石油学报 ›› 2006, Vol. 27 ›› Issue (6): 34-38.DOI: 10.7623/syxb200606007

• 地质勘探 • 上一篇    下一篇

准噶尔盆地腹部白垩系/侏罗系不整合地层剥蚀厚度的恢复方法

李平平1, 邹华耀1, 郝芳1,2, 田建锋2, 佟殿君2   

  1. 1. 中国石油大学油气成藏机理教育部重点实验室 北京 102249;
    2. 中国地质大学资源学院 湖北武汉 430074
  • 收稿日期:2006-06-30 修回日期:2006-09-15 出版日期:2006-11-25 发布日期:2010-05-21
  • 作者简介:李平平,男,1980年6月生,2006年获中国地质大学(武汉)硕士学位,现为中国石油大学(北京)在读博士研究生,主要研究方向为油气成藏机理.E-mail:pingp_li@163.com
  • 基金资助:
    教育部科学技术研究重大项目(10419)资助

Restoration of eroded strata thickness in Cretaceous/Jurassic unconformity in hinterland of Junggar Basin

Li Pingping1, Zou Huayao1, Hao Fang1,2, Tian Jianfeng2, Tong Dianjun2   

  1. 1. Key laboratory of the Ministry of Education for the Machanism of Petroleum Accumulation, China University of Petroleum, Beijing 102249, China;
    2. Faculty of Resources, China University of Geosciences, Wuhan 430074, China
  • Received:2006-06-30 Revised:2006-09-15 Online:2006-11-25 Published:2010-05-21

摘要: 以准噶尔盆地腹部发育于侏罗系顶部和白垩系底部之间的不整合(K/J不整合)为研究对象,基于相同的沉积构造背景下相邻三级层序的地层厚度展布具有相似的趋势,提出了可用于恢复地层剥蚀厚度的参考层序厚度比值法。该方法的具体工作流程为:①在地震剖面上进行三级层序划分,经时-深转换得到各三级层序的地层厚度展布;②选择剥蚀面下未被剥蚀、层序厚度变化范围小的一个或者多个三级层序作为参考层序;③利用单井的地层剥蚀厚度恢复结果,拟合发生剥蚀前的参考层序厚度与参考层序至沉积面的地层厚度(包括参考层的厚度)比值的分布,即拟合剥蚀前的原始沉积面;④用该沉积面深度减去现今的剥蚀面深度就得到地层剥蚀厚度,并根据实际的地质模型对剥蚀厚度进行校正。研究结果表明,研究区西段剥蚀厚度为300~800m,东段剥蚀厚度在300m以下。该剥蚀厚度恢复方法适用于恢复范围大、钻井数量少和研究程度低的地区的剥蚀厚度。

关键词: 准噶尔盆地, 不整合, 剥蚀厚度, 参考层序厚度, 恢复方法

Abstract: A new method for restoration of eroded strata thickness by ratios of reference sequence strata thickness(RRSST)was proposed and used to restore the thickness of eroded strata in the Cretaceous/Jurassic(K/J)unconformity in the hinterland of Junggar Basin. The new method is based upon the similarity distribution of sequences strata thickness under similar tectonic and depositional environment. The restoration steps are as follows. First, the sequence boundaries were plotted on the seismic sections, and the thickness of single sequence was got out according to time-depth conversion. Second, the single sequence or multiple sequences underlying the K/J unconformity with no erosion and small variation range of sequences strata thickness were taken as reference sequences. Third, the distribution of RRSST when erosion just began to happen was modeled using eroded strata thickness and thickness of sequence strata in single well. Last, the eroded strata thickness was worked out using the modeled RRSST, the strata thickness of the reference sequences and the strata thickness from the bottom of the reference sequences to the eroded surface at present. Calibration of restored eroded strata thickness could be made according to geological model. The restoration shows that the eroded strata thickness is from 300 meters to 800 meters in the west part of Junggar Basin and below 300 meters in the east part of the basin. The method can be widely used in large area with few wells and low level of recognitions.

Key words: Junggar Basin, unconformity, eroded strata thickness, strata thickness of reference sequence, restoration method

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