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Volume 39 Issue 1
Jan.  2020
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Article Navigation >  Bulletin of Geological Science and Technology  > 2020  >  39(1): 95-104
Wang Hua, Chen Si, Gong Tianhao, Yu Zhenghong, Huang Chuanyan, Zhang Yuehui, Zhao Rui. Sedimentary process and accumulation mechanism of traction fluidization gravity flow: An example from Qikou Sag, Bohai Bay Basin[J]. Bulletin of Geological Science and Technology, 2020, 39(1): 95-104. doi: 10.19509/j.cnki.dzkq.2020.0111
Citation: Wang Hua, Chen Si, Gong Tianhao, Yu Zhenghong, Huang Chuanyan, Zhang Yuehui, Zhao Rui. Sedimentary process and accumulation mechanism of traction fluidization gravity flow: An example from Qikou Sag, Bohai Bay Basin[J]. Bulletin of Geological Science and Technology, 2020, 39(1): 95-104. doi: 10.19509/j.cnki.dzkq.2020.0111
shu

Sedimentary process and accumulation mechanism of traction fluidization gravity flow: An example from Qikou Sag, Bohai Bay Basin

doi: 10.19509/j.cnki.dzkq.2020.0111
  • Received Date: 26 Dec 2019
    Abstract
  • The high efficiency reservoir in gravity flow deposits with traction flow features is one of the most important aspects in sedimentary research and exploration. The large-scale and multi-stage lacustrine gravity flow deposits developed in the first member of Shahejie Formation in Qikou Sag of Bohai Bay Basin exhibit their unique sedimentary features (The dimensions of gravity flow deposits are about 940 km2 in transverse area and 1.1 km in vertical scale). According to the hydrodynamic conditions and sedimentary process mechanism, the large-scale lacustrine gravity flow depositional system shows three types of relationships between tractive currents and gravity currents, which are identified as ①hierarchical progressive inheritance type, ②progressive transition type, ③merger fusion type. The sedimentary mechanism of gravity flow is divided into five types: muddy debris flow, sandy debris flow, transitional contemporaneous flow, high/low-density turbidity flow and high/low-density quasi-steady turbidity flow. The channelized gravity flow depositional system with gravity flow channel is the dominant feature in the central uplift zone of coastal area in the west, as the sheet-flow pattern is controlled by the sub-sag morphology in the east. This study aims to realize and refine the integration and relevance among sedimentary dynamic process, accumulation mechanism, sedimentary facies, and lithofacies, as well as determine the dominant control factors for the traction fluidized gravity flow. As a potential efficient reservoir target, the research results of traction fluidized gravity flow deposits can improve the theoretical system of lacustrine gravity flow, and at the same time, are significant for frontier breakthrough in petroleum exploration.It has practical production value and important reference for other continental lake basin oil and gas exploration.

     

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