Discussion about Base-level Changes in the Analysis of High-resolution Sequence Stratigraphy
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摘要: 基准面有三个不同的概念,即侵蚀基准面、沉积基准面和地层基准面。目前对于基准面的解释和应用存在争论,在应用中尤其比较模糊。在对高分辨率层序地层学中地层基准面的解释进行分析及基础上,对其在解释以海相沉积环境为主的部分提出了质疑并就可容空间与地层基准面的关系问题进行了讨论。可容空间是层序地层学关键概念,基准面也是层序地层学很重要的概念,两者对于解释层序形成机制是非常重要的。侵蚀基准面、沉积基准面、地层基准面都是势能面,都是动力学界面,都是变化的,只是分析的基准不同、形成的机制不同。为了深入地揭示这三种基准面的特征,还应该考虑基准面的定量研究问题。Abstract: There are three different concep tions about base-level that are base level of erosion, base level of deposition and stratigraphic datum, respectively. At present, the arguments still exist in the explanation and the app lication of base-level, especially bas-level seems amphibious in use. The exp lanation of the stratification base-level in the high-resolution sequence stratigraphy is analyzed in this paper, and, in particular, the portion focused on illustration about marine facies sedimentary environment is questioned. The author discussed the relation between accommodation space and stratigraphic datum. Accommodation space is the key conception in sequence stratigraphy and base-level is also important, so they are very significant to illustrate the mechanism of the formation of sequence. Base level of erosion, base level of deposition and stratigraphic datum are all potential energy levels, kinetic surfaces and are all variable, just differing from the criterion of analyses and the mechanism of formation. To illustrate the features of these three base-levels profoundly, more questions of quantitative research into base-level should be considered.
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Key words:
- accommodation space /
- base-level /
- sea level
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[1] 1 薛良清. 层序地层学研究现状、方法与前景[J].石油勘探与开发,1995,(05):8-13.
2 孟万斌. 从层序地层学到高分辨率层序地层学[J].成都理工学院学报,2000,(04):380-385.
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,(02):89-97.
4 邓宏文. 沉积物体积分配原理-高分辨率层序地层学的理论基础[J].地学前缘,2000,(04):305-313.
5 Cross T.A. High-resolution stratigraphic correlation from the perception of base-level cycles and sediment accommodation[A].1994.105-123.
6 Wheeler H E. Base-level, lithosphere surface and time-stratigraphy[J].Geological Society of America Bulletin, 1964.599-610.
7 Cross T A. Controls on coal distribution in transgressive-regressive cycles, Upper Cretaceous, Western Interior, U. S. A[A].SEPM Special Publication,1988. 371-380.
8 Posamentier H W,Jervey M T,Vail P R. Eustatic controls on clastic deposit ition Ⅱ: Conceptual Framework[J].SEPM Special Publication,1988.109-125.
9 徐怀大. 层序地层学原理[M].北京:石油工业出版社,1993.138-184.
10 池秋鄂,龚福华. 层序地层学基础与应用[M].北京:石油工业出版社,2001.35-36.
11 纪友亮,张世奇. 层序地层学原理及层序成因机制模式[M].北京:地质出版社,1998.93-95.
12 王龙樟,刘海兴. 基准面变化与层序地层--以塔里木盆地陆相地层为例[J].岩相古地理,1998,(03):1-6.
13 李增学,魏久传,韩美莲. 鲁西陆表海盆地高分辨率层序划分与海侵过程成煤特点[J].沉积学报,2000,(03):362-368.
14 李增学,魏久传,魏振岱. 含煤盆地层序地层学[M].北京:地质出版社,2000.146-147.
15 Shanley K W,McCabe P T. Perspective on the continental sequence stratigraphy[J].AAPG Bulletin,1994,(04): 544-568.
16 王嗣敏,刘招君. 基准面与可容空间变化分析及应用[J].世界地质,2001,(01):1-7. -
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