ZHENG Rong cai, PENG Jun, WU Chao rong. Grade Division of Base-level Cycles of Terrigenous Basin and Its Implications[J]. Acta Sedimentologica Sinica, 2001, 19(2): 249-255.
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ZHENG Rong cai, PENG Jun, WU Chao rong. Grade Division of Base-level Cycles of Terrigenous Basin and Its Implications[J]. Acta Sedimentologica Sinica, 2001, 19(2): 249-255.
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Grade Division of Base-level Cycles of Terrigenous Basin and Its Implications
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1 Sedimentary Institute of Chengdu University of Technology, Chengdu 610059;
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2 Postdoctoral Researchers Flow Station of SW China Petroleum Institute, Nanchong Sichuan 637001
- Received Date: 2000-10-20
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Abstract
By applying the thcorv and technology of the high-resolution sequence stratigraphy to the sequence analysis of tcrrigcnous hasin, one of the kcv techniques is to distinguish and divide the different genesis interfaces and the different grades of the base-level cycle.In this paper taking a few basins which have different tectonic characteristics as cases, the authors have recognized six types of interfaces which are controlled by different factors, and have different genetic features, developmcnt scales and identification marks.According to the genetic features and the differences among the interfaces, six-grade division schemes of base-level cycle are proposed which are huge base level cycle and super-long-time long time middle time short time super-short-time base-level cvclc, and division criterions of different base-level cycles arc established.The authors have also discussed the time interval of different base level cycle and considered that the preceding three low frcqucncc and long period cycles are mainly controlled by tectonic factors and the following three high frcqucncc and short period cycles are mainly controlled by the astronomic factor. At the same time the implications of different grade base-level cycles dcaltwith the exploration and development of oil and gas field are discussed respectively.
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References
|
[1]
|
1 Vail P R. Seismic stratigraphy interpretation using seguence stratigraphy.Part 1：seismic stratigraphy interpretation procedure[A]. In：BaIIy A W，ed.Atlas of seismic stratigraphy[C]. AAPG，Studies in Geology，1987，27：11~ 10
2 Cross T A. Controls on coal distribution in transgressive-regressive cycles，Upper Cretaceous，Western Interior，U. S.A.[A]. In：Wilgaus C K，et al.Sea- Ievel changes：An intergrated approach[C]. SEPM Sepcial Publication，42，1988.371 ~ 380
3 邓宏文. 美国层序地层研究中的新学派—高分辨率层序地层学[J].石油与天然气地质，1995，16（2）：9 ~ 97
4 邓宏文，王洪亮，李熙吉吉. 层序地层地层基准面的识别、对比技术及应用[J]. 石油与天然气地质，1996，17（3）：177 ~ 184
5 郑荣才，尹世民，彭军. 基准面旋回结构与叠加样式的沉积动力学分析[J]. 沉积学报，2000，18（3）：369 ~ 375
6 邓宏文，王洪亮，李小孟. 高分辨率层序地层对比在河流相中的应用[J]. 石油与天然气地质，1997，18（2）：90 ~ 95
7 王洪亮，邓宏文. 地层基准面原理在湖相储层预测中的应用[J]. 石油与天然气地质，1997，18（2）：96 ~ 102
8 魏魁生，徐怀大，叶淑蓉等. 松辽盆地白垩系高分辨率层序地层格架[J]. 石油与天然气地质，1997，18（1）：4 ~ 7
9 邓宏文，徐长费，王洪亮. 陆东凹陷上侏罗统层序地层与生储盖组合[J]. 石油与天然气地质，1998，19（4）：275 ~ 279
10 郑荣才. 四川盆地下侏罗统大安寨段高分辨率层序地层学特征[J]. 沉积学报，1998，16（2）：42 ~ 49
11 杜春艳，郑荣才. 陕北长6 油层组短期基准面旋回与储层非均质性的关系[J]. 成都理工学院学报，1999，26（1）：17 ~ 22
12 郑荣才，吴朝容. 西部凹陷深层沙河街组生储盖组合的层序分析[J]. 成都理工学院学报，1999，26（4）：348 ~ 356
13 吴朝容，郑荣才. 辽河油田西部洼陷沙河街组高分辨率层序地层学特征[J]. 成都理工学院学报，1999，26（4）：375 ~ 381
14 柳梅青，陈亦军，郑荣才. 川西新场气田蓬莱镇组陆相地层高分辨率层序地层学研究[J]. 沉积学报，2000，18（1）：50 ~ 56
15 郑荣才，吴朝容，叶茂才. 浅淡陆相盆地高分辨率层序地层研究思路[J]. 成都理工学院学报，2000，27（3）：241 ~ 244
16 Galloway W E. Genetic stratigraphic seguences in basin analysis I：architecture and genesis of flooding-surface bounded depositional units[J].AAPG. 1989，73：125 ~ 142
17 Johnson J G，Klapper G，Sandberg C A. Devonian eustatic fIuctuation in Eurameria[J]. GeoIogicaI Socitery of America BuIIetin，1985，96：567 ~87
18 郭建华，宫少波，吴东胜. 陆相断陷湖盆T—R 旋回沉积层序与研究实例[J]. 沉积学报，1999，16（1）：8 ~ 14 |
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