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塔中岩溶储层地震反射地质特征及其成因机理

Geological Characteristics and Formation Mechanism of Karst Reservoir Seismic Reflection in Tazhong Area

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【作者】 郭军参王振宇屈海洲罗新生

【Author】 GUO Juncan1 WANG Zhenyu1 QU Haizhou1 Luo Xinsheng2(1.Southwest Petroleum University,Chengdu 610500;2.Research Institute of Exploration and Development,Tarim Oilfield Company,PetroChina,Korla 841000)

【机构】 西南石油大学中国石油塔里木油田分公司勘探开发研究院

【摘要】 综合地震反射强弱及反射形态的差异,将地震反射类型划分为串珠状反射、片状反射、杂乱反射和弱反射,并对串珠状反射和片状反射进行细分。总结塔中西部下奥陶统鹰山组地震反射特征与岩溶储层对应关系,在此基础上比较每种地震反射类型所对应地质特征的差异,归纳形成四种地震反射类型的地质原因。

【Abstract】 Combined with the seismic reflection strength and shapes,this article divides seismic reflection into four types,including the string beads reflection,the flaky reflection,the disorderly reflection and the weak reflection.And the string beads reflection and the flaky reflection are subdivided.Based on the summary of the corresponding relations between seismic profile and karst reservoir in Yingshan Formation of the Lower Ordovician in western Tazhong area,the corresponding geological characteristics of the every kind of seismic reflection types have been carefully analyzed.The geological causes of the four seismic reflection types are summed up from the differences of these geological characteristics.

【基金】 国家科技重大专项(2008ZX05004-004);四川省重点学科建设项目(SZD0414)
  • 【文献出处】 重庆科技学院学报(自然科学版) ,Journal of Chongqing University of Science and Technology(Natural Sciences Edition) , 编辑部邮箱 ,2012年02期
  • 【分类号】P618.13
  • 【被引频次】5
  • 【下载频次】134
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