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1)  passive margin
被动边缘
1.
In the Triassic, the sedimentary structural zones developed from passive margin basin to active margin basin as a result of the influence of the Jinshajiang suture zone and Garz Litang suture zone,and split apart into the Baiyu Yidun foreland basin,Chomta Xiangcheng island arc zone and Yulong Daocheng fore.
在三叠纪时期受金沙江缝合带与甘孜—理塘缝合带构造作用的相互影响,其沉积构造性质也由被动边缘盆地演化为活动边缘盆地,同时分裂为白玉—义敦前陆盆地,昌台—乡城岛弧带、玉隆—稻城弧前盆地。
2)  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。
3)  Volcanic passive margin
火山型被动边缘
4)  volcanic passive margins
火山被动边缘
1.
As a global phenomenon, large igneous provinces (LIPs) are continuums of voluminous magnesium_rich and iron_rich effusive rocks, and include continental flood basalts and associated intrusive rocks, volcanic passive margins, oceanic plateaus, submarine ridges, seamount groups and ocean basin flood basalts.
它包括大陆溢流玄武岩和伴生的侵入岩 ,火山被动边缘玄武岩 ,大洋高原、海岭、海山群和洋盆溢流玄武岩。
5)  passive ocean margin
被动大洋边缘
6)  passive plate boundary
被动板块边缘
补充资料:被动过敏反应


被动过敏反应


被动转移的过敏反应。其过程包括:①将已被抗原致敏的同种或异种动物血清注射至正常动物体内。②由于注射抗体导致被动致敏状态,一般需几小时至24小时甚至更长时间。③激发注射相对应的抗原引起过敏反应的发生。
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