formation tempestites in the periphery of the Sichuan Basin[J]. Natural Gas Industry, 2021, 41(10): 39-49.
[9] 张昊,李凤杰,沈凡,等. 四川盆地龙门山区甘溪石沟里泥盆系养马坝组风暴沉积特征及其地质意义[J]. 古地理学报,2019,21(3):441-450.

Zhang Hao, Li Fengjie, Shen Fan, et al. Storm deposits characteristics and its geological significance in the Devonian Yangmaba Formation from Shigouli section, Longmenshan area, Sichuan Basin[J]. Journal of Palaeogeography, 2019, 21(3): 441-450.
[10] 白莹,罗平,刘伟,等. 塔西北下寒武统风暴活动特征及其沉积学响应[J]. 沉积学报,2019,37(3):565-578.

Bai Ying, Luo Ping, Liu Wei, et al. Storm activity characteristics and their sedimentary responses for the Xiaoerbulak Formation, Lower Cambrian, NW Tarim Basin[J]. Acta Sedimentologica Sinica, 2019, 37(3): 565-578.
[11] 钟建华,倪良田,孙宁亮,等. 鄂尔多斯盆地东胜东三叠系—侏罗系湖泊风暴沉积的发现及其意义[J]. 沉积学报,2021,39(2):353-373.

Zhong Jianhua, Ni Liangtian, Sun Ningliang, et al. Discovery and significance of lake storm deposits in the Triassic-Jurassic of eastern Dongsheng, Ordos Basin[J]. Acta Sedimentologica Sinica, 2021, 39(2): 353-373.
[12] 张译丹,姜在兴,杜克峰,等. 鄂尔多斯盆地志丹—富县地区三叠系延长组长8油层组风暴沉积特征及意义[J]. 石油学报,2019,40(7):813-822.

Zhang Yidan, Jiang Zaixing, Du Kefeng, et al. Sedimentary characteristics and significances of storm deposition in Chang-8 oil layer of Triassic Yanchang Formation, Zhidan-Fuxian area, Ordos Basin[J]. Acta Petrolei Sinica, 2019, 40(7): 813-822.
[13] 李强. 鄂尔多斯盆地寒武系风暴沉积研究[D]. 荆州: 长江大学,2017.

Li Qiang. Research on Cambrian storm deposits in Ordos Basin[D]. Jingzhou: Yangtze University, 2017.
[14] 白一鸣,张元福,胡晨林,等. 鄂尔多斯盆地徐庄组碳酸盐岩风暴沉积发育特征及其地质意义[J]. 现代地质,2017,31(6):1233-1240.

Bai Yiming, Zhang Yuanfu, Hu Chenlin, et al. Characteristics and geological significances of Xuzhuang Formation carbonate tempestites in Ordos Basin[J]. Geoscience, 2017, 31(6): 1233-1240.
[15] 赵振宇,郭彦如,王艳,等. 鄂尔多斯盆地构造演化及古地理特征研究进展[J]. 特种油气藏,2012,19(5):15-20.

Zhao Zhenyu, Guo Yanru, Wang Yan, et al. Study progress in tectonic evolution and paleogeography of Ordos Basin[J]. Special Oil & Gas Reservoirs, 2012, 19(5): 15-20.
[16] Cui Y F, Wang G W, Jones S J, et al. 'Prediction of diagenetic facies using well logs:A case study from the Upper Triassic Yanchang Formation, Ordos Basin, China[J]. Marine and Petroleum Geology, 2017, 81: 50-65.
[17] 李文厚,张倩,陈强,等. 鄂尔多斯盆地及周缘地区早古生代沉积演化[J]. 西北大学学报(自然科学版),2020,50(3):456-479.

Li Wenhou, Zhang Qian, Chen Qiang, et al. Sedimentary evolution of Early Paleozoic in Ordos Basin and its adjacent areas[J]. Journal of Northwest University (Natural Science Edition), 2020, 50(3): 456-479.
[18] 张春林,姚泾利,李程善,等. 鄂尔多斯盆地深层寒武系碳酸盐岩储层特征与主控因素[J]. 石油与天然气地质,2021,42(3):604-614.

Zhang Chunlin, Yao Jingli, Li Chengshan, et al. Characteristics of deep Cambrian carbonate reservoirs in the Ordos Basin and main control factors[J]. Oil & Gas Geology, 2021, 42(3): 604-614.
[19] 陈安清. 鄂尔多斯地块早古生代盆地演化与物质聚集规律[D]. 成都:成都理工大学,2010.

Chen Anqing. Basin evolution and sediments accumulation during eopaleozoic in Ordos continental block[D]. Chengdu: Chengdu University of Technology, 2010.
[20] 杜远生. 广西北海涠洲岛第四纪湖光岩组的风暴岩[J]. 地球科学:中国地质大学学报,2005,30(1):47-51.

Du Yuansheng. Tempestite in the Quaternary Huguangyan Formation in Weizhou Island, Beihai city, Guangxi[J]. Earth Science: Journal of China University of Geosciences, 2005, 30(1): 47-51.
[21] 宋金民,罗平,刘树根,等. 塔里木盆地苏盖特布拉克地区下寒武统风暴岩及其地质意义[J]. 地学前缘,2014,21(6):346-355.

Song Jinmin, Luo Ping, Liu Shugen, et al. Lower Cambrian tempestites and their geological significances in Sugaitblak area, Tarim Basin[J]. Earth Science Frontiers, 2014, 21(6): 346-355.
[22] 李壮福,郭英海. 徐州地区震旦系贾园组的风暴沉积[J]. 古地理学报,2000,2(2):19-27.

