[1] Simms M J, Ruffell A H. Synchroneity of climatic change and extinctions in the Late Triassic[J]. Geology, 1989, 17(3): 265-268.
[2] Ogg J G. The mysterious Mid-Carnian “Wet Intermezzo” global event[J]. Journal of Earth Science, 2015, 26(2): 181-191.
[3] 赵向东,薛乃华,王博,等. 三叠纪卡尼期湿润幕事件研究进展[J]. 地层学杂志,2019,43(3):306-314.

Zhao Xiangdong, Xue Naihua, Wang Bo, et al. Carnian (Late Triassic) pluvial episode: Current status and future challenges[J]. Journal of Stratigraphy, 2019, 43(3): 306-314.
[4] Kozur H W, Bachmann G H. The Middle Carnian wet intermezzo of the Stuttgart Formation (Schilfsandstein), Germanic Basin[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2010, 290(1/2/3/4): 107-119.
[5] Klausen T G, Nyberg B, Helland-Hansen W. The largest delta plain in Earth's history[J]. Geology, 2019, 47(5): 470-474.
[6] 张磊. 古特提斯—泛大洋地区三叠纪重要环境气候事件的古海洋学研究[D]. 武汉:中国地质大学,2017:168-175.

Zhang Lei. Paleoceanographic characteristics of key environmental and climatic events during the Triassic in the Paleo-Tethys and Panthalassic Oceans[D]. Wuhan: China University of Geosciences, 2017: 168-175.
[7] 金鑫,时志强,王艳艳,等. 晚三叠世中卡尼期极端气候事件:研究进展及存在问题[J]. 沉积学报,2015,33(1):105-115.

Jin Xin, Shi Zhiqiang, Wang Yanyan, et al. Mid-Carnian (Late Triassic) extreme climate event: Advances and unsolved problems[J]. Acta Sedimentologica Sinica, 2015, 33(1): 105-115.
[8] Schlager W, Schöllnberger W. Das Prinzip stratigraphischer Wenden in der Schichtfolge der Nördlichen Kalkalpen[J]. Mitteilungen der Geologischen Gesellschaft in Wien, 1974, 66-67: 165-193.
[9] Hornung T, Brandner R. Biostratigraphy of the Reingraben Turnover (Hallstatt Facies Belt): Local black shale events controlled by the regional tectonics, climatic change and plate tectonics[J]. Facies, 2005, 51: 460-479.
[10] 时志强,张华,曾德勇,等. 龙门山前缘上三叠统卡尼阶特征及其古环境、古气候意义[J]. 成都理工大学学报(自然科学版),2010,37(4):424-431.

Shi Zhiqiang, Zhang Hua, Zeng Deyong, et al. Characters of Carnian in the frontal area of Mt. Longmenshan: Implications for palaeoenvironment and paleoclimate[J]. Journal of Chengdu University of Technology (Science & Technology Edition), 2010, 37(4): 424-431.
[11] 李相博,刘化清,邓秀芹,等. 干旱环境河流扇概念与鄂尔多斯盆地延长组“满盆砂”成因新解[J]. 沉积学报,2021,39(5):1208-1221.

Li Xiangbo, Liu Huaqing, Deng Xiuqin, et al. The concept of fluvial fans in an arid environment: A new explanation of the origin of “sand-filled basins” in the Yanchang Formation, Ordos Basin[J]. Acta Sedimentologica Sinica, 2021, 39(5): 1208-1221.
[12] 李相博,刘化清,黄军平,等. 干湿气候交替与内陆湖盆河流扇砂体的形成与分布:以鄂尔多斯盆地延长组为例[J]. 地质学报,2021,95:1-17.

