Discovery and significance of Cretaceous-Paleogene freshwater foraminifera in Subei-South Yellow Sea Basin

LIU Yurui

doi:10.11781/sysydz202101001

Volume 43 Issue 1

Jan. 2021

Turn off MathJax

Article Contents

Article Navigation > PETROLEUM GEOLOGY & EXPERIMENT > 2021 > 43(1): 1-13

LIU Yurui. Discovery and significance of Cretaceous-Paleogene freshwater foraminifera in Subei-South Yellow Sea Basin[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2021, 43(1): 1-13. doi: 10.11781/sysydz202101001

Citation:

LIU Yurui. Discovery and significance of Cretaceous-Paleogene freshwater foraminifera in Subei-South Yellow Sea Basin[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2021, 43(1): 1-13. doi: 10.11781/sysydz202101001

Citation:

PDF( 1957 KB)

Discovery and significance of Cretaceous-Paleogene freshwater foraminifera in Subei-South Yellow Sea Basin

doi: 10.11781/sysydz202101001

LIU Yurui

Scientific and Technical-Equipment Department, SINOPEC Jiangsu Oilfield Company, Yangzhou, Jiangsu 225009, China

Received Date: 2020-02-04
Rev Recd Date: 2020-10-10
Publish Date: 2021-01-28

Abstract

Abstract

In previous studies, the "marine facies" fossils in the second member of Taizhou Formation and the second and fourth members of Funing Formation of the Subei-South Yellow Sea Basin were generally considered to be organisms associated with transgression and organisms that lived in saline lakes. However, after reviewing the data, this theory proved to be wrong: most of the foraminifera do not exist in the above mentioned members. The distributions of "marine facies" fossils are not concentrated, and the surrounding rocks do not contain gypsum-salt. The evidence of paleoclimate and paleohydrology is also contrary to lake salinization theory. Formation comparison results show that 97 foraminifera are from 4 new strata, and the remaining 3 are in the second member of Funing Formation. The source of transgression, the ancient East China Sea, does not exist, and there are no marine fossils here. The "marine facies" fossils found here are all euryhaline organisms that can also live in fresh water. During the Late Cretaceous-Paleocene lake invasion period, the ancient climate was humid and the ancient lake was deep, and the water could not be salinized. Glauconite, apatite and trace elements cannot be used as a criterion for distinguishing between marine and terrestrial facies. Different types of euryhaline organisms are usually flourishing separately, and co-exist with a large number of freshwater organisms; meanwhile, the surrounding rocks do not contain gypsum-salt. According to the evidence above, the euryhaline organisms in this area are interpreted to live in freshwater, since foraminifera can live in a freshwater environment, and there was no water salinization in the three stages, of regional lake invasion. The large scale, high quality source rocks in Mesozoic-Cenozoic terrestrial basins in China are mainly freshwater lacustrine sediments, which can provide rich oil and gas resources.
- foraminifera,
- non-marine fossil,
- lacustrine facies,
- Cretaceous,
- Paleogene,
- freshwater source rocks,
- Subei-South Yellow Sea Basin

FullText(HTML)

References(56)

