Journal of Atmospheric & Earth Sciences Category: Agriculture Type: Research Article

Seismic-sedimentary Facies Analysis of Es3x Formation in Southern Region, Laizhou Bay Depression, Bohai Bay Basin, China

Yang Xudong1, Xie Jun1*, Zhou Liang1, Wang Mengqi1 and Jiang Xinyu1
1 College Of Earth Science And Engineer, Shandong University Of Science And Technology, Qingdao, China

*Corresponding Author(s):
Xie Jun
College Of Earth Science And Engineer, Shandong University Of Science And Technology, Qingdao, China

Received Date: Jul 21, 2019
Accepted Date: Aug 05, 2019
Published Date: Aug 12, 2019


The southern region in the Laizhou bay Sag of the Bohai bay Basin has a good oil and gas display in Es3x formation (the lower third sub-member of the Shahejie Formation) through a few wells, indicating that large or medium-sized oil and gas fields may be discovered. Due to less drilling, low seismic reflection interface and low the degree of evolutionary research, it is still difficult to study the sedimentary facies in the study area. In this paper, both seismic facies analysis and logging data analysis are used to infer the sedimentary environment. Firstly, the study of seismic sections are used to identify the seismic facies of the study area. There are mainly four seismic phases in study area: parallel and sub-parallel seismic facies, foreset seismic facies, wedge-shaped seismic facies and filling seismic facies. Secondly, the distribution of sand bodies is predicted by seismic attributes. It is found that there is a strong amplitude region in the south of the study area, and there is a medium-strong amplitude region in the west, which is the sand body development area. The sedimentary characteristics of the study area are clarified by converting seismic facies to sedimentary facies and researching logging data. The research indicates that the braided river delta deposits developed in the western part of the study area, the fan delta deposits developed in the south and southwest part of the study area, and the mixed sediments deposits developed in the middle of the study area.


Laizhou bay sag; Mixed deposits; Sedimentary facies; Seismic facies; Seismic attribute


The southern region is located in Laizhou bay Depression of Bohai bay Basin. Due to the research area is just in the early exploration phase, there are few drilling wells, low research degree of seismic data, incomplete sedimentary evolution, and no similar oil fields have been developed, the relevant researches on the formation, deposition of this area will mainly rely on seismic1 and well logging data. And previous studies on seismic facies and sedimentary facies in this area were relatively weak. For the study on seismic facies, Dong conducted in-depth discussion on the seismic facies in the Liaodong bay area of Bohai bay Basin, reclassified the seismic facies, and combined the seismic facies and sedimentary facies to identify favorable reservoir facies zones [1]. In the study of sedimentary facies, Liu analyzed the mixed sedimentary characteristics, development patterns and main controlling factors in the south of Laizhou bay Depression in detail, and identified the dominant reservoir sub facies[2]. There are some differences between the previous studies and the study area. Therefore, it is particularly important to further study the seismic-sedimentary facies based on some previous views. In this paper, the distribution of sedimentary facies in the study area is studied by using the regional sedimentary environment combined with logging data and seismic data, and thecharacteristics of seismic sedimentology are discussed and summarized, so as to provide guidance and basis for the research and application of seismic facies and sedimentary facies in the study area in the future.


The southern region is located in the southern sea area of Bohaisea, China (Figure 1A). It is a favorable zone for oil and gas migration and accumulation in Nan sag (Figure 1B). Structural traps are well developed and formed (Figure 1C). The structural area is close to the source material, the spatial location of hydrocarbon source rocks, faults and sandstone reservoirs is well matched, and oil and gas migration is unobstructed, which is a favorable exploration target in the southern slope area of Laizhou bay Sag.
Figure 1: Schematic diagram of the location of the study area.