Li Xiangbo, Liu Huaqing, Huang Junping, et al. Alternation of arid-humid climate and formation and distribution of fluvial fan sand in the central area of inland lake basin-taking Yanchang Formation in Ordos Basin as an example[J]. Acta Geologica Sinica, 2021, 95: 1-17.
[13] Simms M J, Ruffell A H. Climatic and biotic change in the Late Triassic[J]. Journal of the Geological Society, 1990, 147(2): 321-327.
[14] Hornung T. Multistratigraphy of the Draxllehen quarry near Berchtesgaden (Tuvalian-Lacian 2): Implication for halstatt limestone sedimentation and palaeoclimate in the aftermath of the “Carnian Crisis”[J]. Austrian Journal of Earth Science, 2007, 100: 82-89.
[15] Rigo M, Preto N, Roghi G, et al. A rise in the carbonate compensation depth of western tethys in the Carnian (Late Triassic): Deep-water evidence for the Carnian Pluvial Event[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2007, 246(2/3/4): 188-205.
[16] Roghi G, Gianolla P, Minarelli L, et al. Palynological correlation of Carnian humid pulses throughout western Tethys[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2010, 290(1/2/3/4): 89-106.
[17] Colombi C E, Parrish J T. Late Triassic environmental evolution in southwestern Pangea: Plant taphonomy of the Ischigualasto Formation[J]. PALAIOS, 2008, 23(11/12): 778-795.
[18] Hochuli P A, Vigran J O. Climate variations in the Boreal Triassic—inferred from palynological records from the Barents Sea[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2010, 290(1/2/3/4): 20-42.
[19] Nakada R, Ogawa K, Suzuki N, et al. Late Triassic compositional changes of Aeolian dusts in the pelagic Panthalassa: Response to the continental climatic change[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2014, 393: 61-75.
[20] 时志强,钱利军,曾德勇,等. 晚三叠世卡尼期碳酸盐生产危机在东特提斯地区的地质记录[J]. 地质论评,2010,56(3):321-328.

Shi Zhiqiang, Qian Lijun, Zeng Deyong, et al. Geological records of Late Triassic Carnian carbonate productivity crisis in eastern Tethys region (SW China)[J]. Geological Review, 2010, 56(3): 321-328.
[21] Hornung T, Krystyn L, Brandner R. A Tethys-wide mid-Carnian (Upper Triassic) carbonate productivity crisis: Evidence for the Alpine Reingraben event from Spiti (Indian Himalaya)?[J]. Journal of Asian Earth Sciences, 2007, 30(2): 285-302.
[22] 刘化清,李相博,陈启林,等. 鄂尔多斯盆地延长组若干石油地质问题分析[M]. 北京:科学出版社,2013.

Liu Huaqing, Li Xiangbo, Chen Qilin, et al. Analysis of some petroleum geological problems of Yanchang Formation in Ordos Basin[M]. Beijing: Science Press, 2013.
[23] 李江海,姜洪福. 全球古板块再造、岩相古地理及古环境图集[M]. 北京:地质出版社,2013.

Li Jianghai, Jiang Hongfu. Atlas of global paleoplate reconstruction, lithofacies paleogeography and paleoenvironment[M]. Beijing: Geological Publishing House, 2013.
[24] 邓秀芹,罗安湘,张忠义,等. 秦岭造山带与鄂尔多斯盆地印支期构造事件年代学对比[J]. 沉积学报,2013,31(6):939-953.

Deng Xiuqin, Luo Anxiang, Zhang Zhongyi, et al. Geochronological comparison on indosinian tectonic events between Qinling orogeny and Ordos Basin[J]. Acta Sedimentologica Sinica, 2013, 31(6): 939-953.
[25] 童金南,楚道亮,梁蕾,等. 中国三叠纪综合地层和时间框架[J]. 中国科学(D辑):地球科学 2019,49(1):194-226.

Tong Jinnan, Chu Daoliang, Liang Lei, et al. Triassic integrative stratigraphy and timescale of China[J]. Science China (Seri. D): Earth Sciences, 2019, 49(1): 194-226.
[26] 邓秀芹,李文厚,刘新社,等. 鄂尔多斯盆地中三叠统与上三叠统地层界线讨论[J]. 地质学报,2009,83(8):1089-1096.

Deng Xiuqin, Li Wenhou, Liu Xinshe, et al. Discussion on the stratigraphic boundary between Middle Triassic and Upper Triassic[J]. Acta Geologica Sinica, 2009, 83(8): 1089-1096.
[27] 吉利明,祝幼华. 鄂尔多斯盆地西南部甘肃西峰地区延长组孢粉组合及古气候研究[J]. 微体古生物学报,2013,30(4):367-378.

Ji Liming, Zhu Youhua. Sporo-pollen assemblages and Paleoclimate of the Yanchang Formation in the Xifeng area, Southwestern Ordos Basin, Gansu province, NW, China[J]. Acta Micropalaeontologica Sinica, 2013, 30(4): 367-378.
[28] 邱振,邹才能. 非常规油气沉积学:内涵与展望[J]. 沉积学报,2020,38(1):1-29.

Qiu Zhen, Zou Caineng. Unconventional petroleum sedimentology: Connotation and prospect[J]. Acta Sedimentologica Sinica, 2020, 38(1): 1-29.
[29] 樊隽轩,彭善池,侯旭东,等. 国际地层委员会官网与《国际年代地层表》(2015/01版)[J]. 地层学杂志,2015,39(2):125-134.