References

[1]	汪品先, 林景星. 我国中部某盆地早第三纪半咸水有孔虫化石群的发现及其意义[J]. 地质学报, 1974(2): 175-181. https://www.cnki.com.cn/Article/CJFDTOTAL-DZXE197402002.htm WANG Pinxian, LIN Jingxing. Discovery of Paleogene brackish-water foraminifers in a certain basin, Central China, and its significance[J]. Acta Geologica Sinica, 1974(2): 175-181. https://www.cnki.com.cn/Article/CJFDTOTAL-DZXE197402002.htm
[2]	汪品先, 闵秋宝, 林景星, 等. 我国东部新生代几个盆地半咸水有孔虫化石群的发现及其意义[C]//地层古生物论文集第二辑. 北京: 地质出版社, 1975: 1-33. WANG Pinxian, MIN Qiubao, LIN Jingxing, et al. Discovery of Paleogene brackish-water foraminifers in several basins, Eastern China, and its significance[C]//A collection of essays on stratigraphical paleontology PartⅡ. Beijing: Geological Publishing House, 1975: 1-33.
[3]	汪品先, 闵秋宝, 卞云华. 我国东部第四纪的海陆过渡相地层[J]. 中国第四纪研究, 1985, 6(1): 35-43. https://www.cnki.com.cn/Article/CJFDTOTAL-DSJJ198501006.htm WANG Pinxian, MIN Qiubao, BIAN Yunhua. Quaternary stratigraphy of marine-continental transitional facies in East China[J]. Quaternaria Sinica, 1985, 6(1): 35-43. https://www.cnki.com.cn/Article/CJFDTOTAL-DSJJ198501006.htm
[4]	汪品先, 闵秋宝, 卞云华. 关于我国东部含油盆地早第三纪地层的沉积环境[J]. 地质论评, 1982, 28(5): 402-411. https://www.cnki.com.cn/Article/CJFDTOTAL-DZLP198205001.htm WANG Pinxian, MIN Qiubao, BIAN Yunhua. On the sedimentary environments of the Paleogene strata in oil-bearing basins in the eastern part of China[J]. Geological Review, 1982, 28(5): 402-411. https://www.cnki.com.cn/Article/CJFDTOTAL-DZLP198205001.htm
[5]	中国科学院古脊椎动物与古人类研究所, 南京地质古生物研究所. 华南中、新生代红层[C]//广东南雄华南白垩纪-早第三纪红层现场会议论文选集. 北京: 科学出版社, 1979: 58-78. Institute of Vertebrate Paleontology and Paleoanthropology, Nanjing Institute of Geology and Palaeontology, Academia Sinica. The Mesozoic and Cenozoic red stages in Southern China[C]. Beijing: Science Press, 1979: 58-78.
[6]	严钦尚, 张国栋, 项立嵩, 等. 苏北金湖凹陷阜宁群的海侵和沉积环境[J]. 地质学报, 1979, 53(1): 74-83. https://www.cnki.com.cn/Article/CJFDTOTAL-DZXE197901006.htm YAN Qinshang, ZHANG Guodong, XIANG Lisong, et al. Marine inundation and related sedimentary environment of Funing Group (Lower Paleogene), in Jinhu Depression, North Jiangsu Plain[J]. Acta Geological Sinica, 1979, 53(1): 74-83. https://www.cnki.com.cn/Article/CJFDTOTAL-DZXE197901006.htm
[7]	俞昌民, 王惠基. 江苏北部下第三系的管状化石[J]. 古生物学报, 1981, 20(5): 406-417. https://www.cnki.com.cn/Article/CJFDTOTAL-GSWX198105003.htm YU Changmin, WANG Huiji. Some tube-like fossils from the Early Tertiary of Northern Jiangsu[J]. Acta Palaeontologica Sinica, 1981, 20(5): 406-417. https://www.cnki.com.cn/Article/CJFDTOTAL-GSWX198105003.htm
[8]	梁名胜. 中国东部早第三纪海侵期的划分[J]. 海洋地质研究, 1982, 2(2): 97-100. https://www.cnki.com.cn/Article/CJFDTOTAL-HYDZ198202011.htm LIANG Mingsheng. The division of transgressive stages of Eogene in Eastern China[J]. Marine Geological Research, 1982, 2(2): 97-100. https://www.cnki.com.cn/Article/CJFDTOTAL-HYDZ198202011.htm
