层序地层主控因素及层序模式研究进展
Advance Research on Main Controlling Factors for Sequence Stratigraphy and Sequence Models
DOI: 10.12677/AG.2018.84095, PDF,    国家自然科学基金支持
作者: 张尚锋:长江大学地球科学学院,湖北 荆州;长江大学油气资源与勘探技术教育部重点实验室,湖北 荆州;张昌民, 王雅宁, 朱锐*:长江大学地球科学学院,湖北 荆州
关键词: 层序地层学海平面变化坡折带层序模式Sequence Stratigraphy Sea Level Changes Slope-Break Zone Sequence Model
摘要: 长期以来,由于对地层层序形成主控因素及层序模式分析观点分歧,限制了层序地层学研究的进一步发展。本文通过海平面变化、古地形坡折带等层序形成主控因素,以及层序模式等研究现状分析,将海平面变化研究概括为研究方法、海平面变化机理及沉积响应分析等五个方面,重点阐述了不同层次海平面变化机理的差异性。同时认为应加强坡折带对层序形成过程控制等方面研究,并对现行的层序地层模式进行评述。认为不存在放之四海而皆准的标准化层序模式,强调总结在主控因素控制下的综合层序地层模式。以上分析的目的,仅为消除对层序地层学的某些误解、以期对层序地层学研究的快速发展有所推动。
Abstract: Because of different opinions on main factors for forming stratigraphical sequence and sequence models, the study of Sequence Stratigraphy has been limited during a long period. Based on current analysis of sea level changes, paleotopography of slope-break, sequence models and other aspects, the author considered that study of the sea level changes can be decomposed to methodology, mechanism and sediment response to sea level changes and the mechanism of different hierarchical sea level changes is the most important. The controlling of slope-break on stratigraphic sequences must be strengthened, and various sequence models should be reviewed so integrated sequence models influenced by main controlling factors should be summed up because none of sequence models is applicable everywhere. Objectives of the study are to dispel misunderstandings so as to hope Promoting research and development on sequence stratigraphy.
文章引用:张尚锋, 张昌民, 王雅宁, 朱锐. 层序地层主控因素及层序模式研究进展[J]. 地球科学前沿, 2018, 8(4): 867-874. https://doi.org/10.12677/AG.2018.84095

参考文献

[1] Miall, A.D. (1997) The Geology of Stratigraphic Sequences. Springer-Verlag, Berlin, 433. [Google Scholar] [CrossRef
[2] 吴亚生, 范嘉松. 根据生物礁定量计算茅口期全球海平面变化幅度[J]. 中国科学(D辑), 2001, 31(3): 233-242.
[3] 李华, 马学平, 韦龙明. 广西菜子岩剖面中上泥盆统界线附近沉积相与海平面变化[J]. 古地理学报, 2009, 11(5): 503-512.
[4] Jinnah, Z.A. and Roberts, E.M. (2011) Facies Associations, Paleoenvironment, and Base-Level Changes in the Upper Cretaceous Wahweap Formation, Utah, U.S.A. Journal of Sedimentary Research, 81, 266-283. [Google Scholar] [CrossRef
[5] 李广雪, 刘勇, 杨子赓. 中国东部陆架沉积环境对末次冰盛期以来海面阶段性上升的响应[J]. 海洋地质与第四纪地质, 2009, 29(4): 13-19.
[6] Carvajal, C. and Steel, R. (2009) Shelf-Edge Architecture and Bypass of Sand to Deep Water: Influence of Shelf-Edge Processes, Sea Level, and Sediment Supply. Journal of Sedimentary Research, 79, 652-672. [Google Scholar] [CrossRef
[7] Jerrett, R.M., Hodgson, D.M., Flint, S.S. and Davies, R.C. (2011) Control of Relative Sea Level and Climate on Coal Character in the Westphalian C (Atokan) Four Corners Formation, Central Appalachian Basin, U.S.A. Journal of Sedimentary Research, 81, 420-445. [Google Scholar] [CrossRef
[8] Desjardins, P.R., Buatois, L.A., Pratt, B.R. and Mángano, M.G. (2012) Forced Regressive Tidal Flats: Response to Falling Sea Level in Tide-Dominated Settings. Journal of Sedimentary Research, 82, 149-162. [Google Scholar] [CrossRef
[9] 陈晓辉, 张训华, 李日辉, 蓝先洪. 辽东半岛南岸海域潮流沙脊及影响因素[J]. 海洋地质与第四纪地质, 2013, 33(1): 11-18.
[10] Fairbanksrg, M.K.G. (1985) Cenozoic 18 O Record of Climate and Sea Level. South African Journal of Science, 81, 248-249.
[11] 邵磊, 乔培军, 庞雄, 韦刚健, 李前裕, 苗卫良, 李昂. 南海北部近代沉积物钕同位素分布及意义[J]. 科学通报, 2009, 54(1): 98-103.
