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    中国百强科技报刊

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    Volume 29 Issue 5
    Sep.  2004
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    Article Contents
    WANG Hua, LU Yong-chao, LIAO Yuan-tao, WANG Zhen-feng, LI Xu-shen, 2004. Sequence Architecture and Favorable Reservoir Prediction of Sanya Formation in the Central and Eastern Qiongdongnan Basin. Earth Science, 29(5): 609-614.
    Citation: WANG Hua, LU Yong-chao, LIAO Yuan-tao, WANG Zhen-feng, LI Xu-shen, 2004. Sequence Architecture and Favorable Reservoir Prediction of Sanya Formation in the Central and Eastern Qiongdongnan Basin. Earth Science, 29(5): 609-614.

    Sequence Architecture and Favorable Reservoir Prediction of Sanya Formation in the Central and Eastern Qiongdongnan Basin

    • Received Date: 2004-07-06
    • Publish Date: 2004-09-25
    • The Sanya Formation is one of the most important exploration layersin the area ajacent ② fault belt, central and eastern Qiongdongnan basin. The Sanya Formation can be divided into two third-order sequences (S60-S52, S52-S50) based on the integrated analysis of seismic and logging well data. The sequence of S60-S52 is formed on the beginning of thermal subsidence after rifting. This sequence and overlying one of S52-S50 are characterized by occurrence of the flexural slope-break, which is controlled by deep buried faults. Two slope-breaks constrain the development of system tracts in third-order sequence. Incised valley and slope fan are observed commonly in lowstand system tracts(LST)of the S60-S52 sequence, progradational wedge and slope fan occur widely in LSTof the S52-S50 sequence. Depositional systemsin transgressive system tracts and highstand system tracts are also controlled by double shelf slope-break zones which are taken as the boundary of different depositional systems from littoral shelf to continental slope, bathyal sea to deep sea. The results suggest that the Sanya Formation near the ② fault belt taken as the slope break zone is a favorable area for hydrocarbon exploration.

       

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