[9]	徐宝政, 王秋. 我国东部沿海地区早第三纪海侵地层的初步探讨[J]. 化工地质, 1982(1): 13-29. https://www.cnki.com.cn/Article/CJFDTOTAL-HGKC198201001.htm XU Baozheng, WANG Qiu. A preliminary study on the Eogene transgressive strata in the eastern coastal areas of China[J]. Geology of Chemical Minerals, 1982(1): 13-29. https://www.cnki.com.cn/Article/CJFDTOTAL-HGKC198201001.htm
[10]	黄宪智. 苏北盆地下第三系石油地质特征及隐蔽油藏的勘探[J]. 大庆石油地质与开发, 1984, 3(1): 141-147. https://www.cnki.com.cn/Article/CJFDTOTAL-DQSK198401012.htm HUANG Xianzhi. Characteristics of petroleum geology and exploration for subtle traps in the Lower Tertiary formation of Northern Jiangsu Basin[J]. Petroleum Geology & Oilfield Development in Daqing, 1984, 3(1): 141-147. https://www.cnki.com.cn/Article/CJFDTOTAL-DQSK198401012.htm
[11]	何炎. 苏北早第三纪有孔虫[J]. 古生物学报, 1987, 26(6): 721-726. https://www.cnki.com.cn/Article/CJFDTOTAL-GSWX198706007.htm HE Yan. Early Tertiary foraminifera from Northern Jiangsu, China[J]. Acta Palaeontologica Sinica, 1987, 26(6): 721-726. https://www.cnki.com.cn/Article/CJFDTOTAL-GSWX198706007.htm
[12]	张国栋, 王慧中. 中国东部早第三纪海侵和沉积环境[M]. 北京: 地质出版社, 1987. ZHANG Guodong, WANG Huizhong. Transgression and sedimentary environment of Eogene in the Eastern China[M]. Beijing: Geological Publishing House, 1987.
[13]	朱静昌, 张国栋, 王益友. 苏北盆地阜宁群时期的古气候和水介质的物理化学条件分析[J]. 岩相古地理, 1992, 12(6): 8-16. https://www.cnki.com.cn/Article/CJFDTOTAL-TTSD199206001.htm ZHU Jingchang, ZHANG Guodong, WANG Yiyou. Palaeoclimatic conditions and physicochemical properties of water bodies in the North Jiangsu Basin during the Funing Group deposition (Palaeogene)[J]. Sedimentary Geology and Tethyan Geology, 1992, 12(6): 8-16. https://www.cnki.com.cn/Article/CJFDTOTAL-TTSD199206001.htm
[14]	傅强, 李益, 张国栋, 等. 苏北盆地晚白垩世-古新世海侵湖泊的证据及其地质意义[J]. 沉积学报, 2007, 25(3): 380-385. https://www.cnki.com.cn/Article/CJFDTOTAL-CJXB200703007.htm FU Qiang, LI Yi, ZHANG Guodong, et al. Evidence of transgression lake of Subei Basin during Late Cretaceous and Paleocene epoch and its geological significance[J]. Acta Sedimentologica Sinica, 2007, 25(3): 380-385. https://www.cnki.com.cn/Article/CJFDTOTAL-CJXB200703007.htm
[15]	张弥曼, 周家健. 我国东部中、新生代含油地层中的鱼化石及有关沉积环境的讨论[J]. 古脊椎动物与古人类, 1978, 16(4): 229-237. https://www.cnki.com.cn/Article/CJFDTOTAL-GJZD197804003.htm ZHANG Miman, ZHOU Jiajian. On the fossil fishes in Mesozoic and Cenozoic oil-bearing strata from East China and their sedimentary environment[J]. Vertebrata Palasiatica, 1978, 16(4): 229-237. https://www.cnki.com.cn/Article/CJFDTOTAL-GJZD197804003.htm
[16]	裘松余, 林景星. 我国第三纪有孔虫动物群及其与找油关系的讨论[J]. 石油与天然气地质, 1980, 1(3): 208-219. https://www.cnki.com.cn/Article/CJFDTOTAL-SYYT198003005.htm QIU Songyu, LIN Jingxing. Tertiary foraminiferal faunas of China and their significance in oil & gas prospecting[J]. Oil & Gas Geology, 1980, 1(3): 208-219. https://www.cnki.com.cn/Article/CJFDTOTAL-SYYT198003005.htm