Fan Junxuan, Peng Shanchi, Hou Xudong, et al. Official website of the international commission on stratigraphy and the release of the international chronostratigraphic chart (V2015/01)[J]. Journal of Stratigraphy, 2015, 39(2): 125-134.
[30] Zhang K, Liu R, Liu Z J, et al. Geochemical characteristics and geological significance of humid climate events in the Middle-Late Triassic (Ladinian-Carnian) of the Ordos Basin, central China[J]. Marine and Petroleum Geology, 2021, 131: 105179.
[31] 邓胜徽,卢远征,罗忠,等. 鄂尔多斯盆地延长组的划分、时代及中—上三叠统界线[J]. 中国科学(D辑):地球科学,2018,48(10):1293-1311.

Deng Shenghui, Lu Yuanzheng, Luo Zhong, et al. Subdivision and age of the Yanchang Formation and the Middle/Upper Triassic boundary in Ordos Basin, north China[J]. Science China (Seri. D): Earth Sciences, 2018, 48(10): 1293-1311.
[32] Jin X, Baranyi V, Caggiati M, et al. Middle Triassic lake deepening in the Ordos Basin of north China linked with global sea-level rise[J]. Global and Planetary Change, 2021, 207: 103670.
[33] 吉利明,吴涛,李林涛. 陇东三叠系延长组主要油源岩发育时期的古气候特征[J]. 沉积学报,2006,24(3):426-431.

Ji Liming, Wu Tao, Li Lintao. Paleoclimatic characteristics during sedimentary period of main source rocks of Yanchang Formation (Triassic) in eastern Gansu[J]. Acta Sedimentologica Sinica, 2006, 24(3): 426-431.
[34] Ji L M, Meng F W. Palynology of Yanchang Formation of Middle and Late Triassic in eastern Gansu province and its paleoclimatic significance[J]. Journal of China University of Geosciences, 2006, 17(3): 209-220.
[35] 王多云,辛补社,杨华,等. 鄂尔多斯盆地延长组长7底部凝灰岩锆石SHRIMP U-Pb年龄及地质意义[J]. 中国科学(D辑):地球科学,2014,44(10):2160-2171.

Wang Duoyun, Xin Bushe, Yang Hua, et al. Zircon SHRIMP U-Pb age and geological implications of tuff at the bottom of Chang-7 member of Yanchang Formation in the Ordos Basin[J]. Science China (Seri. D): Earth Sciences, 2014, 44(10): 2160-2171.
[36] 林畅松. 盆地沉积动力学:研究现状与未来发展趋势[J]. 石油与天然气地质,2019,40(4):685-700.

Lin Changsong. Sedimentary dynamics of basin: Status and trend[J]. Oil & Gas Geology, 2019, 40(4): 685-700.
[37] 朱筱敏,葛家旺,赵宏超,等. 陆架边缘三角洲研究进展及实例分析[J]. 沉积学报,2017,35(5):945-957.

Zhu Xiaomin, Ge Jiawang, Zhao Hongchao, et al. Development of shelf-edge delta researches and typical case analyses[J]. Acta Sedimentologica Sinica, 2017, 35(5): 945-957.
[38] Bullimore S A, Henriksen S, Liestøl F M, et al. Clinoform stacking patterns, shelf-edge trajectories and facies associations in Tertiary coastal deltas, offshore Norway: Implications for the prediction of lithology in prograding systems[J]. Norsk Geologisk Tidsskrift, 2005, 85(1): 169-187.
[39] Bullimore S A, Helland-Hansen W. Trajectory analysis of the Lower Brent Group (Jurassic), northern North Sea: Contrasting depositional patterns during the advance of a major deltaic system[J]. Basin Research, 2009, 21(5): 559-572.
[40] Helland-Hansen W, Hampson G J. Trajectory analysis: Concepts and applications[J]. Basin Research, 2009, 21(5): 454-483.
[41] Henriksen S, Helland-Hansen W, Bullimore S. Relationships between shelf-edge trajectories and sediment dispersal along depositional dip and strike: A different approach to sequence stratigraphy[J]. Basin Research, 2011, 23(1): 3-21.
[42] 丛富云,徐尚. 陆架边缘迁移轨迹研究现状及应用前景[J]. 地球科学进展,2017,32(9):937-948.

Cong Fuyun, Xu Shang. Research status and application prospect of shelf-edge trajectory analysis[J]. Advances in Earth Science, 2017, 32(9): 937-948.
[43] 陈亮,于水,胡孝林,等. 应用陆坡形态—迁移轨迹组合法寻找大型富砂深水扇[J]. 沉积学报,2018,36(1):92-100.

