[1] 陈修，曲希玉，邱隆伟，等. 2016.大牛地气田大18井上古生界致密砂岩储层物性及其成岩主控因素[J]. 沉积学报，34（2）：364-374.

Chen Xiu, Qu Xiyu, Qiu Longwei, et al. 2016. Physical property of the Upper Paleozoic tight sandstone reservoir and its main controlling factors during diagenesis of well D18 in Daniudi gas field[J]. Acta Sedimentologica Sinica, 34(2): 364-374.
[2] 程俊阳，何贤科，段冬平，等. 2023. 渤海湾盆地某油田混积岩名称厘定及储层特征[J]. 中国地质调查，10（5）：27-33.

Cheng Junyang, He Xianke, Duan Dongping, et al. 2023. Name determination and reservoir characteristics of diamictite in a certain oilfield of Bohai Bay Basin[J]. Geological Survey of China, 10(5): 27-33.
[3] 代黎明，牛成民，庞小军，等. 2020. 黄河口凹陷渤中27-A构造沙一二段湖相混积岩储层特征及成因[J]. 地球科学，45（10）：3797-3807.

Dai Liming, Niu Chengmin, Pang Xiaojun, et al. 2020. Reservoir characteristics and forming mechanisms of lacustrine mixed sedimentary rock of First and Second members of Shahejie Formation in BZ27-A structure, Huanghekou Sag[J]. Earth Science, 45(10): 3797-3807.
[4] 杜庆祥，郭少斌，沈晓丽，等. 2016. 渤海湾盆地南堡凹陷南部古近系沙河街组一段古水体特征[J]. 古地理学报，18（2）：173-183.

Du Qingxiang, Guo Shaobin, Shen Xiaoli, et al. 2016. Palaeo-water characteristics of the member 1 of Paleogene Shahejie Formation in southern Nanpu Sag, Bohai Bay Basin[J]. Journal of Palaeogeography, 18(2): 173-183.
[5] 何仕斌，李丽霞，李建红. 2001. 渤中坳陷及其邻区第三系沉积特征和油气勘探潜力分析[J]. 中国海上油气（地质），15（1）：61-71.

He Shibin, Li Lixia, Li Jianhong. 2001. Tertiary sedimentology and hydrocarbon potential in Bozhong Depression and its adjacent area[J]. China Offshore Oil and Gas (Geology), 15(1): 61-71.
[6] 黄雷，周心怀，刘池洋，等. 2012. 渤海海域新生代盆地演化的重要转折期：证据及区域动力学分析[J]. 中国科学：地球科学，42（6）：893-904.

Huang Lei, Zhou Xinhuai, Liu Chiyang, et al. 2012. The important turning points during evolution of Cenozoic basin offshore the Bohai Sea: Evidence and regional dynamics analysis[J]. Science China Earth Sciences, 42(6): 893-904.
[7] 李欢，王清斌，庞小军，等. 2019. 渤海湾盆地辽东凹陷旅大29构造沙二段近源砂砾岩体优质储层形成机理[J]. 吉林大学学报（地球科学版），49（2）：294-309.

Li Huan, Wang Qingbin, Pang Xiaojun, et al. 2019. Generation of high quality near source glutenite reservoir of 2nd member of Shahejie Formation in Lüda-29 structure, Liaodong Sag, Bohai Bay Basin[J]. Journal of Jilin University (Earth Science Edition), 49(2): 294-309.
[8] 刘丹丹，张雪芳，周园园，等. 2020. 渤海海域秦南凹陷东南缘断层活动对古近系油气富集的控制[J]. 海洋地质前沿，36（4）：45-54.

Liu Dandan, Zhang Xuefang, Zhou Yuanyuan, et al. 2020. Fault activities on the southeastern margin of the Qinnan Sag in the Bohai Sea and their control over Paleogene hydrocarbon accumulations[J]. Marine Geology Frontiers, 36(4): 45-54.
[9] 刘士磊，王启飞，龚莹杰，等. 2012. 渤海海域古近纪微体化石组合特征及油气勘探意义[J]. 地层学杂志，36（4）：700-709.

Liu Shilei, Wang Qifei, Gong Yingjie, et al. 2012. Paleogene microfossil assemblages from the Bohai area and their importance for the oil and gas exploration[J]. Journal of Stratigraphy, 36(4): 700-709.
[10] 刘震，邵新军，金博，等. 2007. 压实过程中埋深和时间对碎屑岩孔隙度演化的共同影响[J]. 现代地质，21（1）：125-132.