[17]	侯祐堂, 杨恒仁. 中国中、新生代介形类动物群的特征及其生活环境的探讨[J]. 石油学报, 1980, 1(1): 21-30. https://www.cnki.com.cn/Article/CJFDTOTAL-SYXB198001003.htm HOU Youtang, YANG Hengren. A study of the Mesozoic and Cenozoic ostracod faunas of China with special reference to their ecolo-gical aspects[J]. Acta Petrolei Sinica, 1980, 1(1): 21-30. https://www.cnki.com.cn/Article/CJFDTOTAL-SYXB198001003.htm
[18]	黄第藩, 李晋超. 关于松辽和华北中、新生代沉积相的某些问题[J]. 地质论评, 1982, 28(3): 217-227. https://www.cnki.com.cn/Article/CJFDTOTAL-DZLP198203003.htm HUANG Difan, LI Jinchao. Some questions about Mesozoic-Cenozoic sedimentary facies in the Songliao and North China basins[J]. Geological Review, 1982, 28(3): 217-227. https://www.cnki.com.cn/Article/CJFDTOTAL-DZLP198203003.htm
[19]	郝诒纯, 李蕙生. 渤海沿岸及邻近地区早第三纪钙质超微化石的发现及其意义[J]. 科学通报, 1984, 29(12): 741-745. https://www.cnki.com.cn/Article/CJFDTOTAL-KXTB198412010.htm HAO Yichun, LI Huisheng. Discovery and significance of calca-reous microfossils in the Bohai Sea and the adjacent area[J]. Chinese Science Bulletin, 1984, 29(12): 741-745. https://www.cnki.com.cn/Article/CJFDTOTAL-KXTB198412010.htm
[20]	崔占堂. 冀中地区早第三纪有孔虫及其意义[J]. 海洋地质与第四纪地质, 1987, 7(3): 107-112. https://www.cnki.com.cn/Article/CJFDTOTAL-HYDZ198703019.htm CUI Zhantang. The foraminiferal fauna of Early Tertiary in the central region of Hebei Province and its significance[J]. Marine Geology & Quaternary Geology, 1987, 7(3): 107-112. https://www.cnki.com.cn/Article/CJFDTOTAL-HYDZ198703019.htm
[21]	袁文芳, 陈世悦, 曾昌民. 济阳坳陷古近系沙河街组海侵问题研究[J]. 石油学报, 2006, 27(4): 40-44. https://www.cnki.com.cn/Article/CJFDTOTAL-SYXB200604007.htm YUAN Wenfang, CHEN Shiyue, ZENG Changmin. Study on marine transgression of Paleogene Shahejie Formation in Jiyang Depression[J]. Acta Petrolei Sinica, 2006, 27(4): 40-44. https://www.cnki.com.cn/Article/CJFDTOTAL-SYXB200604007.htm
[22]	李玉文. 四川盆地白垩纪半咸水有孔虫和介形虫的发现及其意义[J]. 地质论评, 1979, 25(1): 2-9. https://www.cnki.com.cn/Article/CJFDTOTAL-DZLP197901001.htm LI Yuwen. Discovery of Cretaceous brackish-water foraminifera and ostracoda in the Sichuan Basin, and their significance[J]. Geological Review, 1979, 25(1): 2-9. https://www.cnki.com.cn/Article/CJFDTOTAL-DZLP197901001.htm
[23]	万传彪, 乔秀云, 王洪艳. 中国东北地区藻类组合序列与5次海侵事件[J]. 大庆石油地质与开发, 1998, 17(6): 11-15. https://www.cnki.com.cn/Article/CJFDTOTAL-DQSK806.003.htm WAN Chuanbiao, QIAO Xiuyun, WANG Hongyan. Algae assemblage sequence and five transgressive events in the northeastern region of China[J]. Petroleum Geology & Oilfield Deuelopment in Daqing, 1998, 17(6): 11-15. https://www.cnki.com.cn/Article/CJFDTOTAL-DQSK806.003.htm
[24]	席党鹏, 万晓樵, 冯志强, 等. 松辽盆地晚白垩世有孔虫的发现: 来自松科1井湖海沟通的证据[J]. 科学通报, 2010, 55(35): 3433-3436. https://www.cnki.com.cn/Article/CJFDTOTAL-KXTB201035016.htm XI Dangpeng, WAN Xiaoqiao, FENG Zhiqiang, et al. Discovery of Late Cretaceous foraminifera in the Songliao Basin: evidence from SK-1 and implications for identifying seawater incursions[J]. Chinese Science Bulletin, 2011, 56(3): 253-256. https://www.cnki.com.cn/Article/CJFDTOTAL-KXTB201035016.htm
