The types and implication of migrated sequence stratigraphic architecture in continental lacustrine rift basin: an example from the Paleogene Wenchang Formation of Zhu I Depression, Pearl River Mouth Basin

被引:4
|
作者
Zhu H. [1 ,2 ]
Li S. [1 ,2 ]
Liu H. [1 ,2 ]
Shu Y. [3 ]
Mei L. [1 ,2 ]
Yang X. [1 ,2 ]
机构
[1] Key Laboratory of Tectonics and Petroleum Resources, China University of Geoscien, Wuhan
[2] Faculty of Earth Resources, China University of Geosciences, Wuhan
[3] China National Offshore Oil Corporation Limited-Shenzhen, Guangzhou
来源
| 1600年 / China University of Geosciences卷 / 41期
关键词
Allogenic migration; Autogenic migration; Hydrocarbons; Migrated sequence stratigraphic architecture; Wenchang Formation; Zhu I depression;
D O I
10.3799/dqkx.2016.028
中图分类号
学科分类号
摘要
Compared with the sequences of marine basins, sequence stratigraphic architecture of non-marine basins is characterized by multi-variation and uncertainty. Migrated sequence stratigraphic architecture is one non-normal type in the evolution of continental lacustrine rift basin, which is rare documented. Based on the sequence stratigraphic units analysis of Paleogene Wenchang Formation of Huizhou and Enping sags, Zhu I Depression, Pearl River Mouth Basin, this paper defined the concept of migrated sequence stratigraphic architecture and divided into autogenic and allogenic migration. Autogenic migrated sequences are mainly controlled by horizontal displacement of low-angle syndepositional normal fault, whereas allogenic migrated sequences are controlled by the different tectonic activation episodes of boundary fault on both sides of the basin. In other words, autogenic and allogenic migrated sequences are controlled by one and two syndepositional boundary fault, respectively. During the lateral migration of sequences, reservoirs and source rocks controlled by sequence stratigraphic units at multiple scales also migrate and stack laterally. This helps the high-efficient configuration of hydrocarbon accumulation factors (e.g., source rock, reservoir, and seal) to generate reservoir combination with multiple blocks and multiple strata. © 2016, Editorial Department of Earth Science. All right reserved.
引用
收藏
页码:361 / 372
页数:11
相关论文
共 35 条
  • [1] Chen H.Z., Wu X.J., Zhou D., Et al., Meso-Cenozoic Faults in Zhujiang River Mouth Basin and their Geodynamic Background, Journal of Tropical Oceanography, 24, 2, pp. 52-61, (2005)
  • [2] Ji Y.L., Zhang S.W., Wang Y.S., Et al., The Relationship between the Scales of Petroleum Collective System and the Scales of Sequence Boundary, Acta Sedimentologica Sinica, 26, 4, pp. 617-623, (2008)
  • [3] Jiang C.F., Zhu S.N., Introduction to Tectonic Migration Theory, Bulletin of the Chinese Academy of Geological Sciences, 13, 1, pp. 1-14, (1992)
  • [4] Jiang Z.X., Principle and Application of Sequence Stratigraphy, (1996)
  • [5] Jiang Z.X., Lu H.B., Yu W.Q., Et al., Transformation of Accommodation Space of the Cretaceous Qingshankou Formation, the Songliao Basin, NE China, Basin Research, 17, 4, pp. 569-582, (2005)
  • [6] Jiang Z.X., Zhang L., Lin W., Et al., Research on the Accommodation Space Transformation System in the Esz3 Member of the Gu'nan Sag, Earth Science Frontiers, 15, 2, pp. 26-34, (2008)
  • [7] Leeder M.R., Tectonic Sedimentology:Sediment Systems Deciphering Global to Local Tectonics, Sedimentology, 58, 1, pp. 2-56, (2011)
  • [8] Lei B.H., Zheng Q.G., Li J.L., Et al., Formation and Evolution of Zhu-3 South Fault and its Control on the Depocenter Shift in Zhu-3 Depression, Pearl River Mouth Basin, Acta Petrolei Sinica, 33, 5, pp. 807-813, (2012)
  • [9] Lerch D.W., Klemperer S.L., Egger A.E., Et al., The Northwestern Margin of the Basin-And-Range Province, Part 1:Reflection Profiling of the Moderate-Angle (~30°) Surprise Valley Fault, Tectonophysics, 488, 1-4, pp. 143-149, (2010)
  • [10] Li S.T., Pan Y.L., Lu Y.C., Et al., Key Technology of Prospecting and Exploration of Subtle Traps in Lacustrine Fault Basins, Earth Science, 27, 5, pp. 592-598, (2002)