藏北羌塘盆地二维反射地震新认识
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引用本文:李忠雄,邱海军,程明道,廖建河,王孝勋,王安志,王玲.2013.藏北羌塘盆地二维反射地震新认识[J].地球学报,34(4):477-484.
DOI:10.3975/cagsb.2013.04.11
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作者单位E-mail
李忠雄 中国地质调查局成都地质调查中心 lzhongxiong@163.com 
邱海军 中石化华北石油局地球物理勘探公司  
程明道 中石化华北石油局地球物理勘探公司  
廖建河 中石化西南石油局第二物探大队  
王孝勋 中石化西南石油局第二物探大队  
王安志 中石化西南石油局第二物探大队  
王玲 中石化西南石油局第二物探大队  
基金项目:中国地质调查局青藏矿产专项“羌塘盆地油气勘探目标优选与科探井井位预研究”(编号: 资[2008]青藏15-01);中国地质调查局青藏油气项目“羌塘盆地及其外围重点盆地油气远景调查”(编号: 资[2011]02-03-01);国家自然科学基金项目(编号: 40972087)
中文摘要:针对羌塘盆地复杂的地震地质条件, 从提高资料信噪比入手, 近几年在羌塘盆地开展了数百千米二维地震采集与处理技术试验, 初步总结出一套适合羌塘盆地地震采集与处理方法技术。试验结果证明: 单井(18 m以上井深)、16~20 kg炸药药量、50 m以下道距、120次以上覆盖次数、“X”型检波器组合图形为较好的激发接收参数。处理获得的地震叠加剖面反射信息丰富, 揭示出盆地古生界基底、三叠系、侏罗系中上部、侏罗系顶界各构造层以及断裂的空间展布特征, 为查明地层埋深、构造圈闭和构造界面等提供了高质量数据。另外, 穿过中央隆起带的地震剖面清楚显示该隆起带不是一个古老构造, 而是一个现今构造。
中文关键词:藏北  羌塘盆地  二维地震剖面  构造特征  中央隆起带
 
Characteristics of New Two-dimensional Seismic Reflection Profiles in Qiangtang Basin, Northern Tibet
Abstract:It is difficult to acquire high-quality seismic sections in Qiangtang basin because of its complex seismic geological condition and low signal-noise ratio. In order to find out suitable technique for this basin, the authors conducted tests along a seismic profile more than several hundred kilometers long on the basis of increasing signal-noise ratio. The results indicate that a single hole with the depth of at least 18 meters, 16~20 kilogram charge sizes, 20~40 meters trace group interval, more than 120 folds and “X” type geophone array map constitute the optimum shooting and receiving parameters suitable for the feature of Qiangtang basin. And the quality of 2D seismic profiles obtained by using these parameters and techniques can be increased greatly and is obviously superior to that of the profiles obtained in the past. The processed stacking profiles show informative reflection and reveal the features of spatial distribution of Palaeozoic basement, Triassic, middle-upper Jurassic, upper Jurassic strata and faults, thus providing high-quality data for ascertaining the layer thickness and the structural traps and boundaries. In addition, the processed stacking profile across the central uplifting belt clearly shows that this up-lifting belt is an anticline structure formed recently instead of an ancient dome.
keywords:northern Tibet  Qiangtang basin  2D seismic profile  structure characteristic  central uplifting belt
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