四川盆地中北部寒武系咸安组层序地层及沉积演化

Zhuangzhuang Bai, Shuyuan Shi, Wei Yang, Wuren Xie, Shiyu Ma, Saijun Wu, Wenzheng Li, Wenliang Shang
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引用次数: 0

摘要

四川盆地寒武系咸安东组碳酸盐岩高频旋回与颗粒滩发育普遍存在一定的耦合关系;这影响了储层预测的准确性和油气有利区带的选择。利用基于matlab的小波变换技术,分析了咸安洞组高频层序特征,建立了层序地层格架,明确了其与颗粒滩发育的垂、水平关系。结果表明,利用Dmey小波对伽马射线(GR)曲线进行连续小波变换能有效反映区域沉积旋回。在仙安洞组中,我们发现了2个3阶序列、5个4阶序列和10个5阶序列,它们都与小波变换得到的一维小波曲线具有较强的相关性。在层序地层格架中,仙安洞组早期沉积短暂地继承了琼竹寺组的海侵作用,随后经历了一个漫长而频繁波动的退退期。阐明了海相退退时期颗粒滩的发育特征,确定了主要岩性为鲕粒灰岩、鲕粒白云岩、白云灰岩、粉砂质鲕粒灰岩和粉砂质鲕粒白云岩。纵向上,颗粒滩主要分布在SQ12、SQ21和SQ22段,具有薄层与厚层互层发育的特点。它们主要形成于四阶序列的回归阶段。平面上,它们在西南-东北方向呈带状分布。这些发现为利用测井资料进行高频层序地层学研究提供了新的见解。对构建高精度层序地层格架以及预测研究区内颗粒滩的分布具有实际意义。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

Sequence stratigraphic and sedimentary evolution of the Cambrian Xiannüdong Formation in the north central Sichuan Basin, SW China

Sequence stratigraphic and sedimentary evolution of the Cambrian Xiannüdong Formation in the north central Sichuan Basin, SW China
The high-frequency cycles seen in the carbonates of the Cambrian Xiannüdong Formation in the Sichuan Basin commonly exhibit a certain coupling relationship with the development of grain shoals; this influences the accuracy of reservoir predictions and the selection of favorable zones for hydrocarbon. MATLAB-based wavelet transform technology is employed to analyze the characteristics of the high-frequency sequences in the Xiannüdong Formation, establish a sequence stratigraphic framework, and clarify their vertical and horizontal relationships with the development of grain shoals. The results indicate that using the Dmey wavelet for continuous wavelet transform of gamma ray (GR) curves effectively reflects regional sedimentary cycles. In the Xiannüdong Formation, we identified two third-order sequences, five fourth-order sequences, and ten fifth-order sequences, all of which exhibit a strong correlation with the one-dimensional wavelet curves derived from wavelet transformations. In the sequence stratigraphic framework, early deposition of the Xiannüdong Formation briefly inherited transgressive processes from the Qiongzhusi Formation, and subsequently underwent a long and frequently fluctuating regressive phase. This study elucidates the development characteristics of grain shoals during marine regressions, and identifies lithology primarily as oolitic limestone, oolitic dolostone, doloarenite, silty oolitic limestone, and silty oolitic dolostone. Longitudinally, grain shoals are primarily distributed in the SQ12, SQ21, and SQ22 intervals, and are characterized by the interbedded development of thin and thick layers. They form predominantly during the regressive phase of fourth-order sequences. Planarly, they exhibit a belt-like distribution in the southwest–northeast direction. These findings provide novel insights for conducting high-frequency sequence stratigraphy studies utilizing logging data. They also possess practical implications for constructing high-precision sequence stratigraphic frameworks as well as for predicting the distribution of grain shoals within the study area.
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