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1)  paired passive continental margin
"对"被动陆缘
1.
This paper expounds tile latest advance of research on continental margin evolution and discusses the model of pure shearing and simple shearing on continental lithosphere extension and new conceptions of paired passive continental margin.
本文讨论了被动陆缘演化研究中的最新进展和大陆岩石圈拉伸的纯剪切模式、简单剪切模式及“对”被动陆缘新概念,详细论述了火山型被动陆缘形成、演化的深部构造背景及拉张期岩浆活动的壳底垫托作用,强调在陆间型褶皱带研究中拉张型过渡壳的划分和研究具有重要意义。
2)  passive continental margin
被动陆缘
1.
They were continental rift and passive continental margin basins formed as a result of the break-up of Gondwana and the spreading of Atlantic Ocean.
西非海岸盆地群的形成和发育,与中生代以来大西洋裂开和后期的持续扩张作用有关,是冈瓦纳大陆解体和大西洋扩张形成的大陆裂谷和被动陆缘盆地。
3)  passive margin
被动陆缘
1.
Hengdan Turbidite terrane:Fillings in a Late Paleozoic forearc basin developed on the passive margin of the Yangtze plate;
南秦岭横丹浊积岩系——晚古生代发育于扬子板块被动陆缘上的弧前盆地充填物
4)  passive continental margin basins
被动陆缘盆地
5)  Passive continental margin
被动大陆边缘
1.
The plate activity is weaker in the passive continental margin of the northern South China Sea,which is favorable for forming the large-scale gas field and gas hydrate reservoirs.
南海北部被动大陆边缘是板块活动相对较弱的地区,业已证实是巨大天然气田形成的有利场所,同时也是水合物发育的有利地区。
2.
The passive continental margin of West Africa is becoming an attractive area for hydrocarbon exploration,and it experienced four tectonic stages,i.
西非被动大陆边缘诸盆地是目前油气勘探的重点和热点地区。
3.
Concerning with the complicated tectonic background of the passive continental margin of Northern South China Sea,this paper discusses the set-up procedure of the geological-physical model based on the integrated geophysical interpretation of the typical profiles in the area.
鉴于南海北部被动大陆边缘的复杂构造背景,从典型剖面的综合物探解释入手,讨论了南海北部地质-物理模型的建立过程,建立了琼东南盆地1104剖面定量物理模型并予地质解释。
6)  passive continental-margin rift
被动陆缘裂谷
补充资料:对缘假
【对缘假】
 (术语)四假之一。(参见:假)
说明:补充资料仅用于学习参考,请勿用于其它任何用途。
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