Journal of Jilin University(Earth Science Edition) ›› 2015, Vol. 45 ›› Issue (5): 1460-1469.doi: 10.13278/j.cnki.jjuese.201505117
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Sun Rongtao1, Zhao Jingtao2,3, Li Jun2,3, Hu Bangqi2,3
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| [1] 中国科学院海洋研究所.渤海地质[M].北京:科学出版社,1985:1-232. Institute of Oceanology, Chinese Academy of Sciences.Geology of the Bohai Sea[M].Beijing: Science Press, 1985:1-232.[2] 李国刚,胡邦琦,毕建强,等. 黄河三角洲ZK1孔晚第四纪以来沉积层序演化及其古环境意义[J].沉积学报,2013,31(6):1050-1058. Li Guogang, Hu Bangqi, Bi Jianqiang, et al. Stratigraphic Evolution of the Huanghe Delta (Bohai Sea) Since the Late Quaternary and Its Paleoenvironmental Implications: Evidence from Core ZK1[J].Acta Sedimentology Sinica,2013, 31(6): 1050-1058.[3] 胥勤勉,袁桂邦,张金起,等.渤海湾沿岸晚第四纪地层划分及地质意义[J].地质学报,2011,85(8):1352-1367. Xu Qinmian, Yuan Guibang, Zhang Jinqi, et al.Stratigraphic Division of the Late Quaternary Strata Along the Coast of Bohai Bay and Its Geology Significance[J].Acta Geologica Sinica, 2011, 85(8): 1352-1367.[4] 庄振业,许卫东,刘东生,等.渤海南部S3孔晚第四纪海相地层的划分及环境演变[J].海洋地质与第四纪地质,1999,19(2): 27-35. Zhuang Zhenye, Xu Weidong, Liu Dongsheng, et al. Division and Environmental Evolution of Late Quaternary Marine Beds of S3 Hole in the Bohai Sea[J].Marine Geology & Quaternary Geology, 1999, 19(2): 27-35.[5] 阎玉忠,王宏,李凤林,等.渤海湾西岸BQ1 孔揭示的沉积环境与海平面波动[J].地质通报,2006,25(3):357-382. Yan Yuzhong, Wang Hong, Li Fenglin, et al.Sedimentary Environment and Sea-Level Fluctuations Revealed by Hole BQ1 on the West Coast of the Bohai Bay, China[J].Geological Bulletin of China, 2006, 25(3): 357-382.[6] 李淑鸾. 辽东湾表层沉积中有孔虫介形虫研究[J]. 北京大学学报:自然科学版,1994,30 (2):181-193. Li Shuluan. A Preliminary Study of Foraminifera and Ostracoda Assemblages in the Liaodong Bay[J].Acta Scientiarum Naturalium Universitatis Pekinensis, 1994, 30(2):181-193.[7] 王海霞,赵全民,李铁刚,等. 辽东湾表层沉积物中底栖有孔虫分布及其与沉积环境的关系[J].海洋地质与第四纪地质,2011,31(2):87-94. Wang Haixia, Zhao Quanmin, Li Tiegang, et al. Distribution of Benthic Foraminifera in Surface Sediments of the Liaodong Bay and Its Bearing on Sedimentary Environments[J].Marine Geology & Quaternary Geology, 2011, 31(2): 87-94.[8] 吴建政,孙洪光,亓发庆,等. 辽东湾北部晚更新世中期以来的地层结构及环境演化[J].海洋科学进展,2005,23(4):452-459. Wu Jianzheng, Sun Hongguang, Qi Faqing, et al. Stratigraphic Structure and Environmental Evolution in the Northern Liaodong Bay Since the Middle Stage of Late Pleistocene[J].Advances in Marine Science, 2005, 23(4): 452-459.[9] 王明田,庄振业,葛淑兰,等.辽东湾中北部浅层埋藏古河道沉积特征及对海上工程的影响[J].黄渤海海洋,2000,18(2): 18-24. Wang Mingtian, Zhuang Zhenye, Ge Shulan, et al. Sediment Characteristics of the Shallow Buried Paleo-Channels in the North-Central Liaodong Bay and Their Negative Effects on Nautical Engineering[J].Journal of Oceanography of Huanghai & Bohai Seas, 2000,18(2):18-24.[10] 汪品先,章纪军,赵泉鸿,等.东海底质中的有孔虫与介形虫[M].北京:海洋出版社,1988:1-438. WangPinxian, Zhang Jijun, Zhao Quanhong, et al. Foraminifera and Ostracoda in Surface Sediments of the East China Sea[M].Beijing: China Ocean Press, 1988:1-438.[11] 汪品先,闵秋宝,卞云华. 南黄海西北部底质中有孔虫、介形虫分布规律及其地质意义[C]//汪品先. 海洋微体古生物论文集. 北京:海洋出版社,1980:61-100. Wang Pinxian, Min Qiubao, Bian Yunhua. Distribution of Foraminifera and Ostracoda in Bottom Sediments of the Northwestern Part of the Southern Yellow Sea and Its Geological Significance[C]//Wang Pinxian. Papers on Marine Micropaleontology, Beijing: China Ocean Press, 1980: 61-100.[12] 何炎,胡兰英,王克良. 江苏东部第四纪有孔虫[C]//中国科学院地质古生物研究所集刊. 北京:科学出版社,1965:51-162. He Yan, Hu Lanying, Wang Keliang. Quaternary Foraminifera in the East Region of Jiangsu Province[C]// Memoirs of the Institute of Geology and Palaeontology, Chinese Academy of Science.Beijing:Science Press, 1965:51-162.[13] 郑守仪,郑执中,王喜堂,等. 山东打渔张灌区第四纪有孔虫及其沉积环境的初步探讨[J].海洋科学集刊,1978(13):16-78. Zheng Shouyi, Zheng Zhizhong, Wang Xitang, et al. The Quaternary Foraminifera of the Dayuzhang Irrigation Area, Shandong Province, and a Preliminary Attempt at an Interpretation of Its Depositional Environment[J].Studia Marina Sinica, 1978(13): 16-78.[14] Stuiver M, Reimer P J. Extended 14C Database and Revised CALIB Radiocarbon Calibration Program[J].Radiocarbon, 1993, 35: 215-230.[15] Hughen K A, Baillie M G L, Bard E, et al. Marine 04 Marine Radiocarbon Age Calibration, 0-26 cal ka BP[J].Radiocarbon, 2004, 46: 1059-1086.[16] 陈永胜,王宏,裴艳东,等. 渤海湾西岸晚第四纪海相地层划分及地质意义[J].吉林大学学报:地球科学版,2012,42(2):747-759. Chen Yongsheng, Wang Hong, Pei Yandong, et al. Division and Its Geological Significance of the Late Quaternary Marine Sedimentary Beds in the West Coast of Bohai Bay, China[J].Journal of Jilin University :Earth Science Edition, 2012,42(2):747-759.[17] 李培英. 辽东海岸带黄土[J].地质学报,1992,66(1):82-94. Li Peiying. The Coastal Zone Loess of the Liaodong Peninsula[J].Acta Geologica Sinica, 1992, 66(1): 82-94.[18] 任凤楼,柳忠权,邱连贵,等. 渤海湾盆地新生代各坳陷沉降的时空差异性[J].地质科学,2008,43(3):546-557. Ren Fenglou, Liu Zhongquan, Qiu Liangui, et al. Space-Time Discrepancy of Depressional Evolution in the Bohai Bay Basin During Cenozoic[J].Chinese Journal of Geology, 2008, 43(3): 546-557. |
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