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地学领域高质量科技期刊分级T2区（2023）

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Volume 41 Issue 3
May  2022
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Article Navigation >  Bulletin of Geological Science and Technology  > 2022  >  41(3): 32-43
Nian Tao, Jiang Zaixing, Liu Huimin, Huang Yiming, Deng Yougen, Meng Jiayi, Li Yang. Cyclic sedimentary record of 'red-greyish green' beds in the first Member of Eocene Kongdian Formation(Ek1), Dongying Sag: An example from the Well Wang 46 in Wangjiagang area[J]. Bulletin of Geological Science and Technology, 2022, 41(3): 32-43. doi: 10.19509/j.cnki.dzkq.2021.0072
Citation: Nian Tao, Jiang Zaixing, Liu Huimin, Huang Yiming, Deng Yougen, Meng Jiayi, Li Yang. Cyclic sedimentary record of "red-greyish green" beds in the first Member of Eocene Kongdian Formation(Ek1), Dongying Sag: An example from the Well Wang 46 in Wangjiagang area[J]. Bulletin of Geological Science and Technology, 2022, 41(3): 32-43. doi: 10.19509/j.cnki.dzkq.2021.0072
shu

Cyclic sedimentary record of "red-greyish green" beds in the first Member of Eocene Kongdian Formation(Ek1), Dongying Sag: An example from the Well Wang 46 in Wangjiagang area

doi: 10.19509/j.cnki.dzkq.2021.0072
  • Received Date: 28 Jun 2021
    Abstract

  • Vertically superimposed "red-greyish green" assemblages are developed in the first member of the Eocene Kongdian Formation (Kong1 member) in the Dongying sag of the Bohai Bay Basin, showing certain cyclic sedimentary characteristics.Inorder to better understand its depositional process and response to paleoclimate variation, the study took the Wang 46 well, which is located in the Wangjiagang area, as an example.Calibrated by the stratigraphic ages, cyclostratigraphy analysis has been conducted in the formation using cores, logging cuttings and gammaray(GR) curve to reveal its cyclic depositional process.The red beds correspond to flooded lacustrinemud and sandy beach deposited during flood events, while the greyish greenrhythm beds belong to the shallow lacustrine sand beach sediments in the intermittent wet period, and the two types of deposits are superposed with abrupt contacts.The continuous wavelet and spectral analysis of the GR curve indicate that the depositional process of the Ek1 member is controlled by the Milankovitch eccentricity and precession cycles, resulting in the thicknesses of the cyclically deposited formations are 39.4 m and 6.9 m, respectively.The "floating" astronomical time scale of the Ek1 member has been established by the band filtering of the 125 ka eccentricity cycle, and the Ek1 member is found to have 33 eccentricity cycles.The apparent average deposition rate changes between 0.236 m/ka and 0.408 m/ka.The eccentricity and precession cycles have controlled the depositional process: the maximum eccentricities mainly correspond to frequent occurrences of temporary lacustrine, on the contrary, it mainly developed flooded lacustrine.And, the temporary and perennial flooded lacustrine occurred during the periodsof minimum and maximum precessions, respectively.

     

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  • [1]
    Milankovitch M. Canon of insolation and the ice-age problem(Beograd: Koniglich Serbische Akademie, 1941) English translation by the Israel program for scientific translations[M]. Washington D C: Published for the US Department of Commerceand the National Science Foundation, 1969.
    [2]
    Berger A. Milankovitch theory and climate[J]. Reviews of Geophysics, 1988, 26(4): 624-657. doi: 10.1029/RG026i004p00624
    [3]
    Hinnov L A, Goldhammer R K. Spectral analysis of middle Triassic latemar limestone[J]. Journal of Sedimentary Petrology, 1991, 61: 1173-1193.
    [4]
    Wu H C, Zhang S H, Jiang G Q, et al. Astrochronology for the Early Cretaceous Jehol Biota in northeastern China[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2013, 385: 221-228. doi: 10.1016/j.palaeo.2013.05.017
    [5]
    张运波, 王根厚, 余正伟, 等. 四川盆地中二叠统茅口组米兰科维奇旋回及高频层序[J]. 古地理学报, 2013, 15(6): 777-786. https://www.cnki.com.cn/Article/CJFDTOTAL-GDLX201306005.htm

