Ager D V. The Nature of the Stratigraphical Record[M]. London: MacMillan, 1973: 1-114.
[2]
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.
[3]
Kumar N, Sanders J E. Storm deposits[M]//Fairbridge R W, Bourgeois J, eds. Encyclopedia of Sedimentology. Stroudsburg, PA: Dowden Hutchinson and Ross, 1978: 767-770.
[4]
Aigner T. Calcareous tempestites: Storm-dominated stratification in upper Muschelkalk limestones (Middle Trias, SW-Germany)[M] //Einsele G, Seilacher A, eds. Cyclic and Event Stratification. Heidelberg. New York, Berlin Heidelberg: Springer-Verlag, 1982: 180-198.
[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(1):55-69. [Liu Baojun, Zhang Jiqing, Xu Xiaosong. On the calcareous tempestites in the Low Permian of Silong, Xingwen, Sichuan[J]. Acta Geologica Sinica, 1986(1): 55-69.]
[6]
吴崇筠,裘亦楠,朱国华. 暴风浪形成的丘状交错层理和洼状交错层理[J]. 石油勘探与开发,1983(4):77-80. [Wu Chongyun, Qiu Yinan, Zhu Guohua. The storm depositional Hummocky cross-stratification and sunken cross-stratification [J]. Petroleum Exploration and Development, 1983(4): 77-80.]
[7]
严钦尚. 论滨岸和浅海的风暴沉积[J]. 海洋与湖沼,1984,15(1):14-20. [Yan Qinshang. Overview of the storm-generated deposits on nearshore zone and open shelf[J]. Oceanologia et Limnologia Sinica, 1984, 15(1): 14-20.]
[8]
余素玉. 沉积学研究的新领域-风暴沉积[J]. 地质科技情报,1985,4(2):48-51. [Yu Suyu. A new domain of sedimentary research-storm deposition[J]. Geological Science and Technology Information, 1985, 4(2): 48-51.]
[9]
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):1-23. [Meng Xianghua, Qiao Xiufu, Ge Ming, et al. Study on ancient shallow sea carbonate storm deposits (tempestites) in North China and Dingjiatan model of facies sequences[J]. Acta Sedimentologica Sinica, 1986, 4(2): 1-23.]
[10]
袁静. 惠民凹陷古近系风暴沉积研究[J]. 中国石油大学学报:自然科学版,2006,30(4):1-6. [Yuan Jing. Study of tempestite sedimentary of Paleogene in Huimin depression[J]. Journal of China University of Petroleum, 2006, 30(4): 1-6.]
[11]
姜在兴,赵澂林,刘孟慧,等. 东濮凹陷西部湖相风暴沉积的初步研究[J]. 沉积学报,1990,8(1):107-114. [Jiang Zaixing, Zhao Chenglin, Liu Menghui, et al. Preliminary research into lacustrine storm-current deposits: An example from the western Dongpu depression[J]. Acta Sedimentologica Sinica, 1990, 8(1): 107-114.]
[12]
高山林,陈海涨,窦伟坦,等. 鄂尔多斯盆地延长组的湖泊风暴沉积[J]. 沉积学报,1999,17(增刊):758-762. [Gao Shanlin, Chen Haihong, Dou Weitan, et al. Lacustrine storm sediment in Yanchang Formation of Ordos Basin[J]. Acta Sedimentologica Sinica, 1999, 17(Suppl.): 758-762.]
[13]
孙顺才,伍贻范. 太湖现代风暴流沉积特征[J]. 科学通报,1986,31(7):537-541. [Sun Shuncai, Wu Yifan. The modern storm depositional character of Lake Taihu[J]. Chinese Science Bulletin, 1986, 31(7): 537-541.]
[14]
郭正吾,邓康龄,韩永辉,等. 四川盆地形成与演化[M]. 北京:地质出版社,1996. [Guo Zhengwu, Deng Kangling, Han Yonghui, et al. The Formation and Evolution of Sichuan Basin[M]. Beijing: Geological Publishing House, 1996.]
[15]
汪泽成,赵文智,张林,等. 四川盆地构造层序与天然气勘探[M]. 北京:地质出版社,2002:80-84. [Wang Zecheng, Zhao Wenzhi, Zhang Lin, et al. Tectonic Sequence and Natural Gas Exploration in Sichuan Basin [M]. Beijing: Geological Publishing House, 2002: 80-84.]
汪少勇,李建忠,李登华,等. 川中地区公山庙油田侏罗系大安寨段致密油资源潜力分析[J]. 中国地质,2013,40(2):477-486. [Wang Shaoyong, Li Jianzhong, Li Denghua, et al. The potential of tight oil resource in Jurassic Da'anzhai Formation of the Gongshanmiao oil field, central Sichuan Basin [J]. Geology in China, 2013, 40(2): 477-486.]
[18]
吴因业,张天舒,陶士振,等. 深水湖盆沉积砂体的层序地层分析-以四川侏罗系为例[J]. 沉积学报,2013,31(5):798-806. [Wu Yinye, Zhang Tianshu, Tao Shizhen, et al. Sequence stratigraphy of depositional sandbodies in the deep-water lake basin: A case from Jurassic Sichuan[J]. Acta Sedimentologica Sinica, 2013, 31(5): 798-806.]
