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作 者:侯中健[1] 陈洪德[1] 田景春[1] 刘文均[1] 李君文[1]
机构地区:[1]成都理工大学沉积地质研究所"油气藏地质及开发工程"国家重点实验室,成都610059
出 处:《成都理工大学学报(自然科学版)》2004年第1期46-52,共7页Journal of Chengdu University of Technology: Science & Technology Edition
摘 要:通过钻井岩芯观察,结合测井资料和地震解释成果,按基准面旋回原理,把鄂尔多斯盆地石盒子组第8段划分为一个超长旋回层序、两个长期、四个中期和若干短期基准面旋回层序,并深入分析了形成中期、短期层序结构类型(A,C型)的背景、层序结构特征及其与储集砂体的展布关系。研究表明:不同的层序结构类型的形成受控于沉积背景、构造活动等所决定的可容纳空间和A/S值的变化。为进一步研究盒8段乃至整个石盒子组高分辨率层序地层学特征奠定了基础。Based on the comprehensive research of rock cores, well loggings and seismic data and according to the principles of base-level cycle, one super-long-term, two long-term, four middle-term and several short-term cycles sequence are distinguished in Member 8 of Shihezi Formation in the Sulige gas field of Ordos Basin. The sedimentary environment, tectonic setting, sequence staking patterns (Type A and C) in the long-term and short-term base-level cycles are discussed. Then, the characteristics of sequences structure and the relationships between that and the distribution of resevoir sand body are also studied in the paper. All the resaerch results show that every change from ratio of accomodation space to sedimentary supply (A/S) which controlled by sedimentary setting and tectonic aotivity leads to each type of sequence structure. And the conclusion gives the basis of a further study on the high-resolution sequence (stratigraphy) for the all and the one in the Shihezi Formation.
关 键 词:高分辨率层序地层 层序结构特征 基准面旋回结构 A/S 石盒子组 苏里格气田 鄂尔多斯盆地
分 类 号:TE121.34[石油与天然气工程—油气勘探]
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