    Zhang Y B, Wang G H, Yu Z W, et al. Milankovitch cycles and high-frequency sequences of the Middle Permian Maokou Formation in Sichuan Basin[J]. Journal of Palaeogeography, 2013, 15(6): 777-786(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-GDLX201306005.htm
    [6]
    金忠慧, 姜在兴, 张建国, 等. 东营凹陷沙四上亚段旋回地层学研究: 以樊页1井为例[J]. 科学技术与工程, 2017, 17(1): 21-28. doi: 10.3969/j.issn.1671-1815.2017.01.005

    Jin Z H, Jiang Z X, Zhang J G, et al. Cyclostratigraphy research on the upper of 4th Member of the Shahejie Formation in Dongying Sag: A case study of FY1[J]. Science Technology and Engineering, 2017, 17(1): 21-28 (in Chinese with English abstract). doi: 10.3969/j.issn.1671-1815.2017.01.005
    [7]
    张建国. 济阳坳陷始新统沙三下亚段湖相细粒沉积岩成因机制研究[D]. 北京: 中国地质大学(北京), 2017.

    Zhang J G. The formation mechanisms of lacustrine fine-grained sedimentary rocks in the Eocene lower Es3 strata, the Jiyang Depression[D]. Beijing: China University of Geosciences(Beijing), 2017(in Chinese with English abstract).
    [8]
    Kemp D B, Van Manen S M. Metre-scale cycles in shallow water carbonate successions: Milankovitch and stochastic origins[J]. Sedimentology, 2019, 66(7): 2590-2604. doi: 10.1111/sed.12609
    [9]
    吴怀春, 张世红, 冯庆来, 等. 旋回地层学理论基础、研究进展和展望[J]. 地球科学: 中国地质大学学报, 2011, 36(3): 409-428. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX201103001.htm

    Wu H C, Zhang S H, Feng Q L, et al. Theoretical basis, research advancement and prospects of cyclostratigraphy[J]. Earth Science: Journal of Chinese University of Geosciences, 2011, 36(3): 409-428(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX201103001.htm
    [10]
    郭刚, 童金南, 张世红, 等. 安徽巢湖早三叠世印度期旋回地层研究[J]. 中国科学: 地球科学, 2007, 37(12): 1571-1578. https://www.cnki.com.cn/Article/CJFDTOTAL-JDXK200712003.htm

    Guo G, Tong J N, Zhang S H, et al. Cyclostratigraphy study on the Early Triassic Induan in Chaohu, Anhui Province[J]. Science China: Earth Sciences, 2007, 37(12): 1571-1578(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-JDXK200712003.htm
    [11]
    彭兴芳, 冯庆来, 李周波, 等. 广西东攀二叠系-三叠系界线剖面地球化学高分辨率旋回研究[J]. 中国科学: 地球科学, 2007, 37(12): 1565-1570. https://www.cnki.com.cn/Article/CJFDTOTAL-JDXK200712002.htm

    Peng X F, Feng Q L, Li Z B, et al. High-resolution geochemical cyclostratigraphy study on the Permian-Triassic boundary section in Dongpan, Guangxi[J]. Science China: Earth Sciences, 2007, 37(12): 1565-1570(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-JDXK200712002.htm
    [12]
    陈建业, 冯庆来, 陈晶, 等. 广西东攀二叠系-三叠系界线剖面基于岩石磁参数的米兰科维奇旋回特征和地层对比[J]. 地层学杂志, 2007, 31(4): 309-316. doi: 10.3969/j.issn.0253-4959.2007.04.001

