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《Acta Petrolei Sinica》 2006-01
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Control of valley and tectonic slope-break zone on sand bodies in rift-subsidence basin

Feng Youliang(Research Institute of Petroleum Exploration and Development,CNPC,Beijing 100083,China)  
The relationship between palaeogeomorphology and development of sand bodies shows that there developed fault through,faults-transfer zone and incised valley in the depression wedges of the Paleogene of Bohai Bay Basin.Three basic valleys all controlled the positions of sandstone and conglomerate fan.The syndepositional tectonic slope-break zone controlled the distributions of sandstone and conglomerate.The thickness of sandstone and conglomerate is bigger at lower part of tectonic slope-break zone,and the distribution directions of sandstone and conglomerate are same as that of the syndepositional tectonic slope-break zone.The characteristics of syndepositional tectonic slope-break zone and its control to the distribution of sand bodies are different in different rifting episode.The main steep-slope faults and gentle-slope faults with dip-reverse strata were developed in the rift initiation episode.The main steep-slope faults and gentle-slope faults with dip-same strata were developed in the rift climax episode.Many syndepositional faulted slope-break zone resulted from above faults controlled the distribution of sand bodies.In post-rift episode,part syndepositional faulted slope-break zone changed into bent slope-break zone.The two kinds of slope-break zones together controlled the distribution of sand bodies.
【Fund】: 国家“十五”科技攻关项目(2003BA613A-01)“中国东部岩性油气藏地质评价和关键技术研究”资助
【CateGory Index】: P544.4;P618.13
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