[25]	冯子辉, 霍秋立, 王雪, 等. 青山口组一段烃源岩有机地球化学特征及古沉积环境[J]. 大庆石油地质与开发, 2015, 34(4): 1-7. https://www.cnki.com.cn/Article/CJFDTOTAL-DQSK201504001.htm FENG Zihui, HUO Qiuli, WANG Xue, et al. Organic geochemical characteristics and paleosedimentary environments of the source rocks in member 1 of Qingshankou Formation[J]. Petroleum Geo-logy and Oilfield Development in Daqing, 2015, 34(4): 1-7. https://www.cnki.com.cn/Article/CJFDTOTAL-DQSK201504001.htm
[26]	李道琪. 苏北盆地古新统泰州组、阜宁组大相环境的讨论[J]. 地质学报, 1984, 58(1): 80-85. https://www.cnki.com.cn/Article/CJFDTOTAL-DZXE198401007.htm LI Daoqi. A discussion on the environment of the large facies of the Paleocene Taizhou and Funing formations in the Northern Jiangsu Basin[J]. Acta Geologica Sinica, 1984, 58(1): 80-85. https://www.cnki.com.cn/Article/CJFDTOTAL-DZXE198401007.htm
[27]	童晓光. 中国东部早第三纪海侵质疑[J]. 地质论评, 1985, 31(3): 261-267. https://www.cnki.com.cn/Article/CJFDTOTAL-DZLP198503009.htm TONG Xiaoguang. Doubts about the validity of Paleogene transgression in Eastern China[J]. Geological Review, 1985, 31(3): 261-267. https://www.cnki.com.cn/Article/CJFDTOTAL-DZLP198503009.htm
[28]	茅绍智, 余静贤. 陆相沟鞭藻的起源和演化及其生油意义[J]. 地球科学(中国地质大学学报), 1990, 15(3): 283-290. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX199003008.htm MAO Shaozhi, YU Jingxian. Origin and evolution of terrestrial dinoflagellates and their significance in source potential for petroleum[J]. Earth Science(Journal of China University of Geosciences), 1990, 15(3): 283-290. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX199003008.htm
[29]	王仪诚, 陈永祥. 苏北盆地早第三纪海侵析疑[J]. 石油学报, 1992, 13(2): 137-142. https://www.cnki.com.cn/Article/CJFDTOTAL-SYXB199202022.htm WANG Yicheng, CHEN Yongxiang. A discussion of the Palaeogene transgression in North Jiangsu Basin[J]. Acta Petrolei Sinica, 1992, 13(2): 137-142. https://www.cnki.com.cn/Article/CJFDTOTAL-SYXB199202022.htm
[30]	王仪诚, 穆曰孔, 居杏珍, 等. 中国油气区第三系(Ⅵ): 东南油气区分册[M]. 北京: 石油工业出版社, 1994. WANG Yicheng, MU Yuekong, JU Xingzhen, et al. Tertiary in petroliferous regions of China, volume Ⅵ: the southeast region of China[M]. Beijing: Petroleum Industry Press, 1994.
[31]	姚益民, 徐金鲤, 单怀广, 等. 山东济阳坳陷早第三纪海侵的讨论[J]. 石油学报, 1992, 13(2): 29-34. https://www.cnki.com.cn/Article/CJFDTOTAL-SYXB199202005.htm YAO Yimin, XU Jinli, SHAN Huaiguang, et al. A discussion of the Paleogene transgression in the Jiyang Depression, Shandong Province[J]. Acta Petrolei Sinica, 1992, 13(2): 29-34. https://www.cnki.com.cn/Article/CJFDTOTAL-SYXB199202005.htm
[32]	刘传联, 成鑫荣. 渤海湾盆地早第三纪非海相钙质超微化石的锶同位素证据[J]. 科学通报, 1996, 41(10): 908-910. https://www.cnki.com.cn/Article/CJFDTOTAL-KXTB199610012.htm LIU Chuanlian, CHENG Xinrong. Isotopic characteristics of the non-marine calcareous nannofossils of Eogene in the Bohaiwan Basin[J]. Chinese Science Bulletin, 1996, 41(10): 908-910. https://www.cnki.com.cn/Article/CJFDTOTAL-KXTB199610012.htm