    Chen J Y, Feng Q L, Chen J, et al. Milankovitch cycle and stratigraphic correlation study by rock magnetic parameter on the Permian-Triassic boundary section in Dongpan, Guangxi[J]. Journal of Stratigraphy, 2007, 31(4): 309-316(in Chinese with English abstract). doi: 10.3969/j.issn.0253-4959.2007.04.001
    [13]
    Prokpha A, Agterberg F E. Wavelet analysis of well-logging data from oil source rock, Egret Member, offshore eastern Canada[J]. AAPG Bulletin, 2000, 84(10): 1617-1632.
    [14]
    郭少斌, 陈成龙. 利用米兰科维奇旋回划分柴达木盆地第四系层序地层[J]. 地质科技情报, 2007, 26(4): 27-30. https://www.cnki.com.cn/Article/CJFDTOTAL-DZKQ200704005.htm

    Guo S B, Chen C L. Division of sequence stratigraphy of Quaternary formation in Qaidam Basin using the Milankvitch cycle[J]. Geological Science and Technology Information, 2007, 26(4): 27-30(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-DZKQ200704005.htm
    [15]
    吴怀春, 张世红, 黄清华. 中国东北松辽盆地晚白垩世青山口组浮动天文年代标尺的建立[J]. 地学前缘, 2008, 15(4): 159-169. doi: 10.3321/j.issn:1005-2321.2008.04.018

    Wu H C, Zhang S H, Huang Q H. Establishment of floating astronomical time scale for the terrestrial Late Cretaceous Qingshankou Formation in the Songliao Basin of Northeast China[J]. Earth Science Frontiers, 2008, 15(4): 159-169(in Chinese with English abstract). doi: 10.3321/j.issn:1005-2321.2008.04.018
    [16]
    Wu H C, Zhang S H, Jiang G Q, et al. The floating astronomical timescale for the terrestrial Late Cretaceous Qingshankou Formation from the Songliao Basin of Northeast China and its stratigraphic and paleoclimate implications[J]. Earth and Planetary Science Letters, 2009, 278(3/4): 308-323. http://www.sciencedirect.com/science/article/pii/S0012821X08007668
    [17]
    徐伟, 杨小丽, 李雪, 等. 乌干达Albert盆地北部上新统旋回地层学研究[J]. 地质科技情报, 2015, 34(1): 57-62. https://www.cnki.com.cn/Article/CJFDTOTAL-DZKQ201501009.htm

    Xu W, Yang X L, Li X, et al. Milankovitch cyclostratigraphy of Pliocene in the north Albert Basin, Uganda[J]. Geological Science and Technology Information, 2015, 34(1): 57-62(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-DZKQ201501009.htm
    [18]
    谭先锋, 蒋艳霞, 李洁, 等. 济阳坳陷古近系孔店组高频韵律旋回沉积机理及成因[J]. 石油与天然气地质, 2015, 36(1): 61-72. https://www.cnki.com.cn/Article/CJFDTOTAL-SYYT201501009.htm

    Tan X F, Jiang Y X, Li J, et al. Sedimentary record and origin of high frequency cycles in the Paleogene Kongdian Formation in the Jiyang Depression[J]. Oil & Gas Geology, 2015, 36(1): 61-72(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-SYYT201501009.htm
    [19]
    李堃宇, 伊海生, 夏国清. 基于测井曲线频谱分析柴达木盆地西部七个泉地区上、下油砂山组米兰科维奇旋回特征[J]. 地质科技情报, 2018, 37(3): 87-91. https://www.cnki.com.cn/Article/CJFDTOTAL-DZKQ201803012.htm

    Li K Y, Yin H S, Xia G Q. Characteristics of Milankovitch cycles of Shangyoushashan and Xiayoushashan formations in Qigequan area, western Qaidam Basin based on the spectral analysis of the logging curve[J]. Geological Science and Technology Information, 2018, 37(3): 87-91(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-DZKQ201803012.htm
    [20]
    刘洋. 东海盆地西湖凹陷沉积记录的天文旋回响应[J]. 地质科技通报, 2020, 39(3): 120-128. doi: 10.19509/j.cnki.dzkq.2020.0313

