沉积盆地物理分析——波动分析

PHYSICAL ANALYSIS METHoD FoR SEDIMENTARY BASIN——WAVE ANALYSIS
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  • 石油大学,北京    
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  • 西西伯利亚油气资源评价与招标政策研 究中心,俄罗斯秋明    
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  • University of Petroleum,Beijing    
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  • western Siberian Research Center for Resource Evaluation and BMdmg Policy,Tyuming    
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    摘要:

    本文试图应用波动原理及波动方程来定量描述沉积盆地的发展与演化过 程。按照反演的思路,首先根据实际钻井和测井资料可以恢复各地质时期的古 沉积速率。这是一条随地质年代变化的不规则曲线。应用滑动窗口方法可将该 曲线逐步分解出一些有规律的周期波,并可以计算它们的周期、振幅,从而建立 描述沉积速率曲线的波动方程。应用该方程可以预测深部及周围无资料地区的 沉积、剥蚀过程,计算剥蚀量和定量地恢复盆地的形成演化史。文中给出了该方 法在西西伯利亚的应用实例。

    Abstract:

    In this paper,the authors describe the evolution process of sedimentary basins quantitatively by the wave principle and wave equation.Based on the deducing approach,the primary deposition rate can be restored revived from the drilling and well logging data.The resuIt obtained is an om— regular curve which changes with the geological age. By means of the sliding—window,a series of cyclic wave cures can be decomposed step by step,and the cycle and amplitude can be calculated; then the wave equations describing the deposition rate can be set up.From these equations the deposition and erosion processes of the deeper part or its vicinity,where strata data are un— known,can be predicted,and the erosion thickness can be calculated and the evolutionary history of the basin can be restored in detail.A case study on western Siberia is given in this paper.

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金之钧,张一伟,刘国臣,李京昌,r.n缅斯尼科娃,B.H.施比伊曼.1996.沉积盆地物理分析——波动分析[J].地质论评,42(sup):170-179,[DOI].
Jin Zhijun, zhang yiwei, Liu Guochen, Li Jingchang, Richard SindingLarsen, B. I. Shbilman.1996. PHYSICAL ANALYSIS METHoD FoR SEDIMENTARY BASIN——WAVE ANALYSIS[J]. Geological Review,42(sup):170-179.

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