胜利探区埕岛地区前古近系断层发育特征及其油气地质意义OA
Characteristics of pre-Paleogene faults and their petroleum geological significance in the Chengdao area of Shengli exploration region
针对埕岛地区前古近系断层控藏作用制约勘探的这一关键问题,基于三维地震资料的精细解释与钻井数据,采用精细几何构造解析与平衡剖面技术,系统探讨了埕岛地区前古近系断层的发育特征,深入剖析了其对潜山储层、圈闭及油气成藏过程的控制作用.研究表明,埕岛地区主控断层包括埕北断层、埕北 20断层及埕北 30断层,它们将埕岛潜山划分为西排山、中排山和东排山 3大区域;中排山与东排山在燕山期受郯庐断裂带左旋走滑影响,发育了一系列NNE向走滑断层,将潜山进一步切割为近SN向条带;近EW向的反向拉张断层加剧了构造复杂性,形成了潜山复杂的EW向断块构造格局.依据构造样式及应力场特征,将埕岛潜山地区划分为伸展构造带、张扭构造带、压扭构造带和走滑构造带.埕岛地区主控断层控制着潜山构造的整体演化,次级断层则决定了圈闭的形成与分布模式;断层的活动性差异是埕岛地区潜山油气藏差异富集的主要控制因素,规模大且活动断裂所控制的裂缝活动范围介于 270~350 m,断层的活动强度、持续时间均与风化壳及裂缝型储层的发育程度呈正相关.整体而言,埕岛地区潜山呈现出多油源供烃与大断层分割的复合油气地质特征.该认识有效指导了有利目标的勘探评价工作,证实了其合理性及对油气勘探实践的重大意义.
Based on detailed interpretation of 3D seismic data and drilling data,we systematically explored the developmental characteristics of pre-Paleogene faults in the Chengdao area using refined geometric structural ana-lysis and balanced cross-section techniques,and deeply analyzed their controlling effects on buried hill reservoirs,traps,and the hydrocarbon accumulation process.Results show that the dominant faults in the Chengdao area in-clude the Chengbei Fault,Chengbei 20 Fault,and Chengbei 30 Fault.As the main controlling faults of buried hills,we divided the Chengdao buried hills into three rows:the western,the middle,and the eastern ones.Moreover,during the Yanshanian period,the middle row and the eastern row of Hills were influenced by the sinis-tral strike-slip of the Tan-Lu Fault Zone,resulting in the development of a series of NNE-trending strike-slip faults,by which further divided the buried hills into several north-south trending strips.The nearly EW-trending reverse extension faults exacerbated the structural complexity,forming a complex east-west fault-block structural pattern in the buried hills.In structural styles and stress field characteristics,the Chengdao buried hill area was di-vided into an extensional tectonic zone,a transtensional tectonic zone,a transpressional tectonic zone,and a strike-slip tectonic zone.The main faults in the Chengdao area controlled the overall evolution of the buried hill struc-ture,while the subordinate faults determined the formation and distribution patterns of traps.In addition,differ-ences in fault activity were the main controlling factors on the differential enrichment of hydrocarbon reservoirs in the buried hills.The range of fracture activity controlled by large-scale active faults is between 270 m and 350 m.The intensity and duration of fault activity are positively correlated with the development degree of weathered crust and fractured reservoirs.Overall,the buried hills in the Chengdao district exhibit characteristics of multiple hydrocarbon sources and segmentation by major faults.
信延芳;王永诗;景安语;郭玉新;张明华;罗阳;马帅;田雯
中国石化胜利石油管理局有限公司,博士后科研工作站,东营 257000||中国石化胜利油田分公司,勘探开发研究院,东营 257015中国石化胜利油田分公司,东营 257001中国石化胜利油田分公司,勘探开发研究院,东营 257015中国石化胜利油田分公司,勘探开发研究院,东营 257015中国石化胜利油田分公司,勘探开发研究院,东营 257015中国石化胜利油田分公司发展规划部,东营 257001中国石化胜利油田分公司,勘探开发研究院,东营 257015中国石化胜利油田分公司,勘探开发研究院,东营 257015
海洋科学
埕岛地区负反转构造潜山构造演化潜山油气藏
Chengdao areanegative inversion structureburied hill tectonic evolutionburied hill hydrocarbon reservoir
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