    Liu Y. Response to astronomical forcing of sedimentary record in Xihu Depression, East China Sea Basin[J]. Bulletin of Geological Science and Technology, 2020, 39(3): 120-128(in Chinese with English abstract). doi: 10.19509/j.cnki.dzkq.2020.0313
    [21]
    徐健, 德勒恰提·加娜塔依. 米兰科维奇旋回识别与天文标尺的建立: 以莫索湾地区莫21井三工河组一段为例[J]. 地质科技通报, 2021, 40(2): 197-207. doi: 10.19509/j.cnki.dzkq.2021.0218

    Xu J, Deleqiati J. Identification of Milankovich's cycle and establishment of astronomical ruler: A case study from the first section of the Sangonghe Formation of Well Mo 21 in Mosuowan area[J]. Bulletin of Geological Science and Technology, 2021, 40(2): 197-207(in Chinese with English abstract). doi: 10.19509/j.cnki.dzkq.2021.0218
    [22]
    蒋一鸣. 西湖凹陷平湖斜坡带平湖组碎屑锆石U-Pb年龄及米兰科维奇旋回: 对源-汇系统及沉积演化的约束[J]. 地质科技情报, 2019, 38(6): 133-140. https://www.cnki.com.cn/Article/CJFDTOTAL-DZKQ201906016.htm

    Jiang Y M. Detrital zircon U-Pb age and Milankovitch cycles of Pinghu Formation in the Pinghu Slope of Xihu Depression: Constraints on source-sink system and sedimentary evolution[J]. Geological Science and Technology Information, 2019, 38(6): 133-140(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-DZKQ201906016.htm
    [23]
    Reinhardt L, Ricken W. The stratigraphic and geochemical record of Playa cycles: Monitoring a Pangaean monsoon-like system(Triassic, Middle Keuper, S. Germany)[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2000, 161: 205-227. doi: 10.1016/S0031-0182(00)00124-3
    [24]
    Bahr A, Kolber G, Kaboth-Bahr S, et al. Mega-monsoon variability during the Late Triassic: Reassessing the role of orbital forcing in the deposition of playa sediments in the Germanic Basin[J]. Sedimentology, 2020, 67(2): 951-970. doi: 10.1111/sed.12668
    [25]
    Aziz H A. Astronomical forcing in continental sediments: An integrated study of Miocene deposits from the Calatayud and Teruel basins, NE Spain[D]. Utrecht: Utrecht University, 2001.
    [26]
    Aziz H A, Dam J V, Hilgen F J, et al. Astronomical forcing in Upper Miocene continental sequences: Implications for the Geomagnetic Polarity Time Scale[J]. Earth and Planetary Science Letters, 2004, 222: 243-258. doi: 10.1016/j.epsl.2004.02.018
    [27]
    Abels H A, Aziz H A, Calvo J P, et al. Shallow lacustrine carbonate microfacies document orbitally paced lake-level history in the Miocene Teruel Basin(North-East Spain)[J]. Sedimentology, 2009, 56: 399-419. doi: 10.1111/j.1365-3091.2008.00976.x
    [28]
    Abels H A, Aziz H A, Krijgsman W, et al. Long-period eccentricity control on sedimentary sequences in the continental Madrid Basin(middle Miocene, Spain)[J]. Earth and Planetary Science Letters, 2010, 289: 220-231. doi: 10.1016/j.epsl.2009.11.011
    [29]
    Magee J W, Miller G H, Spooner N A, et al. Continuous 150 k. y. monsoon record from Lake Eyre, Australia: Insolation-forcing implications and unexpected Holocene failure[J]. Geology, 2004, 32(10): 885-888. doi: 10.1130/G20672.1
    [30]
    Abels H A, Kraus M J, Gingerich P D. Precession-scale cyclicity in the fluvial lower Eocene Willwood Formation of the Bighorn Basin, Wyoming(USA)[J]. Sedimentology, 2013, 60(6): 1467-1483. doi: 10.1111/sed.12039
    [31]
    Wang Z X, Zhang Z, Huang C J, et al. Astronomical forcing of lake evolution in the Lanzhou Basin during Early Miocene period[J]. Earth and Planetary Science Letters, 2021, 554: 116648. doi: 10.1016/j.epsl.2020.116648
    [32]
    薛雁, 吴智平, 李伟, 等. 东营凹陷新生代盆地结构特征及其控藏作用[J]. 大地构造与成矿学, 2013, 37(2): 206-212. doi: 10.3969/j.issn.1001-1552.2013.02.004

