新疆石油地质 ›› 2004, Vol. 25 ›› Issue (3): 280-282.

• 油气勘探 • 上一篇    下一篇

窟隆山逆掩推覆带速度建场及其特征

方晨, 孙万高, 唐光华, 杨克荣   

  1. 中国石油玉门油田分公司勘探开发研究院,甘肃玉门735200
  • 收稿日期:2004-01-15 发布日期:2020-09-18
  • 作者简介:方晨(1975-), 男,新疆奇台人,工程师,石油地质。联系电话:0937-3924003。

Velocity Field and Its Characteristics in Kulongshan Overthrust Nappe :

FANG Chen, SUN W an-gao, TANG Guang-hua, YANG Ke-rong   

  1. Research Institute of Exploration and Development, Yumen Oilfield Company, PetroChina, Y umen, Gansu 735200,China
  • Received:2004-01-15 Published:2020-09-18

摘要: 采用层位控制法,对区内 窟窿山、金海子两块三维探区进行了精细速度建场及成图,对地震速度在纵向、横向上的分布特征进行了初步探讨。分析结果表明,本区速度纵向上成层性较明显,在表层-浅层段及中-深层段存在速度倒转现象;推覆体速度在横向上呈清晰的块状特征;平面速度变化总体趋势由北向南逐渐增大,变化梯度北小南大;速度等值线大体呈北西向分布;两个三维探区均存在速度异常区。深浅层岩性、厚度以及压实程度的差异,是造成速度异常的基本原因。

关键词: 酒泉盆地, 青西油田, 速度分析, 地层, 岩石, 厚度, 压实作用

Abstract: By horizon-controlled method, the velocity fields of Kulongshan and Jinhaizi 3-D areas are mapped,the characteristics ofvertical and transversial distribution of velocity are discussed. The analyzed result shows that distinct velocity layering feature occurs invertical direction, and velocity reversion is found in near surface-shallow zone and mid-deep zone; the velocity of overthrust nappe is ofclear block feature in lateral direction; the variation of lateral velocity tends to grow ing from north to south, with gradient of north-low andsouth-high; the contour of velocity assumes distributing along the north-west direction roughly, and there are abnormal-velocity regionsfor these two 3-D areas. It is shown that differences in deep-shallow lithology, thickness and compaction degrees are the essential causesfor the velocity anomaly in these areas.

Key words: Jiuquan basin, Qingxi oilfield, velocity analysis, formation, rock, thickness, compaction

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