石油学报 ›› 1987, Vol. 8 ›› Issue (2): 33-38.DOI: 10.7623/syxb198702006

• 地质勘探 • 上一篇    下一篇

淮噶尔盆地石炭系墓岩风化壳油藏

雍天寿   

  1. 新疆石油管理局
  • 收稿日期:1985-05-31 出版日期:1987-04-25 发布日期:2013-07-08

CARHONIFEROUS OIL POOL OF BASEMENT WEATHERED CRUST IN JUNGGAR BASIN

Yong Tianshou   

  • Received:1985-05-31 Online:1987-04-25 Published:2013-07-08

摘要: 准噶尔盆地石炭系基岩风化壳包括了不整合面以下500m.风化壳即有盖层——A带,又有储油层——B带和C带,并处于两个生油层系之间,有适合的圈闭就能形成油气藏.石炭系油藏是基岩风化壳油藏、储层性质是孔隙一裂缝型,即风化壳B带是高产油层.编制构造图,古地形图、风化壳厚度和岩性一古地质图等,在准噶尔盆地克一乌油区寻找这类油藏,其它还有陆梁地区、克拉关丽地区和莫索湾隆起区等.

Abstract: The carboniferous basement wethered crust in Junggar Basin extends to 500m below uncoxzforzuity.The existence of cover zone-A and reservoir-zone B and zone C in the weathered crust,and its location between two source laeds give rise to oil pools izx case of suitable trapping.The earbcanifexous oil pool is one of basement weathered crust with porosity-fissure type reservoir having a high production layer in zaneB.The exploration znethads consist of modern structure palaeotopography,weathered crust thickness and lithology-palaeogeologic znapping,etc.Karaznay-Yrheregion is one of the favorable areas for explcyration of such oil pools in Junggar Basin.