    Xue Y, Wu Z P, Li W, et al. Cenozoic basin structure in the Dongying Sag and its control over reservoir[J]. Geotectonica et Metallogenia, 2013, 37(2): 206-212(in Chinese with English abstract). doi: 10.3969/j.issn.1001-1552.2013.02.004
    [33]
    张顺. 东营凹陷南坡西部孔店期-沙四早期原型盆地格局恢复[D]. 山东青岛: 中国石油大学(华东), 2012.

    Zhang S. The period of Ek-Es4x prototype basin research in the western of south slope, Dongying Sag[D]. Qingdao Shandong: China University of Petroleum(Huadong), 2012(in Chinese with English abstract).
    [34]
    王化爱. 东营凹陷古近系岩性地层油气藏层序地层特征[J]. 石油与天然气地质, 2010, 31(2): 158-164. https://www.cnki.com.cn/Article/CJFDTOTAL-SYYT201002007.htm

    Wang H A. Sequence stratigraphic characteristics of the Paleocene lithologic and stratigraphic reservoirs in the Dongying Depression[J]. Oil & Gas Geology, 2010, 31(2): 158-164(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-SYYT201002007.htm
    [35]
    边凤青. 东营凹陷沙四段-孔店组剥蚀厚度与原型盆地的恢复[D]. 山东青岛: 中国海洋大学(华东), 2009.

    Bian F Q. The restored eroded thickness and prototype basin of Kongdian Formation and the fourth Member of the Shahejie Formation in Dongying Depression[D]. Qingdao Shandong: Ocean University of China(Huadong), 2009(in Chinese with English abstract).
    [36]
    于建国, 韩文功, 王金铎, 等. 中国东部断陷盆地中新生代构造演化: 以济阳坳陷为例[M]. 北京: 石油工业出版社, 2009.

    Yu J G, Han W G, Wang J D, et al. Mesozoic-cenozoic tectonic evolution of rifted basins in eastern China: A case study of Jiyang Depression[M]. Beijing: Petroleum Industry Press, 2009(in Chinese).
    [37]
    张世奇, 纪友亮. 东营凹陷早第三纪古气候变化对层序发育的控制[J]. 中国石油大学学报: 自然科学版, 1997, 22(6): 26-30. https://www.cnki.com.cn/Article/CJFDTOTAL-SYDX806.003.htm

    Zhang S Q, Ji Y L. Control of Paleogene paleoclimate on sequence development in Dongying Sag[J]. Journal of the University of Petroleum: Natural Science Edition, 1997, 22(6): 26-30 (in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-SYDX806.003.htm
    [38]
    李守军, 王明镇, 郑德顺, 等. 山东济阳坳陷古近纪的气候恢复[J]. 山东科技大学学报: 自然科学版, 2003, 22(3): 6-9. https://www.cnki.com.cn/Article/CJFDTOTAL-SDKY200303003.htm

    Li S J, Wang M Z, Zheng D S, et al. Recovery of climate of Palaeogene in Jiyang Depression of Shandong[J]. Journal of Shandong University of Science and Technology: Natural Science Edition, 2003, 22(3): 6-9(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-SDKY200303003.htm
    [39]
    徐磊. 东营凹陷沙四下-孔一段沉积特征研究[D]. 山东青岛: 中国石油大学(华东), 2008.

