二维沉积层序计算机模拟研究

林畅松; 解习农; 张燕梅; 刘景彦

二维沉积层序计算机模拟研究

1.
中国地质大学北京 100083;
2.
中国地质大学武汉 430074

基金项目: 国家自然科学基金(49572120、49302030)

详细信息

作者简介:
林畅松,男,39岁,教授,博士生导师,沉积学,盆地分析与模拟

计量

文章访问数: 725
HTML全文浏览量: 62
PDF下载量: 518
被引次数: 0

Tow-Dimensional Depositional Sequence Simulation

1.
China University of Geosciences, Beijing 100083;
2.
China University of Geosciences, Wuhan 430074

摘要

摘要: 本项研究建立了综合性的二维沉积层序模拟系统SSMS。该模拟系统由盆地的沉降过程模拟与盆地充填过程模拟两个子系统构成。盆地的沉降模拟结合了反演的沉降回剥和盆地形成的正演模型；盆地充填过程模拟综合考虑了盆地沉降、重力均衡作用、海（湖）平面升降、沉积物供给、侵蚀作用、沉积物分布和压实等因素。结合实例分析表明，该模拟系统可用于定量分析盆地构造、海（湖）平面、沉积物供给等变化对沉积层序的形成过程、几何形态及其沉积体系分布的控制作用，检验地质模型和进行预测。
- 沉积层序 /
- 计算机模拟
Abstract: A quantitative tow-dimensional depositional sequence model has been formulated to simulate the filling process of sedimentary basins. The system consist s of two subsystems: basin subsidence modelling and basin filling simulation, taking into account sea level change, tectonic subsidence, compaction of sediments, flexural isostatic compensation, erosion and sedimentation. Input basin subsidence rate can be derived by backst ripping technique, or be calculated by quantitative forward basin models. Geometric models, combined with diffusion models, have been used in the system to determine depositional surfaces and facies geometry. The system can be used to analysis the controlling processes of sedimentary basins and to predict sequence architecture and facies distribution within basins. The model has been alogrumthed to simulate the sedimentary filling of continental margin basins and shown that the tectonic subsidence rate variation and the amplitude of sea level change have a strong influence on the geometry and depositional style of basin fills.
- depositional sequence /
- computer simulation

HTML全文

参考文献(21)

