新疆石油地质 ›› 1993, Vol. 14 ›› Issue (4): 385-389.

• 综述 • 上一篇    下一篇

滚动背斜形成机理探讨

祁大晨   

  1. 高级工程师 新疆石油管理局勘探开发研究院 克拉玛依 834000
  • 收稿日期:1992-11-13 发布日期:2020-12-08

INQURY INTO TH PRAION MCHNEN oF ROLIOER ANTCLINES

Qi Dasheng   

  1. Semor Engineer. Research Iutute of Erploratron ard INer enpmet Xin, iang Petrueum AImustratuor Breau. haramay 8340001
  • Received:1992-11-13 Published:2020-12-08

摘要: 滚动背针是两期钩造运动的产物: 第一期. 在区域张应力作用下形成正断层; 第二期.在区域性压应力作用下形成滚动背针。动背针的形成和展布受同期同生断层的撞制。滚动背针常位于这些同生断裂的下降盘.呈串珠状分布。这些同生断层早期可作为油气运移的通道.而后期又被改造为封闭性压性结构面.利于油气的保存. 因而使滚动背针成为良好的油气圈闭。

关键词: 滚动背斜, 同生断层, 张应力, 压应力, 油气圈闭

Abstract: Rollover anticlines were the products of two tectoge nesises:the first was the formation of normal faults under the regional tensile stress. the second was the formation of the rollovet anticiines under the regional compressive stress. The fotmation and distribution of the rollover anticlines were controlled by the synchtonous growth faults. The rollover anticlines were generally located in the downthrow walls of the growth faults and distributed like beads. The growth faults in their eatly stage could act as migration paths for oil and gas. Tn the late stage. the growth faults were reformed into sealed compressive structural planes and were favourable to the preservation of oil and gas. Therefore. the rollover anticlines could become advantageous traps for oil and gas.

Key words: Rollover anticline, Gtowth fault, Tensile stress, Compressive stress, Trap for oil and gas