Ager D V. The Nature of the Stratigraphical Record[M]. New York: MacMillan, 1973: 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. Characteristics of shoreface storm deposits: modern and ancient examples[J]. Journal of Sedimentary Petrology, 1976, 46(1): 145-162.
[4]
Kumar N, Sanders J E. Storm deposits[M]//Fairbridge R W, Bourgeois J. Encyclopedia of Sedimentology, Stmudsburg. PA: Dowden Hutchinson and Ross, 1978: 767-770.
[5]
Aigner T. Schill-tmlpestite im Oberen Muschelkalk(Trias, SW-Deutschland)[J]. Neues Jahrbuch für Geologie und Pal?ontologie-Abhandlungen, 1979, 156: 285-304.
[6]
Aigner T. Calcareous tempestites: storm-dominated stratification in upper Muschelkalk limestones (Middle Trias, SW-Germany)[M]//Einsele G, Serlacher A. Cyclic and Event Stratification. Berlin, Heidelberg: Springer-Verlag, 1982: 180-198.
[7]
魏钦廉,郑荣才,周刚,等. 龙门山甘溪组谢家湾段风暴岩沉积特征及其意义[J]. 中国地质,2011,38(5):1282-1288.[Wei Qinlian, Zheng Rongcai, Zhou Gang, et al. Clastic tempestite in Xiejiawan Member of Ganxi Formation within Longmenshan area and its significance[J]. Geology in China, 2011, 38(5): 1282-1288.]
[8]
张廷山,兰光志,陈晓慧,等. 川西北早志留世陆源碎屑—碳酸盐混积缓坡[J]. 沉积学报,1995,13(4):27-34.[Zhang Tingshan, Lan Guangzhi, Chen Xiaohui, et al. Early Silurian siliciclastic-carbonate ramp deposits in NW Sichuan[J]. Acta Sedimentologica Sinica, 1995, 13(4): 27-34.]
[9]
马文辛,刘树根,黄文明,等. 四川盆地东南缘志留系古油藏特征及其油气勘探意义[J]. 石油与天然气地质,2012,33(3):432-441.[Ma Wenxin, Liu Shugen, Huang Wenming, et al. Characteristics of Silurian Paleo-oil reservoirs and their significance for petroleum exploration on the southeast margin of Sichuan Basin[J]. Oil & Gas Geology, 2012, 33(3): 432-441.]
[10]
张茜. 米仓山隆升时代的沉积学制约[D]. 西安:西北大学,2010.[Zhang Qian. Sedimentary evidence constraint on the uplift of the Micang Shan[D]. Xi'an: Northwest University, 2010.]
[11]
魏显贵,杜思清,何政伟,等. 米仓山地区构造演化[J]. 矿物岩石,1997,17(增刊):107-113.[Wei Xiangui, Du Siqing, He Zhengwei, et al. The tectonic evolution of Micangshan area[J]. Journal of Mineralogy and Petrology, 1997, 17(Suppl.): 107-113.]
[12]
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]. 地质科学情报,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.].
[13]
何镜宇,孟祥化. 沉积岩和沉积相模式及建造[M].北京:地质出版社,1987.[He Jingyu, Meng Xianghua. Sediments and Sedimentary Facies Model and Construction[M]. Beijing: Geological Publishing House, 1987.]
[14]
彭靖淞,刘树根,赵霞飞,等. 川西中三叠统天井山组风暴沉积的发现及古地理意义[J]. 岩性油气藏,2009,21(1):84-88.[Peng Jingsong, Liu Shugen, Zhao Xiafei, et al. Discovery of tempestite in Middle Triassic Tianjingshan Formation in western Sichuan and its paleogeographic significance[J]. Lithologic Reservoirs, 2009, 21(1): 84-88.]
[15]
梁桂香. 风暴沉积及其构造背景[J]. 世界地质,1994,13(3):131-143.[Liang Guixiang. Sedimentary and tectonic setting of the storm[J]. The World Geology, 1994, 13(3): 131-143.]
