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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

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【作者】 卢占武高锐李永铁李秋生王海燕匡朝阳酆少英熊小松

【Author】 LU ZhanWu1,2,GAO Rui1,2**,LI YongTie3,LI QiuSheng1,2,WANG HaiYan1,2,KUANG ChaoYang4,FENG ShaoYing5 and XIONG XiaoSong1,2 1.State Key Laboratory for Continental Tectonics and Dynamics,Institute of Geology,Chinese Academy of Geological Sciences,Beijing 100037,China 2.Earthprobe and Geodynamics Open Laboratory of CAGS,Beijing 100037,China 3.Exploration and Development Academy of CNPC,Beijing 100083,China 4.No.6 Geophysical Prospecting Team,East China Petroleum Bureau,SINOPEC,Nanjing 210007,China 5.Geophysical Exploration Centre of China Earthquake Administration,Zhengzhou 450002,China

【机构】 中国地质科学院地质研究所大陆构造与动力学国家重点实验室中国地质科学院深部探测与地球动力学重点开放实验室中国石油勘探开发研究院中国石化华东石油局第六物探大队中国地震局地球物理勘探中心

【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.

【基金】 国家深部探测专项(SinoProbe-02-01,02-06);国土资源部公益性行业科研专项(201011040、201011045、200811021);国土资源部油气专项(XQ2004-06);国家自然科学基金委创新群体项目(40921001);国家自然科学基金项目(40830316、40874045)联合资助
  • 【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
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