吉林大学学报(地球科学版) ›› 2025, Vol. 55 ›› Issue (1): 70-83.doi: 10.13278/j.cnki.jjuese.20230009

• 地质与资源 • 上一篇    下一篇

低勘探程度地区层序地层分析及沉积规律——以五墩凹陷侏罗系为例

殷文   

  1. 中国石油大学(北京)克拉玛依校区石油学院,新疆 克拉玛依 834000
  • 收稿日期:2023-01-18 出版日期:2025-01-26 发布日期:2025-02-07
  • 作者简介:殷文(1978—),男,教授,博士,主要从事油气储层预测及高精度层序解释方面的研究工作,E-mail:yinwen@cupk.edu.cn
  • 基金资助:
    国家自然科学基金项目(42004089);新疆维吾尔自治区自然科学基金项目(2020D01A141)

Sequence Stratigraphic Analysis and Sedimentary Law Research in Low Exploration Area: Take the Jurassic in Wudun Depression as an Example

Yin Wen   

  1. Petroleum Institute, China University of Petroleum-Beijing at Karamay, Karamay  834000, Xinjiang, China
  • Received:2023-01-18 Online:2025-01-26 Published:2025-02-07
  • Supported by:
    the National Natural Science Foundation of China (42004089) and the Natural Science Foundation of Xinjiang Uygur Autonomous Region (2020D01A141)

摘要: 五墩凹陷属于低勘探程度地区,下侏罗统露头区油源条件较好,多口钻井油气显示良好,但盆地层序地层格架不明确,层序空间演化特征和沉积分布规律尚不清楚,制约了下一步的勘探部署。本文综合应用测井、地震、岩心、分析化验等资料,开展五墩凹陷中下侏罗统层序地层划分和区域层序地层格架研究。首先,采用测井频谱属性趋势分析、时频分析、地球化学分析等多种方法划分层序,共划分了6个三级层序,28个四级层序。然后,利用匹配子波分解和重构方法提高地震资料分辨率,采用地震多属性降维融合技术和井震联合多尺度匹配技术进行层序分析,建立了该区侏罗系层序地层格架。之后,将测井层序划分结果与地震多属性融合分析结果进行交叉验证,明确层序空间演化特征。最后,在高精度层序分析的基础上,在构造精细解释及沉积古地貌的约束下,利用不同级次层序解释成果,落实关键层位的沉积相带展布特征,形成了一套针对低勘探程度地区区域层序地层格架建立和沉积规律研究的思路和方法。

关键词: 低勘探程度地区, 频谱属性分析, 多尺度匹配对比, 层序地层格架, 沉积规律

Abstract: The Wudun depression belongs to an area with a low degree of exploration. The oil source conditions in the Lower Jurassic outcrop area are good, and the oil and gas show well in many wells drilled. However, the sequence stratigraphic framework of the basin, the sequence spatial evolution characteristics and sedimentary distribution rules are not clear, which restricts the later exploration deployment, which restricts the next exploration deployment. The research on the sequence stratigraphic division and regional sequence stratigraphic framework of  Middle and Lower Jurassic in Wudun depression is carried out by comprehensively applying the data of logging, seismic, core, and analysis data. At first, the spectrum-attribute-trend analysis of logging, time-frequency analysis, geochemical analysis and other methods are used to divide the sequence, and six third-order sequences and 28 fourth-order sequences are divided. Then, the matching wavelet decomposition and reconstruction method is used to improve the resolution of seismic data, and the seismic multi-attribute dimensionality reduction fusion technology and multi-scale matching with well-seismic joint are used for sequence analysis, and then the Jurassic sequence stratigraphic framework is established in this area. At the same time, the logging sequence division results and seismic multi-attribute fusion analysis results are cross-verified to clarify the spatial evolution characteristics of the sequence. At the same time, the logging sequence division results and seismic multi-attribute fusion analysis results are cross-verified to clarify the spatial evolution characteristics of the sequence. On the basis of high-precision sequence analysis, under the constraints of fine structural interpretation and sedimentary palaeogeomorphology, the distribution characteristics of sedimentary facies belts at key horizons are finally determined by using the results of sequence interpretation at different levels. A set of ideas and methods for the establishment of regional high-precision sequence stratigraphic framework and the study of sedimentary laws in areas of low exploration degree have been formed.

Key words: low exploration area, spectrum attribute analysis, multi-scale matching comparison, sequence stratigraphic framework, sedimentary law

中图分类号: 

  • TE13
[1] 陈贤良, 纪友亮, 杨克明. 川西坳陷中段须四段层序地层格架内沉积特征[J]. 吉林大学学报(地球科学版), 2020, 50(6): 1615-1627.
[2] 蔡来星, 卢双舫, 李昂, 石蕾, 刘爽. 松辽盆地肇州区块沙河子组层序格架特征及其对沉积和烃源岩的控制作用[J]. 吉林大学学报(地球科学版), 2015, 45(3): 724-735.
[3] 赵灿, 李旭兵, 郇金来, 陈孝红, 刘安, 危凯, 张华. 雪峰山西侧地区中上寒武统——层序地层学特征及层序格架[J]. 吉林大学学报(地球科学版), 2015, 45(2): 518-532.
Viewed
Full text


Abstract

Cited

  Shared   
  Discussed   
[1] 程立人,张予杰,张以春. 西藏申扎地区奥陶纪鹦鹉螺化石[J]. J4, 2005, 35(03): 273 -0282 .
[2] 李 秉 成. 陕西富平全新世古气候的初步研究[J]. J4, 2005, 35(03): 291 -0295 .
[3] 和钟铧,杨德明,王天武,郑常青. 冈底斯带巴嘎区二云母花岗岩SHRIMP锆石U-Pb定年[J]. J4, 2005, 35(03): 302 -0307 .
[4] 陈 力,佴 磊,王秀范,李 金. 绥中某电力设备站场区地震危险性分析[J]. J4, 2005, 35(05): 641 -645 .
[5] 纪宏金,孙丰月,陈满,胡大千,时艳香,潘向清. 胶东地区裸露含金构造的地球化学评价[J]. J4, 2005, 35(03): 308 -0312 .
[6] 初凤友,孙国胜,李晓敏,马维林,赵宏樵. 中太平洋海山富钴结壳生长习性及控制因素[J]. J4, 2005, 35(03): 320 -0325 .
[7] 李斌,孟自芳,李相博,卢红选,郑民. 泌阳凹陷下第三系构造特征与沉积体系[J]. J4, 2005, 35(03): 332 -0339 .
[8] 李涛, 吴胜军,蔡述明,薛怀平,YASUNORI Nakayama. 涨渡湖通江前后调蓄能力模拟分析[J]. J4, 2005, 35(03): 351 -0355 .
[9] 旷理雄,郭建华,梅廉夫,童小兰,杨丽. 从油气勘探的角度论博格达山的隆升[J]. J4, 2005, 35(03): 346 -0350 .
[10] 章光新,邓伟,何岩,RAMSIS Salama. 水文响应单元法在盐渍化风险评价中的应用[J]. J4, 2005, 35(03): 356 -0360 .