盆地波动分析中的数学模型及计算机实现
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NUMERICAL MODEL AND ITS COMPUTERIZATION FOR WAVE ANALYSIS IN BASIN STUDY
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    摘要:

    波动分析的内容包括时间尺度的波动分析和空间尺度的波动分析两个方面。 时间尺度波动分析是通过恢复不同地质时期沉积速度入手,建立沉积速度直方图,对沉积速 度直方图进行三次样条插值、付利叶变换及滑动平均等数学方法处理,可以分解出不同级别 的周期波来;空间尺度的波动分析是从构造形迹的研究入手,选择波束方向、个数,量取波 的波长、振幅,通过计算机模拟构造形态。本文详细介绍了这两者的数学模型及其计算机实 现过程,并探讨了该模型的应用前景及其存在的问题

    Abstract:

    Wave analysis includes two aspects, one is the time scale analysis and the other is the space scale analysis. Time scale wave study begins with the restoration of the sedimentary rates for different geological times, and then a histogram of sediment ary rates is established. Moreover, cycle wave in different scales can b e figured out by some special numerical processing on the histogram e.g. thr eetimes sample plate insert, Fourier regression and sliding average . The space scale wave analysis begin with the study of structural beatures, and th e shape of the structure can be simulated by means of selection of the directio n and nu mbers of the wave beams and measurement of the wavelength and amplitude. Meanwhi l e, this paper introduces the detailed numerical model and computerized process f or both the time cale wave analysis and the space scale wave analysis. Moreover, the prospects of applications of the numerical model of the wave analysis and remaining problems are discussed.

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李京昌,金之钧,孙强.1996.盆地波动分析中的数学模型及计算机实现[J].地质论评,42(sup):276-282,[DOI].
Lihang, Jinjun, Sun Qiang.1996. NUMERICAL MODEL AND ITS COMPUTERIZATION FOR WAVE ANALYSIS IN BASIN STUDY[J]. Geological Review,42(sup):276-282.

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