[1] Hughes J D. Energy: A reality check on the shale revolution[J]. Nature, 2013, 494(7437): 307-308.
[2] Jarvie D M. Shale resource systems for oil and gas: Part 2——Shale-oil resource systems[M]//Breyer J A. Shale reservoirs-giant resources for the 21st century. Tulsa: American Association of Petroleum Geologists, 2012: 89-119.
[3] 邹才能,杨智,崔景伟,等. 页岩油形成机制、地质特征及发展对策[J]. 石油勘探与开发,2013,40(1):14-26.

Zou Caineng, Yang Zhi, Cui Jingwei, et al. Formation mechanism, geological characteristics and development strategy of nonmarine shale oil in China[J]. Petroleum Exploration and Development, 2013, 40(1): 14-26.
[4] 金之钧,白振瑞,高波,等. 中国迎来页岩油气革命了吗?[J]. 石油与天然气地质,2019,40(3):451-458.

Jin Zhijun, Bai Zhenrui, Gao Bo, et al. Has China ushered in the shale oil and gas revolution?[J]. Oil & Gas Geology, 2019, 40(3): 451-458.
[5] 赵文智,胡素云,侯连华,等. 中国陆相页岩油类型、资源潜力及与致密油的边界[J]. 石油勘探与开发,2020,47(1):1-10.

Zhao Wenzhi, Hu Suyun, Hou Lianhua, et al. Types and resource potential of continental shale oil in China and its boundary with tight oil[J]. Petroleum Exploration and Development, 2020, 47(1): 1-10.
[6] 卢双舫,薛海涛,王民,等. 页岩油评价中的若干关键问题及研究趋势[J]. 石油学报,2016,37(10):1309-1322.

Lu Shuangfang, Xue Haitao, Wang Min, et al. Several key issues and research trends in evaluation of shale oil[J]. Acta Petrolei Sinica, 2016, 37(10): 1309-1322.
[7] Hu T, Pang X Q, Jiang S, et al. Oil content evaluation of lacustrine organic-rich shale with strong heterogeneity: A case study of the Middle Permian Lucaogou Formation in Jimusaer Sag, Junggar Basin, NW China[J]. Fuel, 2018, 221: 196-205.
[8] Li M W, Chen Z H, Ma X X, et al. Shale oil resource potential and oil mobility characteristics of the Eocene-Oligocene Shahejie Formation, Jiyang Super-Depression, Bohai Bay Basin of China[J]. International Journal of Coal Geology, 2019, 204: 130-143.
[9] 邹才能, 陶士振, 侯连华,等. 非常规油气地质学[M]. 北京:地质出版社,2014:1-463.

Zou Caineng, Tao Shizhen, Hou Lianhua, et al. Unconventional petroleum geology[M]. Beijing: Geological Publishing House, 2014: 1-463.
[10] 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.
[11] 邱振,卢斌,陈振宏,等. 火山灰沉积与页岩有机质富集关系探讨:以五峰组—龙马溪组含气页岩为例[J]. 沉积学报,2019,37(6):1296-1308.

Qiu Zhen, Lu Bin, Chen Zhenhong, et al. Discussion of the relationship between volcanic ash layers and organic enrichment of black shale: A case study of the Wufeng-Longmaxi gas shales in the Sichuan Basin[J]. Acta Sedimentologica Sinica, 2019, 37(6): 1296-1308.
[12] Pedersen T F, Calvert S E. Anoxia vs. productivity: What controls the formation of organic-carbon-rich sediments and sedimentary Rocks?[J]. AAPG Bulletin, 1990, 74(4): 454-466.
[13] Bohacs K M, Carroll A R, Neal J E, et al. type Lake-basin, potential source, and hydrocarbon character: An integrated sequence-stratigraphic-geochemical framework[M]//Gierlowski-Kordesch E H, Kelts K R. Lake basins through space and time. Tulsa:American Association of Petroleum Geologists, 2000: 3-34.
[14] Katz B J. Factors controlling the development of lacustrine petroleum source rocks-An update[M]//Huc A T. Paleogeography, paleoclimate, and source rocks. Tulsa: American Association of Petroleum Geologists, 1995: 61-79.
[15] Katz B, Lin F. Lacustrine basin unconventional resource plays: Key differences[J]. Marine and Petroleum Geology, 2014, 56: 255-265.
[16] Wang M, Sherwood N, Li Z S, et al. Shale oil occurring between salt intervals in the Dongpu Depression, Bohai Bay Basin, China[J]. International Journal of Coal Geology, 2015, 152: 100-112.
[17] 张洪安,徐田武,张云献. 东濮凹陷咸化湖盆优质烃源岩的发育特征及意义[J]. 断块油气田,2017,24(4):437-441.

