岩性油气藏 ›› 2023, Vol. 35 ›› Issue (2): 113–124.doi: 10.12108/yxyqc.20230211

• 地质勘探 • 上一篇    下一篇

川东地区寒武系高台组白云岩-蒸发岩共生地层高频层序划分及地质意义

胡忠贵1,2, 王纪煊1,2, 李世临3, 郭艳波3, 左云安3, 庞宇来3   

  1. 1. 长江大学 地球科学学院, 武汉 430100;
    2. 长江大学 沉积盆地研究中心, 武汉 430100;
    3. 中国石油西南油气田公司 重庆气矿, 重庆 402160
  • 收稿日期:2022-07-05 修回日期:2022-08-04 出版日期:2023-03-01 发布日期:2023-03-07
  • 第一作者:胡忠贵(1979-),男,博士,教授,主要从事层序地层学及储层沉积学方面的教学和研究工作。地址:(430000)湖北省武汉市蔡甸区蔡甸街大学路111号。Email:hzg1978@yangtzeu.edu.cn。
  • 通信作者: 王纪煊(1996-)男,长江大学在读硕士研究生,研究方向为碳酸盐岩沉积学及储层地质学。Email:1079299440@qq.com。
  • 基金资助:
    “十三五”国家科技重大专项“重点海相层系沉积相研究”（编号：2016ZX05007002）资助。

High-frequency sequence division and geological significance of dolomiteevaporite paragenetic strata of Cambrian Gaotai Formation in eastern Sichuan Basin

HU Zhonggui1,2, WANG Jixuan1,2, LI Shilin3, GUO Yanbo3, ZUO Yun'an3, PANG Yulai3   

  1. 1. School of Geosciences, Yangtze University, Wuhan 430100, China;
    2. Sedimentary Basin Research Center, Yangtze University, Wuhan 430100, China;
    3. Chongqing Gas Mine, PetroChina Southwest Oil and Gas Field Company, Chongqing 402160, China
  • Received:2022-07-05 Revised:2022-08-04 Online:2023-03-01 Published:2023-03-07

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摘要： 白云岩-蒸发岩共生地层中油气资源丰富。基于层序地层学原理，结合钻井、薄片等资料，在三级层序划分的基础上，采用INPEFA和小波变换技术对川东地区寒武系高台组白云岩-蒸发岩共生地层的高频层序进行识别与划分，并探讨了其地质意义。研究结果表明： ①川东地区寒武系高台组白云岩-蒸发岩共生地层可划分为3个三级层序，自下而上分别为Sq1，Sq2，Sq3，可进一步划分为6个四级层序（ssq1—ssq6）。高台组主要为碳酸盐岩台地沉积环境，自西向东依次发育混积台地、局限-蒸发台地、开阔台地相沉积。②研究区高台组的岩性组合序列包括白云岩上覆厚层蒸发岩（A）、厚层白云岩夹蒸发岩（B）、白云岩与蒸发岩互层（C）和蒸发岩上覆厚层白云岩（D）等4种类型。白云岩-蒸发岩共生地层发育在四级层序的接触界面，且多发育于层序内部的高位体系域，反映了海平面较强烈的扰动，尤其是海平面的相对下降有利于白云岩和蒸发岩沉积。③研究区高台组白云岩-蒸发岩共生地层的岩性组合序列在GRinpefa曲线和小波变换曲线上均具有响应特征，对应的64尺度小波系数曲线波动平缓，能量团为弱黄蓝色，GRinpefa曲线以“缺口”的形式表现出蒸发岩与白云岩的岩性差异。

关键词: 白云岩-蒸发岩共生, 最大熵谱分析, 小波变换, 高频层序划分, 高台组, 寒武系, 川东地区

Abstract: The dolomite-evaporite paragenetic strata are rich in oil and gas resources. Based on the principle of sequence stratigraphy, combined with drilling and thin section data, and on the basis of third-order sequence division, INPEFA and wavelet transform technologies were used to identify and divide the high-frequency sequences of dolomite-evaporite paragenetic strata of Cambrian Gaotai Formation in eastern Sichuan Basin. The results show that:(1) The dolomite-evaporite paragenetic strata of Cambrian Gaotai Formation in eastern Sichuan Basin can be divided into three third-order sequences which are respectively Sq1, Sq2 and Sq3 from bottom to top, and can be further divided into six fourth-order sequences(ssq1-ssq6). The Gaotai Formation is mainly in a carbonate platform sedimentary environment, with mixed tidal flats, confined-evaporative platforms and open platform facies deposits developed in turn from west to east.(2) There are four types of intergrowth rock assemblages of Cambrian Gaotai Formation in the study area, including:thick-layered evaporite overlying dolomite, thick-layered dolomite interbedded with evaporite, interbedded dolomite and evaporite, and thick-layered dolomite overlying evaporite. The dolomite-evaporite paragenetic strata are developed at the contact interface of the fourth-order sequence, and are mostly developed in the highstand systems tract inside the sequence, reflecting a strong disturbance of sea level, especially the relative decline of sea level, which is conducive to the deposition of dolomite and evaporite. (3) The rock assemblage sequence of the dolomite-evaporite paragenetic strata of Gaotai Formation can generate response characteristics on the GRinpefa and wavelet transform curves. The corresponding 64-scale wavelet coefficient curve fluctuates smoothly, and the energy clusters are weak yellow-blue. The GRinpefa curve shows lithological difference between evaporite and dolomite in the form of "notch".

Key words: dolomite-evaporite paragenesis, maximum entropy spectral analysis, wavelet transform, high-frequency sequence division, Gaotai Formation, Cambrian, eastern Sichuan Basin

中图分类号: 

  • TE121.3+4
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