[19]
张晓鹏. 内陆湖泊非均质碳酸盐岩油藏勘探技术方法研究[D]. 成都:成都理工大学,2005. [Zhang Xiaopeng. Studies of the exploration technology of interior lake heterogeneous carbonate reservoirs [D]. Chengdu: Chengdu University of Technology, 2005.]
[20]
倪超,郝毅,厚刚福,等. 四川盆地中部侏罗系大安寨段含有机质泥质介壳灰岩储层的认识及其意义[J]. 海相油气地质,2012,17(2):45-56. [Ni Chao, Hao Yi, Hou Gangfu, et al. Cognition and significance of Lower Jurassic Da'anzhai organic muddy shell limestone reservoir in central Sichuan Basin [J]. Marine Origin Petroleum Geology, 2012, 17(2): 45-56.]
[21]
黄开伟,王兴志,张帆,等. 川中小潼场地区大安寨段储层特征研究[J]. 重庆科技学院院报:自然科学版,2010,12(5):14-18, 41. [Huang Kaiwei, Wang Xingzhi, Zhang Fan, et al. Reservoir characteristics of Da'anzhai Member in Xiaotongchang area of central Sichuan[J]. Journal of Chongqing University of Science and Technology: Natural Sciences Edition, 2010, 12(5): 14-18, 41.]
[22]
杜远生,周道华,龚淑云,等. 甘肃靖远-景泰泥盆系湖相风暴岩及其古地理意义[J]. 矿物岩石,2001,21(3):69-73. [Du Yuansheng, Zhou Daohua, Gong Shuyun, et al. Tempestite and its palaeogeographical significance of Devonian in Jingyuan and Jingtai Counties, Gansu province [J]. Journal of Mineralogy and Petrology, 2001, 21(3): 69-73.]
Sherman D J, Greenwood B. Hummocky cross-stratification and post-vortex ripples: Length scales and hydraulic analysis[J]. Sedimentology, 1989, 36(6): 981-986.
[25]
Basilici G, de Luca P H V, Oliveira E P. A depositional model for a wave-dominated open-coast tidal flat, based on analyses of the Cambrian-Ordovician Lagarto and Palmares formations, north-eastern Brazil[J]. Sedimentology, 2012, 59(5): 1613-1639.
[26]
Colombié C, Schnyder J, Carcel D. Shallow-water marl-limestone alternations in the Late Jurassic of western France: Cycles, storm event deposits or both?[J]. Sedimentary Geology, 2012, 271-272: 28-43.
[27]
胡明毅,贺萍. 潮坪风暴沉积特征及其研究意义[J]. 地球科学进展,2002,17(3):391-395. [Hu Mingyi, He Ping. The study of tidal storm deposits and its research significance[J]. Advance in Earth Sciences, 2002, 17(3): 391-395.]
[28]
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.]
[29]
刘树臣. 风暴岩的基本特征及其与浊积岩的区别标志[J]. 岩相古地理,1989,43(5):44-55,43. [Liu Shuchen. The basic character of tempesites and the differences compared with turbidite[J]. Sedimentary Facies and Palaeogeography, 1989, 9(5): 44-55, 43.]
[30]
Greenwood B, Sherman D J. Hummocky cross-stratification in the surf zone: Flow parameters and bedding genesis[J]. Sedimentology, 1986, 33(1): 33-45.
[31]
师庆民,冯乐,窦鲁星,等. 基于驻波理论解释丘状交错层理-以徐州地区贾园组风暴沉积为例[J]. 沉积学报,2013,31(6):1008-1013. [Shi Qingmin, Feng Le, Dou Luxing, et al. Explaining hummocky cross-stratification standing wave: A case from Jiayuan Group based on the theory of storm deposits in Xuzhou [J]. Acta Sedimentologica Sinica, 2013, 31(6): 1008-1013.]
[32]
赵灿,陈孝红,李旭兵,等. 峡东地区埃迪卡拉系灯影组风暴岩的发现及其环境意义[J]. 地质学报,2013,87(12):1901-1912. [Zhao Can, Chen Xiaohong, Li Xubing, et al. Characteristics of tempestite of Ediacaran Dengying Formation, in the Eastern Yangtze gorges area and its geological significance [J]. Acta Geologica Sinica, 2013, 87(12): 1901-1912.]
[33]
马永生,陈洪德,王国力,等. 中国南方层序地层与古地理[M]. 北京:科学出版社,2009:1-603. [Ma Yongsheng, Chen Hongde, Wang Guoli, et al. Sequence Stratigraphy and Paleogeorgaphy of South China[M]. Beijing: Science Press, 2009: 1-603.]
[34]
魏钦廉,王起琮,陈亮,等. 山西中阳上寒武统三山子组下部风暴岩沉积特征及其成因[J]. 海相油气地质,2013,18(4):41-45. [Wei Qinlian, Wang Qicong, Chen Liang, et al. Sedimentary characteristics and genesis of Upper Cambrian Sanshanzi tempestite at Zhongyang in Shanxi province[J]. Marine Origin Petroleum Geology, 2013, 18(4): 41-45.]