[12] 李军, 赵京涛. 冲绳海槽中部稀土元素地球化学特征及其在古环境变化研究中的应用[J]. 自然科学进展, 2009, 19(12): 1333-1342.
[13] 汪凯明, 罗顺社. 海相碳酸盐岩锶同位素及微量元素特征与海平面变化[J]. 海洋地质与第四纪地质, 2009, 29(6): 51-58.
[14] 许中杰, 程日辉, 张莉. 华南陆缘晚三叠-早、中侏罗世海平面相对升降与古气候演化的地球化学记录[J]. 地球科学, 2012, 37(1): 113-124.
[15] Whalen, M.T. and Day, J.E. (2010) Cross-Basin Variations in Magnetic Susceptibility Influenced by Changing Sea Level, Paleogeography, and Paleoclimate: Upper Devonian, Western Canada Sedimentary Basin. Journal of Sedimentary Research, 80, 1109-1127. [Google Scholar] [CrossRef
[16] Stanley, S.M., Ries, J.B. and Hardie, L.A. (2010) Increased Production of Calcite and Slower Growth for the Major Sediment-Producing Alga Halimeda as the Mg/Ca Ratio of Seawater is Lowered to a “Calcite Sea” Level. Journal of Sedimentary Research, 80, 6-16. [Google Scholar] [CrossRef
[17] Haq, B.U., Hardenbol, J. and Vail, P.R. (1988) Mesozoic and Cenozoic Chronostratigraphy and Eustatic Cycles. In: Wilgus, et al., Eds., Sea-Level Changes: An Integrated Approach, SEPM Special Publication No. 42, 71-108. [Google Scholar] [CrossRef
[18] Haq, B.U. and Sehutter, S.R. (2008) A Chronology of Paleozoic Sea-Level Changes. Science, 322, 64-68. [Google Scholar] [CrossRef] [PubMed]
[19] 许仕策, 秦国权, 杨少坤. 南海北部高分辨率生物地层学与相对海平面变化曲线[C]//龚再升, 李思田, 等. 南海北部大陆边缘盆地分析与油气资源. 北京: 科学出版社, 1997: 128-137.
[20] 谢金有, 祝幼华, 李绪深, 麦文, 赵鹏肖. 南海北部大陆架莺琼盆地新生代海平面变化[J]. 海相油气地质, 2012, 27(1): 49-58.
[21] Yoshi, N.S., Shoshirom, N.S., et al. (2008) Decadal Sea Level Variabiliy in the South Pacific in a Global Eddy-Resolving Ocean Model Hindcast. American Meteorological Society, 38, 1731-1746.
[22] Merrifield, M.A., Merrifield, S.T. and Mitchum, G.T. (2009) An Anomalous Recent Acceleration of Global Sea Level Rise. Journal of Climate, 22, 5772-5781. [Google Scholar] [CrossRef
[23] Burgess, E.W., Forster, R.R., Box, J.E., et al. (2010) A Spatially Calibrated Model of Annual Accumulation Rate on the Greenlandice Sheet (1958-2007). Journal of Geophysical Research: Earth Surface, 115, F2004. [Google Scholar] [CrossRef
[24] Munneke, P.K., Picard, G., van den Broeke, M.R., et al. (2012) Insignificant Change in Antarctic Snowmelt Volume since 1979. Geophysical Research Letters, 39, L01501.
[25] 丁明虎. 南极冰盖物质平衡最新研究进展[J]. 地球物理学进展, 2013, 28(1): 24-35.
[26] 邢凤存, 白振瑞, 李祯, 李思田. 塔里木盆地早、中志留世沉积序列及其对构造-海平面变化的响应: 以柯坪露头区为例[J]. 地球科学, 2011, 36(3): 541-554.
[27] 时国, 田景春, 喻美艺. 贵阳花溪地区下、中三叠统层序地层及其海平面变化[J]. 地层学杂志, 2011, 35(4): 397-403.
[28] Miall, A.D. (2005) Testing for Eustatic Sea-Level Control in the Precambrian Sedimentary Record. Sediment Geology, 176, 9-16. [Google Scholar] [CrossRef
[29] 林畅松, 潘元林, 肖建新, 孔凡仙, 刘景彦, 郑和荣. “构造坡折带”——断陷盆地层序分析和油气预测的重要概念[J]. 地球科学, 2000, 25(3): 260-266.
[30] 刘豪, 王英民, 王媛, 齐雪峰, 杜社宽. 大型坳陷湖盆坡折带的研究及其意义——以准噶尔盆地西北缘侏罗纪坳陷湖盆为例[J]. 沉积学报, 2004, 22(1): 95-102.
[31] 王英民, 金武弟, 刘书会, 邱桂强, 李群, 刘豪, 辛仁臣, 杨飞. 断陷湖盆多级坡折带的成因类型、展布及其勘探意义[J]. 石油与天然气地质, 2003, 24(3): 199-203.