    Xu L. The study on sedimentary characteristics of lower the 4th member of Shahejie Formation-the 1st member of Kongdian Formation in Dongying Depression[D]. Qingdao Shandong: China University of Petroleum(Huadong), 2008(in Chinese with English abstract).
    [40]
    杨勇强. 东营南坡红层等时地层分析与划分、对比方法研究[D]. 山东青岛: 中国石油大学(华东), 2009.

    Yang Y Q. Method of isochronous stratigraphic division and correlation using in the red beds on the southern slope of Dongying Sag[D]. Qingdao Shandong: China University of Petroleum(Huadong), 2009(in Chinese with English abstract).
    [41]
    雷华蕊, 姜在兴, 周红科. 早古近纪极热时期古气候演化分析: 以东营凹陷为例[J]. 地学前缘, 2018, 25(4): 176-184. https://www.cnki.com.cn/Article/CJFDTOTAL-DXQY201804017.htm

    Lei H R, Jiang Z X, Zhou H K. Analysis of paleoclimate evolution of the hyperthermal period in the early Paleogene: Taking the Dongying depression as an example[J]. Earth Science Frontiers, 2018, 25(4): 176-184(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-DXQY201804017.htm
    [42]
    操应长, 王健, 高永进, 等. 济阳坳陷东营凹陷古近系红层-膏盐层沉积特征及模式[J]. 古地理学报, 2011, 13(4): 375-386. https://www.cnki.com.cn/Article/CJFDTOTAL-GDLX201104004.htm

    Cao Y C, Wang J, Gao Y J, et al. Sedimentary characteristics and model of red beds-gypsum salt beds of the Paleogene in Dongying Sag, Jiyang Depression[J]. Journal of Palaeogeography, 2011, 13(4): 375-386(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-GDLX201104004.htm
    [43]
    王健, 操应长, 刘惠民, 等. 东营凹陷沙四下亚段沉积环境特征及沉积充填模式[J]. 沉积学报, 2012, 30(2): 274-282. https://www.cnki.com.cn/Article/CJFDTOTAL-CJXB201202008.htm

    Wang J, Cao Y C, Liu H M, et al. Characteristics of sedimentary environment and filling model of the lower submember of the fourth member of Shahejie Formation, Dongying Depression[J]. Acta Sedimentologica Sinica, 2012, 30(2): 274-282(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-CJXB201202008.htm
    [44]
    徐伟. 东营凹陷沙河街组三段、四段高频旋回识别及其地质意义[D]. 武汉: 中国地质大学(武汉), 2011.

    Xu W. High-frequency cycles of the 3rd and 4th member of Shahejie Formation in Dongying Depression and its geological significance[D]. Wuhan: China University of Geosciences(Wuhan), 2011(in Chinese with English abstract).
    [45]
    王秉海, 钱凯. 胜利油区地质研究与勘探实践[M]. 山东东营: 石油大学出版社, 1992.

    Wang B H, Qian K. Geological research and exploration practice in Shengli Oil area[D]. Dongying Shandong: Petroleum University Press, 1992 (in Chinese).
    [46]
    宗国洪, 施央申, 王秉海, 等. 济阳盆地中生代构造特征与油气[J]. 地质论评, 1998, 44(3): 289-294. doi: 10.3321/j.issn:0371-5736.1998.03.009

