东营凹陷滑塌型重力流沉积分布特征及三角洲沉积对其影响

张青青; 操应长; 刘可禹; 杨田; 王艳忠; 贾光华; 刘鑫金

doi:10.3799/dqkx.2017.129

Volume 42 Issue 11

Nov. 2017

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Zhang Qingqing, Cao Yingchang, Liu Keyu, Yang Tian, Wang Yanzhong, Jia Guanghua, Liu Xinjin, 2017. Sedimentary Characteristics of Re-Transported Gravity Flow Deposits and Their Distribution:Influence of Deltaic Sedimentation in the Dongying Sag. Earth Science, 42(11): 2025-2039. doi: 10.3799/dqkx.2017.129

Citation:

Zhang Qingqing, Cao Yingchang, Liu Keyu, Yang Tian, Wang Yanzhong, Jia Guanghua, Liu Xinjin, 2017. Sedimentary Characteristics of Re-Transported Gravity Flow Deposits and Their Distribution:Influence of Deltaic Sedimentation in the Dongying Sag. Earth Science, 42(11): 2025-2039. doi: 10.3799/dqkx.2017.129

Citation:

Zhang Qingqing, Cao Yingchang, Liu Keyu, Yang Tian, Wang Yanzhong, Jia Guanghua, Liu Xinjin, 2017. Sedimentary Characteristics of Re-Transported Gravity Flow Deposits and Their Distribution:Influence of Deltaic Sedimentation in the Dongying Sag. Earth Science, 42(11): 2025-2039. doi: 10.3799/dqkx.2017.129

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Sedimentary Characteristics of Re-Transported Gravity Flow Deposits and Their Distribution:Influence of Deltaic Sedimentation in the Dongying Sag

doi: 10.3799/dqkx.2017.129

1.
School of Geosciences, China University of Petroleum, Qingdao 266580, China
2.
Laboratory for Marine Mineral Resources, Qingdao National Laboratory for Marine Science and Technology, Qingdao 266071, China
3.
Geological Institute of Shengli Oilfield, Dongying 257000, China

Received Date: 2017-05-18
Publish Date: 2017-11-15

Abstract

Abstract

Deltaic sedimentation provides the material source for the formation of re-transported gravity flow, and it has a significant effect on the sedimentary characteristics and distribution of re-transported gravity flow deposits. The sedimentary characteristics of different types of gravity flow deposits and their distribution in the middle part of the third member of Shahejie Formation of the Dongying sag were investigated using core, granularity, seismic and well logging data. The influence of deltaic sedimentation on the re-transported gravity flow deposits was studied. It has been shown that four types of gravity flow deposits were developed in Es₃^z in the Dongying sag, including slide and slump deposits, debrites, and turbidites. There exist differences among different types of gravity flow deposits in terms of sedimentary structures, grain size characteristics, and geophysical responses. In the study area, sandy debrites were best developed, followed sequentially by slide and slump deposits, turbidites, and muddy debrites. There are differences in the abundance of the types and the vertical sequences of diffenent deposits among different locations in the study area. The sedimentary types are mainly composed of sandy debrites with vertical sequences characteristic of amalgamation of sandy debrites being common in the southern Boxing and Xin-133 blocks.There is a big difference among gravity flow deposits and vertical sequences from proximal to distal in the southern of Niuzhuang area and the western central uplift zone.Turbidites are better developed in the Ying-11 block. Sandy debrites and slump deposits are the dominated deposits in the Feng-14 block. The mud content of the delta front deposits appears to have a significant impact on the gravity flow types and their sedimentary characteristics. Deltaic sediments with different grain sizes have different slope angles which is closely related to the formation, types and distribution characteristics of the gravity flow deposits. Under the same conditions, the larger the progradation slope angle is, the better developed the re-transported gravity flow deposits would be, especially for the slide and slump deposits. On the contrary, the sliding distance is shorter. The slide and slump deposits are mainly distributed in the slope break and near the syn-sedimentary faults; turbidites are mainly in the basin floor; while debris flow deposits occur from the slope break to the basin floor.The high accumulation rate contributes to the formation of gravity flows by decreasing the internal friction, and the difference between the accumulation rate and subsidence rate is also of great importance to the vertical superimposed structures and lateral continuity of re-transported gravity flow deposits.
- re-transported gravity flow deposits,
- sedimentary characteristics,
- distribution characteristics,
- delta source,
- Es₃^z,
- Dongying sag,
- petroleum geology

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References(80)

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