The tectonic evolution of Laizhou bay Sag in Bohai bay Basin is mainly influenced by the four stages of tectonic activities. Cenozoic strata are well developed in the study area. The main oil-bearing strata are Shahejieformation, especially Es3x formation, which is revealed by drilling data. From top to bottom of stratum is Nm formation, Ng formation, Ed formation, Es formation. The lithology of Nm formation is medium sandstones, fine sandstones and mudstones. The lithology of Ng formation is medium sandstones, grits and mudstones. The lithology of Ed formation is fine sandstones and mudstones. The lithology of Es formation is siltstones, fine sandstones and mudstones. The color of siltstones and fine sandstones is light grey. The color of mudstones is gray. On the whole, it is a set of sedimentary sequence from semi-deep lake to shore-shallow lake delta [2], the sedimentary range gradually becomes larger from small, and the shoreline gradually recedes(Figure 2A). In the middle well areas of Y3, Y4 and Y5 wells, terrigenous clastic and carbonate mixed sediments are developed. Sand and gravel bodies are the main favorable reservoirs and typical mudstone reservoirs (Figure 2B).
Figure 2: Comprehensive stratigraphic section of the southern region in Laizhou bay Sag.


The study area is located in the sea, with relatively complex geological conditions, low resolution of seismic data (the data is old and not clear). The data collected includes log data from some wells, the 3d seismic data volume of the study area and some lithologic photographs. The distribution characteristics of sand body are studied by analyzing seismic profile and using seismic attribute analysis to identify seismic facies.

Seismic facies analysis

Seismic phase analysis is to qualitatively identify various types of seismic phase markers on the seismic section, divide seismic phase units, make a variety of seismic phase parameter maps, and finally conduct comprehensive analysis of these maps [3]. The external geometry and internal reflection structure of the reflected waves can reflect the overall deposition process, provenance direction and geological background of sediments [4]. In this paper, firstly, the research horizon [5-7] was identified on the seismic profile by means of synthetic record and well seismic combination, andthen the planar distribution characteristics of sedimentary bodies were identified by using seismic attributes, including verification of sediment sources. Finally, seismic facies were converted into sedimentary facies by combining different seismic reflection structures and sedimentary environments.

According to the north-south seismic profile EF of well Y5 in the research area (Figure 3 and the profile position is shown in figure 1C), obvious foreset and truncated reflection structures can be seen in the profile, which is speculated to be a delta sedimentary environment [8-9], and the overall formation is thinning to the south, indicating that a south-to-north provenance sedimentary system near the profile. By analyzing the characteristics of the seismic profile MN in Es3x Formation of the study area, it is found that both parallel-subparallel reflection structures and fore-integrating reflection structures (Figure 4 and the position of the section is shown in figure 1C). In other sections, the characteristics of seismic facies are not only wedge-shaped and fill-shaped, but also sheet-shaped and other low-energy sedimentary environments, which fully reflect the characteristics of rapid deposition in fan delta, great difference in water energy, and rapid sedimentary phase transition. In the classification of seismic facies in the study area, the seismic profiles of several survey lines are dissected and analyzed one by one. It is considered that there are mainly four seismic facies in the study area (Figure 5): parallel to subparallel seismic facies, foreset seismic facies, wedge-shaped seismic facies and filling seismic facies.
Figure 3: Cross-Y5 well seismic profile (Inline461).

Figure 4: Seismic profile of Y2 well and Y5 well (other well locations are projection wells) (Xline1890).

Figure 5: Regional seismic legend of the study area.

Parallel to the horizontal seismic facies: In the study area, it mainly distributed in the central of Y3 well, Y4 well and Y5 well. Internal reflection structure is high amplitude, high continuity, nearly parallel to the shape characteristic. The seismic reflection external form for sheet, the lower level is parallel or nearly parallel to the contact, the thickness of relatively stable. And the lithology mainly mudstone purpose layer, sand ratio is less than 0.2 by analyzing core samples, it reflecting the weak hydrodynamic conditions of deposition as a result, reflects the uneven subsidence of delta platform characteristics