    Zong G H, Shi Y S, Wang B H, et al. Mesozoic structure and their relations to hydrocarbon traps in the Jiyang Basin[J]. Geological Review, 1998, 44(3): 289-294(in Chinese with English abstract). doi: 10.3321/j.issn:0371-5736.1998.03.009
    [47]
    Kraus M J. Paleosols in clastic sedimentary rocks: Their geologic applications[J]. Earth-Science Reviews, 1999, 47: 41-70. doi: 10.1016/S0012-8252(99)00026-4
    [48]
    黄成敏, 王成善. 晚第三纪以前形成古土壤的鉴别、分类及其在古环境研究中的作用[J]. 地球科学进展, 2006, 21(9): 911-917. doi: 10.3321/j.issn:1001-8166.2006.09.004

    Huang C M, Wang C S. Identification, classification and application in paleoenvironment research of pre-Neogene paleosoils[J]. Advance in Earth Science, 2006, 21(9): 911-917(in Chinese with English abstract). doi: 10.3321/j.issn:1001-8166.2006.09.004
    [49]
    王果. 土壤学[M]. 北京: 高等教育出版社, 2009.

    Wang G. Edaphology[M]. Beijing: High Education Press, 2009(in Chinese).
    [50]
    Weedon G. Time-series analysis and cyclostratigraphy[M]. London: Cambridge University Press, 2003.
    [51]
    杨振宇, 马醒华, 黄宝春, 等. 华北地块显生宙古地磁视极移曲线与地块运动[J]. 中国科学: 地球科学, 1998, 28: 44-56. https://www.cnki.com.cn/Article/CJFDTOTAL-JDXK1998S1005.htm

    Yang Z Y, Ma X H, Huang B C, et al. Apparent pole shift curve and block motion of Phanerozoic paleomagnetism in North China Block[J]. Science China: Earth Sciences, 1998, 28: 44-56 (in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-JDXK1998S1005.htm
    [52]
    Scotese C R. Paleomap PaleoAtlas for GPlates and the PaleoData Plotter Program, PALEOMAP Project[EB/OL]. [2016-08-01][2021-04-17], 2016, http://www.earthbyte.org/paleomap-paleoatlas-for-gplates/.
    [53]
    Laskar J, Fienga A, Gastineau M, et al. La2010: A new orbital solution for the long term motion of the Earth[J]. Astronomy & Astrophysics, 2011, 532(A89): 1-15.
    [54]
    王健, 操应长, 高永进, 等. 东营凹陷古近系红层储层成岩作用及成岩相[J]. 中国石油大学学报: 自然科学版, 2013, 37(4): 23-29. doi: 10.3969/j.issn.1673-5005.2013.04.004

    Wang J, Cao Y C, Gao Y J, et al. Diagenesis and diagenetic facies of red beds reservoirsof Paleogene in Dongying Depression[J]. Journal of China University of Petroleum: Natural Science Edition, 2013, 37(4): 23-29(in Chinese with English abstract). doi: 10.3969/j.issn.1673-5005.2013.04.004
    [55]
    田军, 汪品先, 成鑫荣, 等. 从相位差探讨更新世东亚季风的驱动机制[J]. 中国科学: 地球科学, 2005, 35(2): 158-166. https://www.cnki.com.cn/Article/CJFDTOTAL-JDXK200502006.htm

    Tian J, Wang P X, Cheng X R, et al. Discussion on the driving mechanism of east Asian monsoon during the Pleistocene by the phase difference[J]. Science China: Earth Sciences, 2005, 35(2): 158-166 (in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-JDXK200502006.htm
    [56]
    Berger A, Loutre M F, Laskar J. Stability of the astronomical frequencies over the Earth's history for paleoclimate studies[J]. Science, 1992, 255: 560-566. doi: 10.1126/science.255.5044.560
    [57]
    刘晓东, 石正国. 岁差对亚洲夏季风气候变化影响研究进展[J]. 科学通报, 2009, 54(2): 3097-3107. https://www.cnki.com.cn/Article/CJFDTOTAL-KXTB200920021.htm

    Liu X D, Shi Z G. Advances on the influence of precession on climate change of Asian summer monsoon[J]. Chinese Science Bulletin, 2009, 54(2): 3097-3107 (in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-KXTB200920021.htm
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