Cyclostratigraphy Research on the Hanjiang-Wanshan Formations in Zhuyi Depression, Pearl River Mouth Basin
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摘要: 对珠江口盆地珠一坳陷惠州凹陷北部HZ0811井和惠陆低凸起HZ1811井中中新世-上新世的韩江组、粤海组和万山组自然伽马测井曲线进行频谱分析和小波分析, 识别出显著的米兰柯维奇沉积旋回.通过对短偏心率旋回进行高斯带通滤波, 建立了HZ0811井和HZ1811井的"浮动"天文年代标尺.两口井的万山组、粤海组和韩江组分别记录了35个、56个和64个短偏心率旋回, 据此估计出万山组沉积时限约为3.5 Ma, 粤海组沉积时限约为5.6 Ma, 韩江组沉积时限约为6.4 Ma.根据天文年代标尺计算出HZ0811井和HZ1811井韩江组-万山组的沉积速率, 结果表明沉积速率变化显示出明显的1.0 Ma和0.4 Ma的旋回性, 可能与长偏心率周期(1.0 Ma和0.4 Ma)控制的海平面变化有关.Abstract: Spectral analysis and continuous wavelet analysis were conducted on the natural gamma ray logging data from the Middle Miocene-Pliocene Hanjiang, Yuehai and Wanshan formations of well HZ0811 and HZ1811, which locate at northern Huizhou depression and Huilu low uplift at Zhuyi depression, respectively. Significant Milankovitch sedimentary cycles were identified, and "floating" astronomical time scales of well HZ0811 and HZ1811 were established through Gaussian band filtering of short eccentricity signals. The Wanshan, Yuehai and Hanjiang formations record 35, 56 and 64 short eccentricity cycles, which indicate the duration of Wanshan, Yuehai and Hanjiang formations can be estimated as 3.5, 5.6 and 6.4 Ma, respectively. The sedimentary rate of Hanjiang-Wanshan formations of well HZ0811 and HZ1811 were calculated according to floating astronomical time scale. The variations of sedimentary rate indicate significant 1.0 Ma and 0.4 Ma cyclicities, which may be related to the sea level change controlled by long eccentricity cycles.
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图 1 珠江口盆地惠州凹陷和惠陆低凸起构造位置示意
Fig. 1. Simplified structure position of Huizhou depression and Huilu low salient, Pearl River Mouth basin
图 3 HZ0811井岩性剖面、“浮动”天文年代标尺及沉积速率综合
Fig. 3. Synthesize column of lithology, floating astronomical time scale and sedimentary rate of well HZ0811
图 4 HZ1811井岩性剖面、“浮动”天文年代标尺及沉积速率综合
Fig. 4. Synthesize column of lithology, floating astronomical time scale and sedimentary rate of well HZ1811
图 5 HZ0811井小波变换及频谱分析
a.万山组自然伽马测井曲线小波分析图；b.粤海组自然伽马测井曲线小波分析图；c.韩江组自然伽马测井曲线小波分析图.小波图谱中蓝色代表波谱能量低，红色代表波谱能量高；d.万山组自然伽马测井曲线频谱分析图；e.粤海组自然伽马测井曲线频谱分析图；f.韩江组自然伽马测井曲线频谱分析图.图中蓝色实线代表使用多窗谱分析方法(MTM)进行分析结果，红色实线代表使用Redfit软件分析结果
Fig. 5. Wavelet scalogram and spectral analysis of HZ0811
图 6 HZ1811井小波变换及频谱分析
a.万山组自然伽马测井曲线小波分析图；b.粤海组自然伽马测井曲线小波分析图；c.韩江组自然伽马测井曲线小波分析图.小波图谱中蓝色代表波谱能量低，红色代表波谱能量高；d.万山组自然伽马测井曲线频谱分析图；e.粤海组自然伽马测井曲线频谱分析图；f.韩江组自然伽马测井曲线频谱分析图.图中蓝色实线代表使用多窗谱分析方法(MTM)进行分析结果，红色实线代表使用Redfit软件分析结果
Fig. 6. Wavelet scalogram and spectral analysis of HZ1811
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