Foreset seismic facies: The front end of the foreset reflection layer presents a downward superstate toward the pelvic floor, while the proximal end presents a top superstate toward the basin edge. The wedge-shaped foreset in the study area is characterized by wedge-shaped distributionalong the same direction axis and forward accretion. It is mainly distributed in the south of Y4 well and Y8 well. According to the logging data of Y8 well, it indicates the fan delta deposition on the slope 

Wedge-shaped seismic facies: The whole profile is wedge-shaped, and the internal reflection features are composed of medium-strong amplitude and medium-high continuous reflection in the same phase axis, which is the result of different settlement and deposition rates around the lake basin. In the study area, it is mainly distributed in the southwest of Y2 well and located in the slope belt. According to the results of coring interval calibration, the wedge-shaped seismic facies in this area belongs to the sedimentary seismic response of braided river delta 

Filling phase: It is characterized by filling shape of the unit. There are two facies in gulch filling phase: open filling (low-energy environment) and partial filling (high-energy environment), the filling in the study area for filling deposit in valleys. In the seismic section, in local dent, rendered in valleys. For the waveform characteristics of the region, medium strong amplitude and continuity well and parallel reflection can be found. It mainly reflect the shore and shallow lake, half deep lake, braided delta and delta front sedimentary environment

Seismic attribute analysis

Different types of sedimentary environments have different characteristics in the seismic profile, which can also be shown in the attribute map. Analyzing attribute maps to study sedimentary environment and other information can better and more comprehensively reflect the planar distribution characteristics of sedimentary facies. Only by extracting seismic attributes in an appropriate way according to the exploration degree of the research area and the research object can the expected effect be achieved [10].

Under the guidance of seismic sedimentology, the target layer properties are accurately extracted. Appropriate time window layer is selected to extract seismic attributes, and seismic attributes are used to identify the planar distribution characteristics of the sedimentary system, and the sensitivity of the sedimentary system to seismic attributes is comprehensively considered to determine the characteristics of seismic facies [11]. We extracted RMS (root-mean-square) amplitude, mean instantaneous frequency and other attributes for analysis. Finally, it was found that the root-mean-square amplitude attribute had a guiding effect on the sedimentary plane distribution in the study area. By extracting the seismic attributes of RMS amplitude in Es3x formation in the 3D- seismic working area of the study area, it is found that there is a strong amplitude area in the south and southeast area of the study area (Figure 6ii), indicating that sand bodies in these areas are relatively developed and may be the main developed area of the delta. In the western part of the study area (Figure 6i), there is a band of mid-strong amplitude area, which is presumed to be braided river delta deposition. In the central area of the depression, that is, the south of Y8 well and around the northeast (Figure 6iii) are all weak amplitude areas, indicating that these areas are lake mudstone sedimentary areas and lacustrine sediments.
Figure 6: Root-mean-square amplitude attribute map of Es3x Formation.


Conversion of seismic and sedimentary facies

The seismic units were divided by analyzing multiple vertical provenance, parallel provenance profiles and seismic phases, and according to the frequency, amplitude and continuity characteristics of waveform features, the study zones were divided into 4 areas, and the seismic phase distribution map of Es3x formation of the target layer was obtained, which was named as I, II, III and IV (Figure 7).

Figure 7: Characteristics of the plane distribution of the seismic facies in Es3x formation.

According to the plane distribution characteristics of seismic facies in the study area and combined with the regional sedimentary environment [12-15], the corresponding transformation relationship between seismic facies and sedimentary facies was constructed (Table 1).

Phase type

 Facies marks


mixed sedimentary platform

parallel subparallel seismic facies

    mid-low frequency mid-strong amplitude middle continuity


mid frequency mid amplitude middle continuity

braided river delta

wedge-shaped seismic facies

     mid-low frequency mid amplitude middle continuity


    low frequency mid-low amplitude low continuity

fan delta

foreset seismic facies

    mid-low frequency mid-low amplitude low continuity


    mid frequency mid-low amplitude middle-low continuity

    mid frequency strong amplitude good continuity

    low frequency low amplitude middle-low continuity

shore shallow lake

parallel subparallel seismic facies

 mid-low frequency mid-low amplitude middle continuity


    low frequency mid-low amplitude good continuity

Table 1: Seismic reflection characteristics of typical sedimentary facies of Es3x formation in southern region.