[33]	孙镇城, 彭立才, 李东明, 等. 中国东部早第三纪海侵与全球海平面升降[J]. 地质论评, 1996, 42(S1): 181-187. https://www.cnki.com.cn/Article/CJFDTOTAL-DZLP1996S1025.htm SUN Zhencheng, PENG Licai, LI Dongming, et al. Relationship between eustasy and transgression in Early Tertiary in Eastern China[J]. Geological Review, 1996, 42(S1): 181-187. https://www.cnki.com.cn/Article/CJFDTOTAL-DZLP1996S1025.htm
[34]	李守军, 吴智平, 马在平. 中国东部早第三纪有孔虫的生活环境[J]. 石油大学学报(自然科学版), 1997, 21(2): 3-5. https://www.cnki.com.cn/Article/CJFDTOTAL-SYDX702.000.htm LI Shoujun, WU Zhiping, MA Zaiping. Environment of foraminifera of Paleogene in East China[J]. Journal of the University of Petro-leum, China (Edition of Natural Science), 1997, 21(2): 3-5. https://www.cnki.com.cn/Article/CJFDTOTAL-SYDX702.000.htm
[35]	黄福堂, 迟元林, 黄清华. 松辽盆地中白垩世海侵事件质疑[J]. 石油勘探与开发, 1999, 26(3): 104-107. https://www.cnki.com.cn/Article/CJFDTOTAL-SKYK903.027.htm HUANG Futang, CHI Yuanlin, HUANG Qinghua. Doubts about the validity of the Middle Cretaceous transgression in Songliao Basin[J]. Petroleum Exploration and Development, 1999, 26(3): 104-107. https://www.cnki.com.cn/Article/CJFDTOTAL-SKYK903.027.htm
[36]	王世杰, 董丽敏, 林文祝, 等. 泥河湾组有孔虫化石群的锶同位素研究[J]. 科学通报, 1995, 40(22): 2072-2074. https://www.cnki.com.cn/Article/CJFDTOTAL-KXTB199522016.htm WANG Shijie, DONG Liming, LIN Wenzhu, et al. Study on the Sr isotopes of foraminifera fossil group in Nihewan Formation[J]. Chinese Science Bulletin, 1995, 40(22): 2072-2074. https://www.cnki.com.cn/Article/CJFDTOTAL-KXTB199522016.htm
[37]	刘玉瑞. 苏北后生-同生断陷盆地油气成藏规律研究[J]. 石油实验地质, 2016, 38(6): 721-731. doi: 10.11781/sysydz201606721 LIU Yurui. Petroleum accumulation rules in hysterogenetic reconstructive-syngenetic rift basins, North Jiangsu Basin[J]. Petroleum Geology & Experiment, 2016, 38(6): 721-731. doi: 10.11781/sysydz201606721
[38]	郝诒纯, 茅绍智. 微体古生物学教程[M]. 2版. 武汉: 中国地质大学出版社, 1993. HAO Yichun, MAO Shaozhi. The course of the ancient micro-biology[M]. 2nd ed. Wuhan: China University of Geosciences Press, 1993.
[39]	刘玉瑞. 苏北盆地戴南组泥屑流扇沉积[J]. 石油与天然气地质, 2017, 38(3): 419-429. https://www.cnki.com.cn/Article/CJFDTOTAL-SYYT201703001.htm LIU Yurui. Mud debris flow fan deposits in Dainan Formation of the Subei Basin[J]. Oil & Gas Geology, 2017, 38(3): 419-429. https://www.cnki.com.cn/Article/CJFDTOTAL-SYYT201703001.htm
[40]	汪品先. 微体化石在海侵研究中的应用与错用[J]. 第四纪研究, 1992(4): 321-331. https://www.cnki.com.cn/Article/CJFDTOTAL-DSJJ199204003.htm WANG Pinxian. The use and misuse of microfossils in marine transgression studies[J]. Quaternary Sciences, 1992(4): 321-331. https://www.cnki.com.cn/Article/CJFDTOTAL-DSJJ199204003.htm
[41]	吴乃琴. 弱海相性有孔虫群的特征及其代表的沉积环境[J]. 第四纪研究, 1993(3): 267-280. https://www.cnki.com.cn/Article/CJFDTOTAL-DSJJ199303007.htm WU Naiqin. Characteristics of low-marineness foraminiferal faunas in modern and quaternary deposits and their geological implication[J]. Quaternary Sciences, 1993(3): 267-280. https://www.cnki.com.cn/Article/CJFDTOTAL-DSJJ199303007.htm