[1]	.林畅松, 张燕梅. 拉伸盆地模拟理论基础与新进展. 地学前缘, 1995, 2(3): 79～88
[2]	.李思田, 林畅松. 论沉积盆地分析新进展. 当代地质学科前沿, 武汉: 中国地质大学出版社, 1993. 422～426
[3]	.Jervey M T. Quantitative geological modelling of siliciclastic rock sequences and their seismic expression. In: Wilgus C K, et al. ed. Sea-level Changes: an integrated approach. Soc. Econ. Palaeontol. Mineral. Spec. Publ. 1992, 42: 47～69
[4]	.Lawrence D T, Doyle M , Aigner T. Stratigraphic simulation of sedimentary basins: Concepts and calibration, AAPG, 1990, 74(3): 273～295
[5]	.Mckenzie D. Some remarks on the development of sedimentary basins. Earth and Planetary Science Letters, 1978, 40: 25～32
[6]	.Kusznir N J, Ziegler P A. The mechanics of continental extension and sedimentary basin formation: A simple-shear/pureshear flexural cantilever model. Tectonophysics, 1992, 215: 117～131
[7]	.Athy L F. Density, Porosity and compaction of sedimentary rocks. Bull Am Assoc Petro1 Geo1, 1930, 14: 1～24
[8]	.Allen P A, Allen J R. Basin Analysis principles and applications. London: British Petroleum Company plc, 1992. 43～143
[9]	.Falvey D A, Middleton M F. Passive continental margins: evidence for a prebreakup deep crustal metamorphic subsidence mechanism. In: Colloquium on Geology of Continental Margins (C3, Paris, 7-17 July 1980). Oceanologica Acta, 4(Supplement), 1981, 103～114
[10]	.Turcotte D L, Ahern J L. On the thermal and subsidence history of sedimentary basins. Journal of Geophysical Research, 1977, 82: 3762～3766
[11]	.Tetzlaff D M. Clastic simulation model of clastic sedimentary processes. AAPG Bulletin, 1986, 70: 655
[12]	.Bridge J S, Leeder M R. A simulation model of alluvial stratigraphy. Sedimentology, 1979, 26: 617～644
[13]	.Bitzer K, Harbaugh J W. DEPOSIM: a Mackintosh computer model for two-dimensional simulation of transport, deposition, erosion, and compaction of clastic sediments. Computers and Geosciences , 1987, 13(6): 611～637
[14]	.Aigner A, Brandenburg A, Vliet A V, et al. Stratigraphic modelling of epicontinental basins: two applications. Sedimentary Geology, 1990, 69: 167～190
[15]	.Douglas J Cant. Geometric modelling of facies migration: theoretical development of facies successions and local unconformities. Basin Research, 1991, 3: 51～62
[16]	.Nakayama K, Christopher G St C, Kendall. A simulation of basin margin sedimentation to infer geometry and lithofacies: a carbonate example, in: Taira A, Masuda F, ed. Sedimentary Facies in the Active Plate Margin. Terra Scientific Publishing Company, 1989. 17～31
[17]	.David J R, Michael S S, Bermard J C. Modeling the Stratigraphy of Continental Margins, Margin Continental Margin Stratigraphy, 1990 and 1991 report Lamont-Doherty Geological Observatory, An institute of Columbia University dedicated to research in earth sciences, 1991. 77～87
[18]	.Edward J Tarbuck, Frederick K Lutgens. The earth: an introduction to physical geology, Merrill Publishing Company, United States of America. 1987. 196～231
[19]	.Vail P R,Mitchum, Thompson. Global cycles of relative changes of sealevel. AAPG, 1977, 26
[20]	.林畅松, 李思田, 任建业. 断陷湖盆层序地层研究和计算机模拟. 地学前缘, 1995, 2(3): 124～177
[21]	.Lin Changsong, ZhangYanmei, Li Sitian, et al. Sequence stratigraphy modeling of sedimentary basin: application to Erlian and Yinggehai basins in East China. Earth Sciences, Joural of China University of Geosciences, 1996, 7(1): 132～137

