国外海洋岩石圈深部结构的地震学研究进展  

ADVANCE IN RESEARCH ON OCEANIC LITHOSPHERE STRUCTURES USING DEEP SEISMIC REFLECTION PROFILING

作　　者：梁慧云[1] 

机构地区：[1]中国地震局地球物理勘探中心,河南郑州450002

出　　处：《地球物理学进展》1999年第4期28-40,共13页Progress in Geophysics

摘　　要：近十年来,深地震反射波勘探在海洋岩石圈的形成与演化、地壳结构研究中的应用越来越广泛.本文介绍了美、英、法及北欧一些国家在北海、波罗的海、挪威海、大西洋、太平洋,地中海等海域分别进行的垂直入射、宽角反射/折射地震试验,及其在大陆边缘构造、海洋地壳的演化、海底断裂形态。In the recent decade,the deep seismic reflection profiling has been applied widely to studies on formation and evolution of oceanic lithosphere,crust structures and so on. America、Britain、France and other countries in Northern Europe have conducted the deep seismic reflection、wide-angle reflection/refraction experiments in Pacific、Atlantic North Sea、Mediterranean、Baltic Sea et al,respectively. In this paper,the researched results from the experiments on continental margin structures、evolution of oceanic crust、shapes and characters of the faults at oceanic bottom are presented.

关 键 词：海洋 地震反射剖面 岩石圈结构 地震学 地震勘探 

分 类 号：P736.12[天文地球—海洋地质] P631.4[天文地球—海洋科学]