[42]	肖应凯, 肖军, 赵志琦, 等. 延庆杨户庄第四纪有孔虫的非海相生存环境: 硼和锶同位素证据[J]. 科学通报, 2008, 53(7): 801-806. https://www.cnki.com.cn/Article/CJFDTOTAL-KXTB200807011.htm XIAO Yingkai, XIAO Jun, ZHAO Zhiqi, et al. The nonmarine environment of quaternary foraminifers in Yanghuzhuang, China: evidence from boron and strontium isotopes[J]. Chinese Science Bulletin, 2008, 53(14): 2200-2206. https://www.cnki.com.cn/Article/CJFDTOTAL-KXTB200807011.htm
[43]	孙黎明, 李英杰, 陈秀玉, 等. 河北阳原盆地泥河湾组有孔虫来源的探讨[J]. 地理与地理信息科学, 2004, 20(3): 96-98. https://www.cnki.com.cn/Article/CJFDTOTAL-DLGT200403023.htm SUN Liming, LI Yingjie, CHEN Xiuyu, et al. Approach on sources of foraminifera and environment of deposition in Nihewan Group of Yangyuan Basin, Hebei Province[J]. Geography and Geo-Information Science, 2004, 20(3): 96-98. https://www.cnki.com.cn/Article/CJFDTOTAL-DLGT200403023.htm
[44]	孙镇城, 冯晓杰, 杨藩, 等. 中国西部晚第三纪-第四纪有孔虫和钙质超微化石的发现及其地质意义[J]. 现代地质, 1997, 11(3): 269-274. https://www.cnki.com.cn/Article/CJFDTOTAL-XDDZ703.002.htm SUN Zhencheng, FENG Xiaojie, YANG Fan, et al. Discovery of Neogene-Quaternary foraminifera and calcareous nannofossils from Western China and its geological significance[J]. Geoscience, 1997, 11(3): 269-274. https://www.cnki.com.cn/Article/CJFDTOTAL-XDDZ703.002.htm
[45]	勾韵娴, 章炳高. 甘肃玉门地区非海相第四系中的微体化石[J]. 微体古生物学报, 2013, 30(1): 49-57. https://www.cnki.com.cn/Article/CJFDTOTAL-WSGT201301006.htm GOU Yunxian, ZHANG Binggao. Microfossils in non-marine quaternary sediments from Yumen of Gansu Province, China[J]. Acta Micropalaeontologica Sinica, 2013, 30(1): 49-57. https://www.cnki.com.cn/Article/CJFDTOTAL-WSGT201301006.htm
[46]	钱泽书, 陈永祥, 何承全. 苏北东台坳陷古新世至始新世非海相微体浮游藻类[J]. 古生物学报, 1986, 25(1): 17-29. https://www.cnki.com.cn/Article/CJFDTOTAL-GSWX198601003.htm QIAN Zeshu, CHEN Yongxiang, HE Chengquan. Palaeocene-Eocene non-marine microphytoplankton from Dongtai Depression, Northern Jiangsu[J]. Acta Palaeontologica Sinica, 1986, 25(1): 17-29. https://www.cnki.com.cn/Article/CJFDTOTAL-GSWX198601003.htm
[47]	祝幼华, 钟石兰, 杨晓清. 苏北盆地阜宁组钙质超微化石由来初探[J]. 微体古生物学报, 2001, 18(3): 268-273. https://www.cnki.com.cn/Article/CJFDTOTAL-WSGT200103006.htm ZHU Youhua, ZHONG Shilan, YANG Xiaoqing. A preliminary study on the origin of calcareous nannofossils discovered in the Funing Formation from the Northern Jiangsu Basin[J]. Acta Micropalaeontologica Sinica, 2001, 18(3): 268-273. https://www.cnki.com.cn/Article/CJFDTOTAL-WSGT200103006.htm
[48]	邱中建, 龚再升. 中国油气勘探(卷四)[M]. 北京: 石油工业出版社, 地质出版社, 1999: 1054-1087. QIU Zhongjian, GONG Zaisheng. Petroleum exploration in China (Vol. 4)[M]. Beijing: Petroleum Industry Press, Geological Publishing House, 1999: 1054-1087.
[49]	赵艳秋. 东海陆架盆地长江凹陷生油岩研究[J]. 海洋石油, 2003, 23(S1): 40-44. https://www.cnki.com.cn/Article/CJFDTOTAL-HYSY2003S1009.htm ZHAO Yanqiu. The study on source rock of Changjiang Sag of the East China Sea Shelf Basin[J]. Offshore Oil, 2003, 23(S1): 40-44. https://www.cnki.com.cn/Article/CJFDTOTAL-HYSY2003S1009.htm