Single well phase analysis

In Y3-Y4-Y5 wells area, it is still difficult to identify the mixed sedimentary characteristics from the seismic facies alone. The lithologic composition analysis of the raised part of similar platform will be conducted by using the single-well facies analysis to guide the sedimentary system. The sedimentary facies were analyzed by drilling data, and through well seismic combination, the over-well profile and single well phase were established to analyze the sedimentary pattern of the target horizon. Due to the differences in mixed sediments, the Ex3x formation can be divided into three oil groups (mainly oil groups II and III) (Figure 8).
Figure 8: Waveform characteristics and single well phase diagram of Y5 well.

From single well can be found in the phase diagram, III-2 of oil group to II-2 of oil group deposit gray powder sandstone with thin layers of mudstone, through the core can be found in the development of cross-bedding, wedge cross bedding, wavy bedding and other bar sedimentary characteristics, response on seismic profile characteristics of weak amplitude, medium-low frequency, medium continuously. II-1 of oil group to I-2 of oil group deposit thin layer powder sandstone and argillaceous siltstone with a large set of mudstone. Bioclastic can be found in the core photos. Sedimentary characteristics have parallel bedding, tabular and trough cross-bedding delta front. Waveform response on seismic profile for weak amplitude, low frequency, medium continuously; According to the lithologic combination characteristics, there are both carbonate rocks and terrigenous clastic rocks, it can be judged that the Y5 well area has mixed sedimentary morphology, which reveals the characteristics of the sand body being transformed by waves, and it is the lakeside sedimentary environment with shallow water.

It is found that the braided river delta deposits from the far Kendong uplift are developed in the western Y2 well area, while the fan delta deposits from the Weibei uplift are mainly developed in the eastern Y6-Y7-Y8 wells area. However, affected by the bottom uplift and faults, Y3-Y4-Y5 wells in the middle blocks the source materials from the Kendong and Weibei uplift and deposits the mixed sediments belonging to lacuvial facies (Figure 9).

Figure 9: Sediment map of Es3x formation in southern region.


Distribution of sedimentary facies

In Y3-Y4-Y5 wells area develop with mixed sedimentary mode - terrigenous clastic rock and carbonate rock mixed deposits, to the difficulty of mixed deposits has been a research on its mixed sedimentary area, surrounded by two kinds of material sources. One is in the study area of fan delta to the south and east, the other one is from the braided river delta deposits in western area, the terrigenous detrital material is as the waves were taken to mixed sedimentary area. The carbonate rocks were repeatedly changed by sea level at that time, which resulted in the protrusion exposed to the sea level or in the shallow water environment, resulting in the development of carbonate rocks.

Distribution of seismic facies

In the study area, the fan delta seismic facies and braided river delta seismic facies can be identified, which are the main sedimentary facies types in this area. However, the mixed sedimentary part in the middle is not easy to be identified from the seismic facies, which is the focus of the following research, trying to find the basis of mixed sedimentary from the seismic facies.


1. The characteristics of fore-accretion seismic facies, with the characteristics of wedge-like fore-accretion and fore-accretion in the same direction axis, indicating the fan delta front deposition on the slope. The uniformly subsided continental shelf delta platform is characterized by strong amplitude, medium and high continuity and near-parallel reflection structure, which belongs to parallel and subparallel reflection structure. The sedimentary environment of braided river delta is indicated by the seismic facies of sheet reflection and plate forward accretion reflection with medium amplitude, medium frequency and continuity well

2. According to the sedimentary environment, analysis of seismic profiles, seismic facies analysis, seismic attribute analysis, the study area in southern and eastern Y6-Y7-Y8 wells area of fan delta sedimentary facies, provided source by Weibei uplift. The study area in western Y2 well area is braided river delta sedimentary facies, provide source from Kendong uplift. Central Y3-Y4- Y5 wells area is affected by the bottom uplift raised for similar platform, sedimentary lacustrine peperite