[1]	赖维成, 李雪哲, 熊连桥, 谢晓军, 唐武, 王艳忠, 武爱俊, 白海强, 刘子玉, 王诗琪, 王铭乾, 赵振. 莺歌海盆地乐东区黄流组深层碎屑岩储层特征及优质储层控制因素 . 沉积学报, 2026, (): -. doi: 10.14027/j.issn.1000-0550.2026.010
[2]	段知非, 李超, 毕磊, 何中发, 李芳亮, 杨守业. 崇明岛H12孔百年来长江入海沉积物来源变化及原因 . 沉积学报, 2020, 38(6): 1204-1214. doi: 10.14027/j.issn.1000-0550.2020.002
[3]	马立元, 胡才志, 邱桂强, 陈纯芳, 高金慧, 徐士林. 鄂尔多斯盆地镇泾地区长8段储层非均质性及其结构模式 . 沉积学报, 2020, 38(5): 1088-1098. doi: 10.14027/j.issn.1000-0550.2020.039
[4]	王爱华, 叶思源, 刘建坤, 丁喜桂, 李华玲, 许乃岑. 不同选择性提取方法锶钡比的海陆相沉积环境判别探讨 . 沉积学报, 2020, 38(6): 1226-1238. doi: 10.14027/j.issn.1000-0550.2019.118
[5]	曹天宇, 钟大康, 牛胜利, 孙海涛, 曹轩, 王菲. 惠州凹陷东部珠海组储层碱性成岩作用及孔隙演化 . 沉积学报, 2020, 38(6): 1327-1337. doi: 10.14027/j.issn.1000-0550.2020.011
[6]	张耀续, 王利超, 谭秀成. 川北小南海剖面栖霞组岩石微相及沉积环境 . 沉积学报, 2020, 38(5): 1049-1060. doi: 10.14027/j.issn.1000-0550.2019.094
[7]	蒋庆平, 孔垂显, 李维锋, 邱子刚, 卢志远, 常天全, 刘凯, 陈栋梁, 李胜, 袁晓光. 陆相湖盆大型扇三角洲沉积特征与演化规律 . 沉积学报, 2020, 38(5): 923-932. doi: 10.14027/j.issn.1000-0550.2019.089
[8]	吕奇奇, 罗顺社, 官玉龙, 汪泽成, 王铜山, 张严. 华北克拉通南缘中—新元古界沉积充填特征及演化 . 沉积学报, 2020, 38(6): 1123-1139. doi: 10.14027/j.issn.1000-0550.2020.012
[9]	丁超, 庞燕青, 孟亚玲, 黄钰珑, 李闻东, 张顺存, 郭晖, 李佳思, 张明峰. 准噶尔盆地中拐地区上乌尔禾组富火山碎屑砂砾岩储层的古环境及储层机理研究 . 沉积学报, 2020, 38(4): 851-867. doi: 10.14027/j.issn.1000-0550.2020.054
[10]	张平. 稳定湖相沉积物和风成黄土粒度判别函数的建立及其意义 . 沉积学报, 2008, 26(3): 501-507.
[11]	陈陵康郭建秋顾延生. 西藏拉萨河现代河漫滩及一级阶地沉积物植硅体组合特征 . 沉积学报, 2008, 26(3): 480-486.
[12]	张金亮张鑫. 胜坨地区沙河街组沙四上亚段砂砾岩体沉积相与油气分布 . 沉积学报, 2008, 26(3): 361-368.
[13]	郭彦如刘化清李相博完颜容郑希民. 大型坳陷湖盆层序地层格架的研究方法体系 ———以鄂尔多斯盆地中生界延长组为例 . 沉积学报, 2008, 26(3): 384-391.
[14]	张道伟. 柴西南地区古近系—新近系井—震统一层序地层格架的建立 . 沉积学报, 2008, 26(3): 392-398.
[15]	郑庆华柳益群张海军李寿武朱静明马红星. 应用粒度成因单元划分高分辨率层序地层基准面旋回 . 沉积学报, 2008, 26(3): 376-383.
[16]	李磊. 尼日尔三角洲深水区层序地层及地震相研究 . 沉积学报, 2008, 26(3): 407-416.
[17]	刘宗堡. 三肇凹陷葡萄花油层高分辨率层序地层划分及沉积特征研究 . 沉积学报, 2008, 26(3): 399-406.

施引文献

资源附件(0)

访问统计

点击查看大图

计量

文章访问数: 725
HTML全文浏览量: 62
PDF下载量: 518
被引次数: 0

姓名
邮箱
手机号码
标题
留言内容
验证码

留言板

二维沉积层序计算机模拟研究

作者简介:
林畅松,男,39岁,教授,博士生导师,沉积学,盆地分析与模拟

计量

Tow-Dimensional Depositional Sequence Simulation

计量

目录

二维沉积层序计算机模拟研究

1. 中国地质大学北京 100083;

2. 中国地质大学武汉 430074

作者简介:
林畅松,男,39岁,教授,博士生导师,沉积学,盆地分析与模拟

English Abstract

Tow-Dimensional Depositional Sequence Simulation

1. China University of Geosciences, Beijing 100083;

2. China University of Geosciences, Wuhan 430074

全文HTML

目录

友情链接

期刊在线

联系我们

留言板

二维沉积层序计算机模拟研究

作者简介: 林畅松,男,39岁,教授,博士生导师,沉积学,盆地分析与模拟

计量

出版历程

Tow-Dimensional Depositional Sequence Simulation

计量

出版历程

目录

二维沉积层序计算机模拟研究

1. 中国地质大学 北京 100083; 2. 中国地质大学 武汉 430074

作者简介: 林畅松,男,39岁,教授,博士生导师,沉积学,盆地分析与模拟

English Abstract

Tow-Dimensional Depositional Sequence Simulation

1. China University of Geosciences, Beijing 100083; 2. China University of Geosciences, Wuhan 430074

全文HTML

目录

友情链接

期刊在线

联系我们

作者简介:
林畅松,男,39岁,教授,博士生导师,沉积学,盆地分析与模拟

1. 中国地质大学北京 100083;

2. 中国地质大学武汉 430074

作者简介:
林畅松,男,39岁,教授,博士生导师,沉积学,盆地分析与模拟

1. China University of Geosciences, Beijing 100083;

2. China University of Geosciences, Wuhan 430074