供稿: 陈俊亮;吴亮;崔建军 | 时间: 2019-05-31 | 次数: |
作者单位:中国石化华北分公司勘探开发研究院;中国石化华北分公司监理中心
摘要:大牛地气田位于鄂尔多斯盆地伊陕斜坡北部,大牛地气田主要目的层段为上古生界石炭系太原组、二叠系山西组与下石盒子组,经历了海相—海陆过渡相—陆相的沉积过程.通过对气田内50余口井的岩心观察并结合化验分析资料,认为太原组为具障壁砂坝的滨浅海相沉积,山西组为三角洲相沉积,下石盒子组为河流相沉积.在沉积相研究划分的基础之上,对其沉积微相特征进行了描述.
分类号:P618.13
The sedimentography characteristics of Daniudi gas field
Abstract:Daniudi gas field lies in the the norhthern part of Yishan slope of Ordos basin, its main purpose intervals includes: Taiyuan team. CARBONIFEROUS. Late PALEOZOIC, Shanxi team. PERMIAN, late Shihezi. PERMIAN, these intervals went through the sedimentary process of marine facies—the transition of marine and contimental facies—contimental facies. Taiyuan team is considered as the littoralnertic facies deposit (with some barriers bar facies deposit) , Shanxi team is considered as delta facies deposit, late Shihezi team is considered as fluvial facies deposit through the observation of the core of more than 50 wells and the analyse of the core data. The characteristics of the microsedimentography on the basis of the research on the sedimentography is described.