李平平, 邹华耀, 郝芳, 田建锋, 佟殿君. 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[J]. 石油学报, 2006, 27(6): 34-38. DOI: 10.7623/syxb200606007
引用本文: 李平平, 邹华耀, 郝芳, 田建锋, 佟殿君. 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[J]. 石油学报, 2006, 27(6): 34-38. DOI: 10.7623/syxb200606007
Li Pingping, Zou Huayao, Hao Fang, Tian Jianfeng, Tong Dianjun. Restoration of eroded strata thickness in Cretaceous/Jurassic unconformity in hinterland of Junggar Basin[J]. Acta Petrolei Sinica, 2006, 27(6): 34-38. DOI: 10.7623/syxb200606007
Citation: Li Pingping, Zou Huayao, Hao Fang, Tian Jianfeng, Tong Dianjun. Restoration of eroded strata thickness in Cretaceous/Jurassic unconformity in hinterland of Junggar Basin[J]. Acta Petrolei Sinica, 2006, 27(6): 34-38. DOI: 10.7623/syxb200606007

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

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

  • 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。

     

    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.

     

/

返回文章
返回