Li Zhuangfu, Guo Yinghai. Storm deposits in the Sinian Jiayuan Formation of Xuzhou area[J]. Journal of Palaeogeography, 2000, 2(2): 19-27.
[23] 马瑞申,张良,杜远生,等. 豫北地区寒武系风暴岩沉积特征及其地质意义[J]. 地质科技情报,2011,30(4):15-20.

Ma Ruishen, Zhang Liang, Du Yuansheng, et al. Sedimentary characteristics and its geological implications of Cambrian tempestite in northern Henan province[J]. Geological Science and Technology Information, 2011, 30(4): 15-20.
[24] 王家豪,王华,曾劲彪,等. 山东省中部上寒武统碳酸盐风暴沉积的综合模式[J]. 地球科学,2017,42(1):68-77.

Wang Jiahao, Wang Hua, Zeng Jinbiao, et al. Integrative depositional model for carbonate tempestites in Upper Cambrian, central Shandong province[J]. Earth Science, 2017, 42(1): 68-77.
[25] 余宽宏,畅通,邱隆伟,等. 华北地台早古生代竹叶状灰岩岩石特征及成因研究进展[J]. 沉积学报,2015,33(6):1111-1125.

Yu Kuanhong, Chang Tong, Qiu Longwei, et al. Research development of flat-pebble conglomerate characteristics and their origin in Early Paleozoic North China Platform[J]. Acta Sedimentologica Sinica, 2015, 33(6): 1111-1125.
[26] 陈吉涛,韩作振,张晓蕾,等. 鲁西芙蓉统条带灰岩早期成岩变形构造:竹叶状砾屑灰岩形成机理探讨[J]. 中国科学(D辑):地球科学,2009,39(12):1732-1743.

Chen Jitao, Han Zuozhen, Zhang Xiaolei, et al. Early diagenetic deformation structures of the Furongian ribbon rocks in Shandong province of China:A new perspective of the genesis of limestone conglomerates[J]. Science China (Seri. D): Earth Sciences, 2009, 39(12): 1732-1743.
[27] 宋金民,杨迪,李朋威,等. 中国碳酸盐风暴岩发育特征及其地质意义[J]. 现代地质,2012,26(3):589-600.

Song Jinmin, Yang Di, Li Pengwei, et al. Development characteristics and geological significance of carbonate tempestites in China[J]. Geoscience, 2012, 26(3): 589-600.
[28] 王祥珍. 关于“竹叶状灰岩”的命名、分类、分布和形成机理的探讨[J]. 矿物岩石,1981(5):31-41.

Wang Xiangzhen. Discussion on the name, classification, distribution and genesis of flat-pebble limestone conglomerates[J]. Journal of Mineralogy and Petrology, 1981(5): 31-41.
[29] Kwon Y K, Chough S K, Choi D K, et al. Origin of limestone conglomerates in the Choson Supergroup (Cambro-Ordovician), mid-east Korea[J]. Sedimentary Geology, 2002, 146(3/4): 265-283.
[30] 陈世悦,杨怀宇,李文涛,等. 贵州紫云地区上泥盆统风暴重力流沉积特征及地质意义[J]. 地质学报,2010,84(1):127-132.

Chen Shiyue, Yang Huaiyu, Li Wentao, et al. The sedimentary characteristics of the Upper Devonian tempestite and gravity flow in the Ziyun area, Guizhou and its geological implications[J]. Acta Geologica Sinica, 2010, 84(1): 127-132.
[31] 张兴亮,舒德干. 寒武纪大爆发的因果关系[J]. 中国科学(D辑):地球科学,2014,44(6):1155-1170.

Zhang Xingliang, Shu Degan. Causes and consequences of the Cambrian explosion[J]. Science China (Seri. D): Earth Sciences, 2014, 44(6): 1155-1170.
[32] Huang J P, Li X B, He W X, et al. Formation environment and development models for the Lower Cambrian source rocks of the southern North China Plate, China[J]. ACS Omega, 2020, 5(14): 8001-8011.
[33] Hearing T W W, Pohl A, Williams M, et al. Quantitative comparison of geological data and model simulations constrains Early Cambrian geography and climate[J]. Nature Communications, 2021, 12(1): 3868.
[34] Babcock L E, Peng S C, Brett C E, et al. Global climate, sea level cycles, and biotic events in the Cambrian Period[J]. Palaeoworld, 2015, 24(1/2): 5-15.
[35] Marsaglia K M, Klein G D. The paleogeography of Paleozoic and Mesozoic storm depositional systems[J]. The Journal of Geology, 1983, 91(2): 117-142.
[36] Zhao G C, Wang Y J, Huang B C, et al. Geological reconstructions of the East Asian blocks: From the breakup of Rodinia to the assembly of Pangea[J]. Earth-Science Reviews, 2018, 186: 262-286.
[37] Torsvik T H, van der Voo R, Preeden U, et al. Phanerozoic polar wander, palaeogeography and dynamics[J]. Earth-Science Reviews, 2012, 114(3/4): 325-368.
[38] Ford D, Golonka J. Phanerozoic paleogeography, paleoenvironment and lithofacies maps of the circum-Atlantic margins[J]. Marine and Petroleum Geology, 2003, 20(3/4): 249-285.
[39] 周肖贝,李江海,王洪浩,等. 寒武纪全球板块构造与古地理环境再造[J]. 海相油气地质,2014,19(2):1-7.

Zhou Xiaobei, Li Jianghai, Wang Honghao, et al. Reconstruction of Cambrian global paleo-plates and paleogeography[J]. Marine Origin Petroleum Geology, 2014, 19(2): 1-7.