Recognition of Milankovitch cycles in the stratigraphic record: application of the CWT and the FFT to well-log data

Ji-feng YU , Feng-gui SUI , Zeng-xue LI , Hua LIU , Yu-lin WANG
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引用次数: 12

Abstract

The authors applied a the combination of Continuous Wavelet Transform (CWT) and Fast Fourier Transform (FFT) methods to gamma ray well-log data from the Q3, G1 and D2 wells. This high-resolution stratigraphic study was based on Milankovitch's orbital cycle theory. It was found that the CWT scale factors, ‘a,’ of 12, 24 and 60 match the ratios of the periodicities of precession, obliquity and eccentricity very well. Nine intervals of the Permo-carboniferous strata were recognized to have Milankovitch cycles in them. For example, section A of well Q3 has 29 precession cycles, 15 obliquity cycles and 7 short eccentricity cycles. The wavelengths are 2.7, 4.4 and 7.8 m for precession, obliquity and eccentricity, respectively. Important geological parameters such as the stratigraphic completeness and the accumulation rate were also estimated. These results provide basic information for further cyclostratigraphic correlation studies in the area. They are of great significance for the study of ancient and future climate change.

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地层记录中米兰科维奇旋回的识别:CWT和FFT在测井资料中的应用
作者将连续小波变换(CWT)和快速傅立叶变换(FFT)相结合的方法应用于Q3、G1和D2井的伽马测井数据。这项高分辨率地层学研究是基于米兰科维奇的轨道循环理论。结果表明,CWT尺度因子“a”分别为12、24和60,与旋进周期、倾角周期和偏心率周期的比值吻合较好。在二叠-石炭系地层中发现有9个层段存在米兰科维奇旋回。例如,Q3井A段有29个进动旋回、15个倾角旋回和7个短偏心旋回。岁差、倾角和偏心率的波长分别为2.7、4.4和7.8 m。并对地层完整性、成藏速率等重要地质参数进行了估算。这些结果为该区进一步进行旋回地层对比研究提供了基础资料。它们对研究古代和未来的气候变化具有重要意义。
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