[50]	林志强, 蔡洪正. 古长江碎屑物进入东海盆地时间探讨[J]. 上海地质, 1990(2): 26-34. https://www.cnki.com.cn/Article/CJFDTOTAL-SHAD199002003.htm LIN Zhiqiang, CAI Hongzheng. An approach to the initial time of the clastic material of the ancient Yangtze River entering the East China Sea Basin[J]. Shanghai Geology, 1990(2): 26-34. https://www.cnki.com.cn/Article/CJFDTOTAL-SHAD199002003.htm
[51]	唐国良, 谈德麟. 镇江以下长江河段的潮流特征[J]. 海洋通报, 1986(1): 77-80. https://www.cnki.com.cn/Article/CJFDTOTAL-HUTB198601019.htm TANG Guoliang, TAN Delin. The character of the tidal currents in the reaches of the Changjiang River from Zhenjiang Down[J]. Marine Science Bulletin, 1986(1): 77-80. https://www.cnki.com.cn/Article/CJFDTOTAL-HUTB198601019.htm
[52]	陈丕基. 南黄海盆地的叶肢介化石[J]. 古生物学报, 2014, 53(1): 70-76. https://www.cnki.com.cn/Article/CJFDTOTAL-GSWX201401005.htm CHEN Peiji. Fossil conchostracans from the Southern Yellow Sea Basin[J]. Acta Palaeontologica Sinica, 2014, 53(1): 70-76. https://www.cnki.com.cn/Article/CJFDTOTAL-GSWX201401005.htm
[53]	黄第藩, 张大江, 王培荣, 等. 中国未成熟石油成因机制和成藏条件[M]. 北京: 石油工业出版社, 2003. HUANG Dipan, ZHANG Dajiang, WANG Peirong, et al. Genetic mechanism and accumulation condition of immature oil in China[M]. Beijing: Petroleum Industry Press, 2003.
[54]	刘玉瑞. 苏北盆地源岩无双峰生烃和未低熟油[J]. 石油实验地质, 2019, 41(4): 461-474. doi: 10.11781/sysydz201904461 LIU Yurui. Bimodal hydrocarbon generation and immature oil do not exist in the North Jiangsu Basin[J]. Petroleum Geology & Experiment, 2019, 41(4): 461-474. doi: 10.11781/sysydz201904461
[55]	高辉, 何梦卿, 赵鹏云, 等. 鄂尔多斯盆地长7页岩油与北美地区典型页岩油地质特征对比[J]. 石油实验地质, 2018, 40(2): 133-140. doi: 10.11781/sysydz201802133 GAO Hui, HE Mengqing, ZHAO Pengyun, et al. Comparison of geological characteristics of Chang 7 shale oil in Ordos Basin and typical shale oil in North America[J]. Petroleum Geology and Experiment, 2018, 40(2): 133-140. doi: 10.11781/sysydz201802133
[56]	王玮, 黄东, 易海永, 等. 淡水湖相页岩小层精细划分及地球化学特征: 以四川盆地侏罗系大安寨段为例[J]. 石油实验地质, 2019, 41(5): 724-730. doi: 10.11781/sysydz201905724 WANG Wei, HUANG Dong, YI Haiyong, et al. Stratigraphic division and geochemical characteristics of freshwater lacustrine shale: a case study of Jurassic Da'anzhai Section, Sichuan Basin[J]. Petroleum Geology & Experiment, 2019, 41(5): 724-730. doi: 10.11781/sysydz201905724

Relative Articles

Supplements(0)

Cited By

Proportional views

Proportional views

通讯作者: 陈斌, bchen63@163.com

1.
沈阳化工大学材料科学与工程学院沈阳 110142

Figures(3) / Tables(3)

Citation

XML

PDF-CN

Article Metrics

Article views (723) PDF downloads(96)

Discovery and significance of Cretaceous-Paleogene freshwater foraminifera in Subei-South Yellow Sea Basin

doi: 10.11781/sysydz202101001

Abstract

References

Proportional views

Catalog

通讯作者: 陈斌, bchen63@163.com

Article Metrics

Proportional views

Related

Discovery and significance of Cretaceous-Paleogene freshwater foraminifera in Subei-South Yellow Sea Basin

doi: 10.11781/sysydz202101001

Abstract

References

Proportional views

Catalog

通讯作者: 陈斌, bchen63@163.com

Article Metrics

Proportional views

Related

Export File

Citation

Format

Content