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用反射波强度斜率识别层序及沉积环境

Application of Reflection Strength Slope to Identification of Sequence and Sedimentary Environment

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【作者】 冯明友韩强蒲仁海

【Author】 FENG Ming-you1,HAN Qiang2,PU Ren-hai3(1.Northwest Branch,Research Institute of Petroleum Exploration and Development,PetroChina,Lanzhou,Gansu 730020,China; 2.Research Institute of Exploration and Development,Northwest Company,Sinopec,Urumqi,Xinjiang 830011,China;3.Department of Geology,Northwest University,Xi’an,Shaanxi 710069,China)

【机构】 中国石油石油勘探开发科学研究院西北分院中国石化西北石油局勘探开发研究院西北大学地质学系 兰州730020乌鲁木齐830011西安710069

【摘要】 基于岩心和测井综合分析,充分利用反射强度斜率对层序的敏感性,研究塔河地区下石炭统巴楚组底部砂泥岩段的沉积相。根据地震属性反射强度斜率横向变化图,通过沉积旋回对比,识别出涨潮三角洲、沿岸滨面砂、消舄湖、障壁岛等沉积环境,较以往利用地震属性划分沉积相的其他方法更贴近实际。

【Abstract】 Base on core and well log comprehensive analysis and the sensitivity of the slope of reflection strength of seismic attributes to depositional sequence,the sedimentary facies in sand-shale member of Bachu formation of Lower Carboniferous in Tahe oilfield of Tarim basin is studied,identifying flood tidal delta,coastal shoreface sand,lagoon and barrier island etc.from lateral variation map of reflection strength slope and sedimentary cycle correlation.The identified results are closer to real situations than those from utilizing the seismic attributes.

  • 【文献出处】 新疆石油地质 ,Xinjiang Petroleum Geology , 编辑部邮箱 ,2008年03期
  • 【分类号】P631.8
  • 【被引频次】7
  • 【下载频次】141
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