深地震反射剖面揭露大陆岩石圈精细结构  

Fine Structure of the Continental Lithosphere Circle Revealed by Deep Seismic Reflection Profile

作　　者：王海燕[1,2] 高锐[1,2] 卢占武[1,2] 李秋生[1,2] 匡朝阳[2,3] 刘金凯[2,3] 侯贺晟[1,2] 酆少英[1,2,4] 熊小松[1,2] 李文辉[1,2] 邓攻[1,2] 

机构地区：[1]中国地质科学院地质研究所岩石圈中心,北京100037 [2]中国地质科学院地球探测与动力学重点实验室,北京100037 [3]华东石油局第六物探大队,南京210011 [4]中国地震局地球物理勘探中心,郑州450002

出　　处：《地质学报》2010年第6期818-839,共22页Acta Geologica Sinica

基　　金：国家专项"深部探测技术与实验研究"(编号SinoProbe-02);国家自然科学基金重点项目(编号40830316);国家自然科学青年金项目(编号40604010);科技部国际合作重点项目(编号2006DFA21340);国土资源部地质调查项目(编号1212010711813);基本科研业务费项目(编号J0803)联合资助成果

摘　　要：深地震反射技术已被国际地学界公认为是探测岩石圈精细结构、解决深部地质问题的有效技术手段。自上世纪70年代中期以来,以美国为首的等西方国家和中国相继开展了深地震反射探测技术实验,使用该技术揭露盆地、造山带岩石圈的形成和演化、地球动力学过程,并应用于油气资源远景评价、矿产资源勘察等领域,取得了丰硕的成果。本文扼要介绍深地震反射剖面技术的发展及其部分应用实例。Deep seismic reflection has currently been recognized as an effective technological approach in probing fine structure of lithosphere and solving the deep geological problems. Since the 1970s, the western countries with America as a leading one and China have successively carried out deep seismic reflection exploration program. The technology of this kind has been widely used to disclose the formation and evolution of lithosphere in basins and the orogenic belts, geodynamics processes, and has been applied in prospective evaluation of oil and gas resources, mineral resources exploration and other fields. A large amount of results have been achieved. The development of deep seismic reflection technique and its part of the applications example are described briefly in this paper.

关 键 词：深地震反射 岩石圈精细结构 挤压构造 伸展构造 走滑构造 莫霍面 

分 类 号：P631.4[天文地球—地质矿产勘探]