Chen Liang, Yu Shui, Hu Xiaolin, et al. Application from combination of slope geometries and shelf-edge trajectories to find large-scale, sand-rich deepwater fan[J]. Acta Sedimentologica Sinica, 2018, 36(1): 92-100.
[44] 王苏民,张振克. 中国湖泊沉积与环境演变研究的新进展[J]. 科学通报,1999,44(6):579-587.

Wang Sumin, Zhang Zhenke. New progress of lake sediments and environmental changes research in China[J]. Chinese Science Bulletin, 1999, 44(6): 579-587.
[45] Dal Corso J, Mietto P, Newton R J, et al. Discovery of a major negative δ13C spike in the Carnian (Late Triassic) linked to the eruption of Wrangellia flood basalts[J]. Geology, 2012, 40(1): 79-82.
[46] Dal Corso J, Gianolla P, Newton R J, et al. Carbon isotope records reveal synchronicity between carbon cycle perturbation and the “Carnian Pluvial Event” in the Tethys realm (Late Triassic)[J]. Global and Planetary Change, 2015, 127: 79-90.
[47] Mueller S, Krystyn L, Kürschner W M. Climate variability during the Carnian Pluvial Phase—a quantitative palynological study of the Carnian sedimentary succession at Lunz am See, northern Calcareous Alps, Austria[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2016, 441: 198-211.
[48] Sun Y D, Wignall P B, Joachimski M M, et al. Climate warming, euxinia and carbon isotope perturbations during the Carnian (Triassic) Crisis in South China[J]. Earth and Planetary Science Letters, 2016, 444: 88-100.
[49] 吕奇奇,罗顺社,付金华,等. 湖泊深水重力流沉积露头精细解剖:以鄂尔多斯盆地瑶曲剖面长7油层组为例[J]. 地质学报,2017,91(3):617-628.

Qiqi Lü, Luo Shunshe, Fu Jinhua, et al. Outcrop-based analysis of a deep-water gravity flow sediments in lake: A case study from the Chang 7 of Yaoqu section, Ordos Basin[J]. Acta Geologica Sinica, 2017, 91(3): 617-628.
[50] 付金华,李士祥,牛小兵,等. 鄂尔多斯盆地三叠系长7段页岩油地质特征与勘探实践[J]. 石油勘探与开发,2020,47(5):870-883.

Fu Jinhua, Li Shixiang, Niu Xiaobing, et al. Geological characteristics and exploration of shale oil in Chang 7 member of Triassic Yanchang Formation, Ordos Basin, NW China[J]. Petroleum Exploration and Development, 2020, 47(5): 870-883.
[51] Yang R C, Jin Z J, van Loon A J, et al. Climatic and tectonic controls of lacustrine hyperpycnite origination in the Late Triassic Ordos Basin, central China: Implications for unconventional petroleum development: Reply[J]. AAPG Bulletin, 2019, 103(2): 511-514.
[52] 吉利明,王少飞,徐金鲤. 陇东地区延长组疑源类组合特征及其古环境意义[J]. 地球科学:中国地质大学学报,2006,31(6):798-806.

Ji Liming, Wang Shaofei, Xu Jinli. Acritarch assemblage in Yanchang Formation in eastern Gansu province and its environmental implications[J]. Earth Science: Journal of China University of Geosciences, 2006, 31(6): 798-806.
[53] 张才利,高阿龙,刘哲,等. 鄂尔多斯盆地长7油层组沉积水体及古气候特征研究[J]. 天然气地球科学,2011,22(4):582-587.

Zhang Caili, Gao Along, Liu Zhe, et al. Study of character on sedimentary water and palaeoclimate for Chang 7 oil layer in Ordos Basin[J]. Natural Gas Geoscience, 2011, 22(4): 582-587.
[54] 付金华,李士祥,徐黎明,等. 鄂尔多斯盆地三叠系延长组长7段古沉积环境恢复及意义[J]. 石油勘探与开发,2018,45(6):936-946.

Fu Jinhua, Li Shixiang, Xu Liming, et al. Paleo-sedimentary environmental restoration and its significance of Chang 7 member of Triassic Yanchang Formation in Ordos Basin, NW China[J]. Petroleum Exploration and Development, 2018, 45(6): 936-946.
[55] 惠潇,侯云超,喻建,等. 大型陆相坳陷湖盆深湖区前积型地震地层特征及砂体分布规律:以鄂尔多斯盆地陇东地区延长组中段为例[J]. 沉积学报,2022,40(3):787-800.

