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青藏高原羌塘盆地基底结构与南北向变化——基于一条270km反射地震剖面的认识
Structure of basement and its N-S direction transformation in Qiangtang basin in Tibet:Discovered by a 270km seismic reflection profile
【摘要】 通过收集并重新处理已有的反射地震剖面,获得了一条南北向横贯羌塘盆地主体的270km长反射地震剖面。剖面显示:羌塘盆地可能具有元古代的基底并且南羌塘盆地较北羌塘盆地深。在南、北羌塘地壳浅部(约0~3s)变形差异较大,北羌塘褶皱变形强烈,呈现出隆凹变形相间的格局,南羌塘则相对较平缓。羌塘中央隆起之下为连贯的弧形反射,其北侧发育一个深度达8km的半地堑构造,规模较大,可为油气资源储存提供有利空间。
【Abstract】 By collecting and reprocessing current reflection seismic profiles,we get a 270km profile across the Qiangtang basin at S-N direction.Profile shows:there are probably Proterozoic basement in Qiangtang basin.The depth of the basement is changeable;it is deeper in South Qiangtang basin and shallower in North Qiangtang basin.Shallow crustal deformations(about 0~3s) are quite different between North Qiangtang and South Qiangtang.In North Qiangtang,there are strong fold deformations and alternating uplifts and depressions,and relatively flat in South Qiangtang.Continuous arc reflections were found beneath the central uplift of the Qiangtang terrane.There is an 8km-depth half graben on the north side where may be a benefit storage space for oil and gas resources.
【Key words】 Qiangtang basin; Basement structure; N-S transformation; Seismic reflection profile;
- 【文献出处】 岩石学报 ,Acta Petrologica Sinica , 编辑部邮箱 ,2011年11期
- 【分类号】P631.4;P618.13
- 【被引频次】18
- 【下载频次】519