  1. Yanlei D, Yumin Z, Dejiang L, Jun-sheng Y, Yu-yin Z, et al. (2007) Seismic facies of Paleogene in Liaodong Bay area, Bohai Bay Basin.ActaSedimentologicaSinica 4: 554-563.
  2. Wenchao L, Guokun Z, Hongfei Y, et al. (2018) Mixed sedimentary characteristics and developmental patterns of the Paleogene in the southern Laizhou Bay Sag, Bohai Sea. Journal of Palaeogeography 20: 1033-1042.
  3. Ruijie X (2008) Study on sequence stratigraphy and sedimentary facies of the lower member of Shahejie Formation in Minfeng area, Dongying Sag. Lithologic Reservoirs 20: 39-43.
  4. Yonggang W, Youxi L, Junhua Z (2006) Seismic attribute analysis technology. Beijing: China University of Petroleum Press.
  5. Gaiwei W, Xiaofeng D, Donghui J, Qiming W, Jifeng D (2015) High-precision sequence stratigraphic framework and sedimentary system evolution in the middle third member of Shahejie Formation, Laizhou Bay Sag. Sedimentary and Testi Geology 35: 17-24.
  6. KhalifaMK,Mills KJ, Hlal O(2016) Seismic stratigraphic interpretation of megasequence and sequence framework in the Upper Cambrian through Devonian formations in the central part of the Darling Basin, western New South Wales, Australia. Marine and Petroleum Geology 77: 668-692.
  7. Ghani H (2009) Structural and stratigraphic interpretation of seismic data of joyamair area chakwal,Pakistan. Earth Science Frontiers16: 215.
  8. Xiaoping W, Bo C, Guang Z, Quan L, fragrance N (2008) Application of seismic facies analysis technique to sedimentary characteristics analysis of Yitong mantle reservoir. Petroleum Geophysical Prospecting 2: 172-178.
  9. Lei L, Ying-min W, Zhi-chao H, Ya-hong R, Lian-mei Z (2008) Sequence stratigraphy and seismic facies study in the deep waters of the Niger Delta. ActaSedimentologicaSinica 3: 407-416.
  10. Zunde C, Fugui Z (1998) Attribute optimization method in seismic data oil and gas prediction. Geophysical Prospecting for Petroleum 37: 32-40.
  11. XiannaZ (2017) Research on multi-attribute joint inversion reservoir seismic prediction method. Jilin University, Changchun, China.
  12. Gang G, Shangru Y, Tong Q (2018) Current status of mixed deposition research and its relationship with oil and gas enrichment. Geological Science and Technology Information 37: 82-88.
  13. Maosong Y,Xiong J, Changgui X, Xiaofeng D, Zhangqiang S, et al. (2018) Discussion on classification and naming system of mixed rock and its implications for evaluation of mixed rock reservoirs: A case study of mixed rock in Bohai Sea. Geological Review 64: 1118-1131.
  14. Jinliang Z, XueqiangS (2007) Mixed sedimentation of carbonate and terrigenous clastics in faulted basin: A case study of the upper member of the fourth member of the Shahejie Formation of the Paleogene in Jinjia area, Dongying depression.Geological Review 4: 448-453.
  15. Lei H, Qiang W, Qiang W, Qiang W (2012) Evolution of the Cenozoic basin in the Laizhouwan Sag, Bohai Bay Basin. Chinese Journal of Geology, 86: 867-876.

Citation: Xudong Y, Jun X, Liang Z, Mengqi W, Xinyu J (2019) Seismic-sedimentary Facies Analysis of Es3x Formation in Southern Region, Laizhou Bay Depression, Bohai Bay Basin, China. J Atmos Earth Sci 3: 011.

Copyright: © 2019  Yang Xudong, et al. This is an open-access article distributed under the terms of the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited.

© 2022, Copyrights Herald Scholarly Open Access. All Rights Reserved!