层序地层级次对生物碎屑灰岩 沉积演化的控制作用 ——以中东X油田Mishrif组中下段为例

作    者:余义常1,2,郭睿2,李峰峰2,林敏捷2,沈博珩2,沈毅3,韩海英2,宋世琦1
单    位:1 中国石油国际勘探开发有限公司;2 中国石油勘探开发研究院; 3 中国石油集团川庆钻探工程有限公司地质勘探开发研究院
基金项目:
摘    要:
以中东X油田Mishrif组中下段为例,综合利用地震、测井、岩心、铸体薄片及常规物性等资料,开展层序地 层级次识别及层序地层级次对沉积演化的控制作用研究。结果表明:①Mishrif组发育5个三级层序和10个四级层 序,中下段MB2—MC1层段对应三级层序SQ2—SQ3,包括4个四级层序,其内部发育11个五级层序和多个六级层 序。②研究区发育次盆地碳酸盐开阔台地-弱镶边台地沉积,储层主要发育于台内滩和台缘滩中,按照生物碎屑类 型可将滩相进一步细分为5种类型。③六级层序控制单滩体的沉积序列,五级层序控制多滩体的组合特征,四级层 序决定沉积微相演化特征,三级层序决定沉积体系的演化特征。④SQ2层序的PSS3、PSS4四级层序早期为斜坡环 境,发育透镜状滑塌粗粒沉积,后期发育台地边缘滩间→中能滩相沉积序列;SQ3层序的PSS5、PSS6四级层序发育台 地边缘滩间→中能滩相→高能滩相沉积序列。SQ3沉积结束后形成了特殊的下切谷充填沉积。
关键词:生物碎屑灰岩;层序地层级次;沉积演化;Mishrif组;中东

Controlling effects of sequence stratigraphic orders on sedimentary evolution of bioclastic limestone: a case study of middle-lower section of Mishrif Formation in the Middle East X Oilfield

Author's Name: YU Yichang1,2, GUO Rui2, LI Fengfeng2, LIN Minjie2, SHEN Boheng2, SHEN Yi3, HAN Haiying2, SONG Shiqi1
Institution: 
Abstract:
Based on the data of seismic, well logging, core, cast thin sections and conventional physical properties, taking the middle-lower section of Mishrif Formation in the Middle East X Oilfield as an example, the identification of sequence stratigraphic orders and the controlling effects of sequence stratigraphic orders on sedimentary evolution are studied. The results show that: (1) The Mishrif Formation is divided into 5 third-order sequences (SQ1-SQ5) and 10 fourth-order se⁃ quences (PSS1-PSS10). The MB2—MC1 single layers in the middle-lower section of Mishrif Formation correspond to SQ2-SQ3, including 4 fourth-order sequences (PSS3-PSS6), in which multiple fifth-order and sixth-order sequences are developed. (2) Carbonate open platform-weakly rimmed platform of a sub-basin is developed in the study area, and the reservoirs mainly exist in platform margin shoals and open platform shoals. The shoal facies can be further subdivided into rudist shoal, rudist-containing bioclastic shoal, bioclastic-arene shoal, bioclastic-spherical shoal and bioclastic shoal ac⁃ cording to bioclastic types. (3) The sixth-order sequence controls the sedimentary sequence of a single shoal body, the fifth-order controls the combination characteristics of multiple shoal bodies, the fourth-order sequence determines the evolution characteristics of sedimentary microfacies, and the third-order sequence determines the evolution characteristics of sedimentary systems. (4) In the early stage of PSS3 and PSS4 of SQ2 sequence, the two fourth-order sequences are in a platform front slope environment, with the development of lens-shaped collapsed coarse-grained sediments. In the later stage of PSS3 and PSS4, a sedimentary sequence of the platform margin intershoal → medium energy shoal is developed. The PSS5 and PSS6 of the SQ3 sequence develop a sedimentary sequence of platform margin intershoal → medium energy shoal → high energy shoal. After the completion of SQ3 sedimentation, a special incision filling sedimentation is formed.
Keywords: bioclastic limestone; orders of sequence stratigraphy; sedimentary evolution; Mishrif Formation; the Middle East
投稿时间: 2024-04-07  
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