Zhang Hong’an, Xu Tianwu, Zhang Yunxian. Development characteristics and significance of high quality source rocks of salty lake in Dongpu Depression[J]. Fault-Block Oil and Gas Field, 2017, 24(4): 437-441.
[18] 鹿坤,左银辉,梅冰,等. 东濮凹陷古沉积环境及其对有机质丰度的影响[J]. 地质与勘探,2013,49(3):589-594.

Lu Kun, Zuo Yinhui, Mei Bing, et al. Paleo-sedimentary environments in the Dongpu Depression and their impact on organic matter abundance[J]. Geology and Exploration, 2013, 49(3): 589-594.
[19] 陈洁,鹿坤,冯英,等. 东濮凹陷不同环境烃源岩评价及生排烃特征研究[J]. 断块油气田,2012,19(1):35-38.

Chen Jie, Lu Kun, Feng Ying, et al. Evaluation on hydrocarbon source rocks in different environments and characteristics of hydrocarbon generation and expulsion in Dongpu Depression[J]. Fault-Block Oil and Gas Field, 2012, 19(1): 35-38.
[20] Hu T, Pang X Q, Jiang S, et al. Impact of paleosalinity, dilution, redox, and paleoproductivity on organic matter enrichment in a saline lacustrine rift basin: A case study of Paleogene organic-rich shale in Dongpu Depression, Bohai Bay Basin, Eastern China[J]. Energy & Fuels, 2018, 32(4): 5045-5061.
[21] Tang L, Song Y, Pang X Q, et al. Effects of paleo sedimentary environment in saline lacustrine basin on organic matter accumulation and preservation: A case study from the Dongpu Depression, Bohai Bay Basin, China[J]. Journal of Petroleum Science and Engineering, 2020, 185: 106669.
[22] Wang Q F, Jiang F J, Ji H C, et al. Effects of paleosedimentary environment on organic matter enrichment in a saline lacustrine rift basin – A case study of Paleogene source rock in the Dongpu Depression, Bohai Bay Basin[J]. Journal of Petroleum Science and Engineering, 2020, 195: 107658.
[23] 李被,刘池洋,黄雷,等. 东濮凹陷北部沙河街组三段中亚段沉积环境分析[J]. 现代地质,2018,32(2):227-239.

Li Bei, Liu Chiyang, Huang Lei, et al. Analysis of the sedimentary environment in the north of Dongpu Depression during the deposition of the middle section of the third member of the Shahejie Formation[J]. Geoscience, 2018, 32(2): 227-239.
[24] Wang Q F, Jiang F J, Ji H C, et al. Differential enrichment of organic matter in saline lacustrine source rocks in a rift basin: A case study of Paleogene source rocks, Dongpu Depression, Bohai Bay Basin[J]. Natural Resources Research, 2020, 29(6): 4053-4072.
[25] 苏惠,曲丽萍,张金川,等. 裂陷盆地构造演化及盆地伸展模式:以东濮凹陷为例[J]. 石油与天然气地质,2006,27(1):70-77.

