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    中国百强科技报刊

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    Volume 38 Issue 1
    Jan.  2013
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    Article Contents
    ZHU Hong-tao, YANG Xiang-hua, ZHOU Xin-huai, LI Jian-ping, WANG De-ying, LI Min, 2013. Sediment Transport Pathway Characteristics of Continental Lacustrine Basins Based on 3-D Seismic Data: An Example from Dongying Formation of Western Slope of Bozhong Sag. Earth Science, 38(1): 121-129. doi: 10.3799/dqkx.2013.012
    Citation: ZHU Hong-tao, YANG Xiang-hua, ZHOU Xin-huai, LI Jian-ping, WANG De-ying, LI Min, 2013. Sediment Transport Pathway Characteristics of Continental Lacustrine Basins Based on 3-D Seismic Data: An Example from Dongying Formation of Western Slope of Bozhong Sag. Earth Science, 38(1): 121-129. doi: 10.3799/dqkx.2013.012

    Sediment Transport Pathway Characteristics of Continental Lacustrine Basins Based on 3-D Seismic Data: An Example from Dongying Formation of Western Slope of Bozhong Sag

    doi: 10.3799/dqkx.2013.012
    • Received Date: 2012-09-28
    • Publish Date: 2013-01-15
    • Due to insufficient well data, the diversity of sediment transport pathway and their controlling deposits was analyzed using the recent 3D seismic data in the western slope of Bozhong sag. The results show that there are three types of sediment transport pathway in Dongying formation of the western slope of Bozhong sag, including sediment transport pathway of Paleo-channel, faulted trough and structural transfer zones. The deposits of study area were controlled mainly by faulted trough sediment transport pathway derived from Shaleitian uplift, with the belted distribution in NEE direction. The deposits controlled by paleo-channel sediment transport pathway occurred in the local area of southern Shijiutuo uplift. The deposits controlled by structural transfer zones sediment transport pathway are focused on the local area of southeast Shaleitian uplift. Three types of sediment transport pathway display the overall sediment transport methods from the source area to the deposits area in the continental lacustrine basins, and formed three types corresponding coupling patterns of the source area- transport pathway-deposit area. Structural transfer zones sediment transport pathway is considered one special style of faulted trough sediment transport pathway. The presence of faulted trough sediment transport pathway derived from the Shaleitian uplift changes the past understanding that it is the fan delta with proximal and rapid deposit in the eastern Shaleitian uplift, and provides an effective model for seeking potential reservoir.

       

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