Liu Zhen, Shao Xinjun, Jin Bo, et al. 2007. Co-effect of depth and burial time on the evolution of porosity for classic rocks during the stage of compaction[J]. Geoscience, 21(1): 125-132.
[11] 吕正祥，宋修章，张健，等. 2016. 渤海海域中部古近系深埋藏湖相高孔隙度白云岩储层特征及其成因[J]. 天然气工业，36（12）：10-17.

Zhengxiang Lü, Song Xiuzhang, Zhang Jian, et al. 2016. Characteristics and genesis of Paleogene deeply-buried high-porosity lacustrine dolomite reservoirs in the central Bohai Sea area[J]. Natural Gas Industry, 36(12): 10-17.
[12] 潘高峰，刘震，赵舒，等. 2011. 砂岩孔隙度演化定量模拟方法：以鄂尔多斯盆地镇泾地区延长组为例[J]. 石油学报，32（2）：249-256.

Pan Gaofeng, Liu Zhen, Zhao Shu, et al. 2011. Quantitative simulation of sandstone porosity evolution: A case from Yanchang Formation of the Zhenjing area, Ordos Basin[J]. Acta Petrolei Sinica, 32(2): 249-256.
[13] 潘文静，王清斌，杜晓峰，等. 2020. 渤海沙一段生物碎屑混积岩古生物特征及储层意义[J]. 地球科学，45（10）：3827-3840.

Pan Wenjing, Wang Qingbin, Du Xiaofeng, et al. 2020. Paleobiological characteristics and its reservoir significance of bioclastic migmatite in First member of Shahejie Formation in Bohai Sea[J]. Earth Science, 45(10): 3827-3840.
[14] 庞小军，牛成民，杜晓峰，等. 2020a. 渤海海域石臼坨凸起东北缘沙河街组一段+二段砂砾岩储层差异定量表征[J]. 石油学报， 41（9）：1073-1088.

Pang Xiaojun, Niu Chengmin, Du Xiaofeng, et al. 2020b. Quantitative characterization of differences in glutenite reservoir in the member 1 and 2 of Shahejie Formation in the northeastern margin of Shijiutuo uplift, Bohai Sea[J]. Acta Petrolei Sinica, 41(9): 1073-1088.
[15] 庞小军，牛成民，杜晓峰，等. 2020b. 渤海海域环渤中地区沙一二段混积岩优质储层差异及成因[J]. 地球科学，45（10）：3853-3869.

Pang Xiaojun, Niu Chengmin, Du Xiaofeng, et al. 2020a. Differences and genesis of high-quality reservoirs of mixed siliciclasticcarbonate rocks in the Es12 around Bozhong Depression, Bohai Sea[J]. Earth Science, 45(10): 3853-3869.
[16] 庞小军，牛成民，王冠民，等. 2022. 渤海海域深层沙一段混积岩优质储层成因：以渤中13-A构造为例[J]. 中国矿业大学学报， 51（2）：354-369.

Pang Xiaojun, Niu Chengmin, Wang Guanmin, et al. 2022. Genesis of high-quality reservoirs with deeply mixed rocks in the Es1 in BZ13-A structure, Bohai Sea[J]. Journal of China University of Mining & Technology, 51(2): 354-369.
[17] 彭军，杨一茗，刘惠民，等. 2022. 陆相湖盆细粒混积岩的沉积特征与成因机理：以东营凹陷南坡陈官庄地区沙河街组四段上亚段为例[J]. 石油学报，43（10）：1409-1426.

Peng Jun, Yang Yiming, Liu Huimin, et al. 2022. Sedimentary characteristics and genetic mechanism of fine-grained hybrid sedimentary rocks in continental lacustrine basin: A case study of the upper submember of member 4 of Shahejie Formation in Chenguanzhuang area, southern slope of Dongying Sag[J]. Acta Petrolei Sinica, 43(10): 1409-1426.
[18] 王继伟，朱玉双，饶欣久，等. 2020. 鄂尔多斯盆地胡尖山地区长61致密砂岩储层成岩特征与孔隙度定量恢复[J]. 岩性油气藏，32（3）：34-43.

Wang Jiwei, Zhu Yushuang, Rao Xinjiu, et al. 2020. Diagenetic characteristics and quantitative porosity restoration of Chang 61 tight sandstone reservoir in Hujianshan area, Ordos Basin[J]. Lithologic Reservoirs, 32(3): 34-43.
[19] 王琪，马东旭，余芳，等. 2017. 鄂尔多斯盆地临兴地区下石盒子组不同粒级砂岩成岩演化及孔隙定量研究[J]. 沉积学报， 35（1）：163-172.