Su Hui, Qu Liping, Zhang Jinchuan, et al. Tectonic evolution and extensional pattern of rifted basin: A case study of Dongpu Depression[J]. Oil & Gas Geology, 2006, 27(1): 70-77.
[26] 黄建军,纪友亮,王改卫,等. 东濮凹陷古近系含盐地层层序特征及成因分析[J]. 石油与天然气地质,2007,28(4):479-484.

Huang Jianjun, Ji Youliang, Wang Gaiwei, et. al. Sequence characteristics and genesis of the Eogene salt-bearing formation in Dongpu Depression[J]. Oil & Gas Geology, 2007, 28(4): 479-484.
[27] 李渊,强明瑞,王刚刚,等. 晚冰期以来共和盆地更尕海碎屑物质输入过程与气候变化[J]. 第四纪研究,2015,35(1):160-171.

Li Yuan, Qiang Mingrui, Wang Ganggang, et al. Processes of exogenous detrital input to genggahai lake and climatic changes in the gonghe basin since the Late glacial[J]. Quaternary Sciences, 2015, 35(1): 160-171.
[28] Taylor S R, Mclennan S M. The continental crust: Its composition and evolution[M]. Oxford, UK: Blackwell, 1985: 312.
[29] McLennan S M. Rare earth elements in sedimentary rocks: Influence of provenance and sedimentary processes[J]. Reviews in Mineralogy and Geochemistry, 1989, 21(1): 169-200.
[30] Sachsenhofer R F, Bechtel A, Reischenbacher D, et al. Evolution of lacustrine systems along the Miocene Mur-Mürz fault system (Eastern Alps, Austria) and implications on source rocks in Pull-apart Basins[J]. Marine and Petroleum Geology, 2003, 20(2): 83-110.
[31] Boynton W V. Cosmochemistry of the rare earth elements: Meteorite studies[J]. Developments in Geochemistry, 1984, 2: 63-114.
[32] 徐兆辉,胡素云,汪泽成,等. 古气候恢复及其对沉积的控制作用:以四川盆地上三叠统须家河组为例[J]. 沉积学报,2011,29(2):235-244.

Xu Zhaohui, Hu Suyun, Wang Zecheng, et al. Restoration of paleoclimate and its geological significance: As an example from Upper Triassic Xujiahe Formation in Sichuan Basin[J]. Acta Sedimentologica Sinica, 2011, 29(2): 235-244.
[33] McLennan S M. Weathering and global denudation[J]. The Journal of Geology, 1993, 101(2): 295-303.
[34] Rosen M R, Turner J V, Coshell L, et al. The effects of water temperature, stratification, and biological activity on the stable isotopic composition and timing of carbonate precipitation in a hypersaline lake[J]. Geochimica et Cosmochimica Acta, 1995, 59(5): 979-990.
[35] Liu C L, Li H H, Zhang X, et al. Geochemical characteristics of the Paleogene and neogene saline lacustrine source rocks in the western Qaidam Basin, northwestern China[J]. Energy & Fuels, 2016, 30(6): 4537-4549.
[36] Chivas A R, de Deckker P, Shelley J M G. Strontium content of ostracods indicates lacustrine palaeosalinity[J]. Nature, 1985, 316(6025): 251-253.
[37] 孙镇城. 中国新生代咸化湖泊沉积环境与油气生成[M]. 北京:石油工业出版社,1997.

Sun Zhencheng. The current oil product of China mostly comes from eastern China[M]. Beijing: Petroleum Industry Press, 1997.
[38] Ding X J, Liu G D, Zha M, et al. Geochemical characterization and depositional environment of source rocks of small fault basin in Erlian Basin, northern China[J]. Marine and Petroleum Geology, 2016, 69: 231-240.
[39] 徐崇凯,刘池洋,郭佩,等. 潜江凹陷古近系潜江组盐间泥岩地球化学特征及地质意义[J]. 沉积学报,2018,36(3):617-629.

Xu Chongkai, Liu Chiyang, Guo Pei, et al. Geochemical characteristics and their geological significance of intrasalt mudstones from the Paleogene Qianjiang Formation in the Qianjiang gra-ben, Jianghan Basin, China[J]. Acta Sedimentologica Sinica, 2018, 36(3): 617-629.
[40] 朱光有,金强. 东营凹陷两套优质烃源岩层地质地球化学特征研究[J]. 沉积学报,2003,21(3):506-512.

Xu Guangyou, Jin Qiang. Geochemical characteristics of two sets of excellent source rocks in Dongying Depression[J]. Acta Sedimentologica Sinica, 2003, 21(3): 506-512.
[41] Heath G R, Dymond J. Genesis and transformation of metalliferous sediments from the East Pacific Rise, Bauer Deep, and Central Basin, northwest Nazca plate[J]. GSA Bulletin, 1977, 88(5): 723-733.
[42] Ibach L E J. Relationship between sedimentation rate and total organic carbon content in ancient marine sediments[J]. AAPG Bulletin, 1982, 66(2): 170-188.
[43] Tyson R V. Sedimentation rate, dilution, preservation and total organic carbon: Some results of a modelling study[J]. Organic Geochemistry, 2001, 32(2): 333-339.
[44] Ding X J, Liu G D, Zha M, et al. Relationship between total organic carbon content and sedimentation rate in ancient lacustrine sediments, a case study of Erlian Basin, northern China[J]. Journal of Geochemical Exploration, 2015, 149: 22-29.
[45] 袁伟,柳广弟,徐黎明,等. 鄂尔多斯盆地延长组7段有机质富集主控因素[J]. 石油与天然气地质,2019,40(2):326-334.

Yuan Wei, Liu Guangdi, Xu Liming, et al. Main controlling factors for organic matter enrichment in Chang 7 member of the Yanchang Formation, Ordos Basin[J]. Oil & Gas Geology, 2019, 40(2): 326-334.
[46] Chen G, Gang W Z, Tang H Z, et al. Astronomical cycles and variations in sediment accumulation rate of the terrestrial Lower Cretaceous Xiagou Formation from the Jiuquan Basin, NW China[J]. Cretaceous Research, 2019, 109: 104156.
[47] 王鹏万,张磊,李昌,等. 黑色页岩氧化还原条件与有机质富集机制:以昭通页岩气示范区A井五峰组—龙马溪组下段为例[J]. 石油与天然气地质,2017,38(5):933-943.

Wang Pengwan, Zhang Lei, Li Chang, et al. Redox conditions and organic enrichment mechanisms of black shale: A case from the Wufeng-Lower Longmaxi Formations in Well A in Zhaotong shale gas demonstration area[J]. Oil & Gas Geology, 2017, 38(5): 933-943.
[48] Bohacs K M, Grabowski Jr G J, Carroll A R, et al. Production, destruction, and dilution—the many paths to source-rock development[M]//Harris N B. The deposition of organic-carbon-rich sediments: Models, mechanisms, and consequences. Tulsa: SEPM Special Publication, 2005: 61-101.
[49] Li W H, Zhang Z F. Paleoenvironment and its control of the formation of oligocene marine source rocks in the deep-water area of the northern south China Sea[J]. Energy & Fuels, 2017, 31(10): 10598-10611.
[50] 林治家,陈多福,刘芊. 海相沉积氧化还原环境的地球化学识别指标[J]. 矿物岩石地球化学通报,2008,27(1):72-80.

Lin Zhijia, Chen Duofu, Liu Qian. Geochemical indices for redox conditions of marine sediments[J]. Bulletin of Mineralogy, Petrology and Geochemistry, 2008, 27(1): 72-80.
[51] Mao L J, Mo D W, Yang J H, et al. Rare earth elements geochemistry in surface floodplain sediments from the Xiangjiang River, middle reach of Changjiang River, China[J]. Quaternary International, 2014, 336: 80-88.
[52] 刘庆. 东营凹陷樊页1井沙河街组烃源岩元素地球化学特征及其地质意义[J]. 油气地质与采收率,2017,24(5):40-45,52.

Liu Qing. Element geochemical characteristics of source rocks in the Shahejie Formation in Well Fangye-1, Dongying Sag and their geological significance[J]. Petroleum Geology and Recovery Efficiency, 2017, 24(5): 40-45, 52.
[53] 易定红,王建功,石亚军,等. 柴西狮子沟地区渐新统下干柴沟组上段膏盐岩沉积演化特征[J]. 天然气工业,2017,37(5):1-9.

Yi Dinghong, Wang Jiangong, Shi Yajun, et al. Evolution characteristic of gypsum-salt rocks of the upper member of Oligocene Lower Ganchaigou Fm in the Shizigou area, western Qaidam Basin[J]. Natural Gas Industry, 2017, 37(5): 1-9.
[54] Chen G, Gang W Z, Liu Y Z, et al. Organic matter enrichment of the Late Triassic Yanchang Formation (Ordos Basin, China) under dysoxic to oxic conditions: Insights from pyrite framboid size distributions[J]. Journal of Asian Earth Sciences, 2019, 170: 106-117.
[55] Li W H, Lu S F, Xue H T, et al. The formation environment and developmental models of argillaceous dolomite in the Xingouzui Formation, the Jianghan Basin[J]. Marine and Petroleum Geology, 2015, 67: 692-700.
[56] Parrish J T. Paleogeography of Corg-rich rocks and the preservation versus production controversy[M]//Huc A Y. Paleogeography, paleoclimate, and source rocks. Tulsa: American Association of Petroleum Geologists, 1995: 1-20.
[57] Calvert S E, Pedersen T F, Naidu P D, et al. On the organic carbon maximum on the continental slope of the eastern Arabian Sea[J]. Journal of Marine Research, 1995, 53(2): 269-296.
[58] Demaison G J, Moore G T. Anoxic environments and oil source bed genesis[J]. Organic Geochemistry, 1980, 2(1): 9-31.
[59] Tyson R V, Pearson T H. Modern and ancient continental shelf anoxia: An overview[J]. Geological Society, London, Special Publications, 1991, 58(1): 1-24.
[60] Ingall E, Jahnke R. Influence of water-column anoxia on the elemental fractionation of carbon and phosphorus during sediment diagenesis[J]. Marine Geology, 1997, 139(1/2/3/4): 219-229.
[61] Bohacs K M. Sequence stratigraphy of the Monterey Formation, Santa Barbara County: Integration of physical, chemical, and biofacies data from outcrop and subsurface[M]// Miocene and Oligocene Petroleum Reservoirs of the Santa Maria and Santa Barbara-Ventura Basins, California. San Francisco, California: SEPM Special Publication, 1990, 139-201.
[62] Carroll A R, Bohacs K M. Stratigraphic classification of ancient lakes: Balancing tectonic and climatic controls[J]. Geology, 1999, 27(2): 99-102.
[63] Bohacs K M, Carroll A R, and Neal J E. Lessons from large lake systems-thresholds, nonlinearity, and strange attractors[M]//Chan M A, Archer A W. Extreme depositional environments: Mega end members in geologic time. Boulder, Colorado: Geological Society of America, 2003: 75-90.
[64] 马小祥,姚素平,张柏林,等. 渤海湾盆地东濮凹陷古近系古湖盆氧化还原条件及其优质烃源岩的发育模式[J]. 高校地质学报,2019,25(6):801-812.

Ma Xiaoxiang, Yao Suping, Zhang Bolin, et al. Redox conditions of paleogene paleolake and development models of high-quality source rocks in the Dongpu Sag, Bohai Bay Basin[J]. Geological Journal of China Universities, 2019, 25(6): 801-812.
[65] 张慧芳,吴欣松,王斌,等. 陆相湖盆沉积有机质富集机理研究进展[J]. 沉积学报,2016,34(3):463-477.

Zhang Huifang, Wu Xinsong, Wang Bin, et al. Research progress of the enrichment mechanism of sedimentary organics in lacustrine basin[J]. Acta Sedimentologica Sinica, 2016, 34(3): 463-477.