[32] Veiga, G.D., Schwarz, E., Spalletti, L.A. and Assaferro, J.L. (2013) Anatomy and Sequence Architecture of the Early Post-Rift in the Neuquén Basin (Argentina): A Response to Physiography and Relative Sea-Level Changes. Journal of Sedimentary Research, 83, 746-765. [Google Scholar] [CrossRef
[33] 肖军, 王华, 陆永潮, 赵忠新, 陈亮. 琼东南盆地构造坡折带特征及其对沉积的控制作用[J]. 海洋地质与第四纪地质, 2003, 23(3): 56-62.
[34] 任建业, 张青林, 陆永潮. 东营凹陷弧形断裂坡折带系统及其对低位域砂体的控制[J]. 沉积学报, 2004, 12(4): 628-635.
[35] 倪金龙, 吕宝凤, 林玉祥, 王泽利, 夏斌. 渤南洼陷断裂坡折带系统及其沉积模式[J]. 桂林工学院学报, 2007, 27(2): 153-158.
[36] 王颖, 王晓州, 王英民, 辛仁臣, 赵志魁. 大型坳陷湖盆坡折带背景下的重力流沉积模式[J]. 沉积学报, 2009, 27(6): 1076-1083.
[37] 王永凤, 王英民, 李冬, 徐强. 珠江口盆地坡折带特征及其对沉积体系的控制[J]. 沉积与特提斯地质, 2011, 31(3): 1-6.
[38] 王颖, 王英民, 王晓洲, 辛仁臣, 赵志魁, 赵占银. 松辽盆地西部坡折带的成因演化及其对地层分布模式的控制作用[J]. 沉积学报, 2005, 23(3): 498-506.
[39] 邵磊, 庞雄, 乔培军, 陈长民, 李前裕, 苗卫良. 珠江口盆地的沉积充填与珠江的形成演变[J]. 沉积学报, 2008, 26(2): 179-185.
[40] 吕大炜, 李增学, 孙静, 吴立荣, 郭建斌, 刘海燕. 浅析陆相湖盆坡折带理论及其对沉积的控制[J]. 大庆石油勘探与开发, 2008, 27(3): 25-27.
[41] 刘豪, 王英民, 王媛. 浅海陆棚环境下沉积坡折带及其对局部强制海退体系域的控制[J]. 沉积学报, 2011, 29(5): 906-916.
[42] 张尚锋, 张昌民, 施和生. Siliciclastics Sequence Models in Wide and Low-Gradient Continental Margin of Northern South China Sea[C]//美国石油地质学家(AAPG)年会. Pittsburg, 2013: 110.
[43] Embry, A.F. (2002) Transgressive-Regressive (T-R) Sequence Stratigraphy. Sequence Stratigraphic Models for Exploration and Production: Gulf Coast SEPM Conference Proceedings, Houston, 151-172.
[44] 殷鸿福, 童金南. 层序地层界面与年代地层界线的关系[J]. 科学通报, 1995, 40(6): 539-541.
[45] Chakraborty, P.P. and Paul, S. (2008) Forced Regressive Wedges on a Neoproterozoic siliciclastic Shelf: Chandarpur Group, Central India. Precambrian Research, 162, 227-247. [Google Scholar] [CrossRef
[46] Catuneanu, O., Abreu, V., Bhatiacharya, J.P., et al. (2009) Towards the Standardization of Sequence Stratigraphy. Earth—Science Review, 92, 1-33. [Google Scholar] [CrossRef
[47] Helland-Hansen, W. (2009) Towards the Standardization of Sequence Stratigraphy—Discussion. Earth-Science Reviews, 94, 95-97.
[48] 梅冥相. 长周期层序形成机制的探索:层序地层学进展之二[J]. 古地理学报, 2010, 12(6): 711-728.
[49] 李绍虎. 对国外层序地层学研究进展的几点思考及L-H-T层序地层学[J]. 沉积学报, 2010, 28(4): 735-744.
[50] 杨有星, 金振奎, 王濮, 高白水, 刁丽颖, 李娜. 黄骅坳陷港中地区沙二段高分辨率层序地层格架与沉积体系分布[J]. 中南大学学报, 2012, 43(6): 2247-2258.
[51] 杨勇, 雷卞军, 冯永玖, 孟堃, 陈波, 叶武. 鄂尔多斯盆地子洲及邻区山西组二段高分辨率层序地层和煤沉积模式[J]. 石油与天然气地质, 2013, 34(1): 58-68.
[52] 朱红涛, 杨香华, 周心怀, 李建平, 王德英, 李敏. 基于层序地层学和地震沉积学的高精度三维沉积体系分析[J]. 地球科学, 2011, 36(6): 1073-1084.