Hui Xiao, Hou Yunchao, Yu Jian, et al. Progradational seismic strata features and distribution of sandstone in the deep-water area of a large-scale lacustrine depression basin: A case study of the middle Yanchang Formation in Longdong, Ordos Basin[J]. Acta Sedimentologica Sinica, 2022,40(3):787-800.
[56] 潘松圻,邹才能,李勇,等. 重大生物事件与化石能源形成演化:兼论地球系统框架下能源学发展[J]. 石油勘探与开发,2021,48(3):498-509.

Pan Songqi, Zou Caineng, Li Yong, et al. Major biological events and fossil energy formation: On the development of energy science under the earth system framework[J]. Petroleum Exploration and Development, 2021, 48(3): 498-509.
[57] Bohacs K M, Carroll A R, Neal J E, et al. Lake-basin type, source potential, and hydrocarbon character: An integrated sequence-stratigraphic-geochemical framework[M]//Gierlowski-Kordesch E H, Kelts K R. Lake basins through space and time. AAPG, 2000: 3-34.
[58] Carroll A R. Xenoconformities and the stratigraphic record of paleoenvironmental change[J]. Geology, 2017, 45(7): 639-642.
[59] 高远, Carroll A R,王成善. 异整合面:古环境剧变的地层记录[J]. 沉积学报,2021,39(1):46-57.

Gao Yuan, Carroll A R, Wang Chengshan. Xenocomformity: A stratigraphic surface representing fundamental and abrupt paleoenvironmental change[J]. Acta Sedimentologica Sinica, 2021, 39(1): 46-57.
[60] 邓秀芹,蔺昉晓,刘显阳,等. 鄂尔多斯盆地三叠系延长组沉积演化及其与早印支运动关系的探讨[J]. 古地理学报,2008,10(2):159-166.

Deng Xiuqin, Lin Fangxiao, Liu Xianyang, et al. Discussion on relationship between sedimentary evolution of the Triassic Yanchang Formation and the Early Indosinian Movement in Ordos Basin[J]. Journal of Palaeogeography, 2008, 10(2): 159-166.
[61] 刘化清,李相博,完颜容,等. 鄂尔多斯盆地长8油层组古地理环境与沉积特征[J]. 沉积学报,2011,29(6):1086-1095.

Liu Huaqing, Li Xiangbo, Rong Wanyan, et al. Palaeo⁃geographic and sedimentological characteristics of the Triassic Chang 8, Ordos Basin, China[J]. Acta Sedimentologica Sinica, 2011, 29(6): 1086-1095.
[62] 邓秀芹,付金华,姚泾利,等. 鄂尔多斯盆地中及上三叠统延长组沉积相与油气勘探的突破[J]. 古地理学报,2011,13(4):443-455.

Deng Xiuqin, Fu Jinhua, Yao Jingli, et al. Sedimentary facies of the Middle-Upper Triassic Yanchang Formation in Ordos Basin and breakthrough in petroleum exploration[J]. Journal of Palaeogeography, 2011, 13(4): 443-455.
[63] 杨俊杰. 鄂尔多斯盆地构造演化与油气分布规律[M]. 北京:石油工业出版社,2002:36-37.

Yang Junjie. Tectonic evolution and oil-gas reservoirs distribution in Ordos Basin[M]. Beijing: Petroleum Industry Press, 2002: 36-37.
[64] 邱欣卫,刘池洋. 鄂尔多斯盆地延长期湖盆充填类型与优质烃源岩的发育[J]. 地球学报,2014,35(1):101-110.

Qiu Xinwei, Liu Chiyang. Lake-basin filling types and development of high quality hydrocarbon source rocks in Ordos Basin in Late Triassic Yanchang Period[J]. Acta Geoscientia Sinica, 2014, 35(1): 101-110.
[65] 李士祥,牛小兵,柳广弟,等. 鄂尔多斯盆地延长组长7段页岩油形成富集机理[J]. 石油与天然气地质,2020,41(4):719-729.

Li Shixiang, Niu Xiaobing, Liu Guangdi, et al. Formation and accumulation mechanism of shale oil in the 7th member of Yanchang Formation, Ordos Basin[J]. Oil & Gas Geology, 2020, 41(4): 719-729.
[66] 李吉均. 青藏高原的地貌演化与亚洲季风[J]. 海洋地质与第四纪地质,1999,19(1):1-12.

Li Jijun. Studies on the geomorphological evolution of the Qinghai-Xizang (Tibetan) Plateau and Asian monsoon[J]. Marine Geology & Quaternary Geology, 1999, 19(1): 1-12.