[16]
邵龙义. 湘中下石炭统风暴岩的研究[J]. 地质科学,1993,28(4):336-346.[Shao Longyi. Study on tempestites of Lower Carboniferous in Central Hunan, South China[J]. Scientia Geologica Sinica, 1993, 28(4): 336-346.]
[17]
张哲,杜远生,舒雪松,等. 鄂东南地区早三叠世风暴沉积序列及其环境意义[J]. 地质科学情报,2006,25(2):29-34.[Zhang Zhe, Du Yuansheng, Shu Xuesong, et al. Sedimentary successions of the Early Triassic tempestite in southeastern Hubei province and their environment significance[J]. Geological Science and Technology Information, 2006, 25(2): 29-34.]
[18]
张瑞林,申少宁,武征. 甘肃迭部当多沟擦阔合组的风暴沉积[J]. 中国地质科学院西安地质矿产研究所刊,1988,21(1):65-73.[Zhang Ruilin, Sheng Shaoning, Wu Zheng. First finding on storm sedimentation at the profile of Dangduogou, Gansu province[J]. Bull. Xi'an Inst. Geol. Min. Res., Chinese Acad. Geol. Sci., 1988, 21(1): 65-73.]
[19]
张廷山,侯方浩,高卫东,等. 川西北地区早志留世风暴岩及其环境与古生态意义[J]. 沉积学报,1993,11(2):66-74.[Zhang Tingshan, Hou Fanghao, Gao Weidong, et al. Tempestites and the environmental paleoecological significance of Early Silurian, NW Sichuan Area[J]. Acta Sedimentologica Sinica, 1993, 11(2): 66-74.]
[20]
赖志云,赖伟庆. 丘状交错层理的成因探讨[J]. 石油天然气学报,2010,32(5):42-47.[Lai Zhiyun, Lai Weiqing. Study on the genesis of moundy cross-stratification[J]. Journal of Oil and Gas Technology, 2010, 32(5): 42-47.]
[21]
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):589-603.[Song Jinmin, Yang Di, Li Pengwei, et al. Development characteristics and geological significance of carbonate tempestites in China[J]. Geoscience, 2012, 26(3): 589-603.]
[22]
葛思良,郝子文,李庆玉,等.中华人民共和国区域地质测量报告(南江幅)[R]. 成都:地质部四川省地质局,1965.[Ge Siliang, Hao Ziwen, Li Qingyu, et al. The regional geological survey report regional of People's Republic of China[R]. Chengdu: Sichuan Provincial Bureau of Geology Department of Geology, 1965.]
[23]
杜远生,韩欣. 滇中中元古代昆阳群因民组碎屑风暴岩及其意义[J]. 沉积学报,2000,18(2):259-262.[Du Yuansheng, Han Xin. Clastic tempestite and its significance in Yinmin Formation, Kunyang Group (Mesoproterozoic) in Central Yunnan province[J]. Acta Sedimentologica Sinica, 2000, 18(2): 259-262.]
[24]
杨宝忠,杨坤光,夏文臣. 鄂东黄石地区中上寒武统风暴岩的发现及意义[J]. 地质科技情报,2007,26(3):33-36.[Yang Baozhong, Yang Kunguang, Xia Wenchen. Discovery of Middle-Upper Cambrian tempestites and its significance in Huangshi, eastern Hubei province[J]. Geological Science and Technology Information, 2007, 26(3): 33-36.]
[25]
卢小龙,孙林华,陈松. 安徽巢湖市二叠系栖霞组生物碎屑的数量及其地质意义[J]. 中国煤炭地质,2010,22(7):7-13.[Lu Xiaolong, Sun Linhua, Chen Song. Bioclast quantity and its geological significance in Permian Qixia Formation, Chaohu city[J]. Coal Geology of China, 2010, 22(7): 7-13.]