石油与天然气地质 ›› 1985, Vol. 6 ›› Issue (4): 386-394.doi: 10.11743/ogg19850408

• 论文 • 上一篇    下一篇

倾斜断块-潜山油气藏——拉张型断陷盆地内新的油气圈闭类型

李德生   

  1. 石油工业部石油勘探开发科学研究院
  • 收稿日期:1984-10-31 出版日期:1985-12-25 发布日期:2012-01-16

TILTED FAULT BLOCK-BURIED HILL TRAPS——A NEW TYPE OF OIL/GAS TRAPS IN RIFT-RELATED TENSIONAL BASINS

Li Desheng   

  1. Scientific Research Institute of Petroleum Exploration and Development
  • Received:1984-10-31 Online:1985-12-25 Published:2012-01-16

摘要:

倾斜断块指产状呈单面山的断块结构。潜山是一种古地貌特征。倾斜断块-潜山油藏属混合圈闭类型,分布在基岩不整合面以下,具有构造油气藏和地层油气藏的双重特征。

Abstract:

Recent ten years or more,a lot of tilted fault block-buried hill oil/gas traps have been discovered by means of geophysical exploration and drilling in the eastern China Meso-Cenozoic rift-related depression basins,the Viking Gra-ben of North Sea of Europe,the Red Sea Graben of Egypt,Sirte Basin of Libya,Gipslend Basin of Australia and the Baffen-Labrador Basin of Canada.High oil/gas yield was recovered from this new type of traps.They are more likely to develop into good exploration targets both at home and abroad.The mechanism of their occurrence can be explained as follows:1.The crust's tensional stress,resulting from the upswelling of the upper mantle,caused a series of tensional rift-subsidence basins,with heat releasedfrom the upper mantle and creating a rather high geotherm-pressure condi-tions.2.The block-faulting break-up of older platforms or basements formed a series of lineally distributed tilted fault block-buried hill structures.3.The rapid subsiding and infilling environments during the early rifting stage were in favorable conditions for maturation and transformation of sourcematerials.Second crop might occur again from the preserved disconformable ol-der source rocks during the later depression stage.4.Suffering from weathering and karstication for a long geological time,the uplift parts of the tilted fault blocks are often good for reservoir forma-tion.5.Combinations of multiple style of traps and multiple source-reservoir-cap assemblages of the rift-subsidence tensional basins could result in multiple-pay pools.