Wang Qi, Ma Dongxu, Yu Fang, et al. 2017. The diagenetic evolution and quantitative research of porosity in different grain size sandstones of the Lower Shihezi Formation in Linxing area, Ordos Basin[J]. Acta Sedimentologica Sinica, 35(1): 163-172.
[20] 王清斌. 2020. 渤海海域湖相混积岩中流体活动对储集层质量的控制作用[D]. 长春：吉林大学.

Wang Qingbin. 2020. The difference control of fluids to the lacustrine carbonate and clastic mixed deposition reservoir, Bohai Sea area[D]. Changchun: Jilin University.
[21] 王艳忠，操应长，葸克来，等. 2013. 碎屑岩储层地质历史时期孔隙度演化恢复方法：以济阳坳陷东营凹陷沙河街组四段上亚段为例[J]. 石油学报， 34（6）：1100-1111.

Wang Yanzhong, Cao Yingchang, Xi Kelai, et al. 2013. A recovery method for porosity evolution of clastic reservoirs with geological time: A case study from the upper submember of Es4 in the Dongying Depression, Jiyang Subbasin[J]. Acta Petrolei Sinica, 34(6): 1100-1111.
[22] 吴礼明，蒋海军，林新，等. 2015. 塔里木盆地玉北地区奥陶系岩溶作用[J]. 新疆地质，33（4）：504-509.

Wu Liming, Jiang Haijun, Lin Xin, Tan Guanghui. 2015. Karstification of the Ordovician in Yu Bei area, Tarim Basin[J]. Xinjiang Geology, 33(4): 504-509.
[23] 解习农，叶茂松，徐长贵，等. 2018. 渤海湾盆地渤中凹陷混积岩优质储层特征及成因机理[J]. 地球科学，43（10）：3526-3539.

Xie Xinong, Ye Maosong, Xu Changgui, et al. 2018. High quality reservoirs characteristics and forming mechanisms of mixed siliciclastic-carbonate sediments in the Bozhong Sag, Bohai Bay Basin[J]. Earth Science, 43(10): 3526-3539.
[24] 杨宁，王贵文，赖锦，等. 2013. 一种砂岩原始孔隙度计算方法[J]. 物探与化探，37（4）：726-729.

Yang Ning, Wang Guiwen, Lai Jin, et al. 2013. A method for calculating primary porosity of sandstone[J]. Geophysical and Geochemical Exploration, 37(4): 726-729.
[25] 叶茂松，解习农，杜学斌，等. 2025. “组分混合”沉积的储层非均质性及形成机理：以渤海海域古近系沙河街组一、二段为例[J]. 沉积学报，43(2): 635-652.

Ye Maosong, Xie Xinong, Du Xuebin, et al. 2025. Characteristics and formation mechanism of heterogeneity in “compositional mixing” reservoirs: An example from the First-Second member of the Palaeogene Shahejie Formation, Bohai Sea[J]. Acta Sedimentologica Sinica, 43(2): 635-652.
[26] 叶茂松，解习农，徐长贵，等. 2018. 混积岩分类命名体系探讨及对混积岩储层评价的启示：以渤海海域混积岩研究为例[J]. 地质论评，64（5）：1118-1131.

Ye Maosong, Xie Xinong, Xu Changgui, et al. 2018. Discussion for classification—designation system of mixed siliciclastic—carbonate sediments and the implication for their reservoir prediction: A case study of mixed sediments from Bohai Sea area[J]. Geological Review, 64(5): 1118-1131.
[27] 张创，孙卫，高辉，等. 2014. 基于铸体薄片资料的砂岩储层孔隙度演化定量计算方法：以鄂尔多斯盆地环江地区长8储层为例[J]. 沉积学报，32（2）：365-375.

Zhang Chuang, Sun Wei, Gao Hui, et al. 2014. Quantitative calculation of sandstone porosity evolution based on thin section data: A case study from Chang8 reservoir of Huanjiang area, Ordos Basin[J]. Acta Sedimentologica Sinica, 32(2): 365-375.
[28] 张玉晔，高建武，赵靖舟，等. 2021. 鄂尔多斯盆地东南部长6油层组致密砂岩成岩作用及其孔隙度定量恢复[J]. 岩性油气藏， 33（6）：29-38.

Zhang Yuye, Gao Jianwu, Zhao Jingzhou, et al. 2021. Diagenesis and pore evolution of Chang 6 tight sandstone reservoir in southeastern Ordos Basin[J]. Lithologic Reservoirs, 33(6): 29-38.
[29] 赵承锦，蒋有录，刘景东，等. 2021. 基于正演与反演结合的孔隙度演化恢复方法：以川东北地区须家河组为例[J]. 石油学报，42（6）：708-723.

Zhao Chengjin, Jiang Youlu, Liu Jingdong, et al. 2021. A recovery method of porosity evolution based on forward and inverse analyses: A case study of the tight sandstone of Xujiahe Formation, northeast Sichuan Basin[J]. Acta Petrolei Sinica, 42(6): 708-723.
[30] 朱伟林. 2002. 中国近海含油盆地古湖泊学研究[D]. 上海：同济大学：26-37.

Zhu Weilin. 2002. Oil-bearing basins offshore China: A paleolimnological perspective[D]. Shanghai: Tongji University: 26-37.
[31] Du X B, Ye M S, Xie X N, et al. 2022. Why is it easy to form high-quality reservoirs in a mixed siliciclastic-carbonate system? Evidence from diagenetic characteristics[J]. Journal of Petroleum Science and Engineering, 212: 110339.
[32] Gardner K, Dorsey R J. 2021. Mixed carbonate-siliciclastic sedimentation at the margin of a Late Miocene tidal strait, Lower Colorado river valley, south-western USA[J]. Sedimentology, 68(5): 1893-1922.
[33] Hussain A, Butt M N, Olariu C, et al. 2022. Unravelling reservoir quality heterogeneity in mixed siliciclastic-carbonate deposits: An example from Miocene Red Sea rift, NW Saudi Arabia[J]. Marine and Petroleum Geology, 145: 105850.
[34] Li S, Zhu H T, Liang J, et al. 2021. Mixed siliciclastic-carbonate deposition and cyclical evolution of the Upper Shahejie Formation and its impact on reservoir development in the Eocene Huanghekou Sag, Bohai Bay Basin, East China[J]. Interpretation, 9(2): SC17-SC30.
[35] Li T J, Huang Z L, Feng Y, et al. 2020. Reservoir characteristics and evaluation of fluid mobility in organic-rich mixed siliciclastic-carbonate sediments: A case study of the lacustrine Qiketai Formation in Shengbei Sag, Turpan-Hami Basin, Northwest China[J]. Journal of Petroleum Science and Engineering, 185: 106667.
[36] Palermo D, Aigner T, Geluk M, et al. 2008. Reservoir potential of a lacustrine mixed carbonate/siliciclastic gas reservoir: The Lower Triassic rogenstein in the Netherlands[J]. Journal of Petroleum Geology, 31(1): 61-96.
[37] Scherer M. 1987. Parameters influencing porosity in sandstones: A model for sandstone porosity prediction[J]. AAPG Bulletin, 71 (5): 485-491.
[38] Walther J. 1894. Einleitung in die geologie als historische wissenschaft: Beobachtungen über die bildung der gesteine und ihrer organischen einschlüsse[M]. Jena: G. Fischer Verlag.
[39] Wang R F, Shen P P, Zhao L J. 2011. Diagenesis of deep sandstone reservoirs and a quantitative model of porosity evolution: Taking the third member of Shahejie Formation in the Wendong oilfield, Dongpu Sag, as an example[J]. Petroleum Exploration and Development, 38(5): 552-559.
[40] Ye M S, Xie X N, Swennen R, et al. 2021. Depositional characteristics of a lacustrine mixed sediment system: A case study from the eastern Shijiutuo uplift, offshore Bohai Bay Basin, eastern China[J]. Journal of Asian Earth Sciences, 209: 104671.
[41] You L, Qu X Y, Zhong J, et al. 2020. Physical simulation experiments on pore evolution in high-temperature and overpressure reservoirs[J]. Natural Gas Industry B, 7(1): 30-39.
[42] Zhao C J, Jiang Y L, Yang H X, et al. 2022. The genesis of authigenic minerals and the porosity evolution of various lithologies and their implications for identifying high-quality reservoirs in the Fourth member of Xujiahe Formation (northeast-Sichuan Basin, China)[J]. Journal of Petroleum Science and Engineering, 212: 110261.
[43] Zhao Z, Liu Z, He F Q, et al. 2023. roved time–depth dual porosity evolution model and a new parameter for tight sandstone reservoir quality evaluation[J]. Journal